Arid
DOI10.1016/S0899-5362(97)00021-3
The groundwater geochemistry in a semi-arid, fractured crystalline basement area of Dodoma, Tanzania
Nkotagu, H
通讯作者Nkotagu, H
来源期刊JOURNAL OF AFRICAN EARTH SCIENCES
ISSN0899-5362
出版年1996
卷号23期号:4页码:593-605
英文摘要

The chemical character of groundwater is generated through processes including the leaching of surficial and near-surface soil salts, cation exchange and mineral dissolution of, In this case, mainly amphiboles and sodic plagioclase. Molar ratios, thermodynamic analysis using a NETPATH geochemical model and standard Piper (sic) and Gibbs diagrams have been used to establish these geochemical processes. Though the groundwater is dominantly of NaCl type, it is apparently suitable for general irrigation purposes. (C) 1997 Elsevier Science Ltd.


类型Article
语种英语
收录类别SCI-E
WOS记录号WOS:A1996WR43000007
WOS关键词WATER ; CHEMISTRY
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/132910
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GB/T 7714
Nkotagu, H. The groundwater geochemistry in a semi-arid, fractured crystalline basement area of Dodoma, Tanzania[J],1996,23(4):593-605.
APA Nkotagu, H.(1996).The groundwater geochemistry in a semi-arid, fractured crystalline basement area of Dodoma, Tanzania.JOURNAL OF AFRICAN EARTH SCIENCES,23(4),593-605.
MLA Nkotagu, H."The groundwater geochemistry in a semi-arid, fractured crystalline basement area of Dodoma, Tanzania".JOURNAL OF AFRICAN EARTH SCIENCES 23.4(1996):593-605.
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