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Status of Soil Resources in
Lebanon
By Roger FRANCIS
CNRS-National Center for Remote
Sensing
Jordan – Amman 1-5 April
2012
Status of environment and coastal
ecosystem
State of the art on soil studies in LebanonEarly soil studies in Lebanon addressed:
– Soil mapping with the reconnaissance soil map of Lebanon at
1:200.000 scale (Geze, 1956),
– Pedogenesis of red soils on hard limestone (Lamouroux, 1968),
– Soil irrigability and fertility (FAO, 1969) using the old French soil
classification.
Further studies targeted:
– Soil toposequence in arid climate (Verheye, 1973)
– Soil formation on basalt (Osman, 1974),
– Genesis of calcareous soils (Tarzi and Paeth, 1975),
– Phosphorus retention (Ryan and Ayubi, 1981),
– Mineralogy of Lebanese soils (Darwish et al., 1979; Sayegh et al.,
1990)
– Mountain soil formation and genesis (Darwish et al., 1978; Darwish
More recent soil studies addressed:
– Soil salinity on the southern coastal strip (Solh, 1987),
– Causes and impact of soil salinity on the Lebanese coast (Atallah
et al., 2000; Atallah et al., 2009),
– Soil vulnerability to erosion with GIS models (Bou Kheir et al.,
2001),
– Descriptive soil erosion within two Lebanese watersheds (CoLD,
2005),
– Land degradation (Zurayk et al., 2001; Darwish et al., 2004; Youssef
et al., 2009; Darwish and Faour, 2008),
– Soil vulnerability to desertification for NAP to combat
desertification in Lebanon (Darwish, 2003),
– Nitrate and heavy metal pollution risk and status (Moeller et al.,
2003; Nsouli et al., 2004; Darwish et al., 2008; Francis et al., 2011),
– Pesticide adsorption and degradation on soil particles (Thomas et
al., 2005),
– Soil resilience and the adaptation of agricultural sector to climate
change (Hamze et al., 2010),
Soil information updated with :
- Digital soil map of Lebanon at 1:200.000 scale (Darwish et al.,
2002)
- Creation of the new soil map of Lebanon at 1:50.000 scale
(Darwish, 1999; Darwish et al., 2006)
FAO-UNESCO, WRB legends and USDA soil taxonomy
BAALBACK
JEZZINE
Monitoring the status of land
degradation in Lebanon
Several natural and human-induced factors contributed
to land degradation in the country:
• Natural
– Rugged topography with 64% of territory having complex
landform with sloping and steep slopes,
– Old deforestation,
– Poor drainage,
– Weak lithology,
– Torrential rainfall.
– All these factor cause:
• Flash floods
• Erosion
• Mass movements and landslides
• Human induced
– Forest fires
– Chaotic urban sprawl amplify the negative
impact of deforestation.
– Inappropriate irrigation practices and fertilizer
application secondary soil salinization.
– Improper practices also lead to deterioration of
groundwater quality and soil contamination
hazards.
Urban encroachment on arable lands
1. At the national level
Urban expansion over different lands in Lebanon
Landform
Urban area by
category,
ha
% of area
Level land 40.992.12 17.91
Rolling 23.991.3 13.3
Slopping 33.820.12 12.01
Steep 29.204.62 12.31
Very steep 6.050.17 11.61
Karst 756.86 2.073
Urban sprawl into different lands
in Lebanon (Landsat 2005)
Soil aptitude to agriculture
Class Productivity Km2 %
I High 313.36 03.09
II medium 1346.61 13.27
III low 2958.24 29.14
IV Very low 3882.13 38.24
V Non arable 1650.53 16.26
Land capability classification for Lebanon
Recent urban sprawl 2000-2010
A total loss of 30800 ha of productive lands
Land cover/use of Tripoli area in 1964 Urban sprawl on productive lands in 2000
2. At the regional level
Classes
Surface
1964
(ha)
Surface
2000
(ha)
Change
(ha)
%
Horticulture 928 581 -341 -36.7
Olives 3055 2121 -934 -30.6
Forests 32 137 +105 +328.1
Shrubs 133 246 +113 +84.9
Grassland 333 318 -15 -4.5
Non productive lands 769 92 -677 -88.0
Urban area 722 2223 +1501 +207.9
Total area 6053 6053 - -
Impact of quarrying practices on land resources
• Multi temporal analyses of landsat
images and Ikonos between 1996 and
2005 revealed:
– Nbr quarries increased from 711 to
1278
– Quarried area increased from 2875 to
5283 ha.
