AS Soil Flashcards
Contour ploughing
A soil erosion control measure where land is cultivated by ploughing horizontal furrows along the contours of the land.
Crop rotation
The practice of growing a different crop in a field on a cycle of three, four or five years.
Features of fertile soil
Water, soluble nutrients and metals, air, DOM, pH of 5.5 - 7, presence of soil biota, good texture
Sandy soils
lots of air space, drain quickly, loses water and nutrients quickly, less water present so less thermal capacity (warm up and cool down quickly), easy root penetration
Clay soils
less air space, poorly drained, hold water and nutrients for longer, more water present so higher thermal capacity (warm up and cool down slowly), harder for roots to penetrate
Humans activities contributing to soil erosion
removal of vegetation, ploughing, overgrazing, reducing soil biota, soil compaction, cultivating steep slopes
How humans affect soil fertility
aeration by ploughing and draining, Increasing and depleting nutrients, Irrigation, soil compaction, adjusting pH
Mulch
Material placed on the soil surface to reduce evaporation losses and reduce weed growth.
Multicropping
A form of polyculture where two or more different crops are grown in an area at the same time.
Ploughing
The cultivation of the soil by turning over the surface layer.
Soil erosion
the loss of soil in a location due to wind or water, water erosion includes rain splash, surface runoff and landslides
Terracing
The replacement of a sloping landscape by the creation of a series of narrow horizontal stepped strips, often used to reduce soil erosion.
Tied ridging
A method of reducing soil erosion by creating a grid of raised ridges that cause rainfall to collect, increasing infiltration and reducing runoff.
Tillage
The cultivation by turning the soil eg by ploughing.
Universal soil loss equation (USLE)
A formula that can be used to calculate rates of soil erosion.
Windbreaks
Hedgerows and rows of trees that reduce wind velocity to reduce soil erosion.
Soil Texture
The proportion of minerals in soil ie sand, silt and clay
Soil analysis, determining soil texture sedimentation method
- remove stones, twigs
- Separate peds/particles,
- half fill a clear containing with soil
- Add water and invert/shake
- Allow to settle (2 minutes for sand, 2 hours for silt, 2 days for clay)
- Measure the depth of each layer and calculate the proportion/percentage of sand, silt and clay.
Soil analysis, determining soil texture soil sieve method
- Stack the sieves with the coarsest mesh at the top, each sieve size will capture either sand, silt or clay
- Add a dry, crushed soil sample to the top sieve
- Shake/agitate the sieve stack for 2 minutes
- Weigh the contents of each sieve and calculate the proportion/percentage of sand, silt and clay.
Soil triangle
used to determine soil texture once percentages of each are known, read the axes as an inverted triangle, clockwise.
Soil analysis, determining water content
- soil must be stored in a sealed container to prevent water loss
- Remove stones, plant material and living organisms
- Place soil sample in a preweighed evaporating basin/crucible
- Soil is placed in an oven at approx 100°C for 24 hours and until a constant mass is reached
- Soil is reweighed, the mass loss is the original amount of water present in the sample.
- Calculated % water content, mass of water (lost) divided by original mass of soil multiplied by 100
Soil analysis, determining bulk density
mass of dry soil per unit volume. Dry mass over volume. g cm-3
Soil analysis, determining organic matter
- Record the mass of a dry soil sample
- place the soil sample in an oven at around 450°C until a constant mass is reached
- The sample is reweighed and the mass loss is the mass of organic matter in the original dry sample
- Calculate % organic matter, mass of organic matter (lost) divided by dry soil mass multiplied by 100
Soil analysis, determining pH
- use a calibrated electronic pH meter
- use universal indicator solution (soil sample + barium sulphate + water + shake in test tube)
- use universal indicator papers
- never say litmus paper!