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Pakistan Flood Control System (PFCS)

  Flood control and water storage solution for Pakistan
                                      By:    Syed Inam ul Rehman
                                      Email : inam.rehman@gmail.com
                                      Publish Date:   19/11/2010
                                      Last Updated:   17/09/2011
Pakistan Flood Control System (PFCS)
•   PFCS is a Flood control system, designed for Pakistan, that offers control for
    extreme floods in Indus Basin.
•   It contains a system of five dams for flood control(Soan, Rohtas, Khyber, Bhit
    and Nari Bolan) and three canals. (Soan Link Canal, Grand Indus canal and
    optional Makran Canal)
•   Soan Dam is the core of PFCS. Other dams will help, but Soan Dam alone can
    successfully handle floods like 2010.
•   Soan Dam sets foundation for radical changes in Pakistan’s flood control and
    irrigation paradigm by allowing distributed system of large local
    multipurpose projects. Dynamic allocation of water and coordinated flood
    harvesting are some of other main features.
•   Proposed dams increase water storage capacity of Pakistan by 644%. Apart
    from total flood control, PFCS will play a role of “Water Bank of Pakistan”, to
    ensure right amount of water at right time for all provinces, according to
    already defined respective water share.

•   PFCS will successfully block India’s move of internationalizing the flood water
    wastage in Pakistan for propaganda and grabbing more of Pakistan’s water.
Pakistan Flood Control System (PFCS)
•   Proposed system can be built in stages but it is economical enough to be built
    simultaneously. Proposed dams don’t need spillways due to their role, location
    and sizes. Pakistan has most of necessary skills and material to build it alone.
•   Additional power infrastructure can make this system much more profitable by
    producing more electricity than WAPDA’s existing hydroelectric capacity of
    6444 MW.
•   PFCS is designed around historical peak floods in country with 50%+ safety
    factor.
•   Avoiding any urban settlement and thickly populated areas is one of its main
    design consideration.
•   Economic feasibility: 8+ times larger yet cheaper than existing options. System
    will breakeven within first monsoon month of operation. Operating at 40%
    capacity, PFCS will add US$ 70+ billion annually to the national economy.
•   “New Deal”?
•   Strategic and geopolitical impact.
•   Last but not least, PFCS doesn’t need the Kalabagh dam. Instead it addresses
    Kalabagh dam’s potential drawbacks positively due to effective flood control
    in all four provinces, lack of water diversion and decentralization of Water &
    Power storage.
Storage Economy(MAF/Billion US$)
7


6


5


4


3


2


1


0
    Diamer basha dam     Kalabagh Dam   Akhori Dam   Bhit Dam   Soan Dam
Comparison with existing capacity
                          Storage Capacity Comparison(MAF)

40

35

30

25

20

15

10

5

0
     Diamer basha dam   Kalabagh Dam   Akhori Dam     Bhit Dam   Soan Dam
How this presentation is different?


• Problem of lack of flood control, and storage reservoirs in Pakistan is not a
  news.
• Pakistan has experienced massive direct devastation in form of floods, and
  indirectly in form of inflation, high food prices and instability in society.
• This presentation is different because




                  “it discusses the solution.”
Scope of presentation

• This document is the “presentation version of PFCS 2.0 design”.
• Version 2.0 includes upgrades about flood control and irrigation based
  upon version 1.0 design of November 2010.

• Contains details of Topographical feasibility math, supporting hydrology
  calculations and design overview.

• Detail design including detailed hydrological efficiency, reservoir bed rock
  analysis, design considerations, load conditions, stability requirements,
  stress analysis, seismic analysis, structural features, environmental study
  and archeological impact needs detail study, which falls in the scope of
  feasibility study.
Upgrades in PFCS version 2.0
•   19.3 MAF additional capacity and collection of extra water from Indus river right
    bank tributaries.
•   "Devolution of water and power" among provinces. high level Grand Indus Canal
    will deliver water and its hydroelectric potential to respective provinces.
•   Sindh and Balochistan get much needed large local reservoirs. This will decrease
    uncertainty of river flow fluctuations and canal response time.
•   22.23 million acres of possible increase in Irrigation system.
•   Water security for Karachi, the financial and industrial hub of Pakistan.
•   fresh water for Kirthar national park ecosystem and Manchar lake.
•   Water security for Makran coast. Makran can become "California of Pakistan"
    being the only coastal area around gulf with sustainable water supply for whole
    500 miles stretch.
•   Balochistan will be able to use its share of water including flood water for
    sustainable and efficient irrigation in Makran region.
•   Grand Indus canal can act as a "Water Motorway of Pakistan", for efficient and
    quick delivery of water all along Pakistan downstream Tarbela. In addition it will
    help about efficient water transfer from one location to another within provinces.
Upgrades in PFCS version 2.0
•   Grand Indus canal @ 50,000 cusecs can add 10 MAF to the effective storage of
    Soan dam. it will cut cost of Soan dam for same design storage.
•   option of "alternate route" for Indus river will improve the situation of water
    logging and soil salinity in Indus Basin.
•   Grand Indus canal offers potential for channel navigation, however this role needs
    to be evaluated for necessary adjustments in initial design.
•   Enhanced control over river flow will decrease land erosion along Indus river
    during normal flow and floods.
•   optional branching channel just upstream Guddu barrage will provide a shortcut
    for flexibility of water usage in Sindh.
•   Interlinked chain of under construction and proposed optimal sized dams can
    provide better water management for whole country.
•   Most of Pakistani cities are located along river banks and their ever increasing
    waste water and raw sewage is released back into rivers without treatment. this
    phenomenon causes serious health problems for lower Punjab and Sindh.
    proposed design will assure high quality water availability for southern Pakistan.
•   Proposed large dam in Sindh can decrease brackishness of underground water on
    right bank of River Indus. detail study needs to determine the optimal design for
    best possible effect.
2010 Floods in Pakistan
River Indus is the soul of the Indus valley, today’s Pakistan.
Lives of 180+ million people depend upon water of Indus river and its tributaries.

65-70% of Indus water flows during summer Monsoon, and in absence of a
   flood control system, Indus river can be dangerous during this time of year.

In July and August 2010, Indus basin saw extremely high level of floods due to
    extra-ordinary monsoon spells.
Following are some public numbers about flood damage till November 2010.
• Fatalities: 1,974
• Population affected: 20,184,550
• Cropped Areas underwater: 5,546,636 Acres
• District Affected: 78
• Damage estimates: official: $9.7 Billion, Unofficial: $43+ Billion,
    Reconstruction cost: 50+ Billions
Flood Map
Indus River Hydrograph during 2010 flood(cusecs)
Kabul River Hydrograph during 2010 flood
Jhelum River Hydrograph during 2010 flood
Chenab, Ravi and Sutlej
Jhelum, Chenab, Ravi and Sutlej
Khyber Pakhtunkhwa
Between Kalabagh and Taunsa(July 31st, 2010)
Between Kalabagh and Taunsa(Aug 1st, 2010)
Indus river normal flow (Aug-9-2009)
Indus river during flood (Aug-12-2010)
A closer look at Mithan Kot
A closer look at Guddu Barrage(Aug-12-2010)
Northern Sindh province with normal Flow
On August 11th 2010
October 12th 2010
Scale of 2010 flood: Khyber Pakhtunkhwa
Scale of 2010 flood: Khyber Pakhtunkhwa
Scale of 2010 flood: Khyber Pakhtunkhwa
Scale of 2010 flood: Khyber Pakhtunkhwa
Scale of 2010 flood: Khyber Pakhtunkhwa
Scale of 2010 flood: Khyber Pakhtunkhwa
Scale of 2010 flood: Azad kashmir
Scale of 2010 flood: Gilgit Baltistan
Scale of 2010 flood: Punjab
Scale of 2010 flood: Punjab
Scale of 2010 flood: Punjab
Scale of 2010 flood: Balochistan
Scale of 2010 flood: Balochistan
Scale of 2010 flood: Sindh
Scale of 2010 flood: Sindh
Scale of 2010 flood: Sindh
Scale of 2010 flood: Sindh
True, and God helps those, who help themselves
Facts and Figures of 2010 flood
• 55.26 MAF (Equal to 8 full Tarbela lakes) of water passed through Kotri
  barrage into Arabian sea between July 13th and October 4th 2010
• 72.87 MAF water passed through Guddu Barrage during the same
  time(adjusted).
• Below Guddu, 17.61 MAF Indus flood water didn’t reach the sea, submerging
  big areas in Sindh and Balochistan for next several months. (excluding Guddu
  downstream right bank tributaries flood runoff)
• 73.35 MAF water passed through Taunsa and Panjnad together.
• Stagnant water in Punjab cannot be accurately calculated due to unregulated
  right bank flood streams of Suleiman range.
• 3.2 MAF of accounted water stayed in Punjab. an equivalent of all right bank
  catchment from Chashma to Guddu including Tochi, Zhob, Gomal, Tank,
  Vehowa and the Zams stayed in Punjab and lower Khyber Pakhtunkhwa.
• Total water loss during 2010 summer estimates about 85 MAF, equal to winter
  storage for next 8 years at current capacity.
Flood control in Pakistan
•   Pakistan doesn’t have a flood control system due to lack of storage capacity and
    absence of known practical options.
•   Existing dams and proposed Kalabagh dam is too small to handle the amount of
    inflow in 2010 flood.
•   Kalabagh could have stored only 7.5% of total water but not without upstream
    damage in Nowshera and above.
•   In future, due to global warming, region expects increased frequency and intensity
    of flash floods coupled with higher glacier melt runoff. Proposed theory of
    Redistribution precipitation (Seasonal Shift) link increases the need of a serious
    solution for flood control.
•   In absence of a comprehensive plan, such floods can hit the backbone of country’s
    economy after ever few years.
•   This was not the last flood. Floods will certainly happen again, in a year, or a
    decade, or later. No one can say it will never happen again.
•   By taking solid steps, Pakistan can change such disasters into a blessing by saving
    $30-50 billions of flood damage per decade, and earning much bigger amount by
    increased agricultural productivity, extra power generation and food security
What can be controlled?
•   Eastern rivers (Ravi and Sutlej) are controlled by India. Pakistan doesn’t have
    suitable topography to handle floods in these rivers. Although huge flood canals
    can be built to divert a portion of flood water into Cholistan desert to recharge
    underground aquifers and tobas (ponds) for later use.
•   Chenab is a special case. India cannot control it due to lack of rights, and Pakistan
    doesn’t have a suitable site to control it along its length in Pakistan. It is similar to
    Indian situation about Yarlung Tsangpo River (Brahmaputra River) in Arunachal
    Pradesh where India doesn’t have a suitable site to control the 17 times bigger
    river(by annual average flow rate), yet it doesn’t want China to build any reservoir
    or ROR power project.
•   In presence of Kashmir conflict, there is no short term solution for Chenab
    flooding. Proposed Chiniot dam in Punjab (1MAF) can help, but it is too small for
    super floods.
•   Kabul, Jhelum and Indus rivers contribute 83% of Pakistan’s share of Indus system
    water.
•   We will focus on these three rivers, and will discuss the possible options to avoid
    future floods, while using flood water for agriculture and power generation.
•   West Side Tributaries of Indus from Tarbela to Arabian sea carry a significant
    amount of non perennial flood water. Linking of ongoing and future Medium and
    small dams(Kurram Tangi, Gomal Zam, Tank Zam, Baran dam etc) along western
    slopes can control and harvest flash floods.
This wasn’t the biggest flood

• 2010 flood wasn’t the biggest for all Pakistani rivers. Jhelum (at Mangla)
  saw 10,90,000 cusecs on Sept 10th 1992 as compared to 2,67,000 cusecs
  peak on July 31st 2010.
• Chenab’s (Marala) maximum for 2010 was 2,16,000. 26 August 1957 flood
  at Marala was 11,00,000 followed by 8,70,795 on 5/7/1959 and 8,45,090
  on August 28th 1992.
• Ravi’s (Jassar)2010 peak was 21,000 vs 6,80,000 in 1955. flood of 1988
  overflew at Jassar, with a record of 5,76,000 at Shahdara downstream.
• Sutlej stayed around 53,000 in 2010, in contrast to 5,98,872 in 1955 and
  3,99,453 in 1988
• We are not ready for any such record flood.
• In future, as Pakistani population and cities grow, the damage will grow for
  same intensity of floods.
Past 10 Floods through Kotri
•   1976: 64 MAF
•   1983: 43.8 MAF
•   1988 :44.7 MAF
•   1991: 42.0 MAF
•   1992: 69.19 MAF
•   1994: 81. 21 MAF
•   1995: 61. 09 MAF
•   2005: 24.5 MAF
•   2007: 15.82 MAF
•   2010: 55.8 MAF (excludes 33-35 MAF stagnant water)
•   Total 535 MAF, worth 1.07 Trillion US dollars.

