Soil properties Flashcards
1
Q
what are the divisions of particle sizes?
A
- gravel (>2mm diameter)
- sand (2-0.02 mm diameter)
- silt (0.02 to 0.002 mm diameter)
- clay (<0.002 mm or 2micromm diameter)
2
Q
why is soil texture important? (5 reasons)
A
- it influences the soil infiltration rate (thus, overland flow and erosion)
- influences soil permeability (thus, drainage)
- controls available water capacity of soils (ability to supply water to plants)
- influences soil structure (root growth and aeration)
- provides cation exchange capacity (nutrient supply to plants and buffering against acid rain)
3
Q
what is the difference between soil structure and texture?
A
- analogy of bricks as soil texture and walls as soil structure
- structure: spatial arrangement of particles to complex aggregates, pores and channels
4
Q
what are the three main influences of soil structure?
A
- water/air movement
- root growth
- movement of macro/meso fauna
5
Q
what are the 6 major structural forms in soil?
A
- prismatic
- columnar
- angular blocky
- subangular blocky
- platy
- granular
6
Q
what are 4 processes leading to the development of soil structure?
A
- expansion/contraction upon wetting and drying
- root penetration
- earthworms and ingestion/excretion by other soil organisms
- input and decomposition of soil organic matter
7
Q
what are 6 properties that maintain soil structure?
A
- high organic matter content promotes bonding between particles
- clay minerals -> large, reactive surfaces with positive and negative charges
- presence of Fe and Al oxides and hydroxides as cementing agents
- Si coating on minerals -> produces duripans in dry climates
- CaCO3 deposits -> produce caliche in semi-arid soils
- presence of flocculating cations (Ca2+ and Mg 2+)
8
Q
what are 6 processes leading to the destruction of soil structure?
A
- loss of soil organic matter
- raindrop impact on bare soils
- reduction in root growth
- trampling by stock and machinery
- reduction in soil organisms
- loss of flocculating cations (Ca2+ and Mg2+) and replacement by dispersing cations (Na+ and K+)
9
Q
what are the effects of ploughing on soil structure?
A
- breakdown of weakened aggregates as soil surface
1a) erosion removes fine particles and OM, surface crusting reduces seeding emergence - formation of pan at base of plough depth
+
compacted subsoil
2a) impede root growth and water and air movement
10
Q
what are flocculating cations?
A
cations that make clay particles stick together (Mg+ and Ca+)