Technical Papers
Aug 4, 2012

Sensitivity of Land-Use Change to Streamflow in Chaobai River Basin

Publication: Journal of Hydrologic Engineering
Volume 18, Issue 4

Abstract

Water problems and water crises are of widespread concern around the world against the background of climate change and intense human activity. As the only source of drinking water in Beijing being confronted with severe water shortages, the Chaobai River Basin is extraordinarily important. Land use, being a common and variable influence on streamflow, has been studied widely, whereas spatiotemporal differences and the complex mechanism of land use’s effect on runoff are difficult to explain. On the basis of a series of data about land use and runoff depth in the Chaobai River Basin, the sensitivity of land-use change to streamflow was explored using the principle of elasticity. Results of t-tests and F-tests showed that the difference in stream flow between the two river basins is not explained by precipitation; thus, land-use change is the main cause of stream flow variation. The influence of forests on annual runoff depth was significant and increased gradually from 1978 to 2008, whereas the effect of bare land has been insignificant in all time periods. The effect of land use on seasonal and monthly runoff depth showed significant variation. On the whole, the effects of land-use change on streamflow in summer were obvious, especially in August. It is therefore concluded that forest changes are the main factors in streamflow variation in summer.

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Acknowledgments

This research was supported by the National Scientific and Technological Plans (2011BAD38B05), State Forestry Administration, People’s Republic of China for Special Funding Projects of the Forestry Nonprofit Industry Research (Grant No. 201104005) and China Postdoctoral Science Foundation (2012M511938). The authors gratefully acknowledge all the grants for this research.

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Published In

Go to Journal of Hydrologic Engineering
Journal of Hydrologic Engineering
Volume 18Issue 4April 2013
Pages: 457 - 464

History

Received: May 5, 2011
Accepted: May 30, 2012
Published online: Aug 4, 2012
Published in print: Apr 1, 2013

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Jiangkun Zheng [email protected]
Postdoctoral Research Associate and Associate Professor, College of Soil and Water Conservation, Beijing Forestry Univ., No. 35, Qinghua East Rd., Haidian District, Beijing 100083, China; and College of Forestry, Sichuan Agricultural Univ., No. 46, Xinkang Rd., Ya’an, Sichuan Province 625014, China. E-mail: [email protected]
Professor, College of Soil and Water Conservation, Beijing Forestry Univ., No. 35, Qinghua East Rd., Haidian District, Beijing 100083, China (corresponding author). E-mail: [email protected]
Wenping Deng
M.S. Graduate Student, College of Soil and Water Conservation, Beijing Forestry Univ., No. 35, Qinghua East Rd., Haidian District, Beijing 100083, China.
Henian Wang
M.S. Graduate Student, College of Soil and Water Conservation, Beijing Forestry Univ., No. 35, Qinghua East Rd., Haidian District, Beijing 100083, China.
Yousheng Wang, Ph.D.
College of Soil and Water Conservation, Beijing Forestry Univ., No. 35, Qinghua East Rd., Haidian District, Beijing 100083, China.

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