LIU Ai-wen, YU Yan-xiang, FU Chang-hua, CHEN Kun, ZHAO Ji-sheng, ZHOU Zheng-hua, WANG Wei, . Attenuationcharacteristicsandtopographiceffectof ascientificexplosionwith50texplosive[J]. Explosion And Shock Waves, 2010, 30(1): 21-26. doi: 10.11883/1001-1455(2010)01-0021-06
Citation: LIU Ai-wen, YU Yan-xiang, FU Chang-hua, CHEN Kun, ZHAO Ji-sheng, ZHOU Zheng-hua, WANG Wei, . Attenuationcharacteristicsandtopographiceffectof ascientificexplosionwith50texplosive[J]. Explosion And Shock Waves, 2010, 30(1): 21-26. doi: 10.11883/1001-1455(2010)01-0021-06

Attenuationcharacteristicsandtopographiceffectof ascientificexplosionwith50texplosive

doi: 10.11883/1001-1455(2010)01-0021-06
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  • Corresponding author: LIU Ai-wen
  • Publish Date: 2010-01-25
  • Vibrationattenuationandtopographiceffectweremonitoredneartheexplosionplaceof50t explosive.Basedontherecordedvibrationsignals,theattenuationsofverticalvelocityandaccelerationwereanalyzedwiththeSadauskasformula. Therapidattenuationofvibrationwasrelatedwith thelayeredmoderate-hardnessrocksandthelocalterrainandgully.Thetime-frequencydistribution ofthevibrationwasobtainedbythediscretewavelettransform (db8wavelet).Thefrequencyofvibrationenergyconcentrationwasreducedandthedurationofthevibrationwasprolongedwiththeincreaseofthedistancefromt eexplosioncenter.AccordingtotheChineseSeismicIntensityScale,the vibrationintensityclosetotheexplosioncenterisuptoⅦ,however,theblastingvibrationintensity decayfasterthantheattenuationofearthquakeintensity.Thetopographiceffectwasdiscussedby comparingthevibrationrecordsatdifferentlocationsofa14-m-highhill.Duetothefocusingvibrationenergyofthehill, thepeakaccelerationonthetopofthehillis2.4timeslargerthanthatatthe footofthehill,andthespecialfrequencybandswiththeenlargedamplitudeisrelatedwiththesize andtheheightofthehill.Thefigureofparticlemotionsindicatesthatthelateralswingandrotational motiongraduallyincreasefromthefoottothetopofthehill.
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