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�Op: Soil Peneabilit <br /> Note that k denotes the'Permeabllity"of a porous media,while I It k � <br /> represents the"hydiaullo aonduotluity". no two are related bg (datq) Com) (Dmfs) <br /> n los 10 .3 10a <br /> •» t 1`H.,09 10 10 '4 10 <br /> ILH20 10 3 — 10 <br /> wren: _- � � -� -'� 10 -1 <br /> g = acceleradon due to gravity 1980 cmla2; .j 10 10 • #� •a <br /> px,o = viscosity of water [0.01 glcm-o l 1 it} -$ 1U '3 <br /> px,c = density of vater 11 d glcrosl •� <br /> 10 .1 10 10 •{ <br /> W •10 •5 <br /> When ohoosingpermeablilty values Itis ttrrport4mt t to W [ 10 10 10 <br /> to keep M mind that k(or K)often uarlesby a 10 ' 10 •1t 10 -e r <br /> seuval orders of magnitude over small dlstanoes. [ 10 .,t 1 •12 <br /> For thls teasun it is better to ohoose a range of k .�. 0 10 <br /> _j ISO oriv aim 1'ablez Retnto llowate Calcula�an H 13 <br /> i <br />