The Physical Environment (AS); Soil Flashcards

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1
Q

What is soil essential for?

A

Plant growth in natural ecosystems & agroecosystems

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2
Q

What is soil fertility?

A

The ability of soil to sustain plant growth

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3
Q

How is water content a feature of fertile soil?

A

-Water → essential for all organisms living in soil including plants
-Fertile soil allows good drainage so doesn’t become water logged but still retains enough water for soil biota survival
-Plant nutrients = absorbed in ionic form, dissolved in water

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4
Q

How are soluble materials a feature of fertile soil?

A

-Have macronutrients like nitrogen, phosphorus & potassium, present in ionic form ; mainly nitrates, phosphates & potassium ions
-Have micronutrients like boron, cobalt, copper, iron, manganese & magnesium
-Toxin ions like aluminium & heavy metals are absorbed → surface of mineral particles (usually clay); so can’t dissolve in water & harm soil organisms

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5
Q

How is air content a feature of fertile soil?

A

Most living organisms in soil & many processes increasing fertility = aerobic → well aerated soils likely to be more fertile

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6
Q

How does dead organic matter contribute to soil fertility?

A

-Usually have a high dead organic matter content → releases plant nutrients as decomposes
-Increases water retention & provides food for soil biota

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7
Q

How is pH a feature of fertile soil?

A

-Usually in range of pH 5. 5- 7.0 → range of tolerance for most plants, soil biota
-Acidic soils can ↑ leaching of plant nutrients & damage root cell membranes
-Alkaline conditions; phosphates become insoluble

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8
Q

How do soil biota contribute to the fertility of soil?

A

Living organisms = involved in many processes affecting soil fertility;
-Detritivores like beetle larvae, worms break up dead organic matter, release nutrients → soil. Also ↑ soil drainage & aeration by making tunnels in soil
-Decomposers like fungi break down dead organic matter; secrete digestive enzymes + rely on detritivores to physically break up dead organic matter, increase its surface area
-Nitrogen fixing bacteria convert gaseous nitrogen into ammonium ions
-Nitrifying bacteria oxidise ammonium ions → nitrite ions → nitrate ions
-Mycorrhizal fungi form symbiotic relationships w/ plant roots, aid phosphate uptake by plants

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9
Q

What is soil texture controlled by and what does this involve?

A

Proportions of different size categories of mineral particles present in soil;
- Clay; <0.002 mm diameter
-Silt; 0.002 - 0.02 mm diameter
-Sand; 0.02- 2.0 mm diameter

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10
Q

How do drainage rates compare in sandy and clay soils?

A

-Larger pare spaces of sandy soils allows rapid drainage → reduces water content, increases aeration
-Clay soils = poorly drained

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11
Q

How does capillary action compare in sandy and clay soils?

A

-Tiny pore spaces between clay particles allow underground water to rise towards surface
-No capillary rise of water in sandy soils

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12
Q

How does aeration compare in sandy and clay soils?

A

-Pore spaces in well-drained sandy soils; filled w/ air
-clay soils; more likely to be waterlogged w/ low aeration rate

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13
Q

How does nutrient retention compare in sandy and clay soils?

A

Nutrient ions absorb easily onto clay particles but not onto sand particles

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14
Q

How does thermal capacity differ in sandy and clay soils?

A

-High water content of clay soils; high thermal capacity, warm up & cool down slowly
-Sandy soils; low thermal capacity, warm up more rapidly after cold weather

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15
Q

How does root penetration differ in sandy and clay soils?

A

-Clay particles = held together by capillary water on particle surfaces; harder for plant roots to force way between soil particles
-Sandy soils = root penetration easier

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16
Q

How does ease of cultivation compare in sandy and clay soils?

A

Lack of adhesion between particles in sandy soils; easier to cultivate than clay soils

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17
Q

What is the composition of loam soils and why is this advantageous?

A

-Fairly even mix of sand, silt & clay (approx 40:40:20)
-Ideal mix of properties for cultivating most crops; good drainage,water retention, high nutrient content

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18
Q

What is the structure of soil and its different types?

A

-Soil particles form aggregates called peds
-Particles = bound together by polysaccharide gums made by decomposition, by fungal hyphae, by roots, by action of soil biota & hygroscopic clay particles
-Ped type affects soil properties & fertility. Crumb peds= small & round. Produce good drainage, aeration & easy root penetration → improve soil fertility. Platy peds= large & flat. Reduce drainage, aeration & root penetration → less fertile soils

19
Q

How does depth affect soil?

A

-Deeper soils—> less likely to become waterlogged/dry out rapidly
-Can also aid good root anchorage

20
Q

Humans affecting soil fertility; aeration by ploughing & drainage?

A

Ploughing + drainage makes soils more aerobic= increases rates of N fixing, nitrification & decomposition of dead organic matter

21
Q

Humans affecting soil fertility; soil nutrient levels?

A

-Farmers increase soil nutrient levels by adding inorganic fertilisers, organic matter, supporting natural processes increasing nutrient levels like bacterial nitrogen fixation
-Farming can also deplete soil nutrient levels due to soil erosion, biomass removal, inhibiting natural processes increasing nutrient levels/increasing leaching of dissolved nutrients

22
Q

Humans affecting soil fertility; irrigation?