    Historical Kotri downstream flow averages 35.2 MAF (1976-2006 WRMD
    WAPDA). While excluding 10 MAF for Indus delta, average 25.2 MAF water is
    available for harvest annually. PFCS 2.0 design will save water course loss from
    Tarbela to Guddu or Kotri. 40% reduction means 14 MAF extra water per
    year. It will also reduce risk of illegal water theft and evaporation losses.
Jhelum flood comparison, 1992, 1997, 2010
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          1        2           3             4                   5                6        7   8

                       Mangla_outflow_92   Mangla_Outflow_1997       Mangla_outflow_2010
Chenab flood comparison1992,1997,2010
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         1                     2              3             4                5                 6     7   8
         Marala_outflow_1992       Marala_outflow_1997   Marala_wave1_2010       Marala_wave2_2010
Flood control on Indus river

• Tarbela Dam is the only storage available on Indus river so far.
• However, in future, Tarbela and Diamer Basha Dam (2010-2018) together,
  will be able to store 14.2 MAF out of total 65 MAF annual runoff below
  Tarbela.
• Still 50.8 MAF in an average year, and up to twice amount of water in high
  flood years will stay uncontrolled.
• Both of these dams are designed mainly for storage. They can help
  towards flood control, but they may not always be ready for a mega flood.
• More available options include Akhori dam and Kalabagh dam. If ever
  built, these two dams can improve the storage capacity to 26 MAF, thus
  improving flood control capacity while increasing Rabi water availability in
  Pakistan by 32%.
• Next few pages talk about Kalabagh and Akhori Dams.
Kalabagh Dam
• Height: 79 m (259 ft) , Live storage: 6.1 MAF
• Indus river at Kalabagh has an average annual flow of 95 MAF. Kalabagh
  dam can store only 5.8% of total annual water. It cannot control a flood
  like 2010 flood, although it could have trimmed the maximum spike by top
  200000 to 300000 cusecs off the first wave only, like Tarbela.
• Table below shows summer runoff at Kalabagh during last three years.
    Month      Flow(MAF) in 2008   Flow(MAF) in 2009   Flow(MAF) in 2010


    April               4.41                 4.05              3.67
    May                 8.11                 7.65              7.30
    June               11.49                13.18              11.58
    July               18.02                18.13              22.05
    Aug                16.84                15.96              29.40
    Sept                6.43                 7.45              9.72
    Total              65.30                66.42              83.72
Kalabagh Dam issues
Kalabagh dam is controversial due to multiple reasons.
• Khyber Pakhtunkhwa, Sindh and Balochistan have already rejected it.
• Kabul river above Nowshera has no flood control at all. In absence of
   another upstream dam like proposed Khyber Dam, Kalabagh dam will be a
   disaster for Peshawar valley.
• Indus floods add to the magnitude of Kabul river floods by blocking their
   way. Proposed Soan dam (discussed later), will address this concern, by
   sparing entire Indus bed between Tarbela and Kalabagh to drain the Kabul
   river in case of extreme floods.
• Kalabagh dam’s revised reservoir level of 915 feet, still stagnates Kabul
   river upstream of Akora khattak. (initial design height was 925 ft above sea
   level)
• More research is required to address water logging, lake size and flow
   route issues. A practical Kalabagh dam may be another 25-40 ft below the
   current design of 915 ft. which will reduce its live capacity to less than 4
   MAF.
Akhori Dam project

•   Akhori Dam is a 6.0 MAF off channel storage project. Its proposed 400 ft high
    5 KM long main dam and (7 km long saddle dam) makes its construction
    much bigger than Tarbela.
•   With option of 7-8 times larger design capacity of Soan reservoir, Pakistan my
    not need Akhori dam, and same resources can be used to build Rohtas and
    Khyber dam.
•   World Bank team carried out inspection of Akhori and Sanjwal dam locations
    in 1968 . Team head Dr Lieftnick in his report, rejected Akhori Dam for a
    height of 250 ft due to foundation problems,.
•   A 400 ft high design at same site, may become too expensive.
Flood control on Jhelum River
• Mangla Dam stores about 4 MAF of water, but being the single storage
  dam on Jhelum, it is not flexible enough to handle additional flood water
  especially in late summer. Most major floods hit Mangla when it is already
  full.
• Pakistan has minimal control on flooding in Chenab, Ravi and Sutlej. A
  flood in Jhelum river, coupled with flood in these three rivers can be very
  dangerous (like in 1992).
• PFCS suggests “Rohtas Dam” with 9 MAF storage to handle super floods
  up to twice the size of 1992 flood of Jhelum.
• Available storage limit is huge, and it can balance Chenab flow during high
  flow season and large floods.
• Location of Rohtas dam can offer a lake up to 16 MAF size, and southern
  Bunhar river valley can make another 9 MAF lake, but such big reservoirs
  are not needed.
• Next few slides show the amount of water to handle. Please note that
  Jhelum and Chenab usually flood simultaneously, and their combined flow
  rate at Tarimmu and below can become bigger than Indus river’s
  maximum combined flow rate during 2010 flood.
Flood of 1992
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              Tarbela_out_1992   Mangla_out_1992   Marala_out_1992        Jassar_out_1992        Suleimanki_out_1992
Flood of 1997
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         25             26               27               28                29                30             31

              Tarbela_out_1997   Mangla_out_1997   Marala_out_1997   Jassar_out_1997   Suleimanki_out_1997
Jhelum’s deadly peak of 1992; hour by hour
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                           Mangla_inflow_1992   Mangla_outflow_1992
Flood control in Kabul river basin

• In 2010, most of damage in Khyber Pakhtunkhwa occurred due to flood in
  Swat river. future Munda dam has a capacity of 0.76 MAF ,enough for only
  3 days of peak flood. Munda dam needs a design change to increase the
  individual storage capacity by 3-4 times to absorb large floods.
• moving same dam 18 km upstream from current location can store 4 times
  more water while producing more electricity using a power tunnel.
• Kabul river at Nowshera drained 9.12 MAF flood water during 2010 flood
  month, about half of it came out of Swat river at Munda. 71% Swat river’s
  water flew during first 15 days.
• Kabul river is the main river in Peshawar valley. Warsak dam on Kabul river
  is silted to the top, and offers zero storage capacity or flood control.
• PFCS suggests a politically unconventional solution, “Khyber dam”.
• If possible, this is the best and permanent solution for area and region
  for next several centuries.
Overview of proposed reservoirs
#      Dam         River               Role             Max      Dam     Lake area       Storage    Extra Annual
                                                        Water   Height    (Sq KM)        Capacity   Hydro electric
                                                        level   (feet)                    (MAF)       potential
                                                       (MASL)                                          (GWH)
1   Soan Dam     Off         Flood control, Storage,   410      415      1230        38.4           18000
                 channel     Hydel                                                   (48.4
                 for Indus                                                           dynamic)
2   Khyber       Kabul       Flood control, Storage,   500      550      324         10.67          3500
    Dam                      Hydel
3   Rohtas       Off         Flood control, Storage,   340      345      294         9              1000
    Dam          channel     Hydel
                 for
                 Jhelum
4   Bhit Dam     Off         Pumped Storage,           250      510      244         15.5           7000 with
                 channel     Regional Irrigation                                                    GIC
                 for Indus   command, Delta
                             ecosystem support,
                             optional Hydel
5   Nari Bolan   Nari        Flood control, storage,   280      390      112         3.8            200
    Dam          Bolan       Regional Irrigation
                             command
    Total                                                                            77.37          29700
Overview map of PFCS Version 1.0
PFCS 2.0 upgrades
Data References

• ASTER Global Digital Elevation Model (ASTER GDEM) (10 m accuracy)
• digital elevation model (DEM) data collected by NASA's Shuttle Radar
  Topography Mission (SRTM).
• Topographic 1:50,000 maps by Survey of Pakistan.
• India and Pakistan 1:250,000 Series U502, U.S. Army Map Service, 1955
• Calculated capacity is based upon minimum of the results of processed
  datasets, which increases the level of confidence for calculations.
• Soan dam’s axis was manually measured using 2 digital altimeters against
  known benchmarks. Results confirmed a depression of 131 meters (+10m
  bridge) from Dhulian Mor Mosque to top of Dhok Pathan bridge.
• Final figures for Dam design, lake size, capacity and reservoir shape need
  professional physical survey of area.
• Source of water flow data is “Flood forecasting division of Pakistan(FFD)”.
  Mathematical model is based upon daily averages and 6 hour flows at Rim
  stations in Pakistan.
Soan Dam
•   Soan valley is best available site for flood water storage below Tarbela. During 1960’s, World
    Bank team evaluated 5-6 times smaller storage reservoir at this site, with design bottle-neck of
    unlined canal and no option of Tunneling.
•   Lake size was likely never measured, because its listed size, height and dam length figures
    (picture below) are wrong. A 275 feet high dam at Dhok Pathan offers about 25 MAF gross
    storage and 35 MAF live storage for flood control. Thanks to report, as it confirms that minimum
    of 25-35 MAF flood water can be handled at 275 masl. Due to site’s topography and
    geophysical location, much bigger dam is possible. World bank report doesn’t talk about any
    foundation problems like Akhori area. It was either not evaluated, or there was no issue.
    Feasibility study can confirm it.




•   Seismicity of site is favorable (g factor 0.03-0.1, Source GSP Seismic Hazard Map of Pakistan)
•   In World bank’s report, figure of 8.5 MAF was used based upon a design of three parallel canals
    running for three months, needing water-lifting at some locations. It would have needed 15-17
    unlined high maintenance parallel canals for transporting total flood water during flood season.
    It makes sense why this project didn’t get due attention . 45 years later, options of lined channel
    and large diameter tunnel boring can help exploit full potential of this site.
Soan Dam site Geology
Dam axis lies on Pliocene and Miocene sedimentary rocks, same as the site of proposed
  Kalabagh dam. (Source: Geological Map of Pakistan, DG GSP)
Soan Dam site Geology
Soan Dam
•   Soan reservoir, made a dam 1 km upstream from Dhok Pathan bridge offers up to 46.6
    MAF gross storage. A 113 meters deep lake can hold 38.4 MAF water. Several dam
    locations are available between Markhal to upstream Dhok Pathan from 395 m to 415
    masl.
•   A dam at this location will not distribute any water from Indus river. It will collect during
    flood season and drain back to system at right time.
•   Proposed Grand Indus canal at 50000 cusecs can increase its effective capacity to 48.4
    MAF for same height of 113 m.
•   dam at this site will be relatively low cost. Material requirements are 60% of Tarbela
    dam.
•   Mangla’s main dam and dykes length is more than 10 KM. 30 KM long Hirakud Dam on
    Mahanadi river in India (built in 1957) is four times longer than biggest possible Soan
    Dam.
Soan Reservoir
 •Following table shows possible capacity of Soan reservoir (using SRTM DEM V4.1)

             Required Dam   elevation from   contour        Lake       Lake capacity at   Possible gross
   #
              length (KM)    river bed(m) elevation(m)   area(Acres)   level(acre feet)   capacity (MAF)
   1               3.2             95          390         234889         22933956             22.9
   2              3.78            100          395         258212         26978420              27
   3               5.1            105          400         278367         31379494             31.4
   4              5.67            110          405         299656         36120496             36.1
   5              6.72            115          410         319837         41201640             41.2
   5              7.66            120          415         340677         46619241             46.6


