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Impacts & Controls for Blast Noise , 2.3 coot' <br />v,rgres m Ef loco and Eadmiffi t <br />d8-i. PSI kPa <br />180 2.90000 20.0000 <br />170 0.91708 8.3246 <br />180 02WW 2.0000 <br />150 0.09171 0.8325 <br />140 0.AM 62000 <br />134 0.01453 0.10021 <br />120 0.00290 0.0200 <br />110 o.00092 0.0063 <br />100 0.00029 0.0020 <br />90 0.00009 0.0006 <br />6o 0.00003 0.0002 <br />ShWkNal Damage <br />Most VAndowe Break <br />Some Wbub" Break <br />osHA Maximum for Impulse Sound <br />Pressure Produced by 20 mph wind <br />OSHA Maximum for 8 Hours <br />Figure 2.6--0verpressure Effects and Scale Comparisons <br />2.3-2 CentrOUlog Air Oveepressare: <br />It is dillicult to accurately predict airblast with distance. Unlike vibration predictions <br />where seismic energy is generally proportional to the weight of a confined charge, airblast <br />is caused by venting gases, moving rock and the vertical component of vibrating ground, <br />which are hard to predict. It is well known that airblast intensity is reduced when blast <br />charges are well confined. Conversely, when charges are poorly confined due to <br />inadequate stemming or by prematurely breaching through open cracks, the level of <br />airblast is increased. As previously recommended in Section 2.1.4, AG has recommended <br />that at least two feet of dirt be placed over all blastholes before shooting. The confinement <br />provided by this dirt will reduce flyrock and it will also buffer the blast noise. <br />The fc nowing equation developed iii a US Bureau of Mines Study (RI 8485), airblast can <br />be used to estimate overpressure, based on charge weight and distance. <br />Overpressure W = 52.7(D/W°'" 31.067 Equation 3.2 <br />22