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Introductory presentation of the drainage basin systems in the first chapter of Hydrology and Fluvial Geomorphology, suitable for AS students, consisting in the following: the global hydrological cycle, store, flows, the drainage systems, precipitation, evapotranspiration, interception, infiltration, percolation, drainage patterns, the water balance.
Fluvial Morphology handbook for students.
Contents are: definition, scope, importance of Fluvial Morphology, sediment load, channel pattern and process, role sediment to build delta, Reynolds number, Froude Number, channel pattern of Tista and Jamuna River, causes and consequences of flood, benefit of flood, flood and floodplain, hydraulic geometry, water resource management (in Bangladesh), hydrograph, origin and development of river, tributary and distributary and many more.
CAMBRIDGE GEOGRAPHY AS - HYDROLOGY AND FLUVIAL GEOMORPHOLOGY; 1.1. DRAINAGE B...George Dumitrache
Introductory presentation of the drainage basin systems in the first chapter of Hydrology and Fluvial Geomorphology, suitable for AS students, consisting in the following: the global hydrological cycle, store, flows, the drainage systems, precipitation, evapotranspiration, interception, infiltration, percolation, drainage patterns, the water balance.
Fluvial Morphology handbook for students.
Contents are: definition, scope, importance of Fluvial Morphology, sediment load, channel pattern and process, role sediment to build delta, Reynolds number, Froude Number, channel pattern of Tista and Jamuna River, causes and consequences of flood, benefit of flood, flood and floodplain, hydraulic geometry, water resource management (in Bangladesh), hydrograph, origin and development of river, tributary and distributary and many more.
This presentation was given as part of the EPA-funded Catchment Science and Management Course focusing on Integrated Catchment Management, held in June 2015. This course was delivered by RPS Consultants. If you have any queries or comments, or wish to use the material in this presentation, please contact catchments@epa.ie
It is increasingly being recognised internationally that integrated catchment management (ICM) is a useful organising framework for tackling the ongoing challenge of balancing sustainable use and development of our natural resource, against achieving environmental goals. The basic principles of ICM (Williams, 2012) are to:
• Take a holistic and integrated approach to the management of land, biodiversity, water and community resources at the water catchment scale;
• Involve communities in planning and managing their landscapes; and
• Find a balance between resource use and resource conservation
ICM is now well established in Australia, New Zealand, and the United States. In Europe the ICM approach has been proposed as being required to achieve effective water and catchment management, and is the approach being promoted by DEFRA for the UK, where it is called the “Catchment Based Approach” (CaBA). The principles and methodologies behind ICM sit well within the context of the Water Framework Directive with its aims and objectives for good water quality, sustainable development and public participation in water resource management. In Ireland it is proposed that the ICM approach will underlie the work and philosophy in developing and implementing future River Basin Management Plans.
A prudent distribution, pricing and revenue strategy is the need of the hour! Get quick tips on your hotel channel management and distribution strategy from our experts
CAMBRIDGE AS GEOGRAPHY REVISION: HYDROLOGY AND FLUVIAL GEOMORPHOLOGY - 1.2 RA...George Dumitrache
A presentation of the second subchapter (Rainfall Discharge Relationships) from the first chapter (Fluvial Geomorphology) of Revision for Geography AS Cambridge exams.
CAMBRIDGE GEOGRAPHY AS - HYDROLOGY AND FLUVIAL GEOMORPHOLOGY: 1.3 RIVER CHANN...George Dumitrache
Subchapter 3 in the first chapter of Hydrology and Fluvial Geomorphology, suitable for AS students, consisting in the following: river processes, velocity, flows and Hjulstrom Curve.
A general basic case study on the river Ganga at Varanasi covering all the aspects of Pollution, Government'r role, Treatment facilities, Future prospects, Health status of river.
CAMBRIDGE AS GEOGRAPHY REVISION: HYDROLOGY AND FLUVIAL GEOMORPHOLOGY - 1.4 HU...George Dumitrache
A presentation of the fourth subchapter (The Human Impact) from the first chapter (Hydrology and Fluvial Geomorphology) of Revision for Geography AS Cambridge exam.
Unit 8 - Information and Communication Technology (Paper I).pdfThiyagu K
This slides describes the basic concepts of ICT, basics of Email, Emerging Technology and Digital Initiatives in Education. This presentations aligns with the UGC Paper I syllabus.
