62
MILLER AND SARTOR
The values of r,,(100), r/,(100), Tor Tip» Ko, and Dq for each
station are summarized in Table 8. The value of Ky in Table 8 for
Stations having more than one estimated value of K) in Table 7is a
median value. The terrain about the stations generally increased in
roughness! proceeding from station 100 to station 707; however, this
general increase in roughness is not reflected in a corresponding
general decrease in Dq values for these stations. At the stations of
the 800 series, the terrain was fairly smooth andflat at stations 813
and 814 and somewhat rougher at stations 815 and 816. The terrain
features at the remainder of the stations were varied. At the stations
in series
100 through 800,
the GITR’s were calibrated to have a
response factor, D, near unity; thus for these stations the computed
value of Dq is practically equal to q. For the other stations the response factor for the instruments and monitor has not been reported,
but it is assumed to be about 0.7. Therefore, where the computed
value of Dq is in excess of 0.7, either the I, value is too large or the
A, value is too small (i.e., the r;, value is too small).
Table 8—SUMMARY OF CALCULATED rip, rfp, Ky, AND Dq VALUES*
FOR THE SMALL BOY SHOT FALLOUT-COLLECTING STATIONS
Station and
sample No.
Ko,
r/hr at lhr
kt/sq mile
r,,,(100)
rf, (100)
Th
Te,
Dq
100
101
103
0.338
0.355
(0.403)
0.369
0.425
(0.443)
0,194
0.204
(0.232)
u.304
0.346
(0.361)
S11
589
995
0.667
0.731
0.650
200
201
202
203
204
207
209
0.456
0.340
(0.340)
0.341
(0.343)
(0.363)
(0.383)
0.469
0.398
(0.400)
0.400
(0.405)
(0,433)
(0.438)
0.262
0.195
(0.196)
0.196
(0.197)
(0.209)
(0.220)
0.382
0.324
(0.326)
0.326
(0,330)
(0.353)
(0.357)
758
494
530
515
D15
540
578
0.724
0.642
0.685
0.666
0.663
0.678
0.665
300
(0.343)
0.691
303
305
309
311
0.335
0.338
(0,343)
(0.363)
(0.352)
0.361
0.381
(0.405)
(0.433)
(0.197)
(0.287)
519
485
518
531
349
0.640
0.673
0.684
0.665
400
401
403
405
407
409
(0.339)
0.344
0.346
0.350
0.350
(0.383)
(0.352)
0.354
0.357
0.362
0.362
(0.400)
(0.195)
0.198
0,199
0,202
0.202
(0.220)
(0.287) —
0,289
0.291
0.295
0.295
(0.326)
351
44]
961
590
945
589
0.717
0,564
0.715
0.741
0.684
0.678
901
502
303
0.362
(0.355)
0.350
0.378
(0,372)
0.362
0.208
(0.204)
0.202
0.308
(0.303)
0.295
549
540
530
0.669
0.671
0.665
0,192
0.195
(0.197)
(0,209)
0.294
0.310
(0.330)
(0.353)
(Table 8 continues on page 63)