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Transmissivity Equivalency - Design Calculator

 

Problem Statement

When a granular liquid collection layer is replaced by a geosynthetic liquid collection layer, it is often assumed that two liquid collection layers having the same hydraulic transmissivity are equivalent.  In the United States, this approach is often mandated by regulations for the case of leachate collection layers and leakage detection and collection layers used in landfills.  This is true only in the case of confined flow (i.e. if the liquid collection layer is completely filled with liquid).  In reality, liquid collection layers should be designed for unconfined flow, as demonstrated in the paper by Giroud, Zhao and Bonaparte (2000).  To be equivalent under the unconfined flow condition, the geosynthetic liquid collection layer should have a greater hydraulic transmissivity than the granular liquid collection layer.

Formula

     where:


Symbol Name Dimensions
E Equivalency factor -
tsoildrain Thickness of soil drain ft.
L Slope length ft.
s Slope (= tan ß) %
Qsoildrain Soil drainage transmissivity m2/s
QGST Geosynthetic drainage transmissivity m2/s

 

Input Values

Slope (s) %
Slope length (L) ft
Soil drain thickness (tsoildrain) ft

 
References

Giroud, J.P., Zhao, A., and Bonaparte, R., 2000, "The Myth of Hydraulic Transmissivity Equivalency Between Geosynthetic and Granular Liquid Collection Layers", Geosynthetics International, Vol. 7, Nos. 4-5.

Copyright 2001 Advanced Geotech Systems.  All rights reserved.