河南理工大学学报:自然科学版
河南理工大學學報:自然科學版
하남리공대학학보:자연과학판
JOURNAL OF HENAN POLYTECHNIC UNIVERSITY
2011年
4期
401-405
,共5页
非均匀性%裂纹贯通%红外热像%花岗岩
非均勻性%裂紋貫通%紅外熱像%花崗巖
비균균성%렬문관통%홍외열상%화강암
heterogeneity%fracture coalescence%infrared thermal imaging system%granite
采用花岗岩材料通过红外热像和数值实验的方法,对两预制裂纹导致的岩石中新裂纹孕育、繁衍、萌生、扩展和贯通机制,以及由此引起的试样宏观强度变化等进行分析.通过红外热像遥感观测方法以及数值模拟对7块预制双裂纹的试样进行了实验研究.结果表明,裂纹扩展过程中,脆性破裂的声发射前兆不明显,在主破裂发生之前有小规模声发射现象,但释放的能量不多,只有在主破裂发生时产生大量声发射,特别是岩爆类型的破坏.试样破裂过程中有红外异常现象,在破裂处会出现明显的高温区和高温条带,并指出斑状花岗岩在破裂前主要表现为高温前兆.
採用花崗巖材料通過紅外熱像和數值實驗的方法,對兩預製裂紋導緻的巖石中新裂紋孕育、繁衍、萌生、擴展和貫通機製,以及由此引起的試樣宏觀彊度變化等進行分析.通過紅外熱像遙感觀測方法以及數值模擬對7塊預製雙裂紋的試樣進行瞭實驗研究.結果錶明,裂紋擴展過程中,脆性破裂的聲髮射前兆不明顯,在主破裂髮生之前有小規模聲髮射現象,但釋放的能量不多,隻有在主破裂髮生時產生大量聲髮射,特彆是巖爆類型的破壞.試樣破裂過程中有紅外異常現象,在破裂處會齣現明顯的高溫區和高溫條帶,併指齣斑狀花崗巖在破裂前主要錶現為高溫前兆.
채용화강암재료통과홍외열상화수치실험적방법,대량예제렬문도치적암석중신렬문잉육、번연、맹생、확전화관통궤제,이급유차인기적시양굉관강도변화등진행분석.통과홍외열상요감관측방법이급수치모의대7괴예제쌍렬문적시양진행료실험연구.결과표명,렬문확전과정중,취성파렬적성발사전조불명현,재주파렬발생지전유소규모성발사현상,단석방적능량불다,지유재주파렬발생시산생대량성발사,특별시암폭류형적파배.시양파렬과정중유홍외이상현상,재파렬처회출현명현적고온구화고온조대,병지출반상화강암재파렬전주요표현위고온전조.
An experimental research of the infrared thermal image in the process of rock fracture was carried out.The study used the granite with the double crack objection analyze the crack initiation,propagation,coalescence,interaction,and the change of macro-strength leaded by them.I did the infrared thermal image examination and numerical simulation for 7 granite sample with double crack to view the regularity of rock failure.The results evince that the AE prognostic of rock's brittleness fracture is not obviously.There will be small scale AE phenomenon before the rock's main fracture,and they release a little energy.When the rock happens the main failure,it will bring out lots of AE,especially in rock burst.The event of experiment confirmed that there are infrared abnormal phenomenon during the rock facture process,and the high temperature realm or stripe at the fracture field.The experiment results indicated that the infrared characteristic of porphyritic texture granite before failure represents the high temperature prognostic.