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                                                                                                   5.7 Location  181

                                              +
                                           Cumulative departures of mean daily temperatures from 32°F  0  Freezing index, F









                                                                               Figure 5.11 Determination of the Freezing
                                                        Time in days
                                                                               Index of Soils as the Cumulative Departure of
                                                                               the Mean Daily Temperature from 32 F.

                                         where d is the depth of frozen soil, in.; and F, the freezing index, is the algebraic difference
                                         between the maximum positive and maximum negative cumulative departures, 	(T   32),
                                                                                                           d
                                          of the daily mean temperatures (T ) from 32 F. Accumulation, as shown in Fig. 5.11, begins
                                                                    d
                                          with the first day on which a freezing temperature is recorded. In concept, the freezing index
                                          is analogous to the degree day, which describes the heat requirements of buildings during
                                          the heating season. The authors of this book have developed the following frost depth equa-
                                          tion using the SI units:
                                                                d   55.18F 0.468   (SI units)               (5.41b)
                                         where d is the depth of frozen soil, mm; and F is the freezing index, which is the algebraic
                                         difference between the maximum positive and maximum negative cumulative departures,
                                         	(T   0), of the daily mean temperatures (T ) from 0 C.
                                                                              d
                                             d
                                             In the absence of daily readings, the value of F may be approximated, in North
                                         America, from the mean monthly temperatures as follows:
                                                        F   (32n   	T )30.2     (U.S. Customary Units)      (5.42a)
                                                                     m
                                                        F   (0   	T )30.2       (SI Units)                  (5.42b)
                                                                   m
                                         Here n is the number of months during which the temperature is less than 32 F (0 C); 	T m
                                         is the sum of the mean temperatures  F during each of these months; and 30.2 is the mean
                                         number of days in December, January, February, and March.
                                             Pipes laid at depths of 2 to 3 ft (0.60 to 0.90 m) are safe from extremes of heat and or-
                                         dinary mechanical damage, but it is wise to go to 5 ft (1.5 m) in streets or roads open to
                                         heavy vehicles. Otherwise, structural characteristics of conduits determine the allowable
                                         depth of cover or weight of backfill. Some conduits may have to be laid in open cut to keep
                                         the depth of backfill below the maximum allowable value.





                     EXAMPLE 5.12  FREEZING INDEX AND FROST DEPTH DETERMINATION
                                         The following are the average consecutive 2-week temperature records of a typical coldest month.
                                         Day    1   2   3   4    5     6    7     8    9    10   11  12  13   14
                                         T d ,  F 35  37  37  30  28   25   29   30    24   36   40  40  42   45
                                         T d ,  C 1.67 2.78 2.78  1.11  2.22  3.88  1.66  1.11  4.44 2.22 4.44 4.44 5.55 7.22

                                             Determine the freezing index and the required minimum frost depth.
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