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Range of Values of Hydraulic Conductivity <br /> 1 and Permeability <br /> Rocks I Unconsclidcted k K <br /> deposits K <br /> (darty) (CM2) (m/sl (aol/dcy/1tz) <br /> 10� IT-1 -104 1 <br /> o _ <br /> 104 10 4 10 10-1 10 - <br /> CJ <br /> s <br /> _ 10` <br /> I c� 10' i0-5 1 0_a <br /> V <br /> `w a c <br /> -to 10-' [Q-1 10-3 104 <br /> E N <br /> f <br /> H c N t0 i0-7 [p-Z Ip-a 10"3 <br /> ' o c <br /> � C u U <br /> H 1 10-$ [p-3 10-5 10z <br /> t o` a� 10-1 10-9 10� 10'' 10 <br /> � Eci.2 n <br /> ac �, �+ <br /> Zo 0 0 10-- 10-10 10-' 10_` 1 <br /> c r <br /> 4 o in i0-' 10-I1 f0-6 10 10-1 <br /> V) <br /> 10-� 10-Iz 10-7 1O_9 10-- <br /> j <br /> a� <br /> 6 b3 <br /> 10-5 to-13 ITS - to- <br /> 10 10- <br /> v b 47 <br /> 77 <br /> o` 5 14 10-4 <br /> o 10 i0- 10-9 1Q-I1 <br /> 3 <br /> C <br /> d 10-7 10-15 10-10 10 12 10 <br /> I <br /> 1Q-o <br /> �._ 10-s 10-15 10-I1 t0-13 <br /> 10-; <br /> Conversion Factors for Permeability <br /> and Hydraulic Conductivity Units <br /> Permeability,k` Hydraulic conductivity, <br /> cm 'i2 oarcy M/S <br /> c"`- 1 1.08 x 10-3 1.01 x 108 9.30 x 10= <br /> f;- 9.?9 x [0= _.=2 x 103 1.35 x 105 <br /> 1 9.=3 x 1010 9.11 x los ?.09 x 106 1.71 x 10 <br /> 9.37 x ]0-9 1.06 x 10-11 1 <br /> dar <br /> 1 9.66 r. 10-6 =.17 x 10-5 1,52 x ]Oi <br /> m-s 1.0? x 10-3 1.10 x I0-6 I.04 x 105 1 3,?g -.1? 105 <br /> x <br /> ft's x.11 x 10-1 =.=� x ]0-7 3.15 x 101 3.05 x 10-1 1 6.46 x 105 <br /> gal day/fl.j,__ y, 10-10 -13 x ]0-13 5.49 x 10`' 4 -� <br /> . - .7- x l0-' l.» :: 10-6 1 <br /> To o obtain k in f t=, r nultioly k in c,-n2 by 1.08 x 10-3. <br /> (Freeze & Cberry, 1979) <br />