What are the features of fertile soil? Flashcards
How does fertile soil affect water content?
- fertile soil allows good drainage ( doesn’t become waterlogged but still retains enough water for survival of soil biota )
How does fertile soil affect soluble materials?
- contain macronutrients ( nitrogen and potassium ) present in ionic form ( nitrates and potassium ions )
- contain micronutrients ( copper and iron )
- toxic ions ( aluminium and heavy metals ) are adsorbed onto surface of mineral particles
Explain the behaviour of hygroscopic water between soil particles?
- held by adhesive forces on the mineral particle
- cannot by absorbed by plants
Explain the behaviour of capillary water between soil particles?
- water held by soil particles does not drain from the soil
- water can be absorbed by plants
Explain the behaviour of gravitational water between soil particles?
- water can be absorbed by plants
- water drains easily
How does fertile soil affect air content?
- most living organisms that increase fertility are aerobic
- well aerated soils are likely to be more fertile
How does fertile soil affect dead organic matter?
- has a high dead organic matter content
- releases plant nutrients as it decomposes
- increase water retention
- provides food for soil biota
How does fertile soil affect the pH?
- ranges from pH5.5 to pH7.0
- this is the range of tolerance for most plants and other soil biota
- acidic soils can increase leaching of plant nutrients
- acidic soils damage root cell membranes
- under alkaline conditions phosphates become insoluble
How does fertile soil affect soil biota?
- detritivores ( beetle larvae ) break up dead organic matter and release nutrients into soil
- detritivores increase soil drainage and aeration by creating tunnels in the soil
- decomposers ( bacteria and fungi ) break down dead organic matter
- decomposers secrete digestive enzymes
- nitrogen-fixing bacteria convert gaseous nitrogen into ammonium ions
- mycorrhizal fungi - symbiotic relationship
How does fertile soil affect the soil texture?
- soil texture is the property controlled by the promotions of the different size categories of mineral particles in the soil
- clay = <0.002
- silt = 0.002 - 0.02
- sand = 0.02 - 2.0
Compare drainage rate in sandy and clay soils
SANDY - larger pore spaces allow rapid drainage which reduces the water content but increases aeration
CLAY - poorly drained
Compare capillary action in sandy and clay soils?
SANDY - no capillary rise of water
CLAY - tiny pore spaces between particles allow water underground to rise towards surface
Compare aeration in sandy and clay soils
SANDY - pore spaces in well-drained sandy soils are filled with air
CLAY - more likely to be waterlogged with a low aeration rate
Compare nutrient retention in sandy and clay soils
SANDY - nutrient ions don’t adsorb easily onto sand particles
CLAY - nutrient ions adsorb easily onto clay particles
Compare thermal capacity in sandy and clay soils
SANDY - lower thermal capacity ( warms up more rapidly after cold weather )
CLAY - high thermal capacity ( high water content - warm up and cool down slowly )