•Following table shows possible capacity of Soan reservoir (using ASTER GDEM)

  lake depth       Soan Dam       bounded acres    block volume        Cumulative AF         MAF
        0             300              1622
       10             310              7071          142608.665            8694.65         0.00869465
       20             320             16512          386879.115          395573.765        0.39557377
       30             330             35521          853601.365          1249175.13        1.24917513
       40             340             55405          1491641.03          2740816.16        2.74081616
       50             350             94613          2461045.29          5201861.45        5.20186145
       60             360            134786         3763290.595         8965152.045        8.96515205
       70             370            175522          5090602.74         14055754.79        14.0557548
       80             380            220448          6495887.85         20551642.64        20.5516426
       90             390            262908          7929455.18         28481097.82        28.4810978
      100             400            303820          9297172.84         37778270.66        37.7782707
       110            405            325862         5164714.575         42942985.23        42.9429852
Design parameters
•   Soan Dam needs an Earth filled main length with low dykes extending on both sides.
•   main length is 3 km long and 40 to 132m high.
•   Left and right dykes are 2.25 and 1 km in length with average height of 22 m(for average
    lake depth of 17 m)
•   Soan dam needs a 90 km waterway from Tarbela lake to the reservoir, (like Ghazi
    Barotha and proposed Akhori dam). a waterway with flow capacity of 250000 cusecs
    can assure the maximum storage use and flood control from July to September.
•   Soan reservoir will collect extra water from its own catchment area too, which spreads
    from Kallar Kahar to Muree. Dead reserve and local run-off will decrease the required
    size of Link canal.
•   Major design challenge is to connect the reservoir with Tarbela lake. Higher level canal
    will bring lesser silt, is more energy efficient, needs a shorter canal length for
    connection being closer to dam site, but at cost of dam life and flood control capacity
    of Tarbela dam . Adjusting the design flow rate can improve flood control without
    addressing silting of Tarbela. Lower level of link canal can improve life of Tarbela dam.
•   Tunnels can be used near start and end of the link canal to avoid excavation. With
    available maximum TBM diameters (~15 m) , 4 parallel tunnels can provide an
    alternative to excavating open channel at hard locations.
Soan link Canal level
• Optimum height of Soan link canal intake needs detailed study of
  hydrological data trends as well as political aspects, but keeping it closer
  to dead level can keep Tarbela reservoir ready to absorb super floods.
• Following table contains available storage capacity for each canal
  withdrawal level above Tarbela’s dead level. 435-445 offers best range for
  economical canal design. Please note that Diamer Basha dam’s storage will
  be a plus for available volumes in column #3
                                                                 Storage available in Tarbela for flood control
             #           Soan link canal intake level (meters)
                                                                                     (MAF)
             1                           420                                          6.8
             2                           425                                          6.6
             3                           430                                          6.2
             4                           435                                          5.7
             5                           440                                          5.1
             6                           445                                          4.5
             7                           450                                          3.7
             8                           455                                           3
             9                           460                                          2.2
             10                          465                                          1.3
             11                          470                                          0.5
             12                         472.42                                         0
Soan link Canal
•   Pakistan has built largest fresh water link canal between Ghazi and Barotha. (base
    width 58.4m, depth 9m, side slope 1:2, gradient 1/10000, flow rate 56500 cusecs)
•   Duel canals for Balloki Suleimanki link use a width of 340 m for 82 km distance.
    With appropriate route, slope and depth combination, Soan Link Canal requires
    lesser width for lower flow speeds under 3 m sec.
•   By adjusting channel geometry, i.e. cross section, depth and slope, Soan link canal
    can generate up to 350k cusec flow-rates inside “man made gorge”. For last 20 km
    length, that need most digging, this option is very helpful by reducing width of
    canal by 60-80%.
Soan link Canal
•   Concrete lining is ideal for flows above 5m/s. it will be economical to use higher
    range of subcritical flow regime.
•   Lining will eliminate the high maintenance overhead feared in design from 1960s.
•   Upgrades in PFCS Version 2.0 will make it possible to use this canal partially around
    the year, for efficient and economical water and power usage.
•   Optional tunnel lengths discussed later will make things much easier. Cross
    sectional geometry of SLC can be adjusted according to feasibility of its navigable
    role.
SLC size choices vs. flow rates


                                                   flow
Discharge Discharge           manning   Free-    velocity Channel             Channel
 (cusecs) (cumecs) gradient    coeff  board(m)    (m/s) Depth(m)    Froude   lining(m)



165000    4672.28   0.0003     0.012     1.5     5.695    10.37      0.63    111.48



225000    6371.29   0.0003     0.012     1.5     6.224    12.53      0.65    120.09



300000    8495.05   0.0003     0.012     1.5      6.79    14.36      0.66    129.33



350000    9910.9    0.0003     0.012     1.5     7.096    15.59      0.67    134.83
2010 flood scenario with Soan Dam
•   After June 1st, Tarbela lake is kept at dead level 420 m (1378 ft) while diverting all
    extra water to Soan reservoir till a flood arrives.
•   Tarbela dam can absorb 6.8 MAF water, enough to completely stop the river flow
    from 28th July onwards, while diverting 250000 cusecs into Soan lake for next three
    months.
•   Numerical analysis shows that 6.8 MAF of dedicated capacity at Tarbela lake can
    easily absorb all flood spikes of 2010 while Soan link drains it continuously.
•   In this extreme case, mighty Indus can be totally blocked downstream Tarbela
    while collecting entire flood water (up to 38 MAF) into Soan reservoir. In the end,
    another 6.8 MAF capacity will still be available at Tarbela.
•   meanwhile it spares the Indus river bed between Tarbela and Kalabagh for highest
    floods in Kabul or Swat river. This makes second safety layer for Khyber
    Pakhtunkhwa flooding after Khyber dam.
•   In presence of future Diamer Basha Dam, capacity requirement for Soan link canal
    drops to 165000 cusecs for complete flood control.
Power generation at Soan
•   There will be no loss of power potential.
•   Extra water and extra altitude range means much more electricity than Tarbela, Ghazi
    Barotha and Kalabagh Dam together.
•   Soan can generate electricity at both inflow and outflow.
•   Dam site lies next to 380 KV transmission. It will cut the cost of associated power
    infrastructure.
•   Underground power plant at Kot Maliaran with inlet at lake’s dead level (310 m) can
    generate hydro-electric power comparable to Tarbela’s output.
•   Additional turbines on outflow will generate extra power.
•   Grand Indus canal from Soan Dam back to Indus can produce extra electricity, much
    more than Kalabagh Dam.
•   Tarbela offers 85-135m of potential difference with waste of flood water at peak level.
•   Soan Dam can use all water between 120 meter consistent head using tail intake
    design.
More about Soan dam
•   In addition to water storage and flood control, Reservoir area can be used for
    occasional farming(organized or unorganized), sometimes for years. (like in the
    Siran Pocket of Tarbela lake).
•   Storage area cannot be used for permanent settlements and populations need
    to relocate above maximum flooded level.
•   Reservoir area is sparsely populated due to its geography. Ratio of effected
    population is less than people displaced in construction of other big dams
    including Mangla, Tarbela and Diamer Basha. Akhori and Kalabagh dam effect
    higher population density areas.
•   No city will submerge. Both Chakwal and Talagang are 55 m and 120 m higher
    and at a safe distance.
•   Oil fields in Potohar will not submerge.
•   Soan Dam will submerge 40 km of M2 motorway. An elevated road with
    Chakri causeway will help avoid a longer M2. this is far less than 100 km
    submerged KKH in much difficult terrain for Diamer Basha dam.
•   Lake will recharge Soan river ecosystem with fresh water supply.
Geography of Soan lake
Near Soan dam site
Conceptual View
Cost estimate for Soan Reservoir
Total cost of Soan reservoir system will stay about half of Diamer Basha dam’s
   $12.6 billion (2008 estimate) due to type and location of project, while
   providing 7 times more storage capacity.
Soan Dam
• Soan Dam construction volume is much smaller than Tarbela dam.
• 2:1 ratio dam (Tarbela standard)needs 54.3 mcm
   2.5:1 ratio measures 66.3 mcm
   3:1 (overdesign)ratio needs 78.22 mcm
   for 41% additional foundation size(equal to Tarbela) values become. 76.5,
   93.4 and 110.3(51%, 62% and 73% of Tarbela dam size.)
Soan Link Canal(SLC)
• Total cost of Ghazi Barotha Canal was $365.7 Million.
• SLC is 1.9 times longer and at an average, 1.5 times wider and deeper. This
   translates into 4.5 times more building material .
• Gross Earthwork involved is 3.2 times more than GBC, for channel at 445
   m.(4.5 including 1:1 safety step contours all along the length)
• SLC will cost around $1.5 Billion.
• Steep tunnel can be used in last quarter, “Culebra Cut” of SLC, but open
   channel will be more economical and needs low maintenance cost.
Rohtas Dam
•   Rohtas dam , an off channel storage site for Jhelum river on Kahan river bed,
    can provide 100% storage and flood protection in Jhelum river around the
    year.
•   It can completely block Jhelum flow during high floods in Chenab, Ravi and
    Sutlej rivers, to thin out the intensity of flood.
•   It needs a single main Dam, smaller than Tarbela dam in construction volume.
•   Design level of Rohtas lake is 345 m, 40 m below maximum level of raised
    Mangla lake. It can generate power at both intake and exit.
•   two way flow control above Bheli Bathar can make water flow to Rohtas lake
    independent of the water level in Mangla lake. This will enhance the flood
    control capacity by several times.
•   Rohtas lake is 8.5 km from center of Dina city. Mangla lake is 11.75 km away.
    Kahan river bed between Dina and Rohtas reservoir will act as a natural barrier
    for Dina from seepage and other hydrological effects.
Rohtas Reservoir design numbers
                   Rohtas1
above river bed Dam(short axis) bounded acres   volume     Cumm AF     MAF
      0              240            434

      10             250            3050        57155.02   8694.65    0.008695

      20             260            6667        159407.4    168102    0.168102

      30             270           12176        309119.4   477221.5   0.477221

      40             280           19318        516659.1   993880.5   0.993881

      50             290           27963        775644.8   1769525    1.769525

      60             300           36834        1062995    2832520    2.83252

      70             310           46436        1366044    4198564    4.198564

      80             320           55710        1675705    5874270    5.87427

      90             330           66577        2006118    7880388    7.880388

     100             340           76817        2352379    10232766   10.23277

     110             350           86670        2682004    12914771   12.91477
More Rohtas options(SRTM)
   Grand
rohtas1@350                                              Rohtas 2 @380
                                    OWR       Gross                                    Gross
masl     ft     Acres     Acre-ft            Capacity   Acres     Acre-ft    OWR      Capacity
260    852.8    3623     237668.8
280    918.4    16640    1091584    328000              5256    344793.6
300     984     37562    2464067    590400              12527   821771.2    262400
320    1049.6   61177    4013211    721600              24305    1594408    262400
340    1115.2   87239    5722878    721600              32000    2099200    262400
350    1148     97656               164000              42014    2756118    262400
380    1246.4                                           50658               262400


                         13529410 2525600 16055010               7616291    1312000   8928291
Rohtas lake
Location of Rohtas lake
Conceptual view
Khyber Dam
Khyber Dam

•   Proposed 9 km upstream of existing Warsak dam, 500 ft high and 430 m
    long Khyber dam (145 m above river bed ) will create a reservoir of 10.67
    MAF , bigger than Tarbela lake.
•   If required, Khyber dam can be constructed downstream, but it will need
    50% longer dam. Detailed study is required to evaluate both options.
•   Upstream location has a challenge of silt removal. Grout Curtain or pressure
    grouting offers a time tested solution. grout is injected into drilled holes in
    silted riverbed above bed rock. This creates a waterproof barrier of
    overlapping pillars. Aswan dam has successfully used this technique on a
    much bigger scale. (video detail)
•   Proposed dam can absorb any size of flood in known history and Peshawar
    valley will never flood again.
•   Huge Khyber lake will extend 61 miles upstream, including last 30 miles
    inside Afghanistan. Tail of this lake will cover 25,949 hectares area inside
    Mohmand Dara , Lal Pur and Batikot distt in Nangarhar province of
    Afghanistan.
Khyber Dam
• Lake area inside Afghanistan is well known flood zone and unsuitable for
  permanent settlements. It contains riverbed and farmland.
• Lake will not effect Jalalabad which is 250 feet higher and 12 miles upstream
  from the maximum extent of proposed lake.
• Afghanistan has recently built dams on Kabul river without consulting Pakistan.
  Pakistan should not do the same. It is better to discuss and coordinate on such
  issues, for welfare of effected people.
• Effected Nangarhar province is a 100% Pashtun area, and gateway to Khyber
  pass. It can become hub for both trade and low cost energy for Afghanistan.
• Afghanistan needs electricity, being one of the lowest countries by per capita
  power availability(3.6 watts per person)
• Pakistan and Afghanistan should come up with a formula to materialize this
  mutually beneficial project for sake their people. Afghanistan can get share in
  extra electricity generated (~3500Gwh), land use charges or one time payment
  for relocation and development of displaced people.
Khyber Dam
• Pakistan can help building improved irrigation system for alternate location of
  submerged land in Nangarhar.
• Proposed dam can promise deep rooted co-operation for regional stability.
• Aswan High dam on Nile river is another example, where Sudan and Egypt have
  worked together in similar situation. Aswan lake’s area inside Sudan is more
  than three times larger than proposed Khyber lake area inside Afghanistan at
  maximum level of 500 masl.
• There can’t be a better way for Pashtun leadership to help their people while
  solving a permanent threat of flooding for millions of people.
• This Project will help create opportunities on both sides of border, to promote
  peace and eliminate poverty and extremism.
Khyber Dam capacities(ASTER GDEM)

