module 1 - the physical soil Flashcards

1
Q

what do plants require from soils (4 things)

A

support
oxygen
water
nutrients

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2
Q

What is soil fertility?

A

considers the physical (composition), chemical (processes and CEC) and biological (microbes) fertility

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3
Q

inorganic material in soil is

A

gravel
sand
silt
clay

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4
Q

organic material in soil

A
bacteria
fungi
roots
animals
humus
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5
Q

what is soil texture describing

A

prominent particle size only refers to particles less than 2 mm in diamtre

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6
Q

size and texture of clay

A

< 0.002 mm feels plastic and sticky when wet

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7
Q

size and texture of silt

A

> 0.002 - 0.06mm feels smooth or silky

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8
Q

size and texture of sand

A

> 0.06 to 2 mm feels gritty

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9
Q

what ways does soil texture influence soils behaviour (3 ‘s )

A
  • surface area = increased = more reactive (more likely to bond with other particles and retain water)
  • surface charge (clays) - can attract cations and some anions
  • shape of particles- affects cohesion through contact surfaces and SA and pore size
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10
Q

how does texture affect water movement

A

quicker through coarse soils as pores are larger

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11
Q

how does texture effect areation

A

fine textured soils are poorly drained and thus have poor aeration due to the lack of macropores

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12
Q

how does texture effect water retention

A

better in fine textured soils sandy ones at risk of drought due to large presence of macropores

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13
Q

how does texture effect ease of tillage

A

clay is often difficult to cultivate

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14
Q

how does texture impact compaction

A

fine and intermediate texture soils most at risk for compaction

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15
Q

how does texture effect erosion

A

sandy soils most at risk for erosion due to weak particle cohesion

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16
Q

what is soil structure describing and what three things does it focus on

A

the organisation of particles looking at degree of development, form (ie granular, blocky etc) and size of the most common peds

17
Q

management practises for good soil structure (5)

A
  • cultivate at correct water content
  • retain plant residues
  • minimise time surface area is bare
  • perennial pastures
  • add lime to increase ph and enhance soil organism activity
18
Q

A bulk density value of above 1500 kgm3 suggests…

A

soil is compacted enough to limit root growth

19
Q

why do sandy soils commonly have a greater bulk density to clay (expect when clay is mismanaged) although you would initially expect vice versa

A

sand particles are large so although there are larger pores the accumalated area of small pores present in clay soils is greater meaning there is less mass per unit of volume and accordingly a sandy soil has more mass per unit of volume meaning its has a greater bulk density

20
Q

A macro-porosity greater than 0.08 to 0.1 is desirable for ….

A

adequate drainage and aeration

21
Q

if macroporosity is less than 0.05 what happens..

A

have issues with drainage and aeration

22
Q

when does volumetric water content = porosity

A

when the soil is saturated

23
Q

what is field capacity

A

content of water in soil after the excess has drained away

24
Q

what is stress point

A

point where roots can not extract water at the rate demanded by the leaves. the stomata will close and plant will be under stress

25
Q

what is permanent wilting point

A

plant has extracted all water they can, water left in soil will be held in micropores which hold it to tightly for it to be extracted due to the capillary phenomena

26
Q

what is hydraulic conductivity

A

the rate at which water moves through the soil

27
Q

what does soil temp effect

A

seed germination and growth rate
microbial population
accumulation and depletion of om
rate of chemical recations

28
Q

plastic limit is…

A

moisture content at which the soil takes on plasticine characteristics it becomes malleable and will take on the shape opposed on it

29
Q

soil consistence means

A

resistance to deformation or rupture it is dependant on water content of the soil

30
Q

phase lag is ..

A

soils conduct heat relatively slowly thus at a greater depth it takes longer to heat up or cool down this delay is called phase lag

31
Q

damping is

A

the decrease in range between max and min temp due to energy being absorbed as it moves down the soil profile

32
Q

how to calculate readily available water content

A

(volumetric water content at feild capacity - VWC at SP)/ root depth imm = …..mm

33
Q

how to caculate total avaliable water content

A

(VWC at FC - VWC at PWP)/ root depth in mm= ….mm