Land Use/Cover Change and Its Effects on Hydrologic Processes in Nuomin River Basin
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Land Use/Cover Change and Its Effects on Hydrologic Processes in Nuomin River Basin
Bulletin of Soiland Water ConservationVol. 32, Issue 1, Pages: 23-28(2013)
作者机构:
1. 中国科学院东北地理与农业生态研究所,吉林,长春,130012
2. 中国科学院大学,北京,100049
3. 黑龙江省齐齐哈尔水文局,黑龙江,齐齐哈尔,161005
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Published:2013
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SHI Xiao-liang, LI Ying, ZHAO Kai, et al. Land Use/Cover Change and Its Effects on Hydrologic Processes in Nuomin River Basin[J]. Bulletin of Soiland Water Conservation, 2013, 32(1): 23-28.
DOI:
SHI Xiao-liang, LI Ying, ZHAO Kai, et al. Land Use/Cover Change and Its Effects on Hydrologic Processes in Nuomin River Basin[J]. Bulletin of Soiland Water Conservation, 2013, 32(1): 23-28.DOI:
Land Use/Cover Change and Its Effects on Hydrologic Processes in Nuomin River Basin
Land use/cover change and its effects on hydrologic processes are becoming an important aspect of global change research.In order to understand the effects of deforestation on hydrologic processes in theDaxing'anling area
a five-stage land use/cover date base in the Nuomin River basin since 1954was established based on remote sensing imagery data and topographic map.With GIS spatial analysis tools
the paperanalyzed the land use/cover change characteristics and its effects on hydrologic process.Results indicatedthat land use changed prominently in the Nuomin River basin during the past five decades.Forest and grassland decreased by 1 940.10and 748.99km2
respectively
and in contrast
cropland increased by 2 741.7km2.Since the nature forest protection project came into force in the Daxing'anling area in 1998
woodlandreduction and farmland reclamation have showed a declined trend.Land use/cover change had effects on annual runoff and runoff increased during the late land use period with decreased forest and more cropland
andthe impact of land use/cover change on runoff was strengthened in response to increased rainfall.Besides
the effects of land use/cover change on runoff production were characterized by seasonal fluctuation.
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