Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.jhydrol.2010.03.013 |
Regional groundwater flow in structurally-complex extended terranes: An evaluation of the sources of discharge at Ash Meadows, Nevada | |
Bushman, Michelle1; Nelson, Stephen T.1; Tingey, David1; Eggett, Dennis2 | |
通讯作者 | Nelson, Stephen T. |
来源期刊 | JOURNAL OF HYDROLOGY |
ISSN | 0022-1694 |
EISSN | 1879-2707 |
出版年 | 2010 |
卷号 | 386期号:1-4页码:118-129 |
英文摘要 | Ash Meadows, Nevada, USA is a site of major groundwater discharge (similar to 38,000 L/min) in the arid Mojave Desert, and hosts a number of endemic and threatened wetland species. In addition to these resources, Ash Meadows may also represent the future discharge location of radionuclide-laden waters from nuclear weapons testing at the Nevada Test Site. More importantly, however, Ash Meadows provides the opportunity to understand the controls on water transfer between basins through fractured bedrock. 4000+ solute analyses were assembled from the literature into a single database. The data were screened for spatial distribution, completeness, charge balance, and elevated temperatures (>= 20 degrees C and within regional flow systems), with 246 candidate up-gradient water remaining distributed among six potential source areas in addition to and Ash Meadows itself. These potential sources include both carbonate, volcanic and perhaps valley-fill aquifer systems. These waters were characterized by cluster analysis in order to sort similar waters in an objective fashion into potential flow paths and to establish representative endmember waters for inverse geochemical models and other modes of analysis. Isotopic tracers, both conservative and those reflecting water-rock interaction, all suggest that waters at Ash Meadows are derived by southward flow from volcanic terranes, parallel to the preferred permeability structure induced by active regional east-west extension. Solute balances support this conclusion. However, this runs counter to the prevailing model that waters at Ash Meadows are derived from easterly and northeasterly flows from the Spring Mountains and Pahranagat Valley areas by interbasin flow through a continuous fractured carbonate aquifer. This work suggests that carbonate aquifer systems in extended terranes are more compartmentalized than previously appreciated and that anisotropy in fracture permeability is key to compartmentalization and the control of flow directions. (C) 2010 Elsevier B.V. All rights reserved. |
英文关键词 | Interbasin flow Ground water Isotopes Aquifer segmentation |
类型 | Article |
语种 | 英语 |
国家 | USA |
收录类别 | SCI-E |
WOS记录号 | WOS:000278577000010 |
WOS关键词 | FOSSIL SPRING DEPOSITS ; SOUTHERN GREAT-BASIN ; LOCAL RECHARGE ; YUCCA MOUNTAIN ; OASIS VALLEY ; DEATH-VALLEY ; DEVILS-HOLE ; CALIFORNIA ; CARBON ; USA |
WOS类目 | Engineering, Civil ; Geosciences, Multidisciplinary ; Water Resources |
WOS研究方向 | Engineering ; Geology ; Water Resources |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/165295 |
作者单位 | 1.Brigham Young Univ, Dept Geol Sci, Provo, UT 84602 USA; 2.Brigham Young Univ, Dept Stat, Provo, UT 84602 USA |
推荐引用方式 GB/T 7714 | Bushman, Michelle,Nelson, Stephen T.,Tingey, David,et al. Regional groundwater flow in structurally-complex extended terranes: An evaluation of the sources of discharge at Ash Meadows, Nevada[J],2010,386(1-4):118-129. |
APA | Bushman, Michelle,Nelson, Stephen T.,Tingey, David,&Eggett, Dennis.(2010).Regional groundwater flow in structurally-complex extended terranes: An evaluation of the sources of discharge at Ash Meadows, Nevada.JOURNAL OF HYDROLOGY,386(1-4),118-129. |
MLA | Bushman, Michelle,et al."Regional groundwater flow in structurally-complex extended terranes: An evaluation of the sources of discharge at Ash Meadows, Nevada".JOURNAL OF HYDROLOGY 386.1-4(2010):118-129. |
条目包含的文件 | 条目无相关文件。 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。