• Modeling the risk of abandoned
quarries on land resources in Lebanon
using parameters like:
– Slope,
– Climate,
– Previous vegetation cover,
– landuse,
– Soil and rock types
– Groundwater
• 65.9% moderate impact
• 8.2% high impact
Soil erosion
Potential soil erosion as a
function of soil
characteristics:
- Soil depth,
- Soil structure,
- Soil texture,
- Organic matter content,
- Structural stability,
In relation to:
- Geomorphology
- Climatic conditions
Soil salinity
Level of
salinity
dS/m
Non saline
<2
Very slightly
saline
2-4
Slightly
saline
4-8
Saline
8-16
Number of
samples
Year of
observation
1997 2000 1997 2000 1997 2000 1997 2000
75
Proportion % 35.3 15.9 23.5 30.1 31.4 39.3 9.8 14.7
Evolution of soil salinity in a semi arid Lebanese region between
1997 (El Khatib et al., 1998) and 2000 (Darwish et al., 2005)
Soil pollution
450-500
400-450
350-400
300-350
250-300
200-250
150-200
100-150
50-100
0-50
0 50 100 150 200 250 300
Depth[cm]
ExtractableNitrate[mg/kgsoil]
grain-potatorotation
apricottreeplantation
vegetablecultivation
200
180
160
140
120
100
80
60
40
20
0
0 50 100 150 200 250 300 350
Depth[cm]
Nitrate [mg kg-1
]
December 2001
March 2002
September 2002
December 2002
February 2003
Accumulation of soil nitrate in different land use in fall and leaching by spring
200
150
100
50
0
0 50 100 150 200 250 300 350 400
Depth[cm]
Nitrate [mg kg-1
]
December 2001
March 2002
August 2002
November 2002
Depth distribution of soil nitrate (Nmin) as a
function of different land use
Nitrates in the soil and soil solution
Heavy metals in the soil-Nickel Central Bekaa.
Soil Protection effectiveness
Nitrate contamination of groundwater
y = 0.6117 x
R2
= 0.7591
0.00
0.20
0.40
0.60
0.80
1.00
1.20
1.40
1.60
1.80
0.00 0.50 1.00 1.50 2.00 2.50
Log Cle
LogECe
Intensive agricultural
practices on the coastal
area
• In greenhouses on the
coastal area, a steady
increase in the ECe from
0.4 dS.m-1 to 15 dS.m-1 was
observed (Solh et al., 1987)
and explained by poor soil
leveling.
• However, soil salinity rise
up to tenfold inside the
greenhouse compared to
outside soil.
• This was associated with
excess input of fertilizers
(Atallah et al., 2000) and
use of saline water in
irrigation and Chlorine
accumulation in the soil
(Atallah et al., 2009).
Frequency of distribution of soil salinity inside compared to initial soil salinity
outside the greenhouse on the coastal area
(Source: Atallah et al., 2000)
Soil information and national soil monitoring capacities
Cover Scale Theme Date
Type of spatial
object
Author Provider
Format
GIS1,
Paper2
Soil 1:200.000
Reconnaissance soil
map of Lebanon
1956
Polygons and
report
Bernard Geze MoA 1, 2
Soil
1:20.000 and
1:50.000
Soil suitability for
irrigation. In
scattered areas
1969
Polygons and
report
UNDP, FAO
LARI
2
Soil 1:200. 000 Soil Mineralogy
Late 70’s
published in
1990
Polygons and
report
A. Sayegh et
al.
CNRS 2
Soil 1:50.000 Soil Families of 1973
Polygons
and report
W. Verheye CNRS 2
Soil 1:50.000 Detailed soil map 2006
Polygons
Database
T. Darwish
et al.
CNRS 1, 2
Soil 1:200.000 Soil erosion 2002
Polygons
Database
T. Darwish
et al.
CNRS 1, 2
Soil 1:200.000
Soil desertification
index
2002
Polygons
Database
T. Darwish
et al.
