Soil Resources 14.

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Presentation transcript:

Soil Resources 14

Describing a Soil Description of a soil Mineral Component Organic Matter – humus Soil Horizons Importance of the Biological Community Water Holding Capacity Nutrient Holding Capacity Acidity and Alkalinity Mineral Particles (45%) Weathered rock Organic Material (5%) Litter, animal dung, dead remains of plants and animals Water (25%) Air (25%)

Soil Formation Productivity Climate Topography Age Parent Material

Soil Properties Negative charge on clay attracts positively-charged nutrients © 2012 John Wiley & Sons, Inc. All rights reserved.

Soil Horizons © 2012 John Wiley & Sons, Inc. All rights reserved.

Soil Properties Soil Texture Relative proportion of sand, silt and clay Sand: 2mm–0.05mm Silt: 0.05mm–0.002mm Clay: >0.002mm © 2012 John Wiley & Sons, Inc. All rights reserved.

Soil Classification – Step 1 Soil texture affects soil properties Coarse textured soil (sandy) Excellent drainage Fine textured soil (high in clay) Poor drainage Low oxygen levels in soil Due to negatively charged surface, able to hold onto important plant nutrients (K+, Ca2+, NO2-)

Soil Properties Soil Acidity Measured using pH scale pH of most soils range from 4–8 Affects solubility of certain plant nutrients Optimum soil pH is 6–7, because nutrients are most available to plants at this pH Drainage Nutrient Holding Capacity Water Holding Capacity

Biological System There are millions of microorganisms in 1 tsp of fertile agricultural soil Soil organisms provide ecosystem services Def: Important environmental benefits that ecosystems provide Decaying and cycling organic material Breaking down toxic materials Cleansing water Soil aeration

Nutrient Cycling The pathway of various nutrient minerals or elements from the environment through organisms and back to the environment © 2012 John Wiley & Sons, Inc. All rights reserved.

Soil Erosion Caused primarily by water and wind Why a problem? Causes a loss in soil fertility as organic material and nutrients are eroded More fertilizers must be used to replace nutrients lost to erosion Accelerated by poor soil management practices

Throughout human history, our relationship with the soil has affected our ability to cultivate crops and influenced the success of civilizations. This relationship between humans, the earth, and food sources affirms soil as the foundation of agriculture Soil: The Foundation of Agriculture Sanjai J. Parikh (Department of Land, Air and Water Resources, University of California, Davis) & Bruce R. James (Department of Environmental Science and Technology, University of Maryland, College Park

Effects Reduces plant growth Causes loss of soil fertility Requires additional fertilizer applications, Leads to sediment and fertilizer deposition in waterways

Soil Erosion Causes

Case in Point: American Dust Bowl Great Plains has low precipitation and is subject to drought 1930–1937 severe drought No natural vegetation roots to hold soil in place Replaced by annual crops Winds blew soil as far east as NYC and DC. Farmers went bankrupt © 2012 John Wiley & Sons, Inc. All rights reserved.

Soil Erosion, Desertification and Salinization © 2012 John Wiley & Sons, Inc. All rights reserved.

Go over the most important maps Variations in soil forming factors cause variation in soils around globe Soil Taxonomy Separates soils into 12 orders Subdivided into more than 20,000 soil series that vary by locality Five common soil orders Spodosols, alfisols, mollisols, aridosols, oxisols

Nutrient Mineral Depletion © 2012 John Wiley & Sons, Inc. All rights reserved.

Soil Problems - Salinization Gradual accumulation of salt in the soil, usually due to improper irrigation techniques Often in arid and semi-arid areas Salt concentrations get to levels toxic to plants © 2012 John Wiley & Sons, Inc. All rights reserved.

Soil Problems- Desertification Degradation of once-fertile rangeland, agricultural land, or tropical dry forest into nonproductive desert © 2012 John Wiley & Sons, Inc. All rights reserved.

Soil Conservation Conservation Tillage Residues from previous year’s crops are left in place to prevent soil erosion Crop Rotation Planting a series of different crops in the same field over a period of years © 2012 John Wiley & Sons, Inc. All rights reserved.

Soil Conservation Strip Cropping Terracing Contour Plowing Plowing around hill instead of up-down Strip Cropping Alternating strips of different crops along natural contours Terracing Creating terraces on steep slopes to prevent erosion Terracing © 2012 John Wiley & Sons, Inc. All rights reserved.

Preserving Soil Fertility Organic fertilizers Animal manure, crop residue, bone meal and compost Nutrient available to plants only as material decomposes Inorganic fertilizers Manufactured from chemical compounds Soluble Fast acting, short lasting Mobile- easily leach and pollute groundwater

Best way to do this is shelterbelts Soil Reclamation Two steps Stabilize land to prevent further erosion Restoring soil to former fertility Best way to do this is shelterbelts Row of trees planted to reduce wind erosion of soil

Soil Conservation Policies in US Soil Conservation Act 1935 Authorized formation of Soil Conservation Service, now called Natural Resource Conservation Service (NRCS) Assess soil damage and develop policies to improve soil Food Security Act (Farm Bill) 1985 Farmers with highly erodible soil had to change their farming practices Instituted Conservation Reserve Program Pays farmers to stop farming highly erodible land © 2012 John Wiley & Sons, Inc. All rights reserved.