[1]李春晖,杨志峰.黄河流域地表水资源可再生性模糊综合评价[J].水土保持研究,2005,12(01):182-185.
　LI Chun-hui,YANG Zhi-feng.Fuzzy Comprehensive Assessment of the Surface Water Resources Renewability in the Yellow River Basin[J].Research of Soil and Water Conservation,2005,12(01):182-185.
点击复制

黄河流域地表水资源可再生性模糊综合评价

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 12 期数: 2005年01期 页码: 182-185 栏目: 出版日期: 1900-01-01
Title:
Fuzzy Comprehensive Assessment of the Surface Water Resources Renewability in the Yellow River Basin
作者:
李春晖, 杨志峰
北京师范大学环境学院水沙科学教育部重点实验室水环境模拟国家重点实验室, 北京, 100875
Author(s):
LI Chun-hui, YANG Zhi-feng
Key Laboratory for Water and Sediment Sciences, Ministry of Education, State Key Laboratory of Water Environment Simulation, School of Environment, Beijing Normal University, Beijing 100875, China
关键词:
地表水资源; 可再生性; 综合评价; 黄河流域
Keywords:
surface water resources; renewability; comprehensive assessment; the Yellow River basin
分类号:
TV213
摘要:
水资源具有可再生性。从水资源自然再生和社会再生角度，选取18个指标建立黄河流域地表水资源可再生性评价指标体系，利用二层模糊综合评价法对整个黄河流域及其15个分区地表水资源可再生性进行综合评价，结果表明龙羊峡以上、湟水流域、洮河流域和渭河流域可再生性较强，北洛河流域、泾河流域可再生性最弱。
Abstract:
Water resources has renewability.From the views of natural renewal and social renewal of water resources,an assessment index system of surface water resources renewability in the Yellow River basin was built which includes 18 indices and 3 layers.Then the surface water resources renewability assessments in 15 subregions of the Yellow River basin were finished with fuzzy comprehensive assessment method,and the results show that the sub-regions of upper Longyangxia Gorge,the Huangshui basin,the Taohe basin and the Weihe basin had the strongest renewability.However,the Beiluohe basin and the Jinghe basin had the weakest renewability.

参考文献/References:

[1] Sandra L Postel. Human appropriation of renewable fresh water[J].Science, 1996, 271(9): 785-788.
[2] 沈珍瑶, 杨志峰, 刘昌明.水资源的天然可再生能力及其与更新速率之间的关系[J].地理科学, 2002, 22(2):162-165.
[3] 杨志峰, 沈珍瑶, 夏星辉, 等.水资源可再生性基本理论及其在黄河流域的应用[J].中国基础科学, 2002, (5):4-7.
[4] 曾维华, 杨志峰, 蒋勇.水资源可再生能力刍议[J].水科学进展, 2001, 12(2):276-279.
[5] 夏军, 王中根, 刘昌明.黄河水资源可再生性问题及量化研究[J].地理学报, 2003, 58(4):534-541.
[6] 沈珍瑶, 杨志峰. 黄河流域水资源可再生性评价指标体系与评价方法[J].自然资源学报, 2002, 17(2):188-197.
[7] 沈珍瑶, 杨志峰.水资源的可再生性与可持续利用[J].中国人口资源与环境, 2002, 12(5):77-78.
[8] 左其亭, 吴泽宁.基于风险的黄河流域水资源可再生性评价指标[J].人民黄河, 2003, 25(1):38-40.
[9] 王莲芬.层次分析法引论(第一版)[M].北京:中国人民大学出版社, 1990.
[10] 郑成德.流域水资源丰富度评价的模糊综合评判[J].地理学与国土研究, 1998, 14(1):42-46.

相似文献/References:

[1]景可,郑粉莉.黄土高原水土保持对地表水资源的影响[J].水土保持研究,2004,11(04):11.
　JING Ke,ZHENG Fen-li.Effects of Soil and Water Conservation on Surface Water Resource on the Loess Plateau[J].Research of Soil and Water Conservation,2004,11(01):11.

备注/Memo

收稿日期:2004-4-24。
基金项目:国家重点基础研究规划项目（G1999043605）；中国博士后科学基金资助（No.2004036209）
作者简介:李春晖（1976- ），男，安徽阜阳人，博士，主要从事水资源水环境评价研究.

更新日期/Last Update: 1900-01-01