CNRS 1, 2
Soil
Pollution
1:50.000
Heavy metal
pollution, in
Central BeKaa
1999 and
2004
Polygons
Database
T. Darwish
et al.
CNRS 1, 2
AvailablesoilinformationontheLebanese
Republic
• Conservation of diverse
Mediterranean soil of
Lebanon from:
– Sealing
– Salinity
– Contamination
– Erosion
– Quarrying
• Bioremediation to remove
salts from the soil using a
sequence of tolerant crops (El
Moujabber et al., 2006).
• A clear national policy aiming
at the conservation of
Lebanese productive lands
and the promotion of rural
development and agricultural
activities.
• Promote research to estimate
future farmland requirements
in densely populated coastal
areas.
Challenges and capacity building
Challenges and capacity building (Cont.)
• Reconsider current policy
and legislation licensing the
new quarries in Lebanon.
• The need to accomplish the
descriptive erosion mapping
at remaining watersheds to
elaborate a draft
management plan and sets
a series of indicators.
• Elaborate curative and
protective measures to
monitor the progress made
by the stakeholders at
national (government) and
local (municipalities, NGOs)
levels.
• Disseminate good
agricultural practices and
awareness is a national
priority to protect soil and
groundwater from salinity.
• Accomplish the heavy metal
content in Lebanese soils.
• Assess soil quality
nationwide to control crop
cultivation on suitable land
quality.
• Elaborate and implement
landuse planning to
protect arable lands.
• Need to establish collective
irrigation schemes notably on
the coastal area
• Disseminate the research
results and promote know how
transfer to farmers to
overcome the weakness of
participatory management of
land degradation in the
country.
• Increase the number of
associated research units
supported by CNRS to
eradicate the waste of
resources and efforts caused
Conclusion
• Absence of clear policies
and regulations to protect soil
resources.
• Chaotic urban expansion
results in soil irreversible loss.
• Observed mismanagement of
fertilizer and water inputs leads
to soil salinity and
contamination.
• No policies based on land
capability and suitability
• Lack of incentives to
agricultural land use systems
• Absence of control of the
quality of imported fertilizers
(heavy metal content).
Status of Soil Resources in Lebanon By Roger Francis
Status of Soil Resources in Lebanon By Roger Francis
Status of Soil Resources in Lebanon By Roger Francis
Status of Soil Resources in Lebanon By Roger Francis
Status of Soil Resources in Lebanon By Roger Francis
Status of Soil Resources in Lebanon By Roger Francis

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Status of Soil Resources in Lebanon By Roger Francis

  • 1. Status of Soil Resources in Lebanon By Roger FRANCIS CNRS-National Center for Remote Sensing Jordan – Amman 1-5 April 2012
  • 2. Status of environment and coastal ecosystem State of the art on soil studies in LebanonEarly soil studies in Lebanon addressed: – Soil mapping with the reconnaissance soil map of Lebanon at 1:200.000 scale (Geze, 1956), – Pedogenesis of red soils on hard limestone (Lamouroux, 1968), – Soil irrigability and fertility (FAO, 1969) using the old French soil classification. Further studies targeted: – Soil toposequence in arid climate (Verheye, 1973) – Soil formation on basalt (Osman, 1974), – Genesis of calcareous soils (Tarzi and Paeth, 1975), – Phosphorus retention (Ryan and Ayubi, 1981), – Mineralogy of Lebanese soils (Darwish et al., 1979; Sayegh et al., 1990) – Mountain soil formation and genesis (Darwish et al., 1978; Darwish
  • 3. More recent soil studies addressed: – Soil salinity on the southern coastal strip (Solh, 1987), – Causes and impact of soil salinity on the Lebanese coast (Atallah et al., 2000; Atallah et al., 2009), – Soil vulnerability to erosion with GIS models (Bou Kheir et al., 2001), – Descriptive soil erosion within two Lebanese watersheds (CoLD, 2005), – Land degradation (Zurayk et al., 2001; Darwish et al., 2004; Youssef et al., 2009; Darwish and Faour, 2008), – Soil vulnerability to desertification for NAP to combat desertification in Lebanon (Darwish, 2003), – Nitrate and heavy metal pollution risk and status (Moeller et al., 2003; Nsouli et al., 2004; Darwish et al., 2008; Francis et al., 2011), – Pesticide adsorption and degradation on soil particles (Thomas et al., 2005), – Soil resilience and the adaptation of agricultural sector to climate change (Hamze et al., 2010),
  • 4. Soil information updated with : - Digital soil map of Lebanon at 1:200.000 scale (Darwish et al., 2002) - Creation of the new soil map of Lebanon at 1:50.000 scale (Darwish, 1999; Darwish et al., 2006) FAO-UNESCO, WRB legends and USDA soil taxonomy BAALBACK JEZZINE
  • 5. Monitoring the status of land degradation in Lebanon Several natural and human-induced factors contributed to land degradation in the country: • Natural – Rugged topography with 64% of territory having complex landform with sloping and steep slopes, – Old deforestation, – Poor drainage, – Weak lithology, – Torrential rainfall. – All these factor cause: • Flash floods • Erosion • Mass movements and landslides
  • 6. • Human induced – Forest fires – Chaotic urban sprawl amplify the negative impact of deforestation. – Inappropriate irrigation practices and fertilizer application secondary soil salinization. – Improper practices also lead to deterioration of groundwater quality and soil contamination hazards.
  • 7. Urban encroachment on arable lands 1. At the national level Urban expansion over different lands in Lebanon Landform Urban area by category, ha % of area Level land 40.992.12 17.91 Rolling 23.991.3 13.3 Slopping 33.820.12 12.01 Steep 29.204.62 12.31 Very steep 6.050.17 11.61 Karst 756.86 2.073 Urban sprawl into different lands in Lebanon (Landsat 2005)
  • 8. Soil aptitude to agriculture Class Productivity Km2 % I High 313.36 03.09 II medium 1346.61 13.27 III low 2958.24 29.14 IV Very low 3882.13 38.24 V Non arable 1650.53 16.26 Land capability classification for Lebanon Recent urban sprawl 2000-2010 A total loss of 30800 ha of productive lands
  • 9. Land cover/use of Tripoli area in 1964 Urban sprawl on productive lands in 2000 2. At the regional level Classes Surface 1964 (ha) Surface 2000 (ha) Change (ha) % Horticulture 928 581 -341 -36.7 Olives 3055 2121 -934 -30.6 Forests 32 137 +105 +328.1 Shrubs 133 246 +113 +84.9 Grassland 333 318 -15 -4.5 Non productive lands 769 92 -677 -88.0 Urban area 722 2223 +1501 +207.9 Total area 6053 6053 - -
  • 10. Impact of quarrying practices on land resources • Multi temporal analyses of landsat images and Ikonos between 1996 and 2005 revealed: – Nbr quarries increased from 711 to 1278 – Quarried area increased from 2875 to 5283 ha. • Modeling the risk of abandoned quarries on land resources in Lebanon using parameters like: – Slope, – Climate, – Previous vegetation cover, – landuse, – Soil and rock types – Groundwater • 65.9% moderate impact • 8.2% high impact
  • 11. Soil erosion Potential soil erosion as a function of soil characteristics: - Soil depth, - Soil structure, - Soil texture, - Organic matter content, - Structural stability, In relation to: - Geomorphology - Climatic conditions
  • 12. Soil salinity Level of salinity dS/m Non saline <2 Very slightly saline 2-4 Slightly saline 4-8 Saline 8-16 Number of samples Year of observation 1997 2000 1997 2000 1997 2000 1997 2000 75 Proportion % 35.3 15.9 23.5 30.1 31.4 39.3 9.8 14.7 Evolution of soil salinity in a semi arid Lebanese region between 1997 (El Khatib et al., 1998) and 2000 (Darwish et al., 2005)
  • 13. Soil pollution 450-500 400-450 350-400 300-350 250-300 200-250 150-200 100-150 50-100 0-50 0 50 100 150 200 250 300 Depth[cm] ExtractableNitrate[mg/kgsoil] grain-potatorotation apricottreeplantation vegetablecultivation 200 180 160 140 120 100 80 60 40 20 0 0 50 100 150 200 250 300 350 Depth[cm] Nitrate [mg kg-1 ] December 2001 March 2002 September 2002 December 2002 February 2003 Accumulation of soil nitrate in different land use in fall and leaching by spring 200 150 100 50 0 0 50 100 150 200 250 300 350 400 Depth[cm] Nitrate [mg kg-1 ] December 2001 March 2002 August 2002 November 2002 Depth distribution of soil nitrate (Nmin) as a function of different land use Nitrates in the soil and soil solution
  • 14. Heavy metals in the soil-Nickel Central Bekaa. Soil Protection effectiveness Nitrate contamination of groundwater
  • 15. y = 0.6117 x R2 = 0.7591 0.00 0.20 0.40 0.60 0.80 1.00 1.20 1.40 1.60 1.80 0.00 0.50 1.00 1.50 2.00 2.50 Log Cle LogECe Intensive agricultural practices on the coastal area • In greenhouses on the coastal area, a steady increase in the ECe from 0.4 dS.m-1 to 15 dS.m-1 was observed (Solh et al., 1987) and explained by poor soil leveling. • However, soil salinity rise up to tenfold inside the greenhouse compared to outside soil. • This was associated with excess input of fertilizers (Atallah et al., 2000) and use of saline water in irrigation and Chlorine accumulation in the soil (Atallah et al., 2009). Frequency of distribution of soil salinity inside compared to initial soil salinity outside the greenhouse on the coastal area (Source: Atallah et al., 2000)
