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Liming (Soil)
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UEV7BGMLJO3
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Geliefert zwischen Fr., 20.02.2026 und Mo., 23.02.2026
Details
High Quality Content by WIKIPEDIA articles! High Quality Content by WIKIPEDIA articles! Liming is the application of calcium and magnesium rich materials to soil in various forms, including marl, chalk, limestone, or hydrated lime. This neutralises soil acidity and increases activity of soil bacteria. However, oversupply may result in harm to plant life. Lime is a basic chemical, the effect of it makes the soil more basic thus making acidic soils neutral. The degree to which a given amount of lime per unit of soil volume will increase soil pH depends on the cation exchange capacity (CEC). Soils with low CEC will show a more marked pH increase than soils with high CEC. But the low-CEC soils will witness more rapid leaching of the added bases, and so will see a quicker return to original acidity unless additional liming is done. Over-liming is most likely to occur on soil which has low CEC, such as sand which is deficient in buffering agents such as organic matter and clay.
Weitere Informationen
- Allgemeine Informationen
- GTIN 09786131447600
- Editor Lambert M. Surhone, Mariam T. Tennoe, Susan F. Henssonow
- Genre Geowissenschaften
- Anzahl Seiten 72
- EAN 9786131447600
- Titel Liming (Soil)
- Herausgeber Betascript Publishing
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