Compaction Flashcards

1
Q

Soil subjest to 2 types of machinery traffic

A

Compacts - wheel

Loosens - tillage

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2
Q

Rresponse to traffic is described in terms of the change in

A

Bulk density
Porosity
Penetration resistance

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3
Q

What is compaction and what causes it

A

process by which soil grains are rearranged to decrease void space

Machinery or stock movement

Cumulative and difficault to reverse

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4
Q

Compacted soil properties

A

Increases BD
Decreases total porosity
Increases microproes

Restricts water flow
Impedes root extension
Occurs easily in wet soil

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5
Q

Root elongation limited by

A

Penetraion resistance higher than pressure exerted by root = reduced water and nutrient uptake

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6
Q

Preventing soil compaction

A

Lighter machinery
Tire widdth and pressure
Zero till
Controlled traffic

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7
Q

Effects of tyre width and pressure

A

Increasing tyre width or decreasing pressure= spreads compaction pressure over a wider area

Low pressure reduces rut depth and soil damage but increases total area wheeled

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8
Q

Wetness of soil effect on compaction

A

Dry soil not easily compacted

Saturated soil is also not easily compacted because water is not compressible which fills big pores

Moist soil is more compactable

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9
Q

Management solutions to soil compaction problems (4)

A

Controlled Traffic CTF

Mechanical loosening such as Deep Ripping

Primer Crops/ Bio-drilling (strong tap roots)

Addition of OM

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10
Q

OM addition effects

A

Retains soil water = rebound against compaction

Stabilises soil structure

Dec. BD and soil strength

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11
Q

OM addition application methods and reasoning

A

OM to topsoil through incorporation of plant residues is widely used

Less common to solve subsoil compaction

Technical and economical

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12
Q

CTF effects

A

ZT decreases operations but still 50% field area affected by heavy vehicle traffic

CT = permanent, compacted lanes leaving loose rooting zone

Recompaction of a deep tilled soil can be prevented using CT system

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13
Q

Tramping and soil compaction

A

0-20cm

Fine textured soils more susceptible to trampling

Can be reduced with vegetation and prevention of grazing in wet soils

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14
Q

Pros of depe ripping

Subsoil/deep ripping/subsoil cultivation

A

Effective way to relieve subsoil compaction

Increase water conductivity

Decrease soil BD

Increase porosity

Increase water infiltration

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15
Q

Negatives of Deep ripping

A

Recompaction - subsequent machinery and animals

COst - fuel, reduced if using machinery with shallow leading tines and winged shanks

Soil mixing - deep cultivation that inverts soil may also bring dispersive subsoil to the soil surface

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16
Q

Shearing stregth of soil

A

Depends on soil cohesion and friction

Pore water reduces soil particle contact = reduced frictional stregth

17
Q

Soil can deform in 3 ways

A

Brittle loosening disturbance

Compressive Disturbance

Tensile Disturbance

18
Q

Brittle Loosening disturbance

A

Soil mass fractures into smaller units

occurs due to compressive forces

Decrease in overall density but not in the clods

19
Q

Compressive Disturbance

A

SOil is forced on itself

Density of the whole mass increases; eliminating any fissurees or macro pores initially present

20
Q

Tensile disturbanve

A

Similar to brittle but occurs under tensile forse

21
Q

Alleviating comapction

A

Only done by brittle and tensile disturbance

Require upward soil movement

22
Q

Upward movement

A

If it becomes to much due to soil load, and strength of soil, soil moves laterally ratther than upwar = compressive disturbance

23
Q

Confining resistance of upwards movement is dependint upon

A

Working depth

Soil density

moisture content

24
Q

Critical Depth definition and example

A

Transition working depth above which the desired brittle type of disturbance occurs and below which a compressive disturbance occurs

Compaction at plough depth (plough an) is due to compressive disturbance below critical depth

25
Q

Critical Depth depends on

A

Tine Geometry

Soil compressibility

Soil Density

Soil Moisture- high MC decreases critical depth

26
Q

To increase critical depth:

A

Increase tine point width

Increase wing lift height

Relieving confining resistance

27
Q

Deep tillage moisture

A

Too wet = smeared

Too dry = large clods/dust

idea is 50% Field capacity (late spring)

28
Q

Greater water content or lower ther bulk density =

A

Lower critical depthand greater the susceptibility of soil to compaction

29
Q

If loosening at required depth is excessive:

A

Reduced using narrow point

Bring working depth closer to critical depth

30
Q

if desired working is greater than critcal depth, CD is increased by:

A

Wider tine points

Reducing confining resistance of the surface layer

31
Q

Wings =

A

lateral extent of brittle disturbance increases

32
Q

leading tines =

A

Greater working depth

33
Q

Compaction alleviation in grassland requires

A

Tensile disturbance, whilst avoiding grass kill and bringing soil to the surface

34
Q

Moldboard plough

A

Inverts soil
Turns residue under soil surface
Extreme lifting
Little residue left on surface

35
Q

Disk plough

A

Large concave disks
Reduces surface residue by 50-60%

Better in stricky soils

Good weed control

Cut, invert and mix surface soil and stubble

36
Q

Chisel plough

A

Heavy duty tines

Less inversion of soil and crop residue incorportaiton

Uses chisels or sweeps that shatter the soil and good for weed control

Reduce residue 12-50%

Higher risk of disease for tillage with blade/chisel than disk plough (stubble incorporated)

37
Q

Blades and Sweep ploughs

A

Less agressive
Reduce surface cover 10-20%

Used for stubble mulching

Grreater residue handling capacity

38
Q

Ripper

A

Break hard pan

DR greater than 30cm is beneficial only in deep sandy soils

Clayey soils form compacted pans at much shallower depth and