采矿与安全工程学报
採礦與安全工程學報
채광여안전공정학보
JOURNAL OF MINING AND SAFETY ENGINEERING
2013年
4期
583-588
,共6页
刘石%许金余%刘志群%支乐鹏%陈腾飞
劉石%許金餘%劉誌群%支樂鵬%陳騰飛
류석%허금여%류지군%지악붕%진등비
岩石%高温%纵波波速%抗压强度%损伤
巖石%高溫%縱波波速%抗壓彊度%損傷
암석%고온%종파파속%항압강도%손상
rock mass%high temperature%longitudinal wave velocity%compressive strength%damage
通过单轴压缩试验,对经历不同温度(25~1000℃)后大理岩的纵波波速、抗压强度、破坏形态以及损伤特性随温度的变化规律进行研究。试验结果表明:高温后大理岩破坏时,沿轴向存在多个劈裂面,主要体现为劈裂破坏的模式;单轴抗压强度在100℃和400℃时有2次强化作用,从800℃左右,抗压强度开始急剧下降直至1000℃时,基本失去了承载能力;随着加热温度的升高,大理岩试样的纵波波速近似线性下降,损伤因子近似线性增加,反映了大理岩经历高温作用后内部性质的变化;岩石是由不同矿物组成的多晶体,高温环境下各种矿物性质的变化,在一定程度上影响着岩石高温后的物理力学性质。
通過單軸壓縮試驗,對經歷不同溫度(25~1000℃)後大理巖的縱波波速、抗壓彊度、破壞形態以及損傷特性隨溫度的變化規律進行研究。試驗結果錶明:高溫後大理巖破壞時,沿軸嚮存在多箇劈裂麵,主要體現為劈裂破壞的模式;單軸抗壓彊度在100℃和400℃時有2次彊化作用,從800℃左右,抗壓彊度開始急劇下降直至1000℃時,基本失去瞭承載能力;隨著加熱溫度的升高,大理巖試樣的縱波波速近似線性下降,損傷因子近似線性增加,反映瞭大理巖經歷高溫作用後內部性質的變化;巖石是由不同礦物組成的多晶體,高溫環境下各種礦物性質的變化,在一定程度上影響著巖石高溫後的物理力學性質。
통과단축압축시험,대경력불동온도(25~1000℃)후대리암적종파파속、항압강도、파배형태이급손상특성수온도적변화규률진행연구。시험결과표명:고온후대리암파배시,연축향존재다개벽렬면,주요체현위벽렬파배적모식;단축항압강도재100℃화400℃시유2차강화작용,종800℃좌우,항압강도개시급극하강직지1000℃시,기본실거료승재능력;수착가열온도적승고,대리암시양적종파파속근사선성하강,손상인자근사선성증가,반영료대리암경력고온작용후내부성질적변화;암석시유불동광물조성적다정체,고온배경하각충광물성질적변화,재일정정도상영향착암석고온후적물리역학성질。
Based on the uniaxial compressive test, the variation laws of longitudinal wave velocity, failure modes, compressive strength and damage property of marble specimens while experiencing dif-ferent temperatures among 25~1 000 ℃ were studied in this paper. The test results show that there are multiple splitting surfaces along the axial direction of marble after high temperatures, and the split fail-ure mode is the main destructive manner of marble. Meanwhile, the compressive strength of marble in-creases visibly at 100 ℃and 400 ℃, and then presents deterioration with the increase of temperature after 800 ℃. When the temperature reaches to 1 000 ℃, the marble nearly losses bearing capacity. Moreover, the longitudinal wave velocity declines linearly and the damage increases linearly with the increase of temperature, which reflects the changes to internal nature of marble after the high tempera-ture effects. Rock mass is aggregated with mineral components together, thus, the changes of mineral components under high temperatures, to some extent, can affect the physical and mechanical characte-ristics of rock mass.