                         average contour
Khyber   bounded acres    block volume       AF        MAF
 390         4465
 400         6988           187886.465      8694.65   0.008695
 410        11851           309053.795     317748.4   0.317748
 420        16521            465442.66     783191.1   0.783191
 430        22055            632839.28     1416030     1.41603
 440        29193            840723.44     2256754    2.256754
 450        36747            1081745.7     3338500     3.3385
 460        42753            1304197.5     4642697    4.642697
 470        51731           1550010.02     6192707    6.192707
 480        63411           1888904.51     8081612    8.081612
 490        76649           2297684.3      10379296   10.3793
 500        91801           2763422.25     13142718   13.14272
 510        107141          3263643.51     16406362   16.40636
 520        124274         3796363.075     20202725   20.20272
 530        143361         4390552.175     24593277   24.59328
 540        164045          5042995.43     29636272   29.63627
 550        185993          5742373.39     35378646   35.37865
 560        204280         6402428.565     41781074   41.78107
Munda reservoir is 12 miles away and 100+ meters higher than Khyber lake.
In future, Munda lake can be connected to Khyber lake with a steep spillway tunnel to
soften extreme floods in Swat river without wasting water or power.
Hydroelectric potential of Khyber dam

• Kabul river at Nowshera has a flow rate comparable to Jhelum at Mangla.
  Warsak flow makes 80% of total flow at Nowshera.
• Due to low design elevation, Warsak dam generates only 994 GWH(1/5th
  of Mangla’s output)
• Mangla taps 4797 GWH between 55-105 meters potential drop range(
  between dead and peak level of reservoir)
• Raised Mangla will generate 5800 GWH electricity between 55-117 m
  limits.
• Khyber dam offers 67-180 meters, which translates into potential of 4500+
  GWH per year.
Conceptual view
Khyber dam will look like Iran’s Karun-3 dam in dimensions and type
lake Khyber
Afghanistan side of Khyber reservoir:
  WHO map shows the location as flood hazard area
Bhit Dam
• Sindh has a large natural site for Water storage near Bhit, between Bhadra
  and Kirthar mountains. It has never been considered before due to being
  different from conventional storage sites.
• This site offers a perfect location for Pumped-storage hydroelectricity
  reservoir in its simplest form.
• 150 meter high dam at 26.2590, 67.5136 can store 15.5 MAF water. Higher
  dam can create a lake up to 53.7 MAF.
• proposed lake is surrounded with multiple layers of hill ranges on both
  sides, which makes it safer and stable. Reservoir’s design surface area is
  smaller than Manchar lake(0.08 MAF and 520 sq km), but storage capacity
  is about 200 times bigger. (not 200%). Size of Manchar lake can be
  reduced in presence of Bhit reservoir.
• It needs a 6 km long dam, which is shorter than Mangla dam.
Bhit Dam
• Bhit reservoir offers multiple uses, but water storage for Sindh province is
  its main aim. Proposed Grand Indus canal, can deliver hydroelectric
  potential of about 40 MAF water per year with higher relative potential. It
  translates into 1.5 - 2 times more electricity than Mangla dam.
• Without Grand Indus canal, Bhit Dam can use Manchar lake as intake
  reservoir. Operating energy can come from Peak load balancing with
  national grid, Fossil fuel, local coal reserves, or multiple gas fields in same
  area.
• Reservoir’s location and altitude offers opportunity to use wind as one of
  energy source.
• Extended Grand Indus Canal, offers much more benefits than its cost, and
  is recommended as better option for feasibility study.
• Water and power output of Bhit dam can support new urban and rural
  areas on Sindh highlands.
Bhit Dam site
Grand Indus canal
•   option of "alternate route" for Indus river will improve the situation of water
    logging and soil salinity in Indus Basin.
•   Grand Indus canal offers 115-185 meters of potential difference for entire summer
    water. Its integration with dams on western tributaries can multiply the total
    potential, while Kalabagh potential is only 65 m at maximum(controversial) level of
    278 m(915 feet). In Picture: Conceptual view of Grand Indus canal.
Grand Indus canal
•   Grand Indus canal is a proposed concrete lined channel, that will deliver water
    from Soan Dam to Southern Indus basin around the year.
•   Grand Indus canal can act as a "Water Motorway of Pakistan", for efficient and
    quick delivery of water all along Pakistan downstream Tarbela. In addition it can
    help about efficient water transfer from one location to another within provinces.
•   Grand Indus canal @ 50,000 cusecs can add 10 MAF to the effective storage of
    Soan dam. it will cut cost of Soan dam for same design storage.
Grand Indus canal
•   Most of Pakistani cities are located along river banks and their ever increasing waste
    pollutes the rivers. this phenomenon causes serious health problems for lower Punjab
    and Sindh during low flow season. Pakistani rivers are still much cleaner than Ganga or
    Yamuna, but they need to aim higher standards. So far situation is only getting worse.
•   GIC will assure high quality water availability for southern Pakistan.
•   Pictures below show Ravi bridge(left) and 60 km downstream near head Baloki (right).
    This “Black Water” deserves attention.
Grand Indus canal
• Enhanced control over river flow will decrease land erosion along Indus
  river during normal flow and floods.
• optional branching channel between Punjab and Balochistan, just
  upstream Guddu barrage will provide a shortcut for flexibility of water
  usage in Sindh. This site is suitable for a hydroelectric ROR project.
• Interlinked chain of WAPDA's proposed optimal sized dams can provide
  better water management for whole country.
• Grand Indus canal offers potential for channel navigation, however this
  role needs to be evaluated for necessary adjustments in initial design.
Grand Indus canal
• Soan link Canal faces a challenge of crossing Indus river above Kalabagh.
• Siphon tunnel, elevated aqueduct, or an economical hybrid of both can be
  used for this purpose.
• Pont du Gard, France(below) is more than 2000 years old.
Grand Indus canal
• Option of Prestressed concrete Siphon is more secure and easy to
  maintain.
• Figure: Soap Lake siphon in Washington state, USA
Nari Bolan Dam
• Kachhi plane is surrounded with multiple suitable sites for water storage.
  small dams can be built for flood control and water harvesting. Most of
  these sites are suitable to drain flood water into Grand Indus canal.
• 120 m high Nari Bolan dam, 3km upstream of Nari Head offers big storage
  capacity (3.8 MAF) for local flood water and extended grand Indus Canal.
• Nari Bolan site lies in commanding position for sub-basin and its elevation
  is suitable for interface with extended Grand Indus canal.
• Talli Tangi and Bolan dam sites on its left and right can be connected for
  additional storage, if needed.
• Nari Bolan reservoir connected with Grand Indus canal can provide much
  bigger, efficient and elegant irrigation system for Balochistan than Kachhi
  canal due to its design parameters.
Nari Bolan Dam
Makran canal
• Grand Indus canal will deliver water from multiple reservoirs to Bhit dam
  at 250+ masl.
• It provides an option of a smaller canal link with Mirani dam, linking
  reservoirs in Dasht, Gwadar-Ormara, Hingol and Porali river basins.
• This will greatly improve the coastal region for sustainable social and
  efficient agricultural growth.
• Balochistan can use the canal to deliver a part of its flood water share
  across the Balochistan plateau. Government of Pakistan should allocate
  extra water for this region for development of local population and extra
  ordinary potential of this region.
• Interbasin transfer of water is not something new. India uses Indra Gandhi
  canal to transfer Indus basin’s water to Thar desert. It shouldn’t be a
  problem within Balochistan.
• 1151 km long 13,000 cusecs California aqueduct (built 1963) is a good
  model for this canal. Makran canal will be much smaller in capacity and
  length.
Makran canal
• Makran canal can become the backbone for growth and prosperity in
  Makran.
Makran canal
• Makran region has excellent geography and weather. Improved water
  supply can make it “California of Pakistan”, and “Gateway to Middle East.”
Water for Karachi
•   In Pakistan, 90% water is used for Agriculture. Out of rest 10%, Karachi gets a
    fraction of a percent to lead the national economy and industry.
•   Situation of water in Karachi needs a lot of improvement in quality and quantity. It
    is a major contributor towards problems of local population.
Water for Karachi
• Makran canal will cross hub basin upstream Hub reservoir and Karachi can
  get more water according to its growth needs.
Current situation
• During winter, total water inflow in Pakistan’s river system drops to just 3%
  of summer’s peak flows.
• By January, dams in Pakistan are almost empty and total inflow drops to
  35000 -40000 cusecs. On 23rd January 2010, there was 1.5 MAF water left,
  with just 37000 cusecs inflow to the system. total inflow on January 4 th
  2010 was 37,205 and 34000 on 6th Feb. 2010.
• During March, Pakistan’s existing dams hit the dead level. On 12 th March
  2010, Mangla dam was at dead level (1040 ft), and Tarbela was at 1384
  ft(5 feet above dead level). While system inflow was 69,024 cusecs.
• Kharif sowing season in Sindh starts in April and ends well before the
  monsoon or heavy summer melt arrives. A blame game of water theft,
  playing politics and violation of water rights starts between provinces over
  every single drop of water, which makes sense because both dams and
  rivers are empty.
Current situation
• Sindh needs extra storage capacity more than any other province to
  support its Kharif sowing season.
• Cotton , Paddy(rice) and Sugarcane are major Kharif crops in Pakistan.
  Cotton and its products amount 60% of export earnings for Pakistan.
  Sugarcane provides a big portion of caloric intake for population while rice
  is used for both local consumption and export. (rice makes 10% of export
  earnings)
• Monsoon helps Kharif crops in rest of the country, but uncertainty of rain
  delays or flooding is always there. A fluctuation in weather pattern can
  cause a big damage.
• Late arrival of monsoon harms the initial growth of crops while floods
  due to heavy rains destroy the crops in flooded areas.
• Building new dams can assure availability of right amount of
  water at right time, while controlling the floods.
Impact on Pakistan's economy
•   No more floods means stable and safer cities and villages.
•   PFCS can control erosion on banks of rivers that destroys thousands of Acres of
    land annually in Pakistan.
•   Pakistan’s existing water storage capacity for Rabi (and Kharif sowing) is 12.1
    MAF. building these dams will increase the storage capacity to 90 MAF
•   In Pakistan, One MAF stored water’s value is roughly equal to 2 Billion US
    dollars (in 2010). If PFCS is used at 40% potential, it can earn more than 70
    billion 2010 US dollars per year for next several centuries.
•   Pakistan’s population estimate in 2010 is 180 million, which will double to 360
    million by middle of current century.
•   Wheat, the most common staple food in Pakistan is a winter crop, that heavily
    depends upon stored water.
•   In future, Pakistan will need to switch its priority towards growing more winter
    crops for local consumption instead of “wasting” water on low profit water
    intensive exports including rice and cotton.
•   Our current major “cash crops” are at the bottom of food chain in
    international trade. Bangladesh uses them as raw material to export finished
    products to developed markets.
•   With better coordination and control on water losses, new areas can be
    brought under high efficiency cultivation in all four provinces.
Impact on Pakistan's economy
• "Devolution of water and power" among provinces.
• growth of sustainable infrastructure for local population in western plains
  of Indus river.
• food security and increased agriculture and livestock output.
• Project will create jobs for local skilled and non skilled work-force during
  decades of construction, and later for operation and development of
  additional infrastructure in social and agricultural sector.
• Water security for Karachi, the financial and industrial hub of Pakistan.
• fresh water for Kirthar national park ecosystem and Manchar lake
  reservoir.
• Water security for Makran coast. Makran can become the only coastal
  area around gulf with sustainable water supply for whole 500 miles
  stretch.
• Balochistan will be able to use its share of water including flood water for
  sustainable and efficient irrigation in Makran region.
Hydroelectric power generation
• Proposed dams can double the current hydroelectric power generation
  capacity in Pakistan.
• Pakistan has enormous hydro electric potential, which is out of scope of
  this presentation.
• Indus river hydroelectric projects like Pattan, Thakot, Dasu, Diamer Basha,
  Bunji, Yulbo, Tangus, Katzara and Yugo offer about 40000 MW
  hydroelectric power, and are part of WAPDA’s long term vision. A fraction
  of them can manage local flood hazards while coordinating with PFCS.
• Proposed Katzara dam offers 40 MAF storage, more than Indus river’s
  annual flow at Skardu. This dam can ensure regulation of Indus water and
  power above Tarbela during winter, which will cut capacity and tunneling
  costs of power projects into half.
Interesting Trivia
•   Theory of “Redistribution of Precipitation (Seasonal Shift) in Pakistan” by Dr.
    Muhammad Hanif, National Weather Forecasting Centre (link) defines the changed
    pattern of 2010 monsoon. If this shift occurs more frequently, PFCS has already an
    off shelf solution for it. “Darra e Tang Dam” has very huge potential to absorb this
    shift. Site can collect up to 210 MAF water, submerging Laki Marwat and sparing
    Bannu. World bank left this site “blank” in its study. We don’t need such a big
    reservoir, but very low dam at Darra-Tang can offer comparatively large capacity,
    without touching population centers.
•   If Katzara dam is built as tall as Diamer Basha dam, it can hold 90 MAF water, equal
    to 2.5 year flow of Indus at dam site, but it will submerge beautiful Skardu valley.
•   Many possible dams in Balochistan are not included in PFCS 2.0 to avoid
    complexity. Reservoirs for Rashkan basin, Hamun Mashkhel basin, Pishin Lora basin
    and Hamun Lora basin can be handled individually.
•   Dozens of Right bank tributaries of Indus between Kalabagh and Arabian sea can
    be integrated into PFCS in future.
•   Name for Soan dam, the heart of PFCS, was chosen due to multiple factors. Wait
    for details.
Numerical results of PFCS performance for 2010 flood.
Conclusion

• Floods, including Super floods will certainly come again, in a year, or a
  decade, or later.

