| 我国沙漠地区潜水氟的分布、成因及演变 |
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| 引用本文： | 刘亚传,刘冬梅,张振壁,李文智. 我国沙漠地区潜水氟的分布、成因及演变[J]. 地理研究, 1988, 7(2): 28-40. DOI: 10.11821/yj1988020004 |
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| 作者姓名： | 刘亚传 刘冬梅 张振壁 李文智 |
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| 作者单位： | 1. 中国科学院兰州沙漠研究所;2. 甘肃省张掖地区卫生防疫站 |
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| 摘 要： | 本文探讨了沙漠地区潜水中氟的分布、成因、迁移及演变,研究得出不同于砾漠和粘漠,氟是沙漠潜水的标型元素,是沙漠形成和上地沙化的产物。
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| 关 键 词： | 潜水含氟 中国沙漠地区 |
| 收稿时间： | 1985-09-03 |
| 修稿时间： | 1986-03-05 |
A PRELIMINARY STUDY OF DISTRIBUTION, FORMATION AND EVOLUTION OF FLUORINE IN THE PHREATIC WATER OF DESERT AREAS OF CHINA |
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| Liu Yachuan Liu DongMei. A PRELIMINARY STUDY OF DISTRIBUTION, FORMATION AND EVOLUTION OF FLUORINE IN THE PHREATIC WATER OF DESERT AREAS OF CHINA[J]. Geographical Research, 1988, 7(2): 28-40. DOI: 10.11821/yj1988020004 |
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| Authors: | Liu Yachuan Liu DongMei |
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| Affiliation: | 1. Institute of Desert, Acadcmia Sinica, Lanzhou;2. Sanitation and anti-epidemic station, Zhangye area Gansu |
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| Abstract: | Fluorine-rich water is widely distributed over China's sand deserts. For example, the sampling sites where ground water contains more than 1 mg/L of fluorine almost account for 77 percent of the total sampling sites in Ba-dain Jaran Desert and 80 percent in Tengger Desert. The maximum fluorine measured reaches 24 mg/L in Taklimakan Desert, 27.5 mg/L in Tengger Desert, 32 mg/L in Kurbantunggut Desert, 32.5 mg/L in Mu Us sandy land 192 mg/L in Badain Jaran Desert. |
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| Keywords: | fluorine in the phreatic water China's sand deserts |
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