2 edition of Simulations of non-steady flow in a glacial outwash aquifer, southern Franklin County, Ohio found in the catalog.
Simulations of non-steady flow in a glacial outwash aquifer, southern Franklin County, Ohio
Razem, Allan C.
by U.S. Dept. of the Interior, Geological Survey, Open-File Services Section, Western Distribution Branch, USGS [distributor] in Columbus, Ohio, Denver, Colo
Written in English
Bibliography: p. 17.
|Statement||by Allan C. Razem ; prepared in cooperation with the city of Columbus, Ohio.|
|Series||Water resources investigations report -- 83-4022, Water-resources investigations report -- 83-4022.|
|Contributions||Columbus (Ohio), Geological Survey (U.S.)|
|The Physical Object|
|Pagination||iv, 17 p. :|
|Number of Pages||17|
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Get this from a library. Simulations of non-steady flow in a glacial outwash aquifer, southern Franklin County, Ohio. [Allan C Razem; Columbus (Ohio); Geological Survey (U.S.)]. Report of the public schools of Columbus, Ohio: for the years, by Columbus (Ohio) (Book) A communication study for the Columbus Department of Health by Janice M Sabett.
Simulations of non-steady flow in a glacial outwash aquifer, southern Franklin County, Ohio / (Columbus, Ohio: U.S. Dept. of the Interior, Appraisal of water from surficial-outwash aquifers in Todd County and parts of Cass and Morrison Counties, central Minnesota /. Groundwater flow velocity or infiltration rate Derived from Eq.5, the groundwater flow velocity or infiltration rate (v) is simply given by: v = nk h2 hl = nki, (7) x2-x1 where n is the effective aquifer/soil porosity, h2 and are the groundwater heads at locations x2 Simulations of non-steady flow in a glacial outwash aquifer x1 along a flow path, respectively, and i is the hydraulic gradient.
A numerical simulation model of groundwater flow was established first, and four exploitation wells were set in the Tongyu county and Qian Gorlos county respectively so.
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A protocol and methods for monitoring the major physical, chemical, and biological components of stream ecosystems are presented. The monitoring protocol is organized into four stages. At stage 1 information is.
THE HANDBOOK OF GROUNDWATER ENGINEERING Second Edition JACQ: “_c” — /10/19 — — page ii — #2 THE HANDBOOK OF GROUNDWATER ENGINEERING Second Edition Edited by Jacques W. Delleur Boca Raton London New York CRC Press is an imprint of the Taylor & Francis Group, an informa business. Oil emplacement will thus at least retard quartz cementation in sandstones.
A significantly oil-wet sandstone case is more difficult to appraise quantitatively. The rate of diffusion in the oil leg relative to the water leg will be retarded greatly (e.g.
Worden et al., ) and Swi is lower than in water-wet cases leading to less of the.