A

-Increases fertility of soil where water= limiting factor on growth
-Sufficient water allows plants to keep stomata open, continue gaseous exchange when soil would otherwise be dry
-Water dissolves nutrients, can be absorbed by plants in ionic form

23
Q

Humans affecting soil fertility; soil compaction?

A

-Excessive use of heavy machinery/high livestock densities—> soil becomes compacted
-Aeration is reduced & waterlogging is more likely; especially when soil is wet

24
Q

Humans affecting soil fertility; pH?

A

Controlling soil pH helps ensure nutrients= soluble but not too easily leached

25
Q

How does soil erosion occur naturally and what is the rate of this?

A

-Soil particles are removed by wind/water
-Soil erosion rate is likely to equal/less than rate of soil formation

26
Q

Types of soil erosion; what is wind erosion and why is it an issue?

A

-Soil= dry, low clay content—> likely to become loose w/ little cohesion between particles holding soil together
-If it’s windy, soil is unprotected; may blow away
-Can cause issues where soil is deposited as may cover crops/land in urban areas

27
Q

Types of soil erosion; how is water erosion increased?

A

Steeper gradients

28
Q

Types of soil erosion; what is rain splash erosion and why is it an issue?

A

-A type of water erosion
-Soil particles dislodged by splash of a raindrop. Soil particles are dispersed in all directions, those going downhill= likely to travel further
-Overtime, can cause downhill movements of large soil amounts

29
Q

Types of soil erosion; what is surface runoff erosion and how is it an issue?

A

-Caused by surface runoff when infiltration capacity of soil has been exceeded
-Can occur when rainfall= heavy/prolonged, or soil is relatively impermeable so more water flows over ground surface

30
Q

Types of soil erosion; when do slumping and landslides occur and how is this an issue?

A

-When soil on slopes becomes very wet, increased mass & lubrication of water—> downward movement of large soil amounts more likely
-Often occurs when deep soil on steep slopes becomes less stable post deforestation
-As roots that held soil together decompose, soil= held together less strongly & landslides following rain are more likely

31
Q

How does vegetation reduce the rate of soil erosion?

A

-Acts as a natural windbreak, reducing wind velocity & therefore kinetic energy carrying away soil particles
-Vegetation cover & leaf litter reduce impact of raindrops on soil surface—> soil particles less likely to be dislodged
-Soil organic matter, incl colloidal material humus, helps bind soil particles together
-Plant roots hold soil together
-Plants help increase infiltration of water into soil—> reduces rate of runoff & water erosion

32
Q

Humans activities increasing rate of soil erosion; vegetation removal?

A

Removes protection from erosion

33
Q

Humans activities increasing rate of soil erosion; ploughing vulnerable soils?

A

Breaks up soil structure, exposing soil particles to erosion by water/wind

34
Q

Humans activities increasing rate of soil erosion; overgrazing?

A

-If livestock density= too high, vegetation will be eaten faster than it can grow, increasing exposure of soil & risk of erosion
-Disturbance & root damage by hooves increases erosion risk

35
Q

Humans activities increasing rate of soil erosion; reduced soil biota?

A

-Ploughing, reducing soil organic matter & use of agrochemicals can reduce # of living organisms in soil, which play an important part in reducing soil erosion;
-Detritivores & decomposers break down dead organic matter, releasing plant nutrients—> may increase vegetation cover
-Decomposition produces humus—> increases adhesion between soil particles
-Worms aerate soil, increasing drainage rate, infiltration capacity of soil

36
Q

Humans activities increasing rate of soil erosion; soil compaction?

A

-Use of heavy machinery, high livestock densities, reduction in soil detritivores= more likely soil will be compacted
-This has smaller interstitial spaces, reduces infiltration rate so more likely rainfall will produce surface runoff & erosion

37
Q

Humans activities increasing rate of soil erosion; cultivating steep slopes?

A

-Surface runoff water flows more rapidly down steeper slopes, has more kinetic energy to pick up and carry soil particles
-Cultivating w/ techniques disturbing soil (eg ploughing) adds to erosion risk

38
Q

Effects of accelerated soil erosion; reduced productivity?

A

-Soil eroded → often most fertile topsoil lost
-Remaining soil may=less fertile → reduced plant growth + smaller harvests
-Erosions → leave shallower soil, root penetration may = more difficult

39
Q

Effects of accelerated soil erosion; sedimentation in rivers & reservoirs?

A

-Soil particles carried → river may be deposited if water slows down, has less kinetic energy
-Can occur where river naturally slows down in reservoirs/on coastlines if suspended soils reach sea
-Soil that sediments in a river ↓ flow capacity, so river = more likely to overflow & cause flooding post heavy rain

40
Q

Effects of accelerated soil erosion; Increased atmospheric particulates?

A

-Wind erosion ↑ level of atmospheric particulates
-Can make health problems like asthma worse

41
Q

Effects of accelerated soil erosion; Desertification?

A

-Soil erosion → important part of combination of processes causing expansion of deserts
-Makes it mare difficult for vegetation to grow, contributes to further soil erosion, reduced rainfall

42
Q

How do long-term crops reduce soil erosion?

A

-Growth of crops not requiring frequent replanting & soil disturbance =↓ erosion rate
-Eg permanent grassland & tree crops like fruit, tea, coffee

43
Q

TBC page 165 / 169

A