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:
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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
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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:
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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
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Attenuationcharacteristicsandtopographiceffectof ascientificexplosionwith50texplosive
- 1.
InstituteofGeophysics,ChinaEarthquakeAdministration,Beijing100081,China;
- 2.
InstituteofEngineering Mechanics,ChinaEarthquakeAdministration,
More Information
- Corresponding author:
LIU Ai-wen
- Publish Date:
2010-01-25
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Abstract
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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References
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