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ASTM D5777-2018 地下勘探中地震折射波法使用指南 Standard Guide for Using the Seismic Refraction Method for Subsurface Investigation ASTM D5777-2018 地下勘探中地震折射波法使用指南 Standard Guide for Using the Seismic Refraction Method for Subsurface Investigation

ASTM D5777-2018 地下勘探中地震折射波法使用指南 Standard Guide for Using the Seismic Refraction Method for Subsurface Investigation

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  • 标准编号:ASTM D5777-2018
  • 标准状态:现行
  • 更新时间:2023-07-23
  • 下载次数:
标准简介

1.1 Purpose and Application—This guide covers the equipment, field procedures, and interpretation methods for the assessment of subsurface conditions using the seismic refraction method. Seismic refraction measurements as described in this guide are applicable in mapping subsurface conditions for various uses including geologic, geotechnical, hydrologic, environmental (1), mineral exploration, petroleum exploration, and archaeological investigations. The seismic refraction method is used to map geologic conditions including depth of bedrock, or the water table, stratigraphy, lithology, structure, and fractures or all of these. The calculated seismic wave velocity is related to mechanical material properties. Therefore, characterization of the material (type of rock, degree of weathering, and rippability) is made on the basis of seismic velocity and other geologic information.

1.1.1 The geotechnical industry uses English or SI units.

1.2 Limitations: 

1.2.1 This guide provides an overview of the seismic refraction method using compressional (P) waves. It does not address the details of the seismic refraction theory, field procedures, or interpretation of the data. Numerous references are included for that purpose and are considered an essential part of this guide. It is recommended that the user of the s

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