ASTM D4105 - 96(2008) Standard Test Method for (Analytical Procedure) for Determining Transmissivity and Storage Coefficient of Nonleaky Confined Aquifers by the Modified Theis Nonequilibrium Method


    Citing ASTM Standards Citation data is made available by participants in CrossRefs Cited-by Linking service. A comprehensive list of citations to this standard are listed here.

    D653 Standard Terminology Relating to Soil, Rock, and Contained Fluids

    D4043 Standard Guide for Selection of Aquifer Test Method in Determining Hydraulic Properties by Well Techniques

    D4050 Standard Test Method for (Field Procedure) for Withdrawal and Injection Well Tests for Determining Hydraulic Properties of Aquifer Systems

    D5269 Standard Test Method for Determining Transmissivity of Nonleaky Confined Aquifers by the Theis Recovery Method

    D5270 Standard Test Method for Determining Transmissivity and Storage Coefficient of Bounded, Nonleaky, Confined Aquifers

    D5473 Standard Test Method for (Analytical Procedure for) Analyzing the Effects of Partial Penetration of Control Well and Determining the Horizontal and Vertical Hydraulic Conductivity in a Nonleaky Confined Aquifer

    D5880 Standard Guide for Subsurface Flow and Transport Modeling

    D6000 Standard Guide for Presentation of Water-Level Information from Groundwater Sites

    E1943 Standard Guide for Remediation of Ground Water by Natural Attenuation at Petroleum Release Sites


    Referenced ASTM Standards The documents listed below are referenced within the subject standard but are not provided as part of the standard.

    D653 Terminology Relating to Soil, Rock, and Contained Fluids

    D4043 Guide for Selection of Aquifer Test Method in Determining Hydraulic Properties by Well Techniques

    D4050 Test Method for (Field Procedure) for Withdrawal and Injection Well Tests for Determining Hydraulic Properties of Aquifer Systems

    D4106 Test Method for (Analytical Procedure) for Determining Transmissivity and Storage Coefficient of Nonleaky Confined Aquifers by the Theis Nonequilibrium Method