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AP Environmental Science Soil Resources (Ch 14) Living in the Environment , 14th edition, G. Tyler Miller. Soil Characteristics. Understand what soil is and how it forms. Compare and contrast the characteristics of different soils. What type do you have around your house?.
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AP Environmental ScienceSoil Resources(Ch 14)Living in the Environment, 14th edition, G. Tyler Miller
Soil Characteristics Understand what soil is and how it forms. Compare and contrast the characteristics of different soils. What type do you have around your house? 1) clay = “layer silicates that are formed as products of chemical weathering of other silicate minerals at the earth's surface. They are found most often in shales, the most common type of sedimentary rock.” 2) silt = rock worn into tiny pieces (coarser than clay, but finer than sand). usually 1/20 millimeter or less in diameter 3) sand = quartz or silica worn down over time. grains with diameters between 0.06 mm to 2 mm 4) organic matter (humus) 5) Loam = soil containing a mixture of clay, sand, silt and humus. Good for growing most crops.
Soil Porosity and Permeability Porosity - volume of water that “fits between” the soil particles Permeability - rate of flow of water through soil % retention - how much water is “trapped” by soil Porosity and Permeability are directly related; when one is high, the other is high as well. % water retention is inversely related to both. ______________________________________________________________ 1) Clay - porosity permeability, retention 2) Silt - porosity, permeability, retention • 3) Sand - porosity, permeability, retention • 4) Organic matter - porosity, permeability, retention
Soil Conservation Explain what soil erosion is. Describe its causes and effects. List and describe various soil conservation methods. • Soil moves….due to water, wind, people • Loss of topsoil…the most fertile • Soil ends up as sediment in water • Soil IS renewable…WHERE does it come from? http://www.usd.edu/anth/epa/dust.html http://en.wikipedia.org/wiki/Soil_conservation
List and describe some of the pros and cons of using fertilizers. What different sorts of fertilizers are available? Organic… manure adds N and soil bacteria & fungi green manure compost mushroom spores Inorganic…1/4th of the world’s crops depend on this. N, K, P Experimental data comparing methods! Click on the picture!
Soil Formation Soil formation - Parent material is slowly broken down by biological, chemical and physical weathering. Biological - Respiration of plant roots and other organisms produce CO2, which reacts with soil water to produce carbonic acid (H2CO3). Chemical - Acids crack rocks water seeps in breaks down particles. Physical - Weathering introduces water that breaks down particles. Time scale - Formation of 2.5 cm of topsoil takes 200 - 1000 yrs.
Soil Composition Soil Composition 45% Mineral particles (broken down pieces of rock) 5% Organic matter (humus - from dead organisms, worm castings, leaf litter) 25% Water (precipitation) 25% Air (More with sandy soil, less with clay soil) Soil organisms - Millions in one teaspoon of fertile agricultural soil! - bacteria, fungi, algae, microscopic worms. provide ecological services such as worm castings, decomposition to humus, breaking down of toxic materials, cleansing water, nutrient cycling from decomposers or upon death
Soil Texture Loam - ideal agricultural soil 40% sand (larger - structural support, aeration, permeability) 40% silt (smaller - holds nutrient minerals and water) 20% clay (even smaller - holds nutrient minerals and water) Plants grown in sandy soils More susceptible to mineral deficiencies and drought Plants grown in clay soils More susceptible to waterlogging, and oxygen depletion (think small pore size, low porosity)
Soil Acidity (pH) pH - concentration of H+ ions Scale - From 0 (very acidic) to 14 (very basic, or alkaline) pH of most healthy soils - 4 - 8 pH matters because it affects solubility of nutrient minerals Aluminum and Manganese are more soluble in low pH - roots sometimes absorb too much (toxic levels) Soil pH affects leaching - high pH increases leaching of important ions such as K+ Causes of changes - acid rain, decomposition, leaf litter, mining (acid sulfate soils) Remediation - Too high pH, add acidic leaf litter - Too low pH, add lime
Soil Nutrients (NPK) Organic - animal manure, bone meal, compost (slow-acting, long-lasting) Delay in availability to plants, needs time for the organic material to decompose Delay causes low level of nutrient leaching Improves water holding capacity Inorganic - Manufactured from chemical compounds (fast-acting, short-lasting) Highly soluble so immediately available to plants High solubility also makes it leach quickly (pollutes water) Suppresses growth of microorganisms Source of nitrogen gases that increase air pollution Production requires much energy from fossil fuels, increasing CO2 emissions.
Soil Testing Report Conclusion page 76 Soil Testing lab packet #1, 3 (a-e) Due:
