Lecture 2 - Physical properties of soil Flashcards
what is soil texture
proportions of sand, silt and clay
What is sand
particulate matter from rock disintegration (non-plastic) (2-0.02mm)
What is silt
fine mineral material, crumbles when rolled (0.02-0.002mm)
What is clay
fine grained soil, display plastic properties (<0.002)
Characteristics of clay soils
- retain moisture and nutrients
- most stored water is not usually available for plants
- prone to waterlogging
- easily compacts
characteristics of sandy soils
- struggle to retain water and nutrients
- allow plants to extract water and nutrients easily
- prone to nut. leaching
- prone to water repellence (need to add clay to help)
what impacts soil colours
- organic matter content = darker
- mineral matter = retains colour of rock
- form and abundance of iron = avg conds. = yellow oxide, well drained/dry = red oxide, waterlogged = grey/green/blue. More CO2 turns iron more brown
- moisture content = darker
define soil structure
how soil components are arranged into aggregates (combination of sand, loam, clay, OM, fungal hyphae into clusters)
Importance of soil strucure
- permeability to water and air, root penetration and seedling emergence, resistance to erosion (stability)
- better structure (more aggregates) = more pores/voids = movement of air and water
3 ways soil water exists in soil
- gravitational water = water is held in large pores and drains out of soil due to gravity (smaller pores = less draining)
- capillary Water = held in pores small enough to hold against gravity (can mean that plants can’t remove this water as too difficult)
- chemical water = water tightly held by electrostatic forces to clay surfaces (unavailable to plants)
What is field capacity
after saturation, all gravitational water has drained out
what is the wilting point
plants have drawn all accessible water out of soils
What is the issue with water resistance
- uneven pasture germination
- seeds buried in soil may not get any water if only light rains
- established and young plants in same pasture = difficulty using chemicals (different ages)
- increased risk of erosion
What destroys soil structure
- cultivation (turning over soil)
- loss of OM
- mixing dispersive subsoils (wetting with freshwater disperses clay particles)