Mid Term 2 Flashcards

(44 cards)

1
Q

Soil water functions

A

Essential for photosynthesis
Turgor pressure
Transports nutrients
Helps plant for temperature variations

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

What is hydrogen bonding

A

Weak interactions between the partial positive charge of hydrogen and with the partial negative charge of oxygen

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

What is cohesion

A

Sticking of water molecules to each other from hydrogen bonding. Responsible for surface tension

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

What is adhesion

A

Sticking of water molecules to other molecules

Enables water to “climb” up soil pores - capillary action

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

Forms of water in soil and what they are

A

Hygroscopic Water - films around clay particles, only form of water found in air dried condition

Capillary water - held on capillary pores (<1mm thick), main form of available water

Free water - drainage or free draining water found in the bigger pores and moves downward by gravity

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

Definition of field capacity

A

All macro pores have drained, only micro pores are filled. Plants can access this water

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

Definition of permanent wilting point

A

Any water still in soil is not available, plant wilts and dies

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

Infiltration definition

A

A measure of the rate at which rain fall or irrigation is absorbed into the soil (in/hr, mm/hr)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

What are water movements through soil (4)

A

Gravitational flow

Matric flow

Capillary rise

Osmotic potential

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

What is gravitational flow

A

Movement of water through saturated soil

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

What Is matric flow

A

Movement of water through unsaturated soil ( wet to dry)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

What is capillary rise

A

Water is pulled upward from water table in micropores by cohesive/adhesive forces

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

What is Osmotic potential

A

Determined by concentration of solutes in soil water (water flows from zones of low solutes to zones of high solutes) important for root-water interaction

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

Why is water movement important

A

Soil with rapid internal drainage have higher risk of leaching
Helps determine best drainage plan
Understanding how salinity works

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

Chemical properties of soil (5)

A
Anion-Cation exchange capacity 
Reaction (pH)
Calcium carbonate content
Salinity and solicits
Soil organic matter
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

Cation exchange capacity

A

The total number of exchangeable cations a soil can hold

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
17
Q

Anion exchange capacity

A

Relative amount of negatively charged anions which can be held by a given weight of soil

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
18
Q

What is soil pH

A

Soil pH is a measure of acidity or alkalinity of soil
Seldom go beyond 4-9
Soils become acidic as rainfall leaches away basic cations such as (Ca, Mg, K, Na) while Al and H stay behind making the soil acidic
More rain = more acidic

19
Q

Other factors that affect soil pH

A
Type of vegetation 
Type of parent material
Amount +type of OM
Amendments
Salinity and sodicity
20
Q

Why are saline and sodic soils alkaline

A

Not a lot of water movement through soil that causes leaching so basic cations stay in soil making it basic

21
Q

Why do we use lime

A
Reduces Al and other metal toxicities
Improves physical condition of soil
Stimulates microbial activity
Increases CEC in variable charge soils
Increases availability of several nutrients
Supplies Ca and Mg to plants
Improves symbiotic N fixation in legumes
Improve crop yields
22
Q

How does salinity happen

A

Occurs when groundwater containing salt is able to reach the root zone or soil surface where it evaporates and leaves an accumulation of salt

23
Q

Conditions required to create a soil salinity problem

A
  1. Soluble salts in subsoil, ground water or both
  2. High water tables to carry soluble salts into root zone by capillary action (<6 ft from surface)
  3. Plants susceptible to soil salinity (pulses, vegetables, oilseeds)
24
Q

Salinization is a natural process controlled by

A

Hydrology
Geology
Biological processes

25
What is regional or artesian discharge salinity
Occurs when water within an underlying aquifer is under sufficient pressure to reach land surface. Then water evaporates at surface and salts are left behind
26
What is side hill seep salinity
Occurs where permeable glacial drift overlies impermeable materials such as clay or bedrock Lateral movements eventually intersects a side hill surface Groundwater discharges at this point and evaporation of water leave behind salt at surface
27
What is bathtub or evaporitic ring salinity
Occurs adjacent to wet depressions or sloughs Lateral upward capillary flow from the water table concentrates salts adjacent to the slough, leaving salt in a concentric ring surrounding the slough
28
How do we test for salinity
Electrical conductivity-a measure of soluble salts within the soil 2 methods used to measure EC 1. Saturated paste method 2. Soil:Water ratio method
29
Managing primary salinity
Strategic cropping choices to manage water Reduce tillage Increase soil OM
30
Managing secondary salinity
Strategic cropping choices to manage water Drainage strategies to manage water and leach salts out of soil profile
31
Sodic soils
Characterized by: elevated sodium concentration relative to calcium and magnesium pH usually above 8.5 May be able to manage with gypsum addition
32
Components of soil
45% mineral 25% water 25% air 5% OM
33
Components of OM
33-50% decomposing OM 33-50% stabilized OM <10% fresh residue <5% living organisms
34
What is OM
Generally considered to be plant residue in various stages of decomposition in the soil and... Microflora-bacteria, fungi Microfauna-Protozoa and nematodes Macrofauna-earthworms and millipedes
35
What is decomposed residue called in OM
Humus | Responsible for dark colour in Ah horizon
36
How is humus determined
By measuring the amount of organic carbon in the soil
37
What happens when the C:N ratio is high
Immobilization of soil nitrogen
38
What happens when the C:N ratio is low
New mineralization of nitrogen
39
What is C:N ratio
``` Carbon to nitrogen C:N of plant residue depends on crop type 100:1 wide ratio 15:1 narrow ratio >25:1 net mobilization <25:1 net mineralization ```
40
``` C:N ratio numbers Cereal crop Legume residue Soil humus Microbes ```
Cereal 80:1 Legume 25:1 Soil humus 10:1 Microbes 6:1
41
Starting soil conditions
Modest levels of nitrate Low c/n ratio Low microbial activity
42
What happens when you return heavy amounts of cereal crop residue
Can cause a temporary shortage of mineral nitrogen for crops (why we burn residue in fields)
43
Removal of crop residue why
Common on heavy clay soils where cool wet conditions slow decomposition Removal means loss of vital nutrients such as nitrogen and phosphorus will be lost
44
Factors affecting soil OM levels (7)
1. Natural vegetation 2. Temperature 3. Soil moisture 4. Soil texture 5. Aeration 6. Cropping and cultivation 7. Landscape position