The Buffering Capacity of a soil is proportional to a. Percent base saturation b. Cation Exchange capacity c. The level of acidity d. Mineral solubility   pH levels below 3.0 may be associated with a. High bacterial populations in soils b. High rates of organic matter decomposition c. Aluminum toxicity d. Iron toxicity   The lime requirement of soils a. Increases with decreasing organic matter content b. Increases with increasing CEC c. Increases with base saturation percentage d. Mineral solubility

Structural Analysis
6th Edition
ISBN:9781337630931
Author:KASSIMALI, Aslam.
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Chapter2: Loads On Structures
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The Buffering Capacity of a soil is proportional to

a. Percent base saturation

b. Cation Exchange capacity

c. The level of acidity

d. Mineral solubility

 

pH levels below 3.0 may be associated with

a. High bacterial populations in soils

b. High rates of organic matter decomposition

c. Aluminum toxicity

d. Iron toxicity

 

The lime requirement of soils

a. Increases with decreasing organic matter content

b. Increases with increasing CEC

c. Increases with base saturation percentage

d. Mineral solubility

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