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Water and air transmissivity of geotextiles
Journal article   Peer reviewed

Water and air transmissivity of geotextiles

Robert M. Koerner, John A. Bove and Joseph P. Martin
Geotextiles and geomembranes, v 1(1), pp 57-73
1984

Abstract

The in-plane flow characteristics of both water and air in needled, nonwoven geotextiles have been evaluated in this study. Transmissivity (equal to permeability times fabric thickness) versus applied normal stress on the fabric has been measured in a radial flow device for different fabrics and for different thicknesses of a given fabric. The transmissivity response in each case was seen to decrease with increasing stress until a residual value was reached. In none of the cases did the fabric compress to the point where flow was completely shut off, even though stress levels of 2500 psf were applied. In turn, the calculated geotextile permeability varied from a fine gravel to a medium sized sand. Planar air flow in geotextiles has been found to be in excess of two orders of magnitude greater than water flow under comparable conditions. Air flow through partially and fully saturated fabrics is shown to be of little practical interest since the air easily moves around the water in the fabric voids or displaces it entirely. The need for transmissivity test standardization for all types of geotextiles and geotextile composite systems is expressed.

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22 citations in Scopus

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UN Sustainable Development Goals (SDGs)

This publication has contributed to the advancement of the following goals:

#12 Responsible Consumption & Production
#7 Affordable and Clean Energy
#13 Climate Action
#11 Sustainable Cities and Communities

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Web of Science research areas
Engineering, Geological
Geosciences, Multidisciplinary
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