Water Pathways Flashcards

1
Q

What do water pathways control

A

Denudation processes

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2
Q

What are the denudation processes, starting from the smallest scale

A

Solution
Erosion (particles and aggregates)
Mass movement (landslides)

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3
Q

What are the 2 stages of erosion

A

Detachment and transport

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4
Q

What are the two controls of erosion

A

Erodibility

Erosivity

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5
Q

What is erodibility

A

Properties of soil trying to keep it in one place

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6
Q

What is erosivity

A

Kinetic energy of water flow, whatever is resisting erosion

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7
Q

How to prevent erosion

A

Remediate

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8
Q

Where are the locations f erosion on slopes

A
Soil pipes 
Gully’s 
Rills 
Rain splash 
Subsurface 
Sheet flow
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9
Q

What is rainsplash erosion

A

What in rainfall hitting ground and dislodging particles and taking them with it in net transfer of material

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10
Q

If raindrop hits the ground at terminal velocity how far can the particles move

A

1m

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11
Q

How does sheetflow erode

A

Focused on a particular point giving you gully erosion

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12
Q

What are direct evidence of rainsplash erosion

A

Soil pillars - what can’t be eroded

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13
Q

What are the two ways rainsplash erosion effects the landscape

A

Detachment of particles wasn’t away from sheet flow and capping of soil which increases sheet flow

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14
Q

How does capping of soil work

A

Lots of rainfall hits the surface of silty materials and the clay particles orientate horizontal and water fant get in

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15
Q

How to protect against rainsplash erosion

A

Mulch tillage

Cover cropping

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16
Q

What is mulch tillage

A

In between crops out dead vegetable matter to protect the soil this cuts off the evaporation from the soil a little bit

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17
Q

What is cover cropping

A

Put another crop in between crops to stop erosion but don’t want this to take up too many water or nutrients

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18
Q

What is surface sheetflow erosio

A

Uniform surface but water tends to move into tiny little channels called micro-rills rather than staying as a sheet. Goes from laminar into channels and becomes turbulent

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19
Q

When does sheet flow by occur

A

Over cement or tarmac

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20
Q

What equation is used to work out sheet flow

A

Reynolds Number (turbulence at depth) is VD/U. Velocity, depth of flow and kinematic viscosity

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21
Q

What is the range of turbulence in Reynolds number

A

100-500

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22
Q

What are the ways to reduce overland flow amount and velocity

A

Increase infiltration
Reducing flow velocity
Reduce net precipitation

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23
Q

How to increase infiltration

A

Organic matter to improve soil structure - slow it down.

Plough surface induration - don’t allow compacted surface.

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24
Q

What is induration due to

A
Capping
Dessication- hydrophobicitiy 
Burning
Salt precipitates
Salt defloculates
Trampling 
Vehicle compaction
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25
What makes deserts hydrophobic
Months of drying means water won’t go in. Setting fire to them also makes it hydrophobic and destroys soil structure
26
How do salt precipitates cause induration
If you irritate some water is used by plants and some goes out of the water and it pulls salts in the profile to the surface. Sodium causes sobic souls which destroys the structure making it collapse.
27
How does salt deflocculation occur
Clay deflocuates in sobic soils
28
How to reduce flow velocity
Terracing - hold back water and slow it down. Contour bunds - lines of stones across hill slopes to slow the water down. Mulch tillage - rough vegetable matter resits and slows water.
29
How to reduce net precipitation
Afforestation - reduce rainfall that gets to ground.
30
What are the odd circumstances where sub surface erosion occurs
Sapping at seepage face | Piping
31
What is sapping at seepage edge
If water is going through ground it may come out near the river and as it comes out it accelerates and takes some particles with it
32
What is piping
Soil pipes where turbulent flows generate natural tunnels underground - can cause pipe collapse (middle) and pipe emergence (end)
33
Where is the perfect environment for pipes
Silty soils don’t have enough cohesion to maintain the integrity of a pipe whereas clays have too much resistance to form a pipe. Silt has perfect structure for them
34
How to protect against piping
Very difficult Afforestation Controlled drainage
35
How does controlled drainage protect against pipes
Try to get some water out of the soil. Put drains in terraces so the water doesn’t fall into any subsurface drainage
36
How does gully erosion form
From subsurface flows and surface flows
37
What are the kinds of gully erosions
Rill enlargement | Undercutting by scour
38
What is rill enlargement
Little channel gets deeper until it can be called a gully
39
What is undercutting by scour
Overland flow runs off top of gully and botched under the material will cause collapse. Aided by soil fall and Knickpoint lip erosion
40
How to protect against gully erosion
Stop sheet flow | Bunds e.g wire bolsters and log dams
41
How to stop sheet flow and protect gully’s
Obstructions above the gully to stop overland flow to stop enlargement
42
What is the case study for water pans
Borneo
43
What percentage of precipitation in Borneo is hortonian overland flow
1%
44
What is the topography of Borneo
V-shaped so limited saturation excess overland flow
45
Why is their enormous drainage density in Borneo
It’s a young landscape
46
What does the sharp topography in Borneo mean
There’s opportunities for water to come out of the soil before it gets to the river
47
What is the main water pathway in Borneo
Subsurface flow
48
What is the exception in Borneo of HOF
39% of rainfall over these surfaces
49
How to measure sediment load
Measure the rapidity of water to measure the concentration of sediment in water. Take a sample and figure out the mass
50
How much sediment being eroded in Borneo’s roads
600 tonnes per km squares of catchment per year. Natural slopes are only 30-40tonnes per year
51
In Borneo where is sediment production higher
On tracks | 643t/km^2/yr (some only 81). Not predictable
52
Where is most sediment in natural catchments coming from
River banks where water is interacting with sediment constantly
53
What erosion do undisturbed catchments in Borneo favour
Channel bank erosion
54
What does logging in Borneo lead to
Landslides during extreme events as logging adds instability
55
Example of landslide in Borneo
1996. 67t in 1 day
56
What is the annual rate of erosion in Borneo
1467 tonnes
57
What is the average erosion rate in the uk
50 tonnes
58
What is the most extreme erosion rate in New Zealand
10,000 tonnes
59
What did the landslide in Borneo lose in one year
49% of all sediment lost from Baru
60
What does cut and fill timber haulage roads lead to
Landslide impacts seen downstream as they are intrinsically unstable in material
61
What is an important aspect of sustainable forestry
Trying to ensure subsurface hydrology not changed by road construction
62
What did Borneo do to try and create sustainable forestry
Add drain under road which means water percolates into drainage and changes the properties of the soil to which the small rainfall events caused it all to collapse. Done bc it’s essential to how they might finesse their forestry practices so they don’t generate as much sediment