Soils Flashcards

1
Q

Why is soil important?

A

agriculture
supports biodiversity
habitat for some organisms
site of chemical reaction
supports plants for climate regulation

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2
Q

What does soil fertility mean?

A

the ability of soil to sustain plant growth

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3
Q

Components of soil: minerals - sand

A

mixture of small pieces of different rocks or minerals

particles = round

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4
Q

Components of soil: minerals - silt

A

fine sand/clay carried by running water and deposited as a sediment

larger than clay, smaller than sand

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5
Q

Components of soil: minerals - clay

A

grained earth

flat and platey

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6
Q

Components of soil: DOM

A

decomposition - cycling of nutrients

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7
Q

Components of soil: soil biota

A

micro-organisms, spiders, insects, earthworms

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8
Q

Components of soil: missing two

A

water and air

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9
Q

Features of soil which affect soil fertility and productivity: water content

A

essential for all organisms
good soils allow good drainage, but retain enough for soil biota
dissolves nutrients

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10
Q

Features of soil which affect soil fertility and productivity: soluble materials (micro/macro nutrients and metal ions)

A

macro - phosphorus, nitrogen, potassium
micro - boron, cobalt, copper, iron, manganese, magnesium

shortage of nutrients limits plant growth

harmful metals adsorb onto surface of clay particles

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11
Q

Features of soil which affect soil fertility and productivity: air content

A

most processes = aerobic
well aerated = more fertile
aerobic = faster decomposition

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12
Q

Features of soil which affect soil fertility and productivity: DOM

A

more DOM = fertile soils
binds soils
increases nutrients, water retention and food for soil biota

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13
Q

Features of soil which affect soil fertility and productivity: pH

A

fertile soils = 5.5-7
acidic soils = increased leaching and damage to root cell membranes
alkaline soils = phosphates are insoluble

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14
Q

Features of soil which affect soil fertility and productivity: soil biota

A

detritivores break down DOM and release nutrients
decomposers break down DOM and secrete digestive enzymes
nitrogen fixing bacteria
nitrifying bacteria
mycorrhizal fungi

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15
Q

Features of soil which affect soil fertility and productivity: soil texture

A

controlled by different mineral particles
clay = small
silt = medium
sand = small

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16
Q

Features of soil which affect soil fertility and productivity: soil structure

A

soil particles from aggregates (peds)

crumb peds = small and round = good drainage/aeration/root penetration

platy peds = large and flat = decreases drainage/aeration/root penetration

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17
Q

Features of soil which affect soil fertility and productivity: soil depth

A

deeper soil s= dry out rapidly

root anchorage

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18
Q

How particle size affects soil properties: drainage

A

large and spherical = better drainage

quicker in sand than clay soils

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19
Q

How particle size affects soil properties: water content and capillary action

A

more water drawn up in clay soils as water content is higher

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20
Q

How particle size affects soil properties: aeration

A

higher in sandy soils as more porous

21
Q

How particle size affects soil properties: nutrient levels

A

higher in clay as more water available so more nutrients dissolved

some able to adsorb to clay particles

22
Q

How particle size affects soil properties: thermal capacity

A

higher water content = higher thermal capacity

23
Q

How particle size affects soil properties: root penetration

A

higher in sandy soils

24
Q

How particle size affects soil properties: ease of cultivation

A

higher in sandy soils

25
Soil Analysis: soil texture - sedimentation method
handful of soil in tray rub sample through fingers to separate remove obvious pieces of organic particles and any large chunks half fill cylinder with soil fill rest of cylinder with water invert repeatedly to mix and suspend leave for at least a week use graduations to determine % of sand, silt, clay use soil triangle to determine soil type
26
Soil Analysis: soil texture - soil sieve method
stack of sieves = different sizes 1st = stones, sticks, gravel 2nd = sand 3rd = silt 4th = clay collect total mass of each to work out percentage only works if soil is dry and separated
27
Soil Analysis: water content
weigh crucible add soil and reweight place in oven at 100 degrees for 24hrs weigh crucible and dry soil determine mass of water lost work out % mass of water in original sample
28
how do you know if all the water has evaporated?
heat until constant mass
29
Soil Analysis: soil air
add 250ml of soil to 500ml beaker add 250ml of water and stir record new vol work out % air = loss of expected volume/ original vol of soil
30
Soil Analysis: organic matter
weigh empty crucible add dry soil and reweigh determine mass of soil place in oven at 450 degrees and leave overnight weight soil and crucible again determine loss of mass work out %
31
When determining organic matter content, why should the oven temp be kept below 550 degrees?
to not break down sand, silt, clay difficult to distinguish between mass lost due to DOM and mass lost due to minerals
32
Soil Analysis: soil pH - universal indicator
add 2.5cm3 of soil to test tube add 1cm3 of BaSO4 (speeds up settling) add 3.5cm3 distilled water add 10 drops universal indicator bung test tube and shake leave for 15 minutes use colour card to determine pH
33
Soil Analysis: soil pH - universal indicator paper
same test tube set up as universal indicator dip paper into settled solution
34
Soil Analysis: soil pH - pH probe
calibrate using buffer solution take readings at equal depths
35
Soil Analysis: soil organisms - random sampling
suitable for large areas uses a quadrat - place using randomly selected co-ordinates
36
Soil Analysis: soil organisms - soil flooding (using irritant)
suitable for extracting worms flood area of soil in a quadrat, often using irritant (e.g. mustard powder) worms come to surface and are counted
37
Limitations of soil flooding
worms may die worms may move sideways irritant may not percolate deep enough
38
Soil Analysis: soil organisms - soil pit extraction
dig out area of quadrat to an agreed depth hand sort worms out of soil
39
Limitations of soil pit extraction
worms may move sideways small worms may be missed
40
Human activities affecting soil fertility: aeration by ploughing and drainage
makes soils more aerobic increases rate of nitrogen fixation, nitrification and decomposition of DOM
41
Human activities affecting soil fertility: increasing and decreasing soil nutrient levels
increasing = inorganic fertilisers, organic matter, support natural processes (e.g. nitrogen fixation) decreasing = erosion, biomass removal, increased leaching
42
Human activities affecting soil fertility: irrigation
increases soil fertility where water is the limiting factor - allows plants to keep stomata open dissolves nutrients that can be absorbed as ions
43
Human activities affecting soil fertility: soil compaction
caused by excessive use of heavy machinery reduces aeration and increases chance of waterlogging
44
Human activities affecting soil fertility: controlling pH
ensures nutrients are soluble but not too easily leached crushed limestone increases pH digging in sulphur decreases pH
45
Types of soil erosion: wind
picks up soil particles and moves them most likely to happen to dry/sandy soils
46
Types of soil erosion: water
rain splash erosion surface runoff erosion slumping and landslides
47
Ways in which vegetation reduces soil erosion
root binding
48