1. 延边大学理学院地理系, 吉林延吉,133000
2. 长白山生物资源与功能分子教育部重点实验室, 吉林延吉,133000
纸质出版:2015
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徐万玲, 朱卫红, 张健, 等. 基于洛伦兹曲线的图们江干流区间径流分布不均匀性分析[J]. 水土保持通报, 2015,35(1):128-132.
XU Wanling, ZHU Weihong, ZHANG Jian, et al. Analysis on Temporal Inhomogenenity of Runoff in Tumen River Mainstream Based on Lorenz Curve[J]. Bulletin of Soiland Water Conservation, 2015, 35(1): 128-132.
徐万玲, 朱卫红, 张健, 等. 基于洛伦兹曲线的图们江干流区间径流分布不均匀性分析[J]. 水土保持通报, 2015,35(1):128-132. DOI: 10.13961/j.cnki.stbctb.2015.01.024.
XU Wanling, ZHU Weihong, ZHANG Jian, et al. Analysis on Temporal Inhomogenenity of Runoff in Tumen River Mainstream Based on Lorenz Curve[J]. Bulletin of Soiland Water Conservation, 2015, 35(1): 128-132. DOI: 10.13961/j.cnki.stbctb.2015.01.024.
[目的] 为水土流失、旱涝灾害等的成因分析提供科学依据。[方法] 采用构建的基尼系数径流分布不均匀性模型
对图们江干流区间南坪、开山屯、河东及圈河站1959-2011年的(年)径流量、(月径流年内分配)基尼系数和(月径流年内分配)洛伦兹不对称系数的系列进行统计分析
应用Mann-Kendall方法进行趋势分析与检验。[结果] 4个水文站的年径流量均呈下降趋势。南坪和开山屯站的基尼系数呈上升趋势
河东和圈河站呈下降趋势;4个水文站点的(月径流年内分配)洛伦兹不对称系数均呈上升趋势。4个水文站在1961
1965和1979年洛伦兹不对称系数均波动较大且大于1。这主要由径流量大的月份引起的
另外
同期也是历史上水旱灾害发生的年份。[结论] 洛伦兹曲线可以以一种新视角量化评价径流分配的时间不均匀性及其成因。
[Objective] To provide a scientific basis for analyzing the causes of soil erosion
droughts and floods.[Methods] After building the Gini coefficient runoff uneven distribution model
annual runoff
Gini coefficient and Lorenz asymmetry coefficient(annual distribution of monthly runoff) in four hydrometric stations(Nanping
Kaishantun
Hedong and Quanhe) from 1959 to 2011 were statistically analyzed. Mann-Kendall method was employed to do trend analysis and test in annual runoff.[Results] The annual runoffs in the four hydrometric stations showed a decreasing trend during the past years. The Gini coefficient in Nanping and Kaishantun showed an increase tendency
while it showed a decrease trend in Hedong and Quanhe station. The Lorenz asymmetry coefficient in the four hydrological stations showed an upward trend
and the values were greater than 1 for the four stations in 1961
1965 and 1979
which was mainly caused by the months with large runoff volume
it is also period when drought and flood happened in history.[Conclusion] The Lorenz curve can be used to quantify and evaluate the temporal variation of runoff and its influential factor in a new perspective.
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陈军伟,孔祥斌,张凤荣,等.基于空间洛伦茨曲线的北京山区土地利用结构变化[J].中国农业大学学报,2006,11(4):71-74.
史婉丽,杨勤科,李小芳,等.基于洛伦茨曲线的陕北黄土高原降雨分布不均匀性分析[J].干旱地区农业研究,2012,30(4):172-177.
魏凤英.现代气候统计诊断与预测术技[M].北京:气象出版社,2007.
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