Operation “Blue Star” is the only event in the history of Independent India where the state went into war with its own people. Even after about 40 years it is not clear if it was culmination of states anger over people of the region, a political game of power or start of dictatorial chapter in the democratic setup.
The people of Punjab felt alienated from main stream due to denial of their just demands during a long democratic struggle since independence. As it happen all over the word, it led to militant struggle with great loss of lives of military, police and civilian personnel. Killing of Indira Gandhi and massacre of innocent Sikhs in Delhi and other India cities was also associated with this movement.
Synthetic Fiber Construction in lab .pptxPavel ( NSTU)
Synthetic fiber production is a fascinating and complex field that blends chemistry, engineering, and environmental science. By understanding these aspects, students can gain a comprehensive view of synthetic fiber production, its impact on society and the environment, and the potential for future innovations. Synthetic fibers play a crucial role in modern society, impacting various aspects of daily life, industry, and the environment. ynthetic fibers are integral to modern life, offering a range of benefits from cost-effectiveness and versatility to innovative applications and performance characteristics. While they pose environmental challenges, ongoing research and development aim to create more sustainable and eco-friendly alternatives. Understanding the importance of synthetic fibers helps in appreciating their role in the economy, industry, and daily life, while also emphasizing the need for sustainable practices and innovation.
2024.06.01 Introducing a competency framework for languag learning materials ...Sandy Millin
http://sandymillin.wordpress.com/iateflwebinar2024
Published classroom materials form the basis of syllabuses, drive teacher professional development, and have a potentially huge influence on learners, teachers and education systems. All teachers also create their own materials, whether a few sentences on a blackboard, a highly-structured fully-realised online course, or anything in between. Despite this, the knowledge and skills needed to create effective language learning materials are rarely part of teacher training, and are mostly learnt by trial and error.
Knowledge and skills frameworks, generally called competency frameworks, for ELT teachers, trainers and managers have existed for a few years now. However, until I created one for my MA dissertation, there wasn’t one drawing together what we need to know and do to be able to effectively produce language learning materials.
This webinar will introduce you to my framework, highlighting the key competencies I identified from my research. It will also show how anybody involved in language teaching (any language, not just English!), teacher training, managing schools or developing language learning materials can benefit from using the framework.
4. River carries three types of
work:
1. Erosion
2. Transportation
3. Deposition
5. occurs when rivers
erode or wear
away the land
surface over which
they are flowing
The rock particles
which are worn
away from the land
surface are called
sediments
6. is a process where the
sediment produced by erosion
is carried away downstream
by the river
7. happens when the sediment may
settle either on the river bed
where the water flows more
slowly as in the flood plain, or
eventually on the sea bed
8. A process by which the force of the
flowing water may remove particles
from the banks or bed
9. A form of hydraulic action caused by
bubbles of air collapsing
The resultant shock waves hit and
slowly weaken the banks
This is the slowest and least effective
erosion in process
10.
11.
12.
13.
14.
15. A process by which as rocks are carried along by a
river, they knock against each other so pieces break
off and the rock fragments are reduced in size and
become rounded
16. A process by which the rock particles which are
then carried by the river may be used as tools to
help break more rock fragments from the river bed
and banks
Example :
Circular holes called pot holes may be cut in a
rocky river bed
17.
18.
19. A process by which rivers can dissolve some rocks such
as limestone
Example :
At Mulu in Sarawak, rivers have dissolved the limestone
and created huge caverns (large caves) through which
they flow underground
20. Rivers flow in channels and the sides of the channel are called banks,
with the floor of the channel known as the river bed
Rivers can erode river channels in four main ways such as :
HYDRAULIC ACTION
A process by which the force of
the flowing water may remove
particles from the banks or bed
CORRASION
A process by which the rock
particles which are then
carried by the river may be
used as tools to help break
more rock fragments from the
river bed and banks
ATTRITION:
A process by which as rocks
are carried along by a river,
they knock against each
other so pieces break off
and the rock fragments are
reduced in size and become
rounded
SOLUTION
A process by which rivers
can dissolve some rocks
such as limestone
C
A
S
H
21. • is a process where the sediment
produced by erosion is carried
away downstream by the river
• 3 main processes:
• Bedload
• Suspended Load
• Dissolved / Solution Load
22. Larger particles which cannot be
picked up by current may be moved
along the bed of the river in two
ways:
Traction
Saltation
23. when the large particles roll or slide along the
river bed.
