| 同位素^131I测西台吉乃尔湖矿区含水层地质参数 |
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| 引用本文： | 杨海镇,马海州,高东林.同位素^131I测西台吉乃尔湖矿区含水层地质参数[J].盐湖研究,2008,16(1):8-11. |
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| 作者姓名： | 杨海镇 马海州 高东林 |
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| 作者单位： | [1]中国科学院青海盐湖研究所,青海西宁810008 [2]青海师范大学地学院,青海西宁810008 [3]中国科学院研究生院,北京100049 |
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| 摘 要： | 盐湖区的水文地质参数特性与淡水区迥然不同。同位素示踪法可以利用西台盐湖区已有的长现井，机动灵活的随时监测含水层水文地质参数；由于介质的特殊性以及卤水性质的垂直差异性，造成水文地质参数的时空可变性；测试结果表明，对于完整井以及深的非完整井，该方法切实有效，但对于很浅的非完整井，测试结果具有很大的随机性。最后，根据测试结果以及有关的水文地质资料，把研究区分成7个渗透系数分区。
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| 关 键 词： | 放射性同位素 水文地质参数 西台吉乃尔 |
| 文章编号： | 1008-858X（2008）01-0008-04 |
| 收稿时间： | 2007-04-16 |
| 修稿时间： | 2007-12-05 |
Measurement of the Hydrogeological Parameters in the West Taijinnr Lake Mining Area by Using Radioisotope ^131I |
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| YANG Hai-zhen,MA Hai-zhou,GA Dong-lin.Measurement of the Hydrogeological Parameters in the West Taijinnr Lake Mining Area by Using Radioisotope ^131I[J].Journal of Salt Lake Research,2008,16(1):8-11. |
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| Authors: | YANG Hai-zhen MA Hai-zhou GA Dong-lin |
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| Institution: | YANG Hai-zhen, MA Hai-zhou, GA0 Dong-lin |
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| Abstract: | The hydrogeologieal parameter characteristics in salt-lake area are different apparently from that in fresh-water area. The isotope tracing method can be used flexibly to measure the hydrogeologieal parameters of the aquifer at any time with the help of the existed long observing wells in the West Taijinar lake area. As a result of the particularity of the medium and the vertical difference of the brine property, the space-time variability of the hydrogeologieal parameters occurs. The testing results showed that the method was practical and effective for fully penetrated and deep partially penetrated wells, while there existed big randomness for shallow partially penetrated wells. The studying area was divided into 7 permeability coefficient divisions based upon the testing results and the relevant hydrogeological parameter data. |
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| Keywords: | Radioisotope Hydrogeological parameters West Taijinar |
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