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8.8                        CHAPTER EIGHT

         filter was  computed as a  weighted average.  Data in the figure indicate that as the media
         used become coarser,  the required depth is increased, and as the media become finer, the
         depth required is reduced.  Kawamura (1999) uses a length-to-diameter L/d ratio to select
         the  proper  depth  and size of filter beds  (with both L  and d  measured  in millimeters). A
         value of the L/d ratio  should be  >  1,000 in rapid  sand filters,  >  1,250 in trimedia filters,
         and >  1,300 in most coarse deep beds where d is 1.2 to  1.4 mm and >  1,500 is most coarse
         deep beds where d  >  1.5  mm.



         Filtration  Rates
         Slow sand filters, designed for filtration rates of 3 to 6 mgd/acre at a rate of 0.05 to 0.10
         gpm/ft 2 (0.1  to 0.2 m/h), were initially replaced by rapid sand filters that operated at rates
         of  1 to 2  gpm/ft 2 (2.4 to 5.0 m/h). The 2 gprn/ft 2 (4.9  m/h) rate became widely accepted
         as an upper limit in U.S.  water  supply practice  for  many years.  For the past 30 years, it
         has been demonstrated that dual-media and mixed-media, as well as single-medium (sand
         or anthracite), filters can be successfully operated  at much higher rates.
           A number of investigators found dual- and mixed-media filters to operate successfully
         at rates from 3 to 8 gpm/ft 2 (8 to 20 m/h)  in a variety of locations (Conley,  1961,  1965;
         Robeck,  Dostal,  and Woodward,  1964;  Dostal  and Robeck,  1966;  Laughlin and Duvall,
         1968; Tuepker and Buescher,  1968; Rimer,  1968; Westerhoff,  1971; Kirchman and Jones,
         1972). The quantity of evidence of the practicality of high-rate filtration was such that in
         1972  the  AWWA  Committee  on  Filtration Problems  concluded that  it had  been amply
         demonstrated that filters could be designed and operated  to  produce  water of acceptable
         quality at flows  substantially higher than the  rate of 2  gpm/ft 2 (5  m/h), once considered
         the maximum. Over the last 30 years, a number of pilot-scale and full-scale deep-bed uni-
         formly graded  anthracite filters have been operated  reliably at rates  of  10 to  15 gpm/ft 2
         (24 to 37 m/h).
           Average  filtration rates  of roughly 2  to  7  gpm/ft 2 (5  to  17  m/h)  are  reported for  the
         upflow, biflow, and deep-bed filters discussed previously (Hamann and McKinney, 1968;
         Jung and Savage,  1974).
           Logsdon  et al.  (1993)  demonstrated that  deep-bed  monomedia direct filters could be
         operated  at filtration rates  up to 9 gpm/ft 2 on higher-turbidity waters  (up to 60 ntu) with
         proper chemical pretreatment and polymer filter aid selection. Filtration rates are impacted
         by water temperature.  Generally, when water temperatures drop below 45 ° F (8 ° C), wa-
         ter quality and filter run length deteriorate  in high-rate  filters  (Kawamura,  1999).  Many
         regulatory agencies  will  not approve  rates  in excess  of 4  to  5  gpm/ft 2 (10  m/h)  without
         successful pilot-scale testing. The designer should make every effort to obtain approvals
         for operation at higher rates. The quality of the raw water and extent of pretreatment will
         play a large role in the acceptable filtration rate.



         Filter  Operational  Control
         Filtration process  control  is  critical to  successful operation.  Decisions regarding control
         methods must be made early during the design because they affect the physical layout of
         the filtering facilities and its performance. Filter control may be predicated either on head
         loss through the filter bed or on the rate of filtration. In either case, smooth transition dur-
         ing changes in filtration rate is highly desirable. The adverse effects of sudden flow surges
         on filtered water quality have been well documented (Cleasby, Williamson, and Baumann,
         1963; Tuepker and Buescher,  1968).
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