Importance of soil Flashcards
Soil functions
- medium for growth
- recycling system for nutrients and organic waste
- habitat for soil organisms
- system for water supple and purification
- engineering medium
Basic requirements for crop growth
- anchorage
- water
- air, particularly oxygen
- nutrients
- insulation
- phytotoxin control
Soil management
- cultivation
- drainage
- irrigation
- nutrient input
- organic matter
Long term soil quality
- acidification
- salinity
- erosion
- compaction
- waterlogging
- desertification
- chemical pollution
Water and air pollution
- nitrate, ammonia
- phosphorus
- pesticides
- heavy metals
- radionuclides
- erosion
- surface runoff
What are soils made from?
PORE SPACE - 20-30% air - 20-30% water SOIL SOLIDS - 45% mineral - 5% organic
Physical weathering
- thermal, due to differential rates of mineral and rock expansion
- mechanical, due to freeze-thaw and plant root effects, and to differential rates of mineral expansion when exposed to water
Chemical weathering
- hydrolysis (attack inter-mineral bonds and alter mineral compostion)
- carbonation (accelerated hydrolysis)
- hydration (absorption of water)
- dissolution (minerals dissolve in water)
- oxidation and reduction (minerals weaken through a change in their oxidation state)
Physical weathering
- thermal, due to differential rates of mineral and rock expansion
- mechanical, due to freeze-thaw and plant root effects, and to differential rates of mineral expansion when exposed to water
Main organic inputs
- cellulose
- lignin
- fats and waxes
- sugars and starches
- protein
- hemicellulose
Plant and animal remains
Soils vary in the content and age of their organic matter
- days, weeks and months ~(residues) to centuries (humus) old
Transformation of organic inputs
- organic residues are slowly altered by micro-organisms to new material called hums, which is both chemically and physically different from the chemicals that make up plant and animal remains
- organic residues persist in soil fro a few years whilst humus is very stable an can be >1000 years old
- humus is intimately mixed with the mineral fraction and imparts a dark brown colour to soil
Soil horizons definition
the movement and accumulation of mineral and organic materials down through soil as it develops produces a number of distinct layers
- some materials are lost from the soil, determined largely by rate of water movement
- some parts of the profile become enriched, other become depleted of certain minerals
soil horizons
O- plant and animal residues & decomposing organic matter
A - mixture of mineral and humified organic matter
E - eluvial zone, soil is depleted from soluble and insoluble material by leaching
B - illuviation, zone of accumulation
C - parent material