soil
DESCRIPTION
Soil. What is soil?. Mixture of inorganic material (rocks) and organic material (SOM) as well as organisms (microbes). Soil formation involves: Parent Material (glacial deposits? Sediment? Lava?) Biotic Factors Plant roots break up soil, add nutrients and organic material - PowerPoint PPT PresentationTRANSCRIPT
Soil
What is soil? Mixture of inorganic material (rocks) and organic
material (SOM) as well as organisms (microbes). Soil formation involves:
Parent Material (glacial deposits? Sediment? Lava?) Biotic Factors
Plant roots break up soil, add nutrients and organic material Climate influences
Temp, precipitation, wind: leaching: movement solute thru soil Topography
More water flow? Steep slopes? Time
Characteristics of Soil Color
Dark: humus, other colors: minerals present
Texture Gravel, sand, silt, clay
Structure moisture, air capacity and ion exchange ability
Moisture Wet soils vs dry soils support different forms of life
Depth
What role does soil serve in the ecosystem?
Part of both food webs Provides nutrients for plants
Plants are a sink for toxic metals, organic toxins, carbon Plants are a food source Plants prevent erosion
Detritovores: recycle nutrients so they can be used by other organisms
Turn Nitrogen into nitrates Recycle the nitrogen and carbon out of dead things
(mineralization) Eat up pollutants
Holds moisture/ filters water
Structure of Soil: Inorganic
Silicon is to geologists what carbon is to biologists...
Rocks and soils basic structure: Silica: SiO2
Aluminosilicate: AlSi3O8
- or AlSi3O8-
Negative charge allows soil to hold on to important mineral cations: Ca2+, K+, Na+, Mg2+, NH4
+,
Al3+ can be substituted for Si4+
1 in 4 will give a -1 charge
2 in 4 gives a -2 charge
Soil Organic Matter Non-living organic components present in soil
resulting from decomposition of once living creatures Holds onto nutrients to exchange with plants Improves soil structure
Increase air More oxygen, Easier for roots to grow
Increased moisture Heat capacity / smaller temperature deviations
Reduces soil erosion
Soil Organic Matter
The organic material from bacterial breakdown of plants and other organisms Nature's way of recycling important nutrients:
Sugars, amino acids, proteins, polysaccharides Humic acids (Hummus)
Still don't really know what it is Stable organic material that isn't broken down any more by
organisms. Organisms will only “eat” what will give them a net energy
gain.
Soil Ecosystem: Detrital Food Chain
Soil Organic Matter: Possible Structure
Polar parts Hold water Hold inorganic nutrients (ions: nitrate, phosphate)
Importance of Soil Organic Matter
SOM gives the soil better “Structure” More moisture, more oxygen can diffuse, more pockets
for microorganisms to live Better soil structure supports more microorganisms
Microorganisms mineralize nutrients Amino acids → Nitrates → Natural fertilizer for plants
Using compost is a way to increase soil organic matter into bad soil
Pollutants Pesticides Excess Fertilizer Organic Pollutants
VOCs, Semi-VOCs, PCBs, PAHs, petroleum, solvents, organotin compounds
Partition in SOM (humic substances)
Adsorb to surface of inorganic soil
Heavy metals
Sources: Agrichemicals Household cleaners Gasoline, oil Dry cleaning Paints Sludge Landfills Etc (see pg 458 in IB bk)
Soil Degradation Salinization Water used for irrigation leaves
behind salts Too much salt and plant life cannot
survive Water tables rise (due to
deforestation), more evaporation occurs since surface is warmer so salinization occurs
Acid Rain and Storm water runoff Leaching of important nutrients for
plants
Sources Green J., Damji S. Chemistry 3rd Ed. IBID Press, 2007. http://www.science.org.au/nova/032/032box01.htm Smith, T. M., and R. L. Smith. 2009. Elements of Ecology, 7th
edition. Benjamin Cummings.