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824                                                                 Appendix E:  Porous Media Hydraulics



                            6.0  10 –9
                                    Sand-S
                                    Anthracite-A
                            5.0  10 –9  Glass beads - GB                             A-d = 1.71 mm
                                                                                        10
                            4.0  10 –9
                            k (m 2 )  3.0  10 –9            S-d = 1.50 mm      A-d = 1.47 mm
                                                                                  10

                                    GB-d = 1.50 mm            10
                                        10
                            2.0  10 –9
                                                                                  A-d = 1.02 mm
                                                                                    10
                                                            = 1.08 mm
                                                         S-d 10
                            1.0  10 –9
                                                          S-d = 0.47 mm
                                0.0                          10
                                  0.30      0.35      0.40       0.45      0.50      0.55       0.60
                                                               Porosity
            FIGURE E.2 Permeability k versus porosity for different d 10 sizes. (Plots calculated by equation 5.5 from data in Chang, M. et al., Aqua,
            48, pp. 141 & 142, 1999.)



                            10 –8
                                 Sand-S
                                 Anthracite-A                 A-d 10 = 1.02 mm                 0.576
                                 Glass beads-GB                  S-d 10 = 1.08 mm  0.540  0.436
                                 Numbers indicate porosity                                     0.462
                                                        0.556    0.414        0.484   0.350
                                                       CSU x

                           k (m 2 )  10 –9  S-d 10 = 0.47 mm  0.501  0.365        A-d 10 = 1.47 mm  A-d 10 = 1.71 mm


                                  x-CSU  0.433                                       S-d 10 =1.50 mm GB-d 10 = 1.50 mm

                                    0.382


                           10 –10
                               0.40     0.60     0.80      1.0       1.2      1.4       1.6      1.8
                                                              d 10  (mm)
            FIGURE E.3 Permeability k versus d 10 with different porosities. (Plots calculated by Equation 5.5 from data in Chang, M. et al., Aqua, 48,
            pp. 141 & 142, 1999.)


                                                               separation between categories of natural media, e.g., ‘‘clay
            E.3.5 PERMEABILITY DATA FOR AQUIFER MEDIA
                                                               and silt,’’ ‘‘fine sand,’’ etc. The logarithmic scales for both
            The intrinsic permeability, k, depends upon the average grain  axes indicate the wide variation found in grain size and
            size, the pore size distribution, and the packing of the granular  intrinsic permeability of natural media.
            media and so is likely to vary even for media of the same  The shaded area at the top shows the envelope of Figure
            average grain size. Therefore, in natural media these variables  E.4 superimposed and indicates the contrast with natural
            occur in various combinations and some, e.g., porosity and  media. The higher intrinsic permeability values for filter
            packing, may be different in situ compared with a laboratory  media may relate to the generally lower UC, specified usually
            test. This contrasts with granular media used in water treat-  as about 1.5. A datum for the Empire, Colorado, slow
            ment in which such variables are controlled by specifications.  sand filter is shown with d 10 ¼ 0.24 mm and UC ¼ 2.7, with
                                                                             2
              Typical ranges in k for different categories of natural media  k ¼ 7.2   10  11  m . The other dots are for CSU pilot filters
            are shown in Figure E.4. Media grain sizes are shown on  (calculations were from Mosher and Hendricks data, 1986)
            the abscissa with ordinate values showing maximum and  for sand with d 10 ¼ 0.50 mm and UC ¼ 1.5 and k ¼ 4.6   10  10
                                                                 2
            minimum values for k. The lighter vertical lines show the  m ; and for anthracite with d 10 ¼ 0.91 mm and UC ¼ 1.5,
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