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应用生态学报 ›› 2011, Vol. 22 ›› Issue (06): 1559-1565.

• 研究报告 • 上一篇    下一篇

1967—2006年太子河流域径流系数的变化特征

邓珺丽1,2,张永芳1,2,王安志1,关德新1,金昌杰1**,吴家兵1   

  1. 1中国科学院沈阳应用生态研究所, 沈阳 110016;2中国科学院研究生院, 北京 100049
  • 出版日期:2011-06-18 发布日期:2011-06-18

Variation characteristics of runoff coefficient of Taizi River basin in 1967-2006.

DENG Jun-li1,2, ZHANG Yong-fang1,2, WANG An-zhi1, GUAN De-xin1, JIN Chang-jie1, WU Jia-bing1   

  1. 1Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China;2Graduate University of Chinese Academy of Sciences, Beijing 100049, China
  • Online:2011-06-18 Published:2011-06-18

摘要: 利用太子河流域6个主要支流(海城河、南沙河、北沙河、兰河、细河、太子河南支)1967—2006年日均降水和径流资料,分析了各支流径流系数的变化趋势及其与降水的关系.结果表明:1967—2006年,位于高山丘陵区的太子河南支的年均径流系数较大,而人类活动影响较多的海城河流域的年均径流系数较小;除南沙河的年径流系数总体呈上升趋势外,其余各条支流的年径流系数均呈下降趋势,以南支和兰河的下降趋势尤为明显;除细河流域的年径流系数没有发生突变外,其余各条支流的年径流系数都发生了突变,且突变出现的年份各不相同;年降水量对年径流系数的影响极显著.

关键词: 径流系数, Mann-Kendall检验, 突变, 太子河流域

Abstract: Based on the daily precipitation and runoff data of six main embranchments (Haicheng River, Nansha River, Beisha River, Lanhe River, Xihe River, and Taizi River south embranchment) of Taizi River basin in 1967-2006, this paper analyzed the variation trend of runoff coefficient of the embranchments as well as the relationship between this variation trend and precipitation. In 1967-2006, the Taizi River south embranchment located in alpine hilly area had the largest mean annual runoff coefficient, while the Haicheng River located in plain area had the relatively small one. The annual runoff coefficient of the embranchments except Nansha River showed a decreasing trend, being more apparent for Taizi River south embranchment and Lanhe River. All the embranchments except Xihe River had an obvious abrupt change in the annual runoff coefficient, and the beginning year of the abrupt change differed with embranchment. Annual precipitation had significant effects on the annual runoff coefficient.

Key words: runoff coefficient, Mann-Kendall test, abrupt change, Taizi River basin