首页 | 本学科首页   官方微博 | 高级检索  
     检索      


A framework for understanding the hydroecology of impacted wet meadows in the Sierra Nevada and Cascade Ranges, California, USA
Authors:Steven P Loheide II  Richard S Deitchman  David J Cooper  Evan C Wolf  Christopher T Hammersmark  Jessica D Lundquist
Institution:1. Department of Civil and Environmental Engineering, University of Wisconsin-Madison, Madison, WI, USA
2. Nelson Institute for Environmental Studies, University of Wisconsin-Madison, Madison, WI, USA
3. Department of Forest, Rangeland, and Watershed Stewardship, Colorado State University, Fort Collins, CO, USA
4. Center for Watershed Sciences, University of California-Davis, Davis, CA, USA
5. Department of Civil and Environmental Engineering, University of Washington, Seattle, WA, USA
Abstract:Meadows of the Sierra Nevada and Cascade mountains of California, USA, support diverse and highly productive wet-meadow vegetation dominated by sedges, rushes, grasses, and other herbaceous species. These groundwater–dependent ecosystems rely on the persistence of a shallow water table throughout the dry summer. Case studies of Bear Creek, Last Chance, and Tuolumne meadow ecosystems are used to create a conceptual framework describing groundwater–ecosystem connections in this environment. The water requirements for wet-meadow vegetation at each site are represented as a water-table-depth hydrograph; however, these hydrographs were found to vary among sites. Causes of this variation include (1) differences in soil texture, which govern capillary effects and availability of vadose water and (2) elevation-controlled differences in climate that affect the phenology of the vegetation. The field observations show that spatial variation of water-table depth exerts strong control on vegetation composition and spatial patterning. Groundwater-flow modeling demonstrates that lower hydraulic-conductivity meadow sediments, higher groundwater-inflow rates, and a higher ratio of lateral to basal-groundwater inflow all encourage the persistence of a high water table and wet-meadow vegetation, particularly at the margin of the meadow, even in cases with moderate stream incision.
Keywords:
本文献已被 SpringerLink 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号