large rocks are only moved after heavy rain
when the river has a large volume of water
and is fast flowing
24. when particles are temporarily lifted up
by the current and bounced along the
bed in a hopping motion
25. when small particles such as sand and clay
are carried along without touching the river
bed.
these small particles are just floating, and
lightest particles are near to the surface
of the water
26. when rainwater can slowly dissolve
limestone rock.
they cannot be seen by the naked eye
27. SUSPENSION
when small particles such as sand
and clay are carried along without
touching the river bed, small
particles are just floating, and
lightest particles are near to the
surface of the water
SOLUTION
when rainwater can
slowly dissolve
limestone rock.
SALTATION
when particles are
lifted up by the current
and bounced along the
bed in a hopping motion
TRACTION
when the largest particles
roll or slide along the river
bed, moved after heavy rain
when the river has a large
volume of water and is fast
flowing
28.
29. The speed of flow of a river is reduced the river may no
longer have enough energy to transport its load of
sediment
The larger particles will sink and settle first while the
finer particles will be carried further before settling, or
they may be carried all the way to the sea
This sinking and settling of the river’s sediment is called
river deposition
Deposition may occur on the river bed, or on the inside
curve of a river bend, or on the river banks
The sediment which is deposited in the sea at the river
mouth may build up new land known as delta
30. decrease in velocity less energy and no longer had
competence and capacity to carry all its load
Therefore, largest / heaviest particles, materials begins to
be deposited.
Occurs when:
1. Low discharge following a period of low
precipitation
2. Less velocity when river enter sea or lake.
3. Shallower water occurs on inside of a meander.
4. The load suddenly increase (debris from landslide)
5. River overflow its bank so velocity outside channel
32. Velocity: speed of a river (m/s)
Can influenced turbulence:
High Velocity:
the amt of energy still available after friction will be
greater and so turbulence increases
The faster the flow of river the larger the quantity and
size of particles (load) which can be transported
Low Velocity:
Less energy to overcome the friction
Turbulence decreases and may not be visible to human
eye
Sediment will remains undisturbed
Reduction in turbulence may lead to deposition of
sediment
33.
34.
35. Velocity of a river is influence by 3 factors:
(i) Channel shape in cross-section.
(ii) Roughness of the channel’s bed and banks.
(iii) Channel slope.
36. Simply describe by the term ‘Hydraulic radius’
i.e: Cross section area / wetted perimeter
Wetted perimeter - shape of the channel or its cross
section
affects the extent to which water is in
contact with its channel.
The greater the wetted perimeter, the greater the
friction between the water and the banks and the bed
of the channel,
and the slower the flow of river.
37.
38. River volume: 6 sq m (2mx3m)
wetted perimeter: 7 metres (2m+3m+2m).
The 7 metres will be represent the friction
slowing the river down.
39. Volume: 24 sq metres
Wetted perimeter: 14
metres.
shape of the river a major
influence.
A river with the same volume
of water as Example 2 but
with a different shape will
have a different friction
value.
Volume: 24 sq metres
Wetted perimeter is 26
metres almost double that of
Example 2 which means that
the river will be slower as a
larger part of the river energy
is used to overcome friction.
The gradient of the river
channel is only one factor to
influence the speed of the
river.
40. Example:
Stream A: larger hydraulic radius
-small amt of water in contact with the wetted perimeter
- creates less friction reduce energy loss
allows greater velocity
Stream B: smaller hydraulic radius
- large amt of water in contact with the wetted perimeter
- creates greater friction more energy loss
reduce velocity
41. Material such as rocks in the
channel can influence the
speed.
Whether rocks on the river
bed are smooth or rough or
uneven.
Rocks that protrude out from
the bank can slow the pace of
the water as friction slows it
down as it passes the
42. In figure A, the channel is
smooth while that in figure
B is rough or uneven with
boulders on the river bed
as well as rocks that
protrude out from the bank.
A river that flows through
such a river has to
overcome such obstacles
and therefore there will be
more friction and the
velocity of the river is
reduced.