• By building flood control facilities, we will face them more gracefully.

• Pakistani people can pray for floods once PFCS is built.

• We don’t have enough time to waste before materializing such projects.
Thanks for watching

    Email for details & comments
    inam.rehman@gmail.com

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Pakistan Flood Control System

  • 1. Pakistan Flood Control System (PFCS) Flood control and water storage solution for Pakistan By: Syed Inam ul Rehman Email : inam.rehman@gmail.com Publish Date: 19/11/2010 Last Updated: 17/09/2011
  • 2. Pakistan Flood Control System (PFCS) • PFCS is a Flood control system, designed for Pakistan, that offers control for extreme floods in Indus Basin. • It contains a system of five dams for flood control(Soan, Rohtas, Khyber, Bhit and Nari Bolan) and three canals. (Soan Link Canal, Grand Indus canal and optional Makran Canal) • Soan Dam is the core of PFCS. Other dams will help, but Soan Dam alone can successfully handle floods like 2010. • Soan Dam sets foundation for radical changes in Pakistan’s flood control and irrigation paradigm by allowing distributed system of large local multipurpose projects. Dynamic allocation of water and coordinated flood harvesting are some of other main features. • Proposed dams increase water storage capacity of Pakistan by 644%. Apart from total flood control, PFCS will play a role of “Water Bank of Pakistan”, to ensure right amount of water at right time for all provinces, according to already defined respective water share. • PFCS will successfully block India’s move of internationalizing the flood water wastage in Pakistan for propaganda and grabbing more of Pakistan’s water.
  • 3. Pakistan Flood Control System (PFCS) • Proposed system can be built in stages but it is economical enough to be built simultaneously. Proposed dams don’t need spillways due to their role, location and sizes. Pakistan has most of necessary skills and material to build it alone. • Additional power infrastructure can make this system much more profitable by producing more electricity than WAPDA’s existing hydroelectric capacity of 6444 MW. • PFCS is designed around historical peak floods in country with 50%+ safety factor. • Avoiding any urban settlement and thickly populated areas is one of its main design consideration. • Economic feasibility: 8+ times larger yet cheaper than existing options. System will breakeven within first monsoon month of operation. Operating at 40% capacity, PFCS will add US$ 70+ billion annually to the national economy. • “New Deal”? • Strategic and geopolitical impact. • Last but not least, PFCS doesn’t need the Kalabagh dam. Instead it addresses Kalabagh dam’s potential drawbacks positively due to effective flood control in all four provinces, lack of water diversion and decentralization of Water & Power storage.
  • 4. Storage Economy(MAF/Billion US$) 7 6 5 4 3 2 1 0 Diamer basha dam Kalabagh Dam Akhori Dam Bhit Dam Soan Dam
  • 5. Comparison with existing capacity Storage Capacity Comparison(MAF) 40 35 30 25 20 15 10 5 0 Diamer basha dam Kalabagh Dam Akhori Dam Bhit Dam Soan Dam
  • 6. How this presentation is different? • Problem of lack of flood control, and storage reservoirs in Pakistan is not a news. • Pakistan has experienced massive direct devastation in form of floods, and indirectly in form of inflation, high food prices and instability in society. • This presentation is different because “it discusses the solution.”
  • 7. Scope of presentation • This document is the “presentation version of PFCS 2.0 design”. • Version 2.0 includes upgrades about flood control and irrigation based upon version 1.0 design of November 2010. • Contains details of Topographical feasibility math, supporting hydrology calculations and design overview. • Detail design including detailed hydrological efficiency, reservoir bed rock analysis, design considerations, load conditions, stability requirements, stress analysis, seismic analysis, structural features, environmental study and archeological impact needs detail study, which falls in the scope of feasibility study.
  • 8. Upgrades in PFCS version 2.0 • 19.3 MAF additional capacity and collection of extra water from Indus river right bank tributaries. • "Devolution of water and power" among provinces. high level Grand Indus Canal will deliver water and its hydroelectric potential to respective provinces. • Sindh and Balochistan get much needed large local reservoirs. This will decrease uncertainty of river flow fluctuations and canal response time. • 22.23 million acres of possible increase in Irrigation system. • Water security for Karachi, the financial and industrial hub of Pakistan. • fresh water for Kirthar national park ecosystem and Manchar lake. • Water security for Makran coast. Makran can become "California of Pakistan" being the only coastal area around gulf with sustainable water supply for whole 500 miles stretch. • Balochistan will be able to use its share of water including flood water for sustainable and efficient irrigation in Makran region. • Grand Indus canal can act as a "Water Motorway of Pakistan", for efficient and quick delivery of water all along Pakistan downstream Tarbela. In addition it will help about efficient water transfer from one location to another within provinces.
  • 9. Upgrades in PFCS version 2.0 • Grand Indus canal @ 50,000 cusecs can add 10 MAF to the effective storage of Soan dam. it will cut cost of Soan dam for same design storage. • option of "alternate route" for Indus river will improve the situation of water logging and soil salinity in Indus Basin. • Grand Indus canal offers potential for channel navigation, however this role needs to be evaluated for necessary adjustments in initial design. • Enhanced control over river flow will decrease land erosion along Indus river during normal flow and floods. • optional branching channel just upstream Guddu barrage will provide a shortcut for flexibility of water usage in Sindh. • Interlinked chain of under construction and proposed optimal sized dams can provide better water management for whole country. • Most of Pakistani cities are located along river banks and their ever increasing waste water and raw sewage is released back into rivers without treatment. this phenomenon causes serious health problems for lower Punjab and Sindh. proposed design will assure high quality water availability for southern Pakistan. • Proposed large dam in Sindh can decrease brackishness of underground water on right bank of River Indus. detail study needs to determine the optimal design for best possible effect.
  • 10. 2010 Floods in Pakistan River Indus is the soul of the Indus valley, today’s Pakistan. Lives of 180+ million people depend upon water of Indus river and its tributaries. 65-70% of Indus water flows during summer Monsoon, and in absence of a flood control system, Indus river can be dangerous during this time of year. In July and August 2010, Indus basin saw extremely high level of floods due to extra-ordinary monsoon spells. Following are some public numbers about flood damage till November 2010. • Fatalities: 1,974 • Population affected: 20,184,550 • Cropped Areas underwater: 5,546,636 Acres • District Affected: 78 • Damage estimates: official: $9.7 Billion, Unofficial: $43+ Billion, Reconstruction cost: 50+ Billions
  • 12. Indus River Hydrograph during 2010 flood(cusecs)
  • 13. Kabul River Hydrograph during 2010 flood
  • 14. Jhelum River Hydrograph during 2010 flood
  • 16. Jhelum, Chenab, Ravi and Sutlej
  • 18. Between Kalabagh and Taunsa(July 31st, 2010)
  • 19. Between Kalabagh and Taunsa(Aug 1st, 2010)
  • 20. Indus river normal flow (Aug-9-2009)
  • 21. Indus river during flood (Aug-12-2010)
  • 22. A closer look at Mithan Kot
  • 23. A closer look at Guddu Barrage(Aug-12-2010)
  • 24. Northern Sindh province with normal Flow
  • 27. Scale of 2010 flood: Khyber Pakhtunkhwa
  • 28. Scale of 2010 flood: Khyber Pakhtunkhwa
  • 29. Scale of 2010 flood: Khyber Pakhtunkhwa
  • 30. Scale of 2010 flood: Khyber Pakhtunkhwa
  • 31. Scale of 2010 flood: Khyber Pakhtunkhwa
  • 32. Scale of 2010 flood: Khyber Pakhtunkhwa
  • 33. Scale of 2010 flood: Azad kashmir
  • 34. Scale of 2010 flood: Gilgit Baltistan
  • 35. Scale of 2010 flood: Punjab
  • 36. Scale of 2010 flood: Punjab
  • 37. Scale of 2010 flood: Punjab
  • 38. Scale of 2010 flood: Balochistan
  • 39. Scale of 2010 flood: Balochistan
  • 40. Scale of 2010 flood: Sindh
  • 41. Scale of 2010 flood: Sindh
  • 42. Scale of 2010 flood: Sindh
  • 43. Scale of 2010 flood: Sindh
  • 44. True, and God helps those, who help themselves
  • 45. Facts and Figures of 2010 flood • 55.26 MAF (Equal to 8 full Tarbela lakes) of water passed through Kotri barrage into Arabian sea between July 13th and October 4th 2010 • 72.87 MAF water passed through Guddu Barrage during the same time(adjusted). • Below Guddu, 17.61 MAF Indus flood water didn’t reach the sea, submerging big areas in Sindh and Balochistan for next several months. (excluding Guddu downstream right bank tributaries flood runoff) • 73.35 MAF water passed through Taunsa and Panjnad together. • Stagnant water in Punjab cannot be accurately calculated due to unregulated right bank flood streams of Suleiman range. • 3.2 MAF of accounted water stayed in Punjab. an equivalent of all right bank catchment from Chashma to Guddu including Tochi, Zhob, Gomal, Tank, Vehowa and the Zams stayed in Punjab and lower Khyber Pakhtunkhwa. • Total water loss during 2010 summer estimates about 85 MAF, equal to winter storage for next 8 years at current capacity.
  • 46. Flood control in Pakistan • Pakistan doesn’t have a flood control system due to lack of storage capacity and absence of known practical options. • Existing dams and proposed Kalabagh dam is too small to handle the amount of inflow in 2010 flood. • Kalabagh could have stored only 7.5% of total water but not without upstream damage in Nowshera and above. • In future, due to global warming, region expects increased frequency and intensity of flash floods coupled with higher glacier melt runoff. Proposed theory of Redistribution precipitation (Seasonal Shift) link increases the need of a serious solution for flood control. • In absence of a comprehensive plan, such floods can hit the backbone of country’s economy after ever few years. • This was not the last flood. Floods will certainly happen again, in a year, or a decade, or later. No one can say it will never happen again. • By taking solid steps, Pakistan can change such disasters into a blessing by saving $30-50 billions of flood damage per decade, and earning much bigger amount by increased agricultural productivity, extra power generation and food security
  • 47. What can be controlled? • Eastern rivers (Ravi and Sutlej) are controlled by India. Pakistan doesn’t have suitable topography to handle floods in these rivers. Although huge flood canals can be built to divert a portion of flood water into Cholistan desert to recharge underground aquifers and tobas (ponds) for later use. • Chenab is a special case. India cannot control it due to lack of rights, and Pakistan doesn’t have a suitable site to control it along its length in Pakistan. It is similar to Indian situation about Yarlung Tsangpo River (Brahmaputra River) in Arunachal Pradesh where India doesn’t have a suitable site to control the 17 times bigger river(by annual average flow rate), yet it doesn’t want China to build any reservoir or ROR power project. • In presence of Kashmir conflict, there is no short term solution for Chenab flooding. Proposed Chiniot dam in Punjab (1MAF) can help, but it is too small for super floods. • Kabul, Jhelum and Indus rivers contribute 83% of Pakistan’s share of Indus system water. • We will focus on these three rivers, and will discuss the possible options to avoid future floods, while using flood water for agriculture and power generation. • West Side Tributaries of Indus from Tarbela to Arabian sea carry a significant amount of non perennial flood water. Linking of ongoing and future Medium and small dams(Kurram Tangi, Gomal Zam, Tank Zam, Baran dam etc) along western slopes can control and harvest flash floods.
  • 48. This wasn’t the biggest flood • 2010 flood wasn’t the biggest for all Pakistani rivers. Jhelum (at Mangla) saw 10,90,000 cusecs on Sept 10th 1992 as compared to 2,67,000 cusecs peak on July 31st 2010. • Chenab’s (Marala) maximum for 2010 was 2,16,000. 26 August 1957 flood at Marala was 11,00,000 followed by 8,70,795 on 5/7/1959 and 8,45,090 on August 28th 1992. • Ravi’s (Jassar)2010 peak was 21,000 vs 6,80,000 in 1955. flood of 1988 overflew at Jassar, with a record of 5,76,000 at Shahdara downstream. • Sutlej stayed around 53,000 in 2010, in contrast to 5,98,872 in 1955 and 3,99,453 in 1988 • We are not ready for any such record flood. • In future, as Pakistani population and cities grow, the damage will grow for same intensity of floods.
