Agronomy

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Last updated 10:47 PM on 4/19/26
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7 Terms

1
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describe the soil classifications in the Northern region

Vertosols - clay >35%, cracks, slickensides

Sodosols - strong texture-contrast (2 completely different soil textures on top of one another), sodic (high sodium) B horizon. When it rains, these soils erode fast. Can cause water logging. 

Chromosols - strong texture contrast, pH > 5.5 in B horizon. Not sodic. 

Kandosols - Lacking strong texture contrast, massive B horizon. Low nutrient content. 

2
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Describe the soil classifications in the Southern region

Sodosols - strong texture-contrast (2 completely different soil textures on top of one another), sodic (high sodium) B horizon. When it rains, these soils erode fast. Can cause water logging.

Chromosols - strong texture contrast, pH > 5.5 in B horizon. Not sodic. 

Calcarosols - lacking strong texture-contrast, high in calcium

3
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Describe the soil classifications in the Western region

Tenosols - does not retain moisture well. 

Sodosols - strong texture-contrast (2 completely different soil textures on top of one another), sodic (high sodium) B horizon. When it rains, these soils erode fast. Can cause water logging.

Calcarosols - lacking strong texture-contrast, high in calcium

Kandosols - Lacking strong texture contrast, massive B horizon. Low nutrient content. 

4
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What is PAW? What can it be affected by?

Plant Available Water. Can be affected by rainfall, infiltration, drainage, runoff, evaporation, transpiration, and soil-available water capacity

5
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What is PAWC? What is needed to calculate it?

Plant available water capacity. You need

  1. DUL (= Drained Upper Limit - field capacity; amount of water a soil can hold against gravity)

  2. CLL (= Crop Lower Limit - permanent wilting point; amount of water remaining in a soil after a specific crop has extracted all available water) OR LL15 (= Lower Limit 15 - Water remaining in soil at 15 bar pressure.)

  3. Bulk density (g/cm^3) (the mass of dry soil per unit volume, including both solids and pore space.)

6
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What is fallow efficiency and how can it be affected?

Fallow efficiency is how much water is able to be retained in the soil profile within a fallow. It can be affected by infiltration, runoff, erosion, evaporation. 

Some crops like wheat leave residues that are good for fallow efficiency. Weeds can make a big difference in fallow management. 

7
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How do you calculate fallow efficiency?

2 soil samples, one at start of fallow and one at end. Know water inputs into the system during the fallow (rainfall). 

Fallow efficiency = change in plant-available water during fallow / rainfall during fallow