ISO/TC 182/WG 9 - Geotechnical aspects of geophysical methods
Development of standards for determining geotechnical parameters from geophysical tests
Aspects géotechniques des méthodes géophysiques
Elaboration de normes pour la détermination de paramètres géotechniques à partir d'essais géophysiques
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ISO/TC 182/WG 9 is a Working Group within the International Organization for Standardization (ISO). It is named "Geotechnical aspects of geophysical methods" and is responsible for: Development of standards for determining geotechnical parameters from geophysical tests This committee has published 1 standards.
ISO/TC 182/WG 9 develops ISO standards in the area of Information technology. The scope of work includes: Development of standards for determining geotechnical parameters from geophysical tests Currently, there are 1 published standards from this working group.
The International Organization for Standardization (ISO) is an independent, non-governmental international organization that develops and publishes international standards. Founded in 1947 and headquartered in Geneva, Switzerland, ISO brings together experts from 170+ member countries to share knowledge and develop voluntary, consensus-based standards that support innovation and provide solutions to global challenges.
A Working Group in ISO is a specialized group responsible for developing standards or technical work within a defined scope. These bodies bring together international experts to create consensus-based standards that support global trade, safety, and interoperability.
This document specifies requirements for equipment, survey procedure, data analysis and reporting of array measurement of microtremors which is one of the non-destructive testing methods with an array of sensors deployed on the ground surface. This document applies to the array measurement of microtremors to estimate a 1D shear wave velocity profile. This document specifically describes array measurement of microtremors using vertical ground vibration to estimate an S-wave velocity profile by processing microtremor records based on the fundamental mode of Rayleigh waves.
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