  • 49. Past 10 Floods through Kotri • 1976: 64 MAF • 1983: 43.8 MAF • 1988 :44.7 MAF • 1991: 42.0 MAF • 1992: 69.19 MAF • 1994: 81. 21 MAF • 1995: 61. 09 MAF • 2005: 24.5 MAF • 2007: 15.82 MAF • 2010: 55.8 MAF (excludes 33-35 MAF stagnant water) • Total 535 MAF, worth 1.07 Trillion US dollars. Historical Kotri downstream flow averages 35.2 MAF (1976-2006 WRMD WAPDA). While excluding 10 MAF for Indus delta, average 25.2 MAF water is available for harvest annually. PFCS 2.0 design will save water course loss from Tarbela to Guddu or Kotri. 40% reduction means 14 MAF extra water per year. It will also reduce risk of illegal water theft and evaporation losses.
  • 50. Jhelum flood comparison, 1992, 1997, 2010 1000000 900000 800000 700000 600000 500000 400000 300000 200000 100000 0 1 2 3 4 5 6 7 8 Mangla_outflow_92 Mangla_Outflow_1997 Mangla_outflow_2010
  • 51. Chenab flood comparison1992,1997,2010 900000 800000 700000 600000 500000 400000 300000 200000 100000 0 1 2 3 4 5 6 7 8 Marala_outflow_1992 Marala_outflow_1997 Marala_wave1_2010 Marala_wave2_2010
  • 52. Flood control on Indus river • Tarbela Dam is the only storage available on Indus river so far. • However, in future, Tarbela and Diamer Basha Dam (2010-2018) together, will be able to store 14.2 MAF out of total 65 MAF annual runoff below Tarbela. • Still 50.8 MAF in an average year, and up to twice amount of water in high flood years will stay uncontrolled. • Both of these dams are designed mainly for storage. They can help towards flood control, but they may not always be ready for a mega flood. • More available options include Akhori dam and Kalabagh dam. If ever built, these two dams can improve the storage capacity to 26 MAF, thus improving flood control capacity while increasing Rabi water availability in Pakistan by 32%. • Next few pages talk about Kalabagh and Akhori Dams.
  • 53. Kalabagh Dam • Height: 79 m (259 ft) , Live storage: 6.1 MAF • Indus river at Kalabagh has an average annual flow of 95 MAF. Kalabagh dam can store only 5.8% of total annual water. It cannot control a flood like 2010 flood, although it could have trimmed the maximum spike by top 200000 to 300000 cusecs off the first wave only, like Tarbela. • Table below shows summer runoff at Kalabagh during last three years. Month Flow(MAF) in 2008 Flow(MAF) in 2009 Flow(MAF) in 2010 April 4.41 4.05 3.67 May 8.11 7.65 7.30 June 11.49 13.18 11.58 July 18.02 18.13 22.05 Aug 16.84 15.96 29.40 Sept 6.43 7.45 9.72 Total 65.30 66.42 83.72
  • 54. Kalabagh Dam issues Kalabagh dam is controversial due to multiple reasons. • Khyber Pakhtunkhwa, Sindh and Balochistan have already rejected it. • Kabul river above Nowshera has no flood control at all. In absence of another upstream dam like proposed Khyber Dam, Kalabagh dam will be a disaster for Peshawar valley. • Indus floods add to the magnitude of Kabul river floods by blocking their way. Proposed Soan dam (discussed later), will address this concern, by sparing entire Indus bed between Tarbela and Kalabagh to drain the Kabul river in case of extreme floods. • Kalabagh dam’s revised reservoir level of 915 feet, still stagnates Kabul river upstream of Akora khattak. (initial design height was 925 ft above sea level) • More research is required to address water logging, lake size and flow route issues. A practical Kalabagh dam may be another 25-40 ft below the current design of 915 ft. which will reduce its live capacity to less than 4 MAF.
  • 55. Akhori Dam project • Akhori Dam is a 6.0 MAF off channel storage project. Its proposed 400 ft high 5 KM long main dam and (7 km long saddle dam) makes its construction much bigger than Tarbela. • With option of 7-8 times larger design capacity of Soan reservoir, Pakistan my not need Akhori dam, and same resources can be used to build Rohtas and Khyber dam. • World Bank team carried out inspection of Akhori and Sanjwal dam locations in 1968 . Team head Dr Lieftnick in his report, rejected Akhori Dam for a height of 250 ft due to foundation problems,. • A 400 ft high design at same site, may become too expensive.
  • 56. Flood control on Jhelum River • Mangla Dam stores about 4 MAF of water, but being the single storage dam on Jhelum, it is not flexible enough to handle additional flood water especially in late summer. Most major floods hit Mangla when it is already full. • Pakistan has minimal control on flooding in Chenab, Ravi and Sutlej. A flood in Jhelum river, coupled with flood in these three rivers can be very dangerous (like in 1992). • PFCS suggests “Rohtas Dam” with 9 MAF storage to handle super floods up to twice the size of 1992 flood of Jhelum. • Available storage limit is huge, and it can balance Chenab flow during high flow season and large floods. • Location of Rohtas dam can offer a lake up to 16 MAF size, and southern Bunhar river valley can make another 9 MAF lake, but such big reservoirs are not needed. • Next few slides show the amount of water to handle. Please note that Jhelum and Chenab usually flood simultaneously, and their combined flow rate at Tarimmu and below can become bigger than Indus river’s maximum combined flow rate during 2010 flood.
  • 57. Flood of 1992 1000000 900000 800000 700000 600000 500000 400000 300000 200000 100000 0 7 8 9 10 11 12 13 Tarbela_out_1992 Mangla_out_1992 Marala_out_1992 Jassar_out_1992 Suleimanki_out_1992
  • 58. Flood of 1997 800000 700000 600000 500000 400000 300000 200000 100000 0 25 26 27 28 29 30 31 Tarbela_out_1997 Mangla_out_1997 Marala_out_1997 Jassar_out_1997 Suleimanki_out_1997
  • 59. Jhelum’s deadly peak of 1992; hour by hour 1200000 1000000 800000 600000 400000 200000 0 0 5 10 15 20 25 Mangla_inflow_1992 Mangla_outflow_1992
  • 60. Flood control in Kabul river basin • In 2010, most of damage in Khyber Pakhtunkhwa occurred due to flood in Swat river. future Munda dam has a capacity of 0.76 MAF ,enough for only 3 days of peak flood. Munda dam needs a design change to increase the individual storage capacity by 3-4 times to absorb large floods. • moving same dam 18 km upstream from current location can store 4 times more water while producing more electricity using a power tunnel. • Kabul river at Nowshera drained 9.12 MAF flood water during 2010 flood month, about half of it came out of Swat river at Munda. 71% Swat river’s water flew during first 15 days. • Kabul river is the main river in Peshawar valley. Warsak dam on Kabul river is silted to the top, and offers zero storage capacity or flood control. • PFCS suggests a politically unconventional solution, “Khyber dam”. • If possible, this is the best and permanent solution for area and region for next several centuries.
  • 61. Overview of proposed reservoirs # Dam River Role Max Dam Lake area Storage Extra Annual Water Height (Sq KM) Capacity Hydro electric level (feet) (MAF) potential (MASL) (GWH) 1 Soan Dam Off Flood control, Storage, 410 415 1230 38.4 18000 channel Hydel (48.4 for Indus dynamic) 2 Khyber Kabul Flood control, Storage, 500 550 324 10.67 3500 Dam Hydel 3 Rohtas Off Flood control, Storage, 340 345 294 9 1000 Dam channel Hydel for Jhelum 4 Bhit Dam Off Pumped Storage, 250 510 244 15.5 7000 with channel Regional Irrigation GIC for Indus command, Delta ecosystem support, optional Hydel 5 Nari Bolan Nari Flood control, storage, 280 390 112 3.8 200 Dam Bolan Regional Irrigation command Total 77.37 29700
  • 62. Overview map of PFCS Version 1.0
  • 64. Data References • ASTER Global Digital Elevation Model (ASTER GDEM) (10 m accuracy) • digital elevation model (DEM) data collected by NASA's Shuttle Radar Topography Mission (SRTM). • Topographic 1:50,000 maps by Survey of Pakistan. • India and Pakistan 1:250,000 Series U502, U.S. Army Map Service, 1955 • Calculated capacity is based upon minimum of the results of processed datasets, which increases the level of confidence for calculations. • Soan dam’s axis was manually measured using 2 digital altimeters against known benchmarks. Results confirmed a depression of 131 meters (+10m bridge) from Dhulian Mor Mosque to top of Dhok Pathan bridge. • Final figures for Dam design, lake size, capacity and reservoir shape need professional physical survey of area. • Source of water flow data is “Flood forecasting division of Pakistan(FFD)”. Mathematical model is based upon daily averages and 6 hour flows at Rim stations in Pakistan.
  • 65. Soan Dam • Soan valley is best available site for flood water storage below Tarbela. During 1960’s, World Bank team evaluated 5-6 times smaller storage reservoir at this site, with design bottle-neck of unlined canal and no option of Tunneling. • Lake size was likely never measured, because its listed size, height and dam length figures (picture below) are wrong. A 275 feet high dam at Dhok Pathan offers about 25 MAF gross storage and 35 MAF live storage for flood control. Thanks to report, as it confirms that minimum of 25-35 MAF flood water can be handled at 275 masl. Due to site’s topography and geophysical location, much bigger dam is possible. World bank report doesn’t talk about any foundation problems like Akhori area. It was either not evaluated, or there was no issue. Feasibility study can confirm it. • Seismicity of site is favorable (g factor 0.03-0.1, Source GSP Seismic Hazard Map of Pakistan) • In World bank’s report, figure of 8.5 MAF was used based upon a design of three parallel canals running for three months, needing water-lifting at some locations. It would have needed 15-17 unlined high maintenance parallel canals for transporting total flood water during flood season. It makes sense why this project didn’t get due attention . 45 years later, options of lined channel and large diameter tunnel boring can help exploit full potential of this site.
  • 66. Soan Dam site Geology Dam axis lies on Pliocene and Miocene sedimentary rocks, same as the site of proposed Kalabagh dam. (Source: Geological Map of Pakistan, DG GSP)
  • 67. Soan Dam site Geology
  • 68. Soan Dam • Soan reservoir, made a dam 1 km upstream from Dhok Pathan bridge offers up to 46.6 MAF gross storage. A 113 meters deep lake can hold 38.4 MAF water. Several dam locations are available between Markhal to upstream Dhok Pathan from 395 m to 415 masl. • A dam at this location will not distribute any water from Indus river. It will collect during flood season and drain back to system at right time. • Proposed Grand Indus canal at 50000 cusecs can increase its effective capacity to 48.4 MAF for same height of 113 m. • dam at this site will be relatively low cost. Material requirements are 60% of Tarbela dam. • Mangla’s main dam and dykes length is more than 10 KM. 30 KM long Hirakud Dam on Mahanadi river in India (built in 1957) is four times longer than biggest possible Soan Dam.
  • 69. Soan Reservoir •Following table shows possible capacity of Soan reservoir (using SRTM DEM V4.1) Required Dam elevation from contour Lake Lake capacity at Possible gross # length (KM) river bed(m) elevation(m) area(Acres) level(acre feet) capacity (MAF) 1 3.2 95 390 234889 22933956 22.9 2 3.78 100 395 258212 26978420 27 3 5.1 105 400 278367 31379494 31.4 4 5.67 110 405 299656 36120496 36.1 5 6.72 115 410 319837 41201640 41.2 5 7.66 120 415 340677 46619241 46.6 •Following table shows possible capacity of Soan reservoir (using ASTER GDEM) lake depth Soan Dam bounded acres block volume Cumulative AF MAF 0 300 1622 10 310 7071 142608.665 8694.65 0.00869465 20 320 16512 386879.115 395573.765 0.39557377 30 330 35521 853601.365 1249175.13 1.24917513 40 340 55405 1491641.03 2740816.16 2.74081616 50 350 94613 2461045.29 5201861.45 5.20186145 60 360 134786 3763290.595 8965152.045 8.96515205 70 370 175522 5090602.74 14055754.79 14.0557548 80 380 220448 6495887.85 20551642.64 20.5516426 90 390 262908 7929455.18 28481097.82 28.4810978 100 400 303820 9297172.84 37778270.66 37.7782707 110 405 325862 5164714.575 42942985.23 42.9429852
  • 70. Design parameters • Soan Dam needs an Earth filled main length with low dykes extending on both sides. • main length is 3 km long and 40 to 132m high. • Left and right dykes are 2.25 and 1 km in length with average height of 22 m(for average lake depth of 17 m) • Soan dam needs a 90 km waterway from Tarbela lake to the reservoir, (like Ghazi Barotha and proposed Akhori dam). a waterway with flow capacity of 250000 cusecs can assure the maximum storage use and flood control from July to September. • Soan reservoir will collect extra water from its own catchment area too, which spreads from Kallar Kahar to Muree. Dead reserve and local run-off will decrease the required size of Link canal. • Major design challenge is to connect the reservoir with Tarbela lake. Higher level canal will bring lesser silt, is more energy efficient, needs a shorter canal length for connection being closer to dam site, but at cost of dam life and flood control capacity of Tarbela dam . Adjusting the design flow rate can improve flood control without addressing silting of Tarbela. Lower level of link canal can improve life of Tarbela dam. • Tunnels can be used near start and end of the link canal to avoid excavation. With available maximum TBM diameters (~15 m) , 4 parallel tunnels can provide an alternative to excavating open channel at hard locations.
