Lecture 3: Chemical and bio properties of soil Flashcards
Key macronutrients for soils:
- nitrogen (growth)
- phosphorus
- potassium
- sulphur
- calcium
- iron
- copper
What are Exchangeable cations:
- positively charged ions that are loosely attached to the negative surface sites of clay particles or organic matter by electrostatic forces
- main cations = Ca2+, Mg2+, Na+, NH4+, K+
what is Cation Exchange capacity and why is it needed
- total capacity of soil to hold exchangeable cations
- influences soil ability to hold essential nutrients
- indicator of water retention - allows water adheration
causes of soil acidifcation
- insufficient use of nitrogen -> when NH4 used, breaks into NO3- and H+, H+ can build up if NO3- leaches
- removal of plant material -> plant material usually slightly alkaline, removing will leave excess H+ in soil
what are the effects of soil acidification
- aluminium becomes soluble, soluble Al retards root growth and limits access to water and nutrients
- decreased availability of major nutrients
- lower microbial activity -> especially less nitrogen fixing rhizobia (killed)
How to fix acidification
- ameliorating/liming (CaCO3) -> most economical
- add species to soil that will increase pH
causes of increased soil salinity
- clearing
- using shallow rooted annuals -> use less rainwater which then adds to groundwater, leads to slat being brought up to surface and left when water evaporates
impacts of soil salinity
- salt destroys protective plant cover
- plant death
- waterlogging
- increased water usage for farmers
how to fix soil salinity
- increase water use by planting perennials
- manage soil water content (drain)
- enhance remnant vegetation
- re-plant trees on recharge zones
- plant salt tolerant species
Phosphorus cycle process
- decomposed by organisms, released to soils or added to reservoirs
- runoff and erosion, leaching and plant uptake = out of soil
- manures, plant residues, fertilizers, atmospheric deposition = into soil
what is the Phosphorus buffering Index
PBI (phos buffering Index) = capacity of soil to fix P.
- Higher = need more P supplied in fertilizers to maintain P level
- how much P soil absrobs
Why can legumes fix atmospheric Nitrogen
- symbiotic relationship with rhizobium bacteria -> live in nodules
- they fix it into an inorganic state so plants can absorb it
- N -> NH4+ -> NO3-
- nitrate is highly mobile in roots but leaches quickly due to this, ammonium less so due to pos charge so leaching less -> thus need legumes
why is nitrogen so important?
- needed in highest amounts
- major component of chlorophyll
- major component of amino acids -> needed to build proteins for growth
why are bilogical components so important to soils
humus formation, OM breakdown, N fixing and cycling, soil structure maintenance
- macrofauna break down OM, microfauna aid nutrient transfer, mesofauna spread disease or prevent it
- fungi agregate the soil, decomposers
- worms and insects aerate the soil