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    Soil ppt Soil ppt Presentation Transcript

    • APES
    • 6 Major components of soil Eroded rock Mineral nutrients Decaying organic matter Water Air Living organisms
    • Importance of Soil Provides nutrients Recycles/filters water Stores water Soil is the basis of life on Earth…why do you think?  Plants get nutrients from soil and plants provided glucose and oxygen (producers)
    • Terms associated with creation ofsoil Infiltration  Downward movement of water through the soil Leaching  Dissolving of minerals and organic matter in upper layers carrying them to lower layers ***soil type determines degree of leaching and infiltration
    • Formation of Soil (clay + mix of dead vegetation) Physical weathering  Mechanical weathering  Any process that breaks down rock into smaller pieces without changing chemistry of rock  Wind and water Chemical Weathering  Result of chemical interactions between water and atmospheric gases and the bedrock of the region  Oxidation: reaction with O2  Hydrolysis: rxn with H2O  Acid action: Rxn with acids (H2CO3, H2CO4, H2SO3)  Dissoultion: chemical weathering from acid rain Biological weathering  Takes place as a result of activities of living organisms  Can be combined with chemical processes  Chemosynthesis of bacteria  Roots of trees creating fissures in rocks exposing them to further mechanical and chemical weathering
    • Soil 1 gram of soil has over 50,000 protozoa as well as bacteria, algae, fungi, earthworms and nematodes Pores between grains of minerals in soil are filled with air or water  Plants need water and oxygen  Need to make glucose-use photosynthesis and cell respiration  Size of the particles that make up the soil determine the size of the pores between the soil particles USDA has many ways to categorize  Color  Texture
    • Soil Horizons O horizon (surface litter)  Uppermostorganic matter (leaves, twigs, crop waste, animal waste, organic matter)  Dark, crumbly material that results from decomposition of organic matter  Brown or black A Horizon (Topsoil layer)  Porous mix of HUMUS and some inorganic particles (weathered rock)  LEACHING/ELUVIATION zone  Fertile soil=better crops  Holds water and nutrients for plants *** O and A are anchored by vegetation B Horizon (subsoil)  Composed of inorganic minerals  Broke down rock (clay, silt, sand/gravel)  Receives all minerals leached out of A horizon as well as organic material that is washed down from the topsoil above  ILLUVIATION/ACCUMULATION zone  accumulation of soluble or suspended organic material, clay, iron, or aluminum C Horizon (parent material)  Large pieces of rock that have not undergone much weathering R Horizon  Bedrock
    • Soil Textures-3 major divisions Clay  Smallest, very fine  Less than 0.002mm in diameter  Easily stick to each other  Little room between particles to store water  Extremely compact, feels sticky Silt  0.002-0.05 mm in diameter  Feels smooth  Holds water well  Resists filtration Sand  0.05-2.0 mm in diameter  Coarsest particle  Too large to stick together  Creates soil with large pores  Water filter through (Gravel)  2.0 mm and larger  Does not hold water well
    • Acidity and Alkalinity of Soil What is pH? Most soils pH= 4-8 (neutral to slightly acidic) pH affects solubility of nutrients Determines nutrient availability for absorption by roots of plants If soil in a region is too acidic or basic, certain soil nutrients in that region will not be able to be taken up by plants pH too acidic=BIG problems  Ions of heavy metals mercury (Hg) or aluminum (Al) can leach into the groundwater  These ions will then travel to streams and rivers=negative impact to plants and aquatic life  Ex. Aluminum ions can damage fish gills=suffocation of fish
    • Loamy Soil composed of roughly the same amount of all three textures (clay, silt, sand) and organic matter Loose and rich When you squeeze it, forms a ball that crumbles when poked Good at absorbing and storing water Best for plant growth
    • Soil Types- Based on Water content Pedocal  Dry, semi arid climate  Little organic matter  No mineral leaching  High limestone content  praries Pedalfer  Enriched with aluminum and iron  Greater organic matter and leaching  Found in areas with high temp. and lots of forest cover Laterite  Soggiest type  Tropical and subtropical climate zones  High organic matter  Low nutrients (lots of rain)  Aluminum hydroxide=red soil
    • Soil Porosity Measure of the volume of pores or air spaces per volume of soil AND average distance between those spaces  Fine particles help retain water (precipitation goes into pores)  Large particles help create air spaces for filtration Pores b/t organic solid particles and inorganic solid particles in upper and lower layers Contain varying amounts of air (N and O) and water Porous soil  Many pores  Can hold more water Non porous soil  Not a lot of spaces  Cannot hold much water
    • Soil Permeability Rate at which water and air move through the soil Sand  High permeability  Water moves through quickly  Filters water Clay  Low permeability  Water moves through slowly  Retain water
    • Topography Mapping of the land by contours and physical features of areas Since water runs downhill, it is easy for soil to be carried away during a heavy rainstorm Slope percentage affects the speed of the water’s down hill path  Ex. 5% grade= more erosion than 1% grade
    • Soil Formation is influenced by 5interrelated factors
    • How Soil is Formed
