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Global Trend: Where Did All the Farms Go? Poor farming practices = loss of soils and farmland  Erosion  Salinization Development in United States = loss.

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Presentation on theme: "Global Trend: Where Did All the Farms Go? Poor farming practices = loss of soils and farmland  Erosion  Salinization Development in United States = loss."— Presentation transcript:

1 Global Trend: Where Did All the Farms Go? Poor farming practices = loss of soils and farmland  Erosion  Salinization Development in United States = loss of 1.4 million acres of farmland per year

2 Why a Study of Soil Is Important 90% of the world’s food comes from land- based agriculture. Maintenance of soil – key to sustainable civilizations. Foundation of terrestrial life.

3 Topsoil Formation

4 Soil Profile

5 Soil Texture Soil texture refers to the percentage of each type of mineral particle found in the soil. Loam soil – good for agriculture  40% sand, 40% silt, and 20% clay.

6 Soil Texture Particle size  Large  Sand > Silt > Clay  Small  Size of particles determines… Water and nutrient holding capacity Infiltration Aeration

7 Soil Texture and Properties TextureWater Infiltration Water- holding Capacity Nutrient- holding Capacity Aeration SandGoodPoor Good SiltMedium ClayPoorGood Poor LoamMedium

8 Plant–Soil–Water Relationships

9 Water Transport by Transpiration

10 Soil pH and Salinity Plants require near neutral pH and low salt Causes of pH and salinity changes  Erosion  Salt water intrusion  Fertilizer runoff  Salination

11 Productive Soil Good supply of nutrients and nutrient- holding capacity Infiltration, good water-holding capacity, resists evaporative water loss Porous structure for aeration Near-neutral pH Low salt content

12 Humus Partly decomposed organic matter High capacity for holding water and nutrients Typically found in O horizon

13 Formation of Humus

14 The Soil Community

15 The Results of Removal of Topsoil: Sand and Gravel

16 Erosion Wind and Water  Deforestation  Use of inorganic fertilizers  Over irrigation  Over tilling  Over grazing

17 Dry lands and Desertification: Formation of Desert Pavement

18 Causes of Soil Degradation

19 Overcultivation Tilling soil exposes top soil to erosion  Alternative No-till/Low-till farming  Top soil remains intact  Dead weeds or previous crop allowed to form humus

20 Fertilizer  Inorganic Large yields but…  Humus forming organic matter removed during harvesting  Mineralization and soil degradation occurs  Organic Lower yields but…  Helps support biotic community of detritus  Decreases water loss and improves aeration  Improves LONG TERM use of agricultural land

21 Salinization: Results

22 Salinization Occurs in drylands  Area is irrigated  Water is allowed to evaporate  Salts remain Runoff can be devastating to nearby fertile lands A form of desertification, since land is rendered useless

23 Conserving the Soil Cover the soil Minimal or zero tillage Mulch for nutrients Maximize biomass production Maximize biodiversity


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