地理研究 ›› 1984, Vol. 3 ›› Issue (4): 1-11.doi: 10.11821/yj1984040001
• 论文 •
吴俐俐1, 马文展1, 唐渊2
Wu Lili1, Ma Wenzhang1, Tang Yuan2
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.
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.
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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