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Range of Values of Hydraulic Conductivity <br /> and Permeability <br /> Rocks I Unconsolidated k k K K <br /> deposits (dart•) (c.-r ) z <br /> _ >' ) (c�/sl {�/s] {goi/day/,t ) <br /> to: -5 10` I <br /> 100 <br /> 104 10` to Io"' <br /> U <br /> � l0� <br /> 10' to"5 I 10-'` <br /> iO4 <br /> C <br /> o a <br /> -102 10 ' 10-[ 10-3 <br /> c <br /> N C <br /> �.I c10 10-7 10-2 Io-4 10 <br /> Y1 � C v1 G <br /> c— v -310Z <br /> c w " <br /> o a 1 l0-s 10-3 to <br /> U y � <br /> 10 _ 4 <br /> to-' ,0-9 1a, <br /> C: N _— <br /> - o <br /> cc) I 10-'- 10-10 10-; to 1 <br /> .E = a 11 a i0-i <br /> ,0- 10- 10 - to-- <br /> f � = � <br /> ,o-'- <br /> 10-4 10-�Z to-7 to-9 <br /> QJ T U tQ <br /> 6 p V <br /> vca - 10-5 10 13 to-e i0-10 <br /> a C:c 10-e 10-14 10-9 t0-n 10" <br /> 0 <br /> m5 <br /> 0 0;a 10 7 10-15 t0-1O to <br /> f0 <br /> c O Fn <br /> Z& ] 10-6 L 10-1e 10-11 ,o-t3 10- <br /> 0 <br /> 0" <br /> E 10-` <br /> Conversion Factors for Permeability <br /> and Hydraulic Conductivity Units <br /> Yerne_biliry,k' Hydraulic conductivity, K <br /> CM, 112 darty rn/s r/s LI.S. cal/gay/ft2 <br /> cr 1 1.08 x 10-3 1.01 x 108 9.30 x 10= 3.12 x 103 1.3: x 109 <br /> f. 9.29 x 102 1 9.-2 x 1010 9-11 x 105 2.99 x 106 1.71 x 101' <br /> dart.- 9.87 x 10-9 1.06 x 10-11 1 9.66 x 10-5 3.17 x 10-5 1.82 x 101 <br /> m's 1.02 x 10-3 1.10 x 10-6 1.01 r. 105 1 3.28 2.12 X 106 <br /> f<<s 3.11 x 10-1 3.35 x 10-7 3.15 x 10' 3.05 x 10-1 1 6.46 x los <br /> U-S. gal'dav/fC4;.4_ x 10-10 5.33 x 10-13 5.49 r. 10`= 4.72 x l0-- 1.55 :'- 10 l <br /> 'i o obtain k in ft'-, multiply k in ctn'- by 1.08 x 10-1. (Freeze & Cherry, 1974) <br /> X. =n <br />