Particles, Structures and Water Flashcards

1
Q

What is soil texture based on?

A

Proportion of sand, silt and clays

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2
Q

Example of soil texture…

A

10% clay, 60% silt and 30% sand being sandy loam

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3
Q

Example of soil porosity…

A

Clay gaps small whilst sand large

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4
Q

What does porosity influecenc?

A

Drainage and water retainment

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5
Q

What does texture influence?

A

Soil fertility based on storage and plant nutrient supply

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6
Q

Soil Structure

A

Refers to sand/silt/clay bonded into aggreagets

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7
Q

How does aggregation occur?

A

Formation then stabilisation, formation by shrinking/swelling of soil by freezing or root penetration breaking soils into discrete units

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8
Q

Types of aggregate?

A

Microaggregates (<250micrometres) (Macroaggregates(>250micrometres_

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9
Q

Microaggregates formation…

A

First clay flocculation where clay paritcles conglomerate

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10
Q

What enhances microaggreagate microbial adegradation?

A

Organic matter association

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11
Q

What does macroaggregates derive from?

A

Microaggregate coalescing

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12
Q

What does stability depend on in low clay concentration?

A

OM

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13
Q

What does stabilising OM consist of?

A

Plant by-products like polysaccharide glue and the other and roots and fungal hyphae

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14
Q

How is pore and aggregate arrangement altered?

A

Tillage, plant roots and swelling

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14
Q

How can pore space be calculated?

A

Rastio of weight to volume, as greater amount of soil particles with least amount of pore space weighs more3

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15
Q

Why is pore size important?

A

Determine retention, larger pores holding water more loosley whilst smaller more tightly

15
Q

How is bulk density measured?

A

Mass of soil divided by volume of a cylinder

16
Q

Three pore classificaitons?

A

Macropores
Mesopores
Micropores

17
Q

What is soil moisture characterisitcs determined by?

A

Composition of pores

18
Q

Hyrdrualic Conducitivty

A

How easily water can move through profile, determining wetting front

19
Q

Wetting Front

A

Water infiltration moving down the profile

20
Q

What does HC depend on?

A

Water flow resistance by soil particles
Pressure generated by water in soil

21
Q

What is pressure a function of?

A

Elevation and pressure generation of overlying water columb

22
Q

What is pore resistance to water flow?

A

Determined by how well pores are connected, pore-size distribution and water ocntent of the soil

23
Darcy Law
Refers to discharge being proportional to the loss
24
Field Capacity
Emptying of macropores where remaining water held is within meso/micropores
25
Why is aggregation important?
Allows withstanding slaking and compaction preventing poor water infiltration and gas exchange
26
Where is aggregate instability most present?
Sand and silt
27
Soil crusting
Where aggregates release into soil pores, preventing further water infilitration
28
Why might water tension be bad?
Limit nutrient uptake due to the energy required to extract them
29
What does pore size distribution determine?
Plant-availabe wateM
30
Moisture Release Curve
Gives water content against water tension
31
Why shouuld large and small pores be balanced?
Gas exchange and water storage
32
What are the best agriculture soils?
Loamy textures with equal silt, clay and sand for enough water for plant growht and pores for gas exchange
33