| 青藏高原高硼卤水的水化学特征及其成因 |
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| 引用本文： | 吴俐俐,马文展,唐渊.青藏高原高硼卤水的水化学特征及其成因[J].地理研究,1984,3(4):1-11. |
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| 作者姓名： | 吴俐俐 马文展 唐渊 |
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| 作者单位： | 1. 武汉化工学院;2. 中国科学院盐湖研究所 |
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| 摘 要： | 本文就青藏高原高硼卤水的分布、水化学特征、硼与共生元素的相关性及硼矿沉积的某些规律作了阐述,进而探讨了高硼卤水的成因。
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| 收稿时间： | 1982-06-30 |
| 修稿时间： | 1984-04-24 |
ON THE WATER-CHEMICAL PROPERTIES AND FORMATIVE CONDITIONS OF HIGH-BORON BRINE IN QINGHAI-XIZANG PLATEAU |
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| Wu Lili,Ma Wenzhang,Tang Yuan.ON THE WATER-CHEMICAL PROPERTIES AND FORMATIVE CONDITIONS OF HIGH-BORON BRINE IN QINGHAI-XIZANG PLATEAU[J].Geographical Research,1984,3(4):1-11. |
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| Authors: | Wu Lili Ma Wenzhang Tang Yuan |
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| Institution: | 1. Wu Han Institute of Chemical Engineering;2. Institute of Saline Lakes, Academia Sinica |
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| Abstract: | This paper deals with distributive regularity of brine with high-boron content (B2O3 is higher than 400 mg/1). This paper is based on the data of more than 90 saline lakes obtained from Qinghai-Xizang field obtervations and laboratory studies.The component,water-chemical properties and formative con-ditiont of the brine are also discussed in this paper. It has been discovered that boron not only coexists with Li+,K+,Mg2+,but also is well interrelated to them; but then, the content of boron is inversely proportionate to that of magnestium in carbonate-type's brine. The reason why there is difference of water-chemical components between the brine of Chaidamu Basin and Northern-Xizang is explained here. We also inquired into the material source of the brine rich in B3+, Li+, K+, R+, Cs+, F+, As3+, and the contributing factors of high-boron brine. |
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