NF ISO 20244

NF ISO 20244

December 2018
Standard Current

Soil quality - On-site test method to quickly determine gravimetric water contents in soil by refractometry

This document specifies a method for rapid determination of water content in soils. The method is based on refractive index measurement of a sucrose solution after it is mixed with a soil sample.It is applicable to the determination of water content in geological or geotechnical research as well as geotechnical engineering. In addition, it can be used for commercial work in a variety of fields, e.g. agriculture and civil engineering.The working range is up to approximately 50 % moisture content. The precision of the method typically ranges between 0,5 % and 1 % and depends on the type of refractometer that is used.The result of this method is strongly influenced by soil matrices. Higher contents of clay and/or organic matter will lead to significant lower values for water content compared to standard methods such as that described in ISO 11465.

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Main informations

Collections

National standards and national normative documents

Publication date

December 2018

Number of pages

12 p.

Reference

NF ISO 20244

ICS Codes

13.080.10   Chemical characteristics of soils

Classification index

X31-019

Print number

1

International kinship

Sumary
Soil quality - On-site test method to quickly determine gravimetric water contents in soil by refractometry

This document specifies a method for rapid determination of water content in soils. The method is based on refractive index measurement of a sucrose solution after it is mixed with a soil sample.

It is applicable to the determination of water content in geological or geotechnical research as well as geotechnical engineering. In addition, it can be used for commercial work in a variety of fields, e.g. agriculture and civil engineering.

The working range is up to approximately 50 % moisture content. The precision of the method typically ranges between 0,5 % and 1 % and depends on the type of refractometer that is used.

The result of this method is strongly influenced by soil matrices. Higher contents of clay and/or organic matter will lead to significant lower values for water content compared to standard methods such as that described in ISO 11465.

Table of contents
  • 1 Domaine d'application
  • 2 Références normatives
  • 3 Termes et définitions
  • 4 Principe
  • 5 Appareillage et réactifs
  • 6 Mode opératoire
  • 7 Calcul des résultats
  • 8 Contrôle qualité
  • 9 Rapport d'essai
  • Annexe A Résultats de validation et évaluation statistique
  • Bibliographie
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