A Study on Fluoride Sorption by Montmorillonite and Kaolinite
作者： Meetu Agarwal , Kavita Rai , Rohit Shrivastav , Sahab Dass , None
关键词:
摘要: Fluoride (F) sorption by acidified montmorillonite, montmorillonite and kaolinite has been investigated as a function of period agitation, pH, initial fluoride concentration clay amount. In case kaolinite, F is insignificant at pH > 7, while it maximum 4. Enhanced noted 4, are potent sink for in montmorillonite. Soluble fluoro-complexes also detected ≈ Saturation indices (SIs) over the studied range (2–10) computed.
springer.com
harvard.edu
sci-hub.se 参考文章(22)
Garrison Sposito, The surface chemistry of soils ,(1984)
Willard Lyman Lindsay, Chemical equilibria in soils ,(1979)
Bernard M. Wagner, Health effects of ingested fluoride National Academy Press. ,(1993)
N. J. Barrow, J. Goldshmid, Makhon le-ḳarḳaʿ u-mayim, B. Bar-Yosef, Inorganic Contaminants in the Vadose Zone ,(1989)
Andrew Eaton, A.E. Greenberg, Lenore S. Clesceri, Standard methods for the examination of water and wastewater Published in <b>1998</b> in Washington DC) by American public health association. ,(1992)
Régis R Simard, Pierre Lafrance, Fluoride sorption and desorption indices in Quebec soils Communications in Soil Science and Plant Analysis. ,vol. 27, pp. 853- 866 ,(1996) , 10.1080/00103629609369602
A. Violante, P. Violante, Interactions between H-bentonite and aluminous chlorite-like complexes Geoderma. ,vol. 21, pp. 147- 159 ,(1978) , 10.1016/0016-7061(78)90023-X
F W Gilcreas, Standard methods for the examination of water and waste water. American Journal of Public Health and the Nations Health. ,vol. 56, pp. 387- 388 ,(1966) , 10.2105/AJPH.56.3.387
K. W. PERROTT, B. F. L. SMITH, R. H. E. INKSON, THE REACTION OF FLUORIDE WITH SOILS AND SOIL MINERALS European Journal of Soil Science. ,vol. 27, pp. 58- 67 ,(1976) , 10.1111/J.1365-2389.1976.TB01975.X
S. R. DICKMAN, R. H. BRAY, Replacement of Adsorbed Phosphate from Kaolinite by Fluoride Soil Science. ,vol. 52, pp. 263- 274 ,(1941) , 10.1097/00010694-194110000-00002