The size of pore space and interconnectivity of the spaces help determine permeability, so shape and arrangement of grains play a role. Permeability is a measure of a soil's or rock's ability to transmit a fluid, usually water. Often the term hydraulic conductivity is used when discussing groundwater and aquifer properties. Hydraulic conductivity simply assumes that water is the fluid moving through a soil or rock type.
Thanks and Regards,
|All times are GMT. The time now is 05:47 PM.|
Powered by vBulletin® Version 3.8.4
Copyright ©2000 - 2014, Jelsoft Enterprises Ltd.
Copyright 2005 - 2012 Molecular Station | All Rights Reserved