    • Soil Problems For and Caused By Humans Properties humans look for in soil  Top soil  Nutrient rich soil layer, millimeters to meters deep  Contains a mix of organic matter and minerals  Renewable when replenished and cared for properly  Currently, thousands of acres bare due to erosion, nutrient deficiency, overtillage, and misuse  Arable: soil suitable/fertile for plant growth…  Fertility refers to soils ability to provide essential nutrients: N, K, and P  Humus also important b/c its rich in organic matter  Loamy soil  Composed of same amount of clay, silt, sand  Ability to aggregate (clump)  Best soils are aggregates of different soil types bound together by organic matter
    •  Tillage Repeated plowing  Breaks down soil aggregates leaving “plow pan” or “hard pan” (hard, unfertile soil)  Opening up Earth to plant new seeds  Increases soil erosion  It is done b/c it is thought to increase soil nutrients  Today, narrow chisel plows are used that leave 75% of crop residue on surface and open up only a thin ridge for seeds  No-till methods are beneficial  Pierce seeds through ground cover without opening up a seam in the earth  Keeps soil in place and prevents erosion
    •  Monoculture  Planting of just one type of crop in large area  Decrease in genetic diversity of crop species  Lack of genetic variation=increased susceptibility to pests and diseases  Consistent planting of one plant in area LEACHES soil of specific nutrients needed for plant growth  Prevention Method: CROP ROTATION  Different crops are planted in growing area in each growing season Machinery  Large machines  Agriculture industry is a huge consumer of energy  Energy is consumed by:  Production of pesticides  Production of Fertilizers  Use of fossil fuels to power farm machinery
    •  Green Revolution=boom in agricultural productivity  Industrial revolution  mechanization of farming  increase world wide agricultural productivity in last 50 years of =detrimental to environment  Drawbacks  Increase in irrigation = Over irrigated soils= SALINIZATION  Soil becomes water logged and when it dries out, salt forms a layer on the surface, which leads to land-degradation  Drip irrigation is one way scientists have started combating problem  Allots area only necessary amounts of water  Water delivered straight to roots  Chemical pesticides=new insect species that are pesticide-resistant  Recently GM plants are helping solve pesticide problem
    • Soil Erosion Bare soil=soil in which no plants are growing  More susceptible to erosion than soil covered by organic matter Erosion: normal and natural process  Constant movement of wind and water on Earth’s surface  Drawbacks:  Removes valuable top soil  Over 25 billion tons of soil lost due to wind and water erosion  Erosion can lead to DESERTIFICATION  Deposits soil in undesirable places (i.e. bodies of water)  Farmers need healthy soil for planting  Humans rely on water uncontaminated water for drinking/living  Soil can contaminate water with pesticides and other harmful chemical Causes  Deforestation  logging and slash-and-burn  Plants anchor in O and A horizons of soil  Removal of plants make soil susceptible to erosion  Over-cultivation of agricultural fields  Overgrazing  Urbanization ***All of these will continue to make ARABLE land for farmers hard to find ***New techniques must be utilized to preserve the integrity of the soil
    • Effects of Erosion Top soil blown away by wind or washed away by rainfall Weakened land Leads to…  Downstream flooding  Reduced water quality  Increased river and lake sedimentation  Build up of silt in reservoirs and navigation channels  Dust storms  Health issues  Allergies  Eye infections  Upper respiratory problems
    • Soil Conservation Several management practices utilized to conserve soil resources 1. Return organic matter to soil 2. Slow down effects of wind 3. Reduce amount of damage done to soil by tillage (plowing) Examples:  Use animal waste and the residue of plants to increase the amount of organic material in soil  Modify tillage practices to reduce the breakup of soil and reduce the amount of erosion (contour plowing and strip planting)  Use trees and other wind barriers to reduce forces of winds
    •  Soil conservation Contour planting  Plant across a hillside (instead of up and down), slows run off Strip farming  Planting alternating crops in strips across land  In combination with contour planting, this slows erosion Terracing  Similar to strip farming  Land is shaped…level ridges of land are created to hold water and soil in place  More expensive and time consuming but allows cultivation on steep grades and increases sustainability (this is how rice is grown in Asia) Perennial plant growing  Coffee and tea  Plants that grow during several seasons  Do not have to harvested yearly AND hold soil longer  Ground cover plants (alfalfa) hold and protect soil from erosion if planted right after initial harvest
    • Soil Laws 1977 Soil and Water Conservation Act  Soil and water conservation programs to aid landowners and users  Sets up conditions to continue evaluating the condition of the US soil, water and related resources 1984 Food Security Act “Swampbuster” Act  Discouraged conversion of wetlands to non-wetlands  1990 federal legislation denied federal farm supplements to those who converted wetlands to agriculture  Provided restoration of benefits to those who unknowingly converted lands to wetlands
    • Prepared by:Chasey Gabrielle CiudadKathleen BaesRonna Badoles