Arid
DOI10.2172/138335
报告编号LBL--29700
来源IDOSTI_ID: 138335
Variation and correlation of hydrologic properties
Wang, J.S.Y. [Lawrence Berkeley Lab., CA (United States)]
英文摘要Hydrological properties vary within a given geological formation and even more so among different soil and rock media. The variance of the saturated permeability is shown to be related to the variance of the pore-size distribution index of a given medium by a simple equation. This relationship is deduced by comparison of the data from Yucca Mountain, Nevada (Peters et al., 1984), Las Cruces, New Mexico (Wierenga et al., 1989), and Apache Leap, Arizona (Rasmussen et al., 1990). These and other studies in different soils and rocks also support the Poiseuille-Carmen relationship between the mean value of saturated permeability and the mean value of capillary radius. Correlations of the mean values and variances between permeability and pore-geometry parameters can lead us to better quantification of heterogeneous flow fields and better understanding of the scaling laws of hydrological properties.
出版年1991
报告类型Technical Report
语种英语
国家美国
来源学科分类58 GEOSCIENCES ; 05 NUCLEAR FUELS ; 54 ENVIRONMENTAL SCIENCES ; RESERVOIR ROCK ; PERMEABILITY ; POROSITY ; ARIZONA ; CAPILLARY FLOW ; CORRELATIONS ; DISTRIBUTION ; FLOW MODELS ; FLUID FLOW ; GEOLOGIC FORMATIONS ; HYDROLOGY ; MICROSTRUCTURE ; NEW MEXICO ; PROGRESS REPORT ; SCALING LAWS ; SOILS ; YUCCA MOUNTAIN ; Yucca Mountain Project
URLhttp://www.osti.gov/scitech/servlets/purl/138335
资源类型科技报告
条目标识符http://119.78.100.177/qdio/handle/2XILL650/264457
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GB/T 7714
Wang, J.S.Y. [Lawrence Berkeley Lab., CA . Variation and correlation of hydrologic properties,1991.
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