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I <br /> Hie : Soil Permeability <br /> P. <br /> Note that denotes the"permeabillty"of aporousmedia,wUle K k k K <br /> represents the'Mydraulio oonditotlulty". The two are related by (darn!) (OM) (MIS) <br /> f 10 10 "g 10a <br /> K = k L 104 - 10 '4 10 <br /> 1k14 , 10 10 " K 1 <br /> rrY►ete: 10 10 '6 <br /> g = acceientWn due to gwity [980 cmislj C _ 10 10 10 -a <br /> Jux,o - viscosity of water [0,01 grcm-s) in m 110 'e 10 "3 <br /> px,O - density of water [I 0 glcros] an u <br /> [ 10 .1 10 .g 104 <br /> .2 S <br /> '10 <br /> Men choosingpe"eability values It Is rrrmpottant t �� ( 10 10 10 • <br /> tokeep in mind thatk(ot K)o{ten variesby to 10 " -•- 10 '11 — 10 'e <br /> several orders ofmagnitude ounr small distamaes I, .,t <br /> � 10 10 '12 10 '7 <br /> For this reason It!:better to ohoose a range of k . . , <br /> See GOWPTstcm Table s ,6rrnto Flowrate Calculaticm H 13 <br />