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)