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11 1 01 <br /> f �' A ? � r � • ri <br /> Or Soil permeauility <br /> Note that denotes the '�emjeabfllq,of a porous media,w1jile K k k <br /> represents the'"hydratilto enirduotiwiy The two are related by a, � <br /> (daro�) �crri 1 (MIs) <br /> 105 1Q -3 103 <br /> �i�a�� , <br /> K -'_ �k a 104 10 -,t 10 <br /> 1110 cL. 10s — 10 -5 1 <br /> Awe, C <br /> g = accelsar�tir.�n dm � � , 10 -1 <br /> � gM%dty (goo cm1 j r c 10 1Q <br /> PX.O = viscosity of Vater [0,01 g1cm-3 j � � � 10 .2 <br /> px,o = density of vatar (i 0 glem3 l 1 3 <br /> 10 �� - <br /> � "" <br /> +1 -f <br /> ( 10 10 'g 10 -d <br /> W .2 s <br /> then ohaasingperrneabilltivolues It Is important to 10 -- 10 •1010 •5 <br /> to keep in mind that (or K)often variesbq =p 3 ` <br /> _ <br /> serrata!orders ofmacp7ltude otrersmaif dfstamoes ;;li v�� t4 10 -fi 10 -� <br /> For this reason10 ft Is to cliaase a rage of k 10 -� <br /> •ia 10 <br /> See Ccmuarsi m Tables <br /> •� Relum to Flowrate Calculahan H 13 <br />