Soil Infiltration Unit: Soil Science.

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Presentation transcript:

Soil Infiltration Unit: Soil Science

Objectives Define: infiltration rate, restrictive layers, soil aggregates, soil porosity, steady-state infiltration List and describe inherent factors that affect soil infiltration Describe soil infiltration management practices Explain soil infiltration problems and how they affect soil function Measure soil infiltration and interpret results

Definitions Infiltration Rate: measurement of how fast water enters soil, (inches per hour); recorded in minutes for each inch of water applied to the soil surface Restrictive Layers: compacted layers and layers of dense clay, bedrock or other restrictive features than limit infiltration below the surface of the soil Soil Aggregates: soil particles held together by organic matter and related substances Soil Porosity: amount of pore space in the soil Steady-State Infiltration: the infiltration rate is steady and does not increase or decrease as more water is added. It typically occurs when the soil is nearly saturated

Managing Soil Infiltration Soil crusting Soils dry out, causing pore space to increase as cracks form Water fills the cracks quickly, wetting the soil As water becomes wetter, the infiltration rate slows because of restrictive layers Compaction Results from equipment and tillage practices Minimizes pore space Slows water movement through the soil profile

Managing Soil Infiltration Soil Organic Matter Bare soil is more drastically affected by erosion by rain drops Dislodged soil particles fill in and block surface pores OM binds soil particles together, forming aggregates; aggregates increase porosity and infiltration rates OM encourages a living environment for organisms such as earthworms; organisms move about in the soil and increase pore space Improve Infiltration Rates by Avoiding soil disturbance and equipment operation when soils are wet Using designated field roads or rows for equipment traffic Reducing the number of trips across the space Sub-soiling to break up existing compacted layers Using continuous no-till Adding solid manure or other organic materials Using rotations with high-residue crops, such as corn and small grain and perennial crops, such as grass or alfalfa Planting cover crops and green manure crops Farming on the contour Establishing terraces to minimize run-off and erosion