地理科学进展 ›› 2014, Vol. 33 ›› Issue (1): 65-75.doi: 10.11820/dlkxjz.2014.01.008
• 2013年全国地貌与第四纪学术研讨会专栏 • 上一篇 下一篇
王彦君1,2, 王随继1, 苏腾1,2
收稿日期:
2013-10-01
修回日期:
2013-12-01
出版日期:
2014-01-25
发布日期:
2014-01-22
通讯作者:
王随继(1966-),甘肃静宁人,副研究员,主要从事河流地貌学与河流沉积学研究,E-mail:wangsj@igsnrr.ac.cn。
作者简介:
王彦君(1989- ),女,河北邢台人,硕士生,主要研究方向为河流水文学、河流地貌学,E-mail:wangyj.11s@igsnrr.ac.cn。
基金资助:
WANG Yanjun1,2, WANG Suiji1, Su Teng1,2
Received:
2013-10-01
Revised:
2013-12-01
Online:
2014-01-25
Published:
2014-01-22
摘要: 为了定量区分气候变化和人类活动对松花江流域不同区段径流量变化的影响程度,应用线性趋势分析、累积距平等方法,对流域内4 个不同区段1955-2010 年径流量序列进行分析,揭示了径流量在各区段呈现不同的规律。其中江桥以上、江桥—大赉和哈尔滨—佳木斯3 个区段各存在3 个突变点以及被其分割的4 个变化阶段,而大赉—哈尔滨区段只有一个突变点。应用累积量斜率变化率比较方法,在不考虑蒸散的情况下,定量估算了不同阶段降水和人类活动对径流量的影响程度,并探讨了主要人类活动因素的影响。结果表明:与基准期(T1)相比,人类活动对径流量的变化起着主导作用,其中江桥以上、江桥—大赉和哈尔滨—佳木斯3 个区段人类活动对径流量变化的影响程度在T2、T3、T4(1998-2010 年)3 个阶段分别为75%、95%和80%;而降水的影响程度分别为25%、5%和20%;大赉—哈尔滨区段T2时期降水和人类活动对径流的影响程度分别为25%和75%;主要与不同区段人口变动和水利工程修建这两项人类活动相关。
中图分类号:
王彦君, 王随继, 苏腾. 1955-2010年松花江流域不同区段径流量变化影响因素定量评估[J]. 地理科学进展, 2014, 33(1): 65-75.
WANG Yanjun, WANG Suiji, Su Teng. Quantification of impacts of precipitation and human activities on runoff changes in different sections of Songhua River during 1955-2010[J]. PROGRESS IN GEOGRAPHY, 2014, 33(1): 65-75.
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