  • 16. Soil information and national soil monitoring capacities Cover Scale Theme Date Type of spatial object Author Provider Format GIS1, Paper2 Soil 1:200.000 Reconnaissance soil map of Lebanon 1956 Polygons and report Bernard Geze MoA 1, 2 Soil 1:20.000 and 1:50.000 Soil suitability for irrigation. In scattered areas 1969 Polygons and report UNDP, FAO LARI 2 Soil 1:200. 000 Soil Mineralogy Late 70’s published in 1990 Polygons and report A. Sayegh et al. CNRS 2 Soil 1:50.000 Soil Families of 1973 Polygons and report W. Verheye CNRS 2 Soil 1:50.000 Detailed soil map 2006 Polygons Database T. Darwish et al. CNRS 1, 2 Soil 1:200.000 Soil erosion 2002 Polygons Database T. Darwish et al. CNRS 1, 2 Soil 1:200.000 Soil desertification index 2002 Polygons Database T. Darwish et al. CNRS 1, 2 Soil Pollution 1:50.000 Heavy metal pollution, in Central BeKaa 1999 and 2004 Polygons Database T. Darwish et al. CNRS 1, 2 AvailablesoilinformationontheLebanese Republic
  • 17. • Conservation of diverse Mediterranean soil of Lebanon from: – Sealing – Salinity – Contamination – Erosion – Quarrying • Bioremediation to remove salts from the soil using a sequence of tolerant crops (El Moujabber et al., 2006). • A clear national policy aiming at the conservation of Lebanese productive lands and the promotion of rural development and agricultural activities. • Promote research to estimate future farmland requirements in densely populated coastal areas. Challenges and capacity building
  • 18. Challenges and capacity building (Cont.) • Reconsider current policy and legislation licensing the new quarries in Lebanon. • The need to accomplish the descriptive erosion mapping at remaining watersheds to elaborate a draft management plan and sets a series of indicators. • Elaborate curative and protective measures to monitor the progress made by the stakeholders at national (government) and local (municipalities, NGOs) levels. • Disseminate good agricultural practices and awareness is a national priority to protect soil and groundwater from salinity. • Accomplish the heavy metal content in Lebanese soils. • Assess soil quality nationwide to control crop cultivation on suitable land quality. • Elaborate and implement landuse planning to protect arable lands.
  • 19. • Need to establish collective irrigation schemes notably on the coastal area • Disseminate the research results and promote know how transfer to farmers to overcome the weakness of participatory management of land degradation in the country. • Increase the number of associated research units supported by CNRS to eradicate the waste of resources and efforts caused Conclusion • Absence of clear policies and regulations to protect soil resources. • Chaotic urban expansion results in soil irreversible loss. • Observed mismanagement of fertilizer and water inputs leads to soil salinity and contamination. • No policies based on land capability and suitability • Lack of incentives to agricultural land use systems • Absence of control of the quality of imported fertilizers (heavy metal content).