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2.loWer infiltration, greater percolation, less plant available water, lower com

ID: 113435 • Letter: 2

Question

2.loWer infiltration, greater percolation, less plant available water, lower compaction, lower runoff Soil texture influences the quantity of plant available H2O by.... circle best answer). a. less pore space and particle surface area reduces plant available H:0 in sill compared to sand b. more pore space and particle surface area reduces plant available H:O in silt compared to clay c. greater infiltration in a sand increases plant available H2O compared to a clay d. greater runoff in a clay reduces plant available H2O compared to a sand e. less pore space and particle surface area reduces plant available H2O in sand compared to silt 7. Circle best answer Soil texture represents the % by weight of sand, clay, and silt Most fresh H20 on the planet is groundwater......................... DES represents the Daily Evaporation from Soil...... Chronic malnutrition affects about 0.8 billion people worldwide.... Soil structure cannot influence how water moves through soil. Houses with a basement are recommended in regions with a ... Stomates open to allow H:O to enter the leaf Crop rotation with deep rooted crops can help reduce effects of soil compactio on plani growth Aggregation in soils is detrimental to plant growth... A spring is groundwater that resupplies and maintains the water table Soils are used as a filter to detoxify wastes A groundwater aquifer represents a zone of porous rock materials saturated with H20 Furrow irrigation is best suited for a field with a steep slope and sandy soil texture . Irrigation efficiency has decreased with adoption of low pressure center pivot systems.... To meet future world food demand, crop yield/acre must increase on fewer crop acres T What property of H20 molecules causes adhesion and cohesion? Two h+ ions bond with I oxgen-2 ion 8.

Explanation / Answer

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