Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/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
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ISSN | 0899-5362 |
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 |
推荐引用方式 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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