  • 71. Soan link Canal level • Optimum height of Soan link canal intake needs detailed study of hydrological data trends as well as political aspects, but keeping it closer to dead level can keep Tarbela reservoir ready to absorb super floods. • Following table contains available storage capacity for each canal withdrawal level above Tarbela’s dead level. 435-445 offers best range for economical canal design. Please note that Diamer Basha dam’s storage will be a plus for available volumes in column #3 Storage available in Tarbela for flood control # Soan link canal intake level (meters) (MAF) 1 420 6.8 2 425 6.6 3 430 6.2 4 435 5.7 5 440 5.1 6 445 4.5 7 450 3.7 8 455 3 9 460 2.2 10 465 1.3 11 470 0.5 12 472.42 0
  • 72. Soan link Canal • Pakistan has built largest fresh water link canal between Ghazi and Barotha. (base width 58.4m, depth 9m, side slope 1:2, gradient 1/10000, flow rate 56500 cusecs) • Duel canals for Balloki Suleimanki link use a width of 340 m for 82 km distance. With appropriate route, slope and depth combination, Soan Link Canal requires lesser width for lower flow speeds under 3 m sec. • By adjusting channel geometry, i.e. cross section, depth and slope, Soan link canal can generate up to 350k cusec flow-rates inside “man made gorge”. For last 20 km length, that need most digging, this option is very helpful by reducing width of canal by 60-80%.
  • 73. Soan link Canal • Concrete lining is ideal for flows above 5m/s. it will be economical to use higher range of subcritical flow regime. • Lining will eliminate the high maintenance overhead feared in design from 1960s. • Upgrades in PFCS Version 2.0 will make it possible to use this canal partially around the year, for efficient and economical water and power usage. • Optional tunnel lengths discussed later will make things much easier. Cross sectional geometry of SLC can be adjusted according to feasibility of its navigable role.
  • 74. SLC size choices vs. flow rates flow Discharge Discharge manning Free- velocity Channel Channel (cusecs) (cumecs) gradient coeff board(m) (m/s) Depth(m) Froude lining(m) 165000 4672.28 0.0003 0.012 1.5 5.695 10.37 0.63 111.48 225000 6371.29 0.0003 0.012 1.5 6.224 12.53 0.65 120.09 300000 8495.05 0.0003 0.012 1.5 6.79 14.36 0.66 129.33 350000 9910.9 0.0003 0.012 1.5 7.096 15.59 0.67 134.83
  • 75. 2010 flood scenario with Soan Dam • After June 1st, Tarbela lake is kept at dead level 420 m (1378 ft) while diverting all extra water to Soan reservoir till a flood arrives. • Tarbela dam can absorb 6.8 MAF water, enough to completely stop the river flow from 28th July onwards, while diverting 250000 cusecs into Soan lake for next three months. • Numerical analysis shows that 6.8 MAF of dedicated capacity at Tarbela lake can easily absorb all flood spikes of 2010 while Soan link drains it continuously. • In this extreme case, mighty Indus can be totally blocked downstream Tarbela while collecting entire flood water (up to 38 MAF) into Soan reservoir. In the end, another 6.8 MAF capacity will still be available at Tarbela. • meanwhile it spares the Indus river bed between Tarbela and Kalabagh for highest floods in Kabul or Swat river. This makes second safety layer for Khyber Pakhtunkhwa flooding after Khyber dam. • In presence of future Diamer Basha Dam, capacity requirement for Soan link canal drops to 165000 cusecs for complete flood control.
  • 76. Power generation at Soan • There will be no loss of power potential. • Extra water and extra altitude range means much more electricity than Tarbela, Ghazi Barotha and Kalabagh Dam together. • Soan can generate electricity at both inflow and outflow. • Dam site lies next to 380 KV transmission. It will cut the cost of associated power infrastructure. • Underground power plant at Kot Maliaran with inlet at lake’s dead level (310 m) can generate hydro-electric power comparable to Tarbela’s output. • Additional turbines on outflow will generate extra power. • Grand Indus canal from Soan Dam back to Indus can produce extra electricity, much more than Kalabagh Dam. • Tarbela offers 85-135m of potential difference with waste of flood water at peak level. • Soan Dam can use all water between 120 meter consistent head using tail intake design.
  • 77. More about Soan dam • In addition to water storage and flood control, Reservoir area can be used for occasional farming(organized or unorganized), sometimes for years. (like in the Siran Pocket of Tarbela lake). • Storage area cannot be used for permanent settlements and populations need to relocate above maximum flooded level. • Reservoir area is sparsely populated due to its geography. Ratio of effected population is less than people displaced in construction of other big dams including Mangla, Tarbela and Diamer Basha. Akhori and Kalabagh dam effect higher population density areas. • No city will submerge. Both Chakwal and Talagang are 55 m and 120 m higher and at a safe distance. • Oil fields in Potohar will not submerge. • Soan Dam will submerge 40 km of M2 motorway. An elevated road with Chakri causeway will help avoid a longer M2. this is far less than 100 km submerged KKH in much difficult terrain for Diamer Basha dam. • Lake will recharge Soan river ecosystem with fresh water supply.
  • 81. Cost estimate for Soan Reservoir Total cost of Soan reservoir system will stay about half of Diamer Basha dam’s $12.6 billion (2008 estimate) due to type and location of project, while providing 7 times more storage capacity. Soan Dam • Soan Dam construction volume is much smaller than Tarbela dam. • 2:1 ratio dam (Tarbela standard)needs 54.3 mcm 2.5:1 ratio measures 66.3 mcm 3:1 (overdesign)ratio needs 78.22 mcm for 41% additional foundation size(equal to Tarbela) values become. 76.5, 93.4 and 110.3(51%, 62% and 73% of Tarbela dam size.) Soan Link Canal(SLC) • Total cost of Ghazi Barotha Canal was $365.7 Million. • SLC is 1.9 times longer and at an average, 1.5 times wider and deeper. This translates into 4.5 times more building material . • Gross Earthwork involved is 3.2 times more than GBC, for channel at 445 m.(4.5 including 1:1 safety step contours all along the length) • SLC will cost around $1.5 Billion. • Steep tunnel can be used in last quarter, “Culebra Cut” of SLC, but open channel will be more economical and needs low maintenance cost.
  • 82. Rohtas Dam • Rohtas dam , an off channel storage site for Jhelum river on Kahan river bed, can provide 100% storage and flood protection in Jhelum river around the year. • It can completely block Jhelum flow during high floods in Chenab, Ravi and Sutlej rivers, to thin out the intensity of flood. • It needs a single main Dam, smaller than Tarbela dam in construction volume. • Design level of Rohtas lake is 345 m, 40 m below maximum level of raised Mangla lake. It can generate power at both intake and exit. • two way flow control above Bheli Bathar can make water flow to Rohtas lake independent of the water level in Mangla lake. This will enhance the flood control capacity by several times. • Rohtas lake is 8.5 km from center of Dina city. Mangla lake is 11.75 km away. Kahan river bed between Dina and Rohtas reservoir will act as a natural barrier for Dina from seepage and other hydrological effects.
  • 83. Rohtas Reservoir design numbers Rohtas1 above river bed Dam(short axis) bounded acres volume Cumm AF MAF 0 240 434 10 250 3050 57155.02 8694.65 0.008695 20 260 6667 159407.4 168102 0.168102 30 270 12176 309119.4 477221.5 0.477221 40 280 19318 516659.1 993880.5 0.993881 50 290 27963 775644.8 1769525 1.769525 60 300 36834 1062995 2832520 2.83252 70 310 46436 1366044 4198564 4.198564 80 320 55710 1675705 5874270 5.87427 90 330 66577 2006118 7880388 7.880388 100 340 76817 2352379 10232766 10.23277 110 350 86670 2682004 12914771 12.91477
  • 84. More Rohtas options(SRTM) Grand rohtas1@350 Rohtas 2 @380 OWR Gross Gross masl ft Acres Acre-ft Capacity Acres Acre-ft OWR Capacity 260 852.8 3623 237668.8 280 918.4 16640 1091584 328000 5256 344793.6 300 984 37562 2464067 590400 12527 821771.2 262400 320 1049.6 61177 4013211 721600 24305 1594408 262400 340 1115.2 87239 5722878 721600 32000 2099200 262400 350 1148 97656 164000 42014 2756118 262400 380 1246.4 50658 262400 13529410 2525600 16055010 7616291 1312000 8928291
  • 89. Khyber Dam • Proposed 9 km upstream of existing Warsak dam, 500 ft high and 430 m long Khyber dam (145 m above river bed ) will create a reservoir of 10.67 MAF , bigger than Tarbela lake. • If required, Khyber dam can be constructed downstream, but it will need 50% longer dam. Detailed study is required to evaluate both options. • Upstream location has a challenge of silt removal. Grout Curtain or pressure grouting offers a time tested solution. grout is injected into drilled holes in silted riverbed above bed rock. This creates a waterproof barrier of overlapping pillars. Aswan dam has successfully used this technique on a much bigger scale. (video detail) • Proposed dam can absorb any size of flood in known history and Peshawar valley will never flood again. • Huge Khyber lake will extend 61 miles upstream, including last 30 miles inside Afghanistan. Tail of this lake will cover 25,949 hectares area inside Mohmand Dara , Lal Pur and Batikot distt in Nangarhar province of Afghanistan.
  • 90. Khyber Dam • Lake area inside Afghanistan is well known flood zone and unsuitable for permanent settlements. It contains riverbed and farmland. • Lake will not effect Jalalabad which is 250 feet higher and 12 miles upstream from the maximum extent of proposed lake. • Afghanistan has recently built dams on Kabul river without consulting Pakistan. Pakistan should not do the same. It is better to discuss and coordinate on such issues, for welfare of effected people. • Effected Nangarhar province is a 100% Pashtun area, and gateway to Khyber pass. It can become hub for both trade and low cost energy for Afghanistan. • Afghanistan needs electricity, being one of the lowest countries by per capita power availability(3.6 watts per person) • Pakistan and Afghanistan should come up with a formula to materialize this mutually beneficial project for sake their people. Afghanistan can get share in extra electricity generated (~3500Gwh), land use charges or one time payment for relocation and development of displaced people.
  • 91. Khyber Dam • Pakistan can help building improved irrigation system for alternate location of submerged land in Nangarhar. • Proposed dam can promise deep rooted co-operation for regional stability. • Aswan High dam on Nile river is another example, where Sudan and Egypt have worked together in similar situation. Aswan lake’s area inside Sudan is more than three times larger than proposed Khyber lake area inside Afghanistan at maximum level of 500 masl. • There can’t be a better way for Pashtun leadership to help their people while solving a permanent threat of flooding for millions of people. • This Project will help create opportunities on both sides of border, to promote peace and eliminate poverty and extremism.
  • 92. Khyber Dam capacities(ASTER GDEM) average contour Khyber bounded acres block volume AF MAF 390 4465 400 6988 187886.465 8694.65 0.008695 410 11851 309053.795 317748.4 0.317748 420 16521 465442.66 783191.1 0.783191 430 22055 632839.28 1416030 1.41603 440 29193 840723.44 2256754 2.256754 450 36747 1081745.7 3338500 3.3385 460 42753 1304197.5 4642697 4.642697 470 51731 1550010.02 6192707 6.192707 480 63411 1888904.51 8081612 8.081612 490 76649 2297684.3 10379296 10.3793 500 91801 2763422.25 13142718 13.14272 510 107141 3263643.51 16406362 16.40636 520 124274 3796363.075 20202725 20.20272 530 143361 4390552.175 24593277 24.59328 540 164045 5042995.43 29636272 29.63627 550 185993 5742373.39 35378646 35.37865 560 204280 6402428.565 41781074 41.78107
  • 93. Munda reservoir is 12 miles away and 100+ meters higher than Khyber lake. In future, Munda lake can be connected to Khyber lake with a steep spillway tunnel to soften extreme floods in Swat river without wasting water or power.
  • 94. Hydroelectric potential of Khyber dam • Kabul river at Nowshera has a flow rate comparable to Jhelum at Mangla. Warsak flow makes 80% of total flow at Nowshera. • Due to low design elevation, Warsak dam generates only 994 GWH(1/5th of Mangla’s output) • Mangla taps 4797 GWH between 55-105 meters potential drop range( between dead and peak level of reservoir) • Raised Mangla will generate 5800 GWH electricity between 55-117 m limits. • Khyber dam offers 67-180 meters, which translates into potential of 4500+ GWH per year.
  • 95. Conceptual view Khyber dam will look like Iran’s Karun-3 dam in dimensions and type
  • 97. Afghanistan side of Khyber reservoir: WHO map shows the location as flood hazard area
