Influence of Physicochemical Properties of Soil on pH of Pore Water

pH of soil pore water is the important factor in heavy metal retention and migration in soil. Buffer capacity of clays such as kaolinite, hectorite, attapulgite, and Na-bentonite were determined. The magnitude of buffer capacity is in the order of hectorite>Na-bentonite>attapulgite>kaolinit...

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Veröffentlicht in:	KSCE Journal of Civil Engineering 2000-12, Vol.4 (4), p.233-237
1. Verfasser:	Kim, Geonha
Format:	Artikel
Sprache:	eng
Schlagworte:	Algorithms Bentonite Buffers Carbonates Chemical interactions Electric double layer Functional groups Heavy metals Kaolinite Metals pH effects Physicochemical processes Physicochemical properties Pore water Soil Soil chemistry Soil pH Soil properties Soil water Soils Studies
Online-Zugang:	Volltext
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