2.3) Biosphere Flashcards
1
Q
- What are the summary of soil INPUTS?
A
- Soil inputs include:
1. Water from atmosphere π¦
2. Organic matter from decaying organisms π¦
3. Nutrients from weathered rocks β¨
4. Excretions from plant roots π«
5. Respiration from soil animals π¨
6. Solar energy and gases from the atmosphere βοΈ
2
Q
- What are summary of soil OUTPUTS?
A
- Soil outputs include:
1. Evaporation π€οΈ
2. Water and nutrient loss by capillary action π¦
3. Nutrients taken up by plants π±
4. Nutrient loss due to water passing through the soil π§οΈ
5. Losses of soil material due to soil creep (downhill) ποΈ
3
Q
- What is the role of CLIMATE in soil formation?
A
- Climate is the long-term weather pattern in an area determined by:
1. Precipitation π¦οΈ
2. Temperature π‘οΈ - Climate is the most important factor in the formation of soils. Soil produced from the same parent material under different climates contrast.
β When precipitation exceeds evaporation, leaching of the soil will occur.
β Temperature determines the rate of chemical and biological reactions. It influences the rate of decay of organic matter and weathering.
4
Q
- What is the role of ORGANIC MATTER in soil formation?
A
- Organisms in the soil influence soil development in a number of ways:
1. Decomposers: Microorganisms carry out the decomposition of animal and plant material.
2. Detritivores: Such as earthworms, aerate and mix the soil.
3. Plants: Determine the nature of the humus and leaf litter. Roots bind soil paticles together.
5
Q
- What is the role of RELIEF in soil formation?
A
- Relief is a term used to describe the shape of the land, including the height and steepness.
- Relief influences:
1. Soil thickness (as slope angle increases so does erosion) ποΈ
2. Temperature π‘οΈ
3. Runoff π¦
4. Drainage π
5. Plant cover π±
6
Q
- What is the role of PARENT MATERIAL in soil formation?
A
- Parent material is the material from which the soil has developed (e.g., soild rock or clay).
- Parent material can influence:
1. Colour π«
2. Structure π±
3. Texture β
4. Mineral composition β¨
5. Permeability π§οΈ
7
Q
- What is the role of TIME in soil formation?
A
- Soils develop very slowly.
- Young soils retain many characteristics of the parent material. Over time they acquire other features resulting from the addition of organic matter and activity of organisms.
- Soils pass through a number of stages as they develop, resulting in a deep profile with many well differentiated horizons (layers).
8
Q
- What is weathering?
A
- Weathering:
β is the exposure and breaking down or dissolving of rocks and minerals on the Earthβs surface due to interaction with the atmosphere.
9
Q
- What are the types of weathering (physical, chemical and biological)?
A
-
PHYSICAL:
β weathering caused by changes in temperature, freeze-thaw, or effects of wind, rain and waves. -
CHEMICAL:
β where rainwater reacts with mineral grains in rocks to form new minerals (clay) and soluble salts (especially when rainwater is acidic). -
BIOLOGICAL:
β is a form of physical weathering caused by animals, plants, fungi and microorganisms.
10
Q
- What is humification?
A
- Humification:
β is the transformation of raw organic matter (e.g., leaves) into humus, where no recognisable plant parts remain. - The process is carried out by detritivores.
11
Q
- What is decomposition?
A
- Decomposition:
β is the breaking down of organic materials into smaller constituent parts, especially by the action of decomposers.
(e.g., the role of bacteria in the breakdown of organic proteins during the nitrogen cycle)
12
Q
- What is translocation?
A
- Translocation:
β is the movement of materials within the soil. There are several translocation processes:
1. Leaching
2. Eluviation
3. Illuviation
4. Capillary action
13
Q
- Describe the processes of translocation? (leaching, eluviation, illuviation, capillary action)
A
- Leaching:
β is the movement of dissolved substances (e.g., nutrients) with percolating water in soil. - Eluviation:
β is the movement of suspended or dissolved compounds (e.g., salts) by percolating water from an upper into a lower horizon. The upper horizon is described as eluviated or E-horizon. - Illuviation:
β is the deposition of soil materials moved from the upper (eluviated) horizon to the lower (illuviated) horizon. - Capillary action:
β is the movement of water through pore spaces from wet areas to drier areas in soil. Often results in salts from groundwater being raised to the soil surface.
14
Q
- What are the biotic and abiotic factors that compose soil?
A
- Mineral matter: from disintegration and decomposition of rocks.
- Organic matter: from the decay of plant residues, animal remains and microbial tissues.
- Water: from the atmosphere and reactions in the soil (chemical, physical and microbial).
- Air or gases: from the atmosphere and from reactions of roots, microbes and chemicals in the soil.
- Organisms: macro (worms, insects) and micro (bacteria).
15
Q
- What is particle size?
A
- The particles that make up soil are categorised into three groups by size - sand, silt and clay.
- Sand particles are the largest and clay particles are the smallest. Most soils are a combiantion of the three.
- The relative percentage of sand, silt and clay are what give soil its texture.