  • 98. Bhit Dam • Sindh has a large natural site for Water storage near Bhit, between Bhadra and Kirthar mountains. It has never been considered before due to being different from conventional storage sites. • This site offers a perfect location for Pumped-storage hydroelectricity reservoir in its simplest form. • 150 meter high dam at 26.2590, 67.5136 can store 15.5 MAF water. Higher dam can create a lake up to 53.7 MAF. • proposed lake is surrounded with multiple layers of hill ranges on both sides, which makes it safer and stable. Reservoir’s design surface area is smaller than Manchar lake(0.08 MAF and 520 sq km), but storage capacity is about 200 times bigger. (not 200%). Size of Manchar lake can be reduced in presence of Bhit reservoir. • It needs a 6 km long dam, which is shorter than Mangla dam.
  • 99. Bhit Dam • Bhit reservoir offers multiple uses, but water storage for Sindh province is its main aim. Proposed Grand Indus canal, can deliver hydroelectric potential of about 40 MAF water per year with higher relative potential. It translates into 1.5 - 2 times more electricity than Mangla dam. • Without Grand Indus canal, Bhit Dam can use Manchar lake as intake reservoir. Operating energy can come from Peak load balancing with national grid, Fossil fuel, local coal reserves, or multiple gas fields in same area. • Reservoir’s location and altitude offers opportunity to use wind as one of energy source. • Extended Grand Indus Canal, offers much more benefits than its cost, and is recommended as better option for feasibility study. • Water and power output of Bhit dam can support new urban and rural areas on Sindh highlands.
  • 101. Grand Indus canal • option of "alternate route" for Indus river will improve the situation of water logging and soil salinity in Indus Basin. • Grand Indus canal offers 115-185 meters of potential difference for entire summer water. Its integration with dams on western tributaries can multiply the total potential, while Kalabagh potential is only 65 m at maximum(controversial) level of 278 m(915 feet). In Picture: Conceptual view of Grand Indus canal.
  • 102. Grand Indus canal • Grand Indus canal is a proposed concrete lined channel, that will deliver water from Soan Dam to Southern Indus basin around the year. • Grand Indus canal can act as a "Water Motorway of Pakistan", for efficient and quick delivery of water all along Pakistan downstream Tarbela. In addition it can help about efficient water transfer from one location to another within provinces. • Grand Indus canal @ 50,000 cusecs can add 10 MAF to the effective storage of Soan dam. it will cut cost of Soan dam for same design storage.
  • 103. Grand Indus canal • Most of Pakistani cities are located along river banks and their ever increasing waste pollutes the rivers. this phenomenon causes serious health problems for lower Punjab and Sindh during low flow season. Pakistani rivers are still much cleaner than Ganga or Yamuna, but they need to aim higher standards. So far situation is only getting worse. • GIC will assure high quality water availability for southern Pakistan. • Pictures below show Ravi bridge(left) and 60 km downstream near head Baloki (right). This “Black Water” deserves attention.
  • 104. Grand Indus canal • Enhanced control over river flow will decrease land erosion along Indus river during normal flow and floods. • optional branching channel between Punjab and Balochistan, just upstream Guddu barrage will provide a shortcut for flexibility of water usage in Sindh. This site is suitable for a hydroelectric ROR project. • Interlinked chain of WAPDA's proposed optimal sized dams can provide better water management for whole country. • Grand Indus canal offers potential for channel navigation, however this role needs to be evaluated for necessary adjustments in initial design.
  • 105. Grand Indus canal • Soan link Canal faces a challenge of crossing Indus river above Kalabagh. • Siphon tunnel, elevated aqueduct, or an economical hybrid of both can be used for this purpose. • Pont du Gard, France(below) is more than 2000 years old.
  • 106. Grand Indus canal • Option of Prestressed concrete Siphon is more secure and easy to maintain. • Figure: Soap Lake siphon in Washington state, USA
  • 107. Nari Bolan Dam • Kachhi plane is surrounded with multiple suitable sites for water storage. small dams can be built for flood control and water harvesting. Most of these sites are suitable to drain flood water into Grand Indus canal. • 120 m high Nari Bolan dam, 3km upstream of Nari Head offers big storage capacity (3.8 MAF) for local flood water and extended grand Indus Canal. • Nari Bolan site lies in commanding position for sub-basin and its elevation is suitable for interface with extended Grand Indus canal. • Talli Tangi and Bolan dam sites on its left and right can be connected for additional storage, if needed. • Nari Bolan reservoir connected with Grand Indus canal can provide much bigger, efficient and elegant irrigation system for Balochistan than Kachhi canal due to its design parameters.
  • 109. Makran canal • Grand Indus canal will deliver water from multiple reservoirs to Bhit dam at 250+ masl. • It provides an option of a smaller canal link with Mirani dam, linking reservoirs in Dasht, Gwadar-Ormara, Hingol and Porali river basins. • This will greatly improve the coastal region for sustainable social and efficient agricultural growth. • Balochistan can use the canal to deliver a part of its flood water share across the Balochistan plateau. Government of Pakistan should allocate extra water for this region for development of local population and extra ordinary potential of this region. • Interbasin transfer of water is not something new. India uses Indra Gandhi canal to transfer Indus basin’s water to Thar desert. It shouldn’t be a problem within Balochistan. • 1151 km long 13,000 cusecs California aqueduct (built 1963) is a good model for this canal. Makran canal will be much smaller in capacity and length.
  • 110. Makran canal • Makran canal can become the backbone for growth and prosperity in Makran.
  • 111. Makran canal • Makran region has excellent geography and weather. Improved water supply can make it “California of Pakistan”, and “Gateway to Middle East.”
  • 112. Water for Karachi • In Pakistan, 90% water is used for Agriculture. Out of rest 10%, Karachi gets a fraction of a percent to lead the national economy and industry. • Situation of water in Karachi needs a lot of improvement in quality and quantity. It is a major contributor towards problems of local population.
  • 113. Water for Karachi • Makran canal will cross hub basin upstream Hub reservoir and Karachi can get more water according to its growth needs.
  • 114. Current situation • During winter, total water inflow in Pakistan’s river system drops to just 3% of summer’s peak flows. • By January, dams in Pakistan are almost empty and total inflow drops to 35000 -40000 cusecs. On 23rd January 2010, there was 1.5 MAF water left, with just 37000 cusecs inflow to the system. total inflow on January 4 th 2010 was 37,205 and 34000 on 6th Feb. 2010. • During March, Pakistan’s existing dams hit the dead level. On 12 th March 2010, Mangla dam was at dead level (1040 ft), and Tarbela was at 1384 ft(5 feet above dead level). While system inflow was 69,024 cusecs. • Kharif sowing season in Sindh starts in April and ends well before the monsoon or heavy summer melt arrives. A blame game of water theft, playing politics and violation of water rights starts between provinces over every single drop of water, which makes sense because both dams and rivers are empty.
  • 115. Current situation • Sindh needs extra storage capacity more than any other province to support its Kharif sowing season. • Cotton , Paddy(rice) and Sugarcane are major Kharif crops in Pakistan. Cotton and its products amount 60% of export earnings for Pakistan. Sugarcane provides a big portion of caloric intake for population while rice is used for both local consumption and export. (rice makes 10% of export earnings) • Monsoon helps Kharif crops in rest of the country, but uncertainty of rain delays or flooding is always there. A fluctuation in weather pattern can cause a big damage. • Late arrival of monsoon harms the initial growth of crops while floods due to heavy rains destroy the crops in flooded areas. • Building new dams can assure availability of right amount of water at right time, while controlling the floods.
  • 116. Impact on Pakistan's economy • No more floods means stable and safer cities and villages. • PFCS can control erosion on banks of rivers that destroys thousands of Acres of land annually in Pakistan. • Pakistan’s existing water storage capacity for Rabi (and Kharif sowing) is 12.1 MAF. building these dams will increase the storage capacity to 90 MAF • In Pakistan, One MAF stored water’s value is roughly equal to 2 Billion US dollars (in 2010). If PFCS is used at 40% potential, it can earn more than 70 billion 2010 US dollars per year for next several centuries. • Pakistan’s population estimate in 2010 is 180 million, which will double to 360 million by middle of current century. • Wheat, the most common staple food in Pakistan is a winter crop, that heavily depends upon stored water. • In future, Pakistan will need to switch its priority towards growing more winter crops for local consumption instead of “wasting” water on low profit water intensive exports including rice and cotton. • Our current major “cash crops” are at the bottom of food chain in international trade. Bangladesh uses them as raw material to export finished products to developed markets. • With better coordination and control on water losses, new areas can be brought under high efficiency cultivation in all four provinces.
  • 117. Impact on Pakistan's economy • "Devolution of water and power" among provinces. • growth of sustainable infrastructure for local population in western plains of Indus river. • food security and increased agriculture and livestock output. • Project will create jobs for local skilled and non skilled work-force during decades of construction, and later for operation and development of additional infrastructure in social and agricultural sector. • Water security for Karachi, the financial and industrial hub of Pakistan. • fresh water for Kirthar national park ecosystem and Manchar lake reservoir. • Water security for Makran coast. Makran can become the only coastal area around gulf with sustainable water supply for whole 500 miles stretch. • Balochistan will be able to use its share of water including flood water for sustainable and efficient irrigation in Makran region.
  • 118. Hydroelectric power generation • Proposed dams can double the current hydroelectric power generation capacity in Pakistan. • Pakistan has enormous hydro electric potential, which is out of scope of this presentation. • Indus river hydroelectric projects like Pattan, Thakot, Dasu, Diamer Basha, Bunji, Yulbo, Tangus, Katzara and Yugo offer about 40000 MW hydroelectric power, and are part of WAPDA’s long term vision. A fraction of them can manage local flood hazards while coordinating with PFCS. • Proposed Katzara dam offers 40 MAF storage, more than Indus river’s annual flow at Skardu. This dam can ensure regulation of Indus water and power above Tarbela during winter, which will cut capacity and tunneling costs of power projects into half.
  • 119. Interesting Trivia • Theory of “Redistribution of Precipitation (Seasonal Shift) in Pakistan” by Dr. Muhammad Hanif, National Weather Forecasting Centre (link) defines the changed pattern of 2010 monsoon. If this shift occurs more frequently, PFCS has already an off shelf solution for it. “Darra e Tang Dam” has very huge potential to absorb this shift. Site can collect up to 210 MAF water, submerging Laki Marwat and sparing Bannu. World bank left this site “blank” in its study. We don’t need such a big reservoir, but very low dam at Darra-Tang can offer comparatively large capacity, without touching population centers. • If Katzara dam is built as tall as Diamer Basha dam, it can hold 90 MAF water, equal to 2.5 year flow of Indus at dam site, but it will submerge beautiful Skardu valley. • Many possible dams in Balochistan are not included in PFCS 2.0 to avoid complexity. Reservoirs for Rashkan basin, Hamun Mashkhel basin, Pishin Lora basin and Hamun Lora basin can be handled individually. • Dozens of Right bank tributaries of Indus between Kalabagh and Arabian sea can be integrated into PFCS in future. • Name for Soan dam, the heart of PFCS, was chosen due to multiple factors. Wait for details.
  • 120. Numerical results of PFCS performance for 2010 flood.
  • 121. Conclusion • Floods, including Super floods will certainly come again, in a year, or a decade, or later. • By building flood control facilities, we will face them more gracefully. • Pakistani people can pray for floods once PFCS is built. • We don’t have enough time to waste before materializing such projects.
  • 122. Thanks for watching Email for details & comments inam.rehman@gmail.com