Figure A
Figure B
43. Velocity of a mountain stream is less than that of
a lowland
Mountain stream is likely to pick up loose material
and carry it downstream
Example:
Mountainous / Upper course of a river:
Despite high velocity in waterfalls, the large number
of angular rocks, coarse-grained banks and
protrusions increase frictions and reduce overall
velocity
Lower course of a river:
As there is little resistance from the smooth bed and
banks, there is little friction and river flows faster
44. A river flowing down a
steep slope or gradient has
higher velocity than one
which flows down a gentler
gradient.
For example, the speed
of flow in a river that
plunges down a steep slope
in the form of a waterfall
is much higher than the
speed of flow in a river
that winds down a gentler
slope.
45. Gradient = steepness
As more tributaries and water from the
surface, throughflow join the main river
the discharge, channel cross-section and
hydraulic radius increases.
less energy will be loss through friction
erosive power will decrease
river flows over a gradually decrease gradient
46. Changes in gradient are related to changes
in discharge.
Discharge is higher in the lower course
Since gradient decreases as discharge
increases, river can transport the same
quantity and size of sediment load in the
gentler lower course as it can in the steeper
upper course.
49. - River water has a certain amount of available energy.
- greatest when there is a large amt of water and when there is steep
gradient.
- Most of the river’s energy used up in overcoming friction with the bed and
banks
- Friction high in the upper reaches of a river where large boulders
may protrude into large river’s flow
There are three patterns of flow:
1. Laminar flow
2. Turbulent flow
3. Helicoidal flow
50. Horizontal movement of water
Travel over the sediment in the river bed without
disturbing it
Rare in reality but common in the lower reaches
Condition:
Smooth
Straight channel
Shallow water
Non-uniform velocity
51. Series of erratic (inconsistent) eddies
Both vertical & horizontal in downstream
direction
Depends on the amt of energy available after
friction has been overcome
Conditions:
Complex channel shape eg. Winding channels, riffles
and pools
Cavitation as eddies trap air in pores, cracks
crevices which is then release under great pressure
52.
53.
54. Usually occur in meanders
A corkscrew movement in a meander
It is responsible for moving material
from the outside of one meander bend
and depositing on the inside of the next
bend.
58. a graph used by hydrologists to
determine whether a river will erode,
transport or deposit sediment.
The graph takes sediment size and
channel velocity into account.
The curve shows several key ideas
about the relationships between
erosion, transportation and deposition.
59. Hjulstrom Curve
shows that particles of a size around 1mm
require the least energy to erode, as they
are sands that do not coagulate.
Particles smaller than
these fine sands are
often clays require
a higher velocity to
produce the energy
required to split the
small clay particles
which have coagulated.
60. Larger particles
pebbles are eroded at
higher velocities
very large objects
boulders require the
highest velocities to
erode.
When the velocity
drops below this
velocity called the line
of critical velocity,
particles will be
deposited or
transported, instead
of being eroded,
depending on the
river's energy
61.
62.
63. Critical erosion velocity : the lowest velocity at which grains of a
certain size can be moved.
Critical deposition velocity: The velocity at which particles of
particular sizes are laid down
Entrainment: materials being picked up by river
Flocculate: materials stick together in the river
Clay particles: Tiny particles between 0.001 and 0.01mm in size
Sand particles: Sediments between 0.1 and 2mm in size
Cobbles: Sediments between 20 and 300mm in size
64. Key:
Silt / sand are picked up (entrained) at the
lowest velocities
Clays are difficult to pick up as pebbles –
although they are small particles, they are very
cohesive and the claybed is very smooth
Large boulders are dropped easily
Clay particles can be transported in suspension
at very low velocities
66. 1. Name the type of sediment that requires the lowest
velocity to be eroded. [1]
2. Name the type of sediment that is likely to be
transported at all velocities. [1]
3. Describe and explain the relationship between
water velocity and the erosion of clay
and sand particles. [4]
4. Explain the variation in water velocity that is
required to transport and to deposit
sediments of different particle diameter. [4]
67. 1. Sand
2. Clay
3. Clay – requires higher energy to be eroded
- tend to stick together
- are difficult to pick up as pebbles
– although they are small particles, they are very
cohesive
Sand – requires lower energy
- sand particles are unconsolidated (loose)
4. Boulders – require large velocities to be transported
Small particles – Clay & silt – can be held in suspension area
at low velocity
Energy velocity to transport is always lower than energy
to erode