| 熵理论在韩城矿区流域地貌研究上的应用 |
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| 引用本文： | 毛明陆,阎嘉祺.熵理论在韩城矿区流域地貌研究上的应用[J].西安科技大学学报,1991(3). |
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| 作者姓名： | 毛明陆 阎嘉祺 |
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| 作者单位： | 陕西煤田地勘公司，西安矿业学院 |
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| 摘 要： | 本文选择了韩城矿区的三个流域——白矾河、寺庄河及清水河,分别代表矿区的北部、中部及南部,在用斯特拉勒积分研究矿区流域地貌发育阶段的基础上,根据熵理论,分别研究了这三个流域地貌系统信息熵,进而进行了矿区区域稳定性评价。结论是现今矿区地貌发育处于壮年期、矿区区域稳定性东北部比西南部差。
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| 关 键 词： | 信息熵 地貌系统 流域 新构造运动 |
APPLICATION OF ENTROPY THEORY TO RESEARCH OF STREAM BASIN IN HANCHENG MINING FIEND |
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| Mao Minglu Yan Jiagi.APPLICATION OF ENTROPY THEORY TO RESEARCH OF STREAM BASIN IN HANCHENG MINING FIEND[J].JOurnal of XI’an University of Science and Technology,1991(3). |
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| Authors: | Mao Minglu Yan Jiagi |
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| Institution: | Mao Minglu Yan Jiagi |
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| Abstract: | Three stream basins, Baifan, Sizhuang and Qingshui rivers, representing the northern,middle and southern parts of Hancheng mining field respectively have been selected. The information entropy of the three stream basins is studied on the basis of studying the geomorphic development stages by using Strahlers lntegral and according the entropy theory, and then, the evalution of region stability is made. The main conclusion is that the geomorphic development is in its prime period at present and the stability at northeastern is worse than that at southwestern part. |
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| Keywords: | information entropy geomorphic system stream basin neotectonism |
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