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PERMFILE67045
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PERMFILE67045
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Last modified
8/24/2016 11:12:44 PM
Creation date
11/20/2007 9:40:41 PM
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Template:
DRMS Permit Index
Permit No
M2001035
IBM Index Class Name
Permit File
Doc Name
COPY OF PAGES FROM BOOK
Media Type
D
Archive
No
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Chapter 26 <br />RELATIONSHIP OF NOISE LEVEL TO TEMPERATURE PROFILE <br />EarIY Mornlny Mitl M\/ornlny Lele Morning Early Aaemoon <br />- CIeYO. TryO C> <br />t lap OI InrerNen u <br />moupe m bWre b <br />p,e..nl Q O <br />A. e. C. D. <br />Temperslure <br />A. sign end low temperature Inrenlone Present -sound Inlensilication refulla <br />B. Loner inrenlOn perllsllY disappean - sound intenellY near source diminnnltl- tocufing <br />al Inver nnpo <br />G. Surface lemperalure eaceeda nigM1esl upper elr Nmpenlure -sound not relurnad IP <br />surface oy relrecllon <br />p. Temparelure Inrenlom wiped out -upward rcfraclan copses minimum sound lanais a1 <br />ell dnlmco <br />the colder months because oC the higher u7nd speed that prevails <br />during this time of the year. In the warmer months wind speeds are <br />normally lower and help to prevent the formation of temperature <br />inversions by promoting mixing in the lower atmosphere. <br />Figure 26-P shows a composite of raw path diagrams calculated (rum <br />radiosonde data obtained from Kennedy Airport in New York Citv. <br />The ray paths were calculated at intervals of two degrees elevation. <br />Southerly winds caused downward refraction and produced high-noise <br />level conditions in the northwest, north, and northeast directions and <br />caused upward refraction and produced low-noise level conditions in <br />the southwest, south, and southeast directions. Normal sound levels <br />would occur in the easterlyand westerly directions as isovelocity con- <br />ditions yielded straight ray paths. Calculations such as these are ex- <br />pensive and rely on having access to nearby radiosonde data. Con- <br />stantly changing weather conditions and high cost make this ap- <br />proach impractical for most blasting operations. In critical operations <br />the use of a pilot charge orlow-frequency sound generator to calibrate <br />the atmosphere may be preferable. <br />Favorable atmospheric conditions for blasting: ~' <br />• Clear to partly cloudy skies with fleecy clouds, light winds and a <br />steadily increasing surface air temperature from daybreak to shot <br />time. Blast time should be delayed to midmorning to allow eazly <br />morning temperature inversion, if any, to be eliminated. <br />Unfavorable atmospheric conditions for blasting: <br />• Foggy, hazy, or smoky days with little or no wind. Condition typical <br />of temperature inversion and high air-pollution index. <br />• During strong winds accompanying passage of a cold front. <br />• During periods of the day when surface temperature is falling. <br />444 <br />Vibration and Air Blast <br />Overpressure Air Blasi Effect <br />dBL psi <br />181 3.0 Convenltonel structures severely damaged. <br />171 1.0 Most windows break. <br />161 0.3 <br />151 0.1 Some windows break. <br />141 0.03 Some large plate glass windows may break. <br /> USBM interim limit of allowable air blast 136 dBL <br />131 0.01 <br />dBL = 20 log F where Pp is the reference pressure of <br /> <br />0.0002 mlerober. The L signifies linear Irequency response. <br />rrgure co-u. a summary of the resuitc of many Stutliea on the effect of shock waves /mm <br />chemical explosions, nuclear explosions end supersonic elrerafl on ordinary structures. <br />• Too early in the morningor after sunset on clear days with very light <br />winds. <br />• Cloudy days with a low ceiling, especially when there is little or no <br />wind. <br />Air Blast Damage Levels. Many studies have been made on the <br />effects of shock waves From chemical explosions, nuclear explosions, <br />and supersonic aircraft on structures. These studies have established <br />that the most critical parts of ordinary structures to blast waves are <br />window panes. As a consequence, most damage criteria are presently <br />based on window pane breakage. A summary of the results of these <br />studies is given in Figure 26-Q. Because air blast data from blasting <br />operations frequently show considerable variation, the preferred ap- <br />proach is to take the steps recommended below to minimize the source <br />level, so that safe levels will be maintained even under adverse at- <br />mospheric conditions that cannot be reliably detected or avoided. <br />Methods of controlling air blast: <br />• Avoid [he use of unconfined explosives. <br />1. Bury detonating cord one foot or more. <br />2. Use ]ow•]oad detonating cord and bury a few inches or more if <br />necessary. <br />3. Do not mudcap in populated areas unless absolutely necessazy. <br />445 <br />~~ <br />• <br />
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