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    • Hydrology and Water Resources in Arizona and the Southwest, Volume 05 (1975)
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    The Application of Step-Drawdown Pumping Tests for Determining Well Losses in Consolidated Rock Aquifers

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    Author
    Uhl, V. W., Jr.
    Joshi, V. G.
    Alpheus, A.
    Sharma, G.
    Affiliation
    Hydrology and Water Resources, University of Arizona, Tucson, Arizona
    Evangelical Lutheran Church Water Development Project, Getul, M.P., India
    Issue Date
    1975-04-12
    Keywords
    Hydrology -- Arizona.
    Water resources development -- Arizona.
    Hydrology -- Southwestern states.
    Water resources development -- Southwestern states.
    Aquifers
    Step-downs
    Drawdown
    Water level fluctuations
    Pumping
    Wells
    Water levels
    Transmissivity
    Rock properties
    India
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    Copyright ©, where appropriate, is held by the author.
    Collection Information
    This article is part of the Hydrology and Water Resources in Arizona and the Southwest collections. Digital access to this material is made possible by the Arizona-Nevada Academy of Science and the University of Arizona Libraries. For more information about items in this collection, contact anashydrology@gmail.com.
    Publisher
    Arizona-Nevada Academy of Science
    Journal
    Hydrology and Water Resources in Arizona and the Southwest
    Abstract
    The concept of a step -drawdown test was first introduced by Jacob, and further modifications in the technique were made by Rorabaugh. Analysis of step -drawdown test data enables the quantification of the components of drawdown due to formation or aquifer loss, and due to well losses in a pumped well. This technique has been used to test approximately 100 wells that were drilled in crystalline and basalt formations in central India. Test data have been analyzed by Rorabaugh's method and by a graphical method, and the results of a number of tests are presented and discussed. Anomalies in the test analysis often proved helpful for interpreting aquifer irregularities. In general, the well loss constant decreases with an increase in specific capacity and the aquifer loss constant decreases with increasing transmissivity. Significant reductions in specific capacity during a step test occur in wells with high well losses. An attempt is made to quantify the well losses in a consolidated rock well, and a number of practical applications of step -drawdown tests are discussed.
    ISSN
    0272-6106
    Collections
    Hydrology and Water Resources in Arizona and the Southwest, Volume 05 (1975)

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