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� � � �: � �_� _. � A� .F: t .� •- j $ice F"h,��''",�vy ;� � 4� <br /> y„a <br /> 4—a <br /> C.. <br /> .• FYORAULIC CONDUCTIVITY APPRO11MTION <br /> FROM gNVENTIONAL GRAIN SIZE ANALYSIS MING <br /> i HAIER AND XRUNEIA h MDU APPRGII WOAS <br /> PROJECT H40-:0-12 PROJECT Ntrity <br /> ANALYZED ejc DATE: 11-17-81 <br /> I <br /> - SAMPLE I:sbrr3 r+�s.^� ,•.1. v - +am+ _. . <br /> DE°TH: 16 <br /> f STATIC VALUES: <br /> GRAIN SIZE OF PERCENT FINER IMA) <br /> dIO Permtiles 0.04 <br /> --�.- 616 Percentile:— 0.05`- <br /> d50 Percentila= 0.114 <br /> ' d84 Percentiles 0.247 <br /> STATISTICAL CALCULATIONSs <br /> _ GEOMETRIC P.Ew 0.153733 <br /> I <br /> MRT1#6 3.017417 <br /> HAIER — ..._ _ �.. ._ KRifxB:IN AND MOIGC_ <br /> Ka 0.0016 ice/sec) K■ 0.602074 (calsec) <br /> 4.553433 fit/day) .341237 Iftldiy) <br /> T PIFERENCESs <br /> Naxen: Freeze. R.A. I J.A Cherry, Groundrater, o.5S0, 1474. <br /> i <br /> Kruebeir. S Rank: Krusnein, N.C. I S.D. Mani, PRraeability is i Function <br /> of the Sire Paraeeters of 6intansolidated Sands. %!E-163, 1443. <br />