[1]韩贻强,胡晓敏.基于集中期的大沽夹河年内水文特征分析[J].水土保持研究,2009,16(04):220-224.
　HAN Yi-qiang,HU Xiao-min.Analysis on Runoff Variation Characteristics in the Typical River Basin of Hilly Area in Shandong Peninsula[J].Research of Soil and Water Conservation,2009,16(04):220-224.
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基于集中期的大沽夹河年内水文特征分析

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 16 期数: 2009年04期 页码: 220-224 栏目: 出版日期: 2009-08-20
Title:
Analysis on Runoff Variation Characteristics in the Typical River Basin of Hilly Area in Shandong Peninsula
作者:
韩贻强1, 胡晓敏2
1. 滨州学院 地理旅游系, 山东 滨州 256603;
2. 东营市东营区辛店街道办事处, 山东 东营 257085
Author(s):
HAN Yi-qiang1, HU Xiao-min2
1. Department of Geography and Tourism, Binzhou Universty, Binzhou, Shandong 256603, China;
2. Subdistrict office, Dongying District, Dongying, Shandong 257085, China
关键词:
径流; 变差系数; 大沽夹河; 山东半岛
Keywords:
runoff; variation coefficient; Dagujia River; Shandong Peninsula
分类号:
P343.1
摘要:
选取无过境河流的山东半岛丘陵地区的大沽夹河流域作为研究对象，采用滑动平均、集中期、集中度等方法，在年际、季节、年代及年内各月等时间尺度上，对流域径流的特征进行了较为全面的分析研究。结果显示：大沽夹河1966-2004年间的径流量年际变化呈波浪式减少趋势，没有规律性，波动性较大，变差系数值为0.788。季节上，径流量主要集中在夏秋季节，断流主要出现在春冬季节，夏秋季节断流较少。各年代段的年内平均径流量均集中在6-10月，11月至次年5月径流量很少，最高径流量均为8月。
Abstract:
Taking Dagujia River basin, located in Jiaodong hilly area, as a case study, the characteristic of runoff was analyzed by using moving-average and Cv (Variation Coefficient) methods. Results showed that the annual runoff decreased obviously from 1966 to 2004.It was changing from 0.007×108 m3 to 8.93×108 m3, and the Cv is 0.788.Seasonal runoff centralized in summer and autumn. Cutoff mainly occurred in spring and winter. The Cv of seasons are all larger. The monthly runoff distribution was very uneventful, it mainly concentrated from June to October, and the largest runoff occurred in August. The decadal analysis of Cd and D showed that the Cd had been increasing from 1966 to 2004, and the maximum D were all in August. It is important to the design of local sustainable development and provide the useful database for water resource planning.

参考文献/References:

[1] 孙凡,邱方,孟令彬.重庆市地区可持续发展的水资源问题探讨[J].西南农业大学学报:自然科学版,2004,26(4):501-505.
[2] 牟海省.我国水资源持续开发的零增长模式初探[J].地理研究,1995,14(1):80-84.
[3] 吴凯,许越先.黄淮海平原水资源开发的环境效应及其调控对策[J].地理学报,1997,52(2):114-122.
[4] Gao Ge,Huang Chaoying.Climate change and its impact on water resources in north China [J].Advances in Atmospheric Sciences,2001,18(5):718-732.
[5] Mimikou M A,Baltas E,Varanou E,et al.Regional impacts of climate change on water resources quantity and quality indicators[J].Journal of hydrology,2000,234: 95-109.
[6] Wolfgang L,Pierre S,Ludovic C.Evaluating the impact of the recent temperature increase on the hydrology of Ted River (southern France)[J].Journal of hydrology,2004,289: 204-221.
[7] 朱九龙,陶晓燕,王世军,等.淮河流域水资源价值测算与分析[J].自然资源学报,2005,20(1):126-131.
[8] 郑红星,刘昌明.黄河流域水资源演化模式分析[J].地理学报,2004,59(2):267-273.
[9] 郭敬辉.川西滇北地区河流分类的初步研究[J].地理学报,1965,31(3):212-225.
[10] 李世泰,隋干城.烟台市经济持续发展的水资源问题与对策[J].烟台师范学院学报:自然科学版,2000,16(4):297-301.
[11] 冯光扬.水文年内不均匀系数的探讨[J].山地研究,1991,9(1):27-32.
[12] 杨远东.河川径流年内分配的计算方法[J].地理学报,1984,39(2):218-227.
[13] 蒋艳,周成虎,程维明.阿克苏河流域径流补给及径流变化特征分析[J].自然资源学报,2005,20(1):27-34.

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　LU Guang-hui.Function and Application of Runoff Restraint Technique of Lowering Impact[J].Research of Soil and Water Conservation,2001,8(04):91.

备注/Memo

收稿日期:2009-01-04。
基金项目:山东省教育厅科研发展计划项目（j08we67）
作者简介:韩贻强（1966-），男，山东滨州人，讲师，主要从事地理科学研究工作。E-mail：bzdlxhyq@163.com

更新日期/Last Update: 1900-01-01