Lecture 1 - Intro to soils Flashcards
1
Q
What is soil
A
the layer of unconsolidated material on the Earth’s surface that serves as a natural medium for plant growth
2
Q
importance of soils
A
- releases nutrients required for life in waterways and for land animals (ag)
- store water for plants
- improve water quality
- recycle nutrients and carbon -> nutrient cycles
- recycle wastes -> decomp
- food
- physical support for building and construction
3
Q
function of voids
A
- allow space for root growth deep into the soil
- provide water storage
- store carbon and air for plant growth – aeration of roots
4
Q
major components of soils
A
- mineral (45%)
- OM (1-5%)
- air (25%)
- water (25%)
- soil organisms – billions
5
Q
How do soils support plants
A
- physically
- aeration of roots
- water storage
- thermal insulation
- control toxicity (filtration + pH)
- nutrient supply (recycle)
6
Q
how is Australian soil difficult?
A
- slow formation (~ 300 years per cm)
- nutritionally impoverished, structurally challenging, salty, N2 and P deficiency
- infertile and mostly sandy loams
7
Q
what factors impact soil formation
A
- parental material, climate (precip and temp), macro and microorganisms, topography (elevation, slope, position), time
8
Q
process of soil formation
A
- weathering of top layer (lichens etc)
- water movement into the soil
- cracking and voids occur
- roots able to penertrate soils
9
Q
how do soils change compared to parent material
A
- ## physically, biologically, chemically and structurally
10
Q
what is WA soils parental material?
A
- major rock types contains quartz, orthoclase, plagioclase
- Most of Australia is covered in a deeply weathered regolith which is covered in resistant duricrust (major parent material in Aus)
11
Q
define soil profiling
A
recording of morphological properties for each horizon recognised
12
Q
What are the different ways to describe a soil
A
- horizons (depths and thickness)
- texture
- pedality (ped shape, size, stability, abundance)
- colour (when wet)
- roots
- mottles (two different colours of soil next to each other)
- coarse fragments
- segregations
- moisture status
- pans (dense layer, might stop roots growing if hard)
13
Q
what are the soil horizons in a profile and how to ID
A
- topsoil/Horizon A (top and high OM) - usually darker
- subsoil/ Horizon B – different composition (lighter), materials leached from A, more clay (leached)
- Parental material/ partially weathered rock (roots unlikely to penetrate -> rock or partly decomposed sand/clay
- very slightly weathered area (no roots)
14
Q
what is soil fertility?
A
- ability to support plant growth
15
Q
A