平顶山矿区煤岩冲击试验及冲击地压预测研究
详细信息    本馆镜像全文|  推荐本文 |  |   获取CNKI官网全文
摘要
随着矿山开采深度的不断增大,冲击地压问题越来越严重,已经成为制约矿山生产和安全主要重大灾害之一。本文结合平顶山矿区实际地质条件、煤层条件及开采技术条件情况,对冲击地压发生的影响因素、预测及防治进行研究。
     采用弹性能指数、冲击能指数、动态破坏时间及弯曲能量指数对平顶山矿区部分矿井主要煤层及顶、底板冲击倾向性进行研究,得出各煤层及顶、底板大多具有中等或者弱冲击倾向性;与此同时,对煤在单轴压缩破坏及加、卸载以及煤层顶底板在单轴压缩及弯曲破坏各个阶段的声发射特性进行研究,得出煤、岩在破坏前声发射大多有一个“平静期”,为冲击地压的预测预报提供依据。
     针对发生冲击地压地点,对冲击地压影响因素进行分析。采用FLAC2D数值模拟软件对煤层硬度及坚硬顶板距煤层的距离对冲击地压的影响进行模拟,得出在一定范围内,坚硬厚层砂岩顶板距离煤层的距离越近,越容易发生冲击地压;煤体越硬,煤体应力集中程度越高。
     采用综合指数法对发生冲击地压的己15-16-24110工作面进行预测,得出该工作面具有中等冲击危险;与此同时,在该工作面机、风巷进行钻屑法现场试验,预测支承压力对冲击地压的影响,认为风巷在支承压力影响范围内,都具有冲击危险,而机巷在距采面30m内具有冲击危险,30m外冲击危险逐渐减弱。
With the increasing depth of mining, rock burst is becoming more and more serious. It has become a major disaster for the production and safety of mining. The influences, prediction and prevention of rock burst were studied in this thesis, based on the real geological, coal seam and mining technology conditions in Pingdingshan coal area.
     The rock burst tendency of coal and its roof and floor in Pingdingshan were studied, using the elastic energy index, burst energy index, dynamic failure duration and bending energy index. The tests concluded that most coal seams and their roofs and floors have moderate or weak rock burst tendency. The acoustic emission under uniaxial compression damage and loading and unloading for coal seams was studied, as well as the uniaxial compression damage and flexural failure for its roof and floor. It concluded that most samples had a“quiet period”before damage. This conclusion provided a basis for the forecasting of rock burst.
     The factors of rock burst at the location of bump were studied. Through numerical simulation software of FLAC2D, the effects of coal bed hardness and the distance from hard and thick roof to coal seam on rock burst were studied. The distance from hard and thick roof to coal seam is closer, the rock burst is more likely to appear. The harder of coal seam, the higher of the stress in coal seam.
     The shock hazard of J15-16-24110 was predicted with composite index method, and moderate rock burst tendency appears in this working face. Meanwhile, the cuttings tests were conducted in the headway and gateway of the working face, and abutment pressure effect to shock hazard were predicted. It concluded that shock hazard appears in gateway under abutment pressure, it appears in headway within 30m to the working face, and becomes weaker beyond 30m to the working face.
引文
[1]谢和平.深部高应力下的资源开采──现状、基础科学问题与展望.见香山科学会议编.科学前沿与未来[C].北京:中国环境科学出版社,2002,179-191
    [2]郭然,潘长良,于润沧.有岩爆倾向性硬岩矿床采矿理论与技术[M].北京:北京冶金工业出版社,2003
    [3]煤炭部矿山压力科技情报中心站冲击地压分站,冲击地压机理研究与防治经验文集(全国冲击地压会议资料)1985年11月
    [4] Tan Jiong Kie Rockburst.Case Record.Theory and Control.Proceedings of the international symposium on engineering in complex rock formations[J]. Min.Sci,1986:33-37
    [5]侯发亮,贾愚如.地下硐室中岩爆与围岩应力的关系[M].复杂岩石中建筑物国际学术研讨会论文集,1989
    [6] Cook N G W.A note on rock bursts considered as a problem of stability[J].J.South Afr Int.Min and Metallurgy,1965,65:437-446.
    [7] Wawersik W K and Fairhurst C A.A study of brittle rock fracture in laboratory compression experiments[J].Int.J.Rock Mech.Min.Sci.&Geomech.Abstr,1970,7:561-575
    [8] Hudson J A,Croush S L,Fairhurst C.Soft,stiff and servo-controlled testing machines: a review with reference to rock failure[J].Eng.Geo,1972,6:155-189
    [9]耿乃光,陈颙,姚孝新.拼合岩石样品破裂的初步研究[J].地球物理学报,1981(24),No.2:238-241
    [10] Bieniawski Z T,Mechanism of brittle fractute of rocks[J].PartⅠ,Ⅱ, andⅢ.Int.J.Rock Mech.Min.Sci,1967,6:395-430
    [11] Bieniawski Z T,Denkhaus H G,Vogler U W.Failure of Fracture Rock[J].Int.J.Rock Mech.Min.Sci,1969,6:323-341
    [12]中华人民共和国煤炭部.中华人民共和国煤炭行业标准[M].北京:煤炭工业出版社,2000
    [13]张万斌,王淑坤,滕学军.我国冲击地压的研究与防治进展[J].煤炭学报,1992,17(3):27-35
    [14] Kleczek&Zorychta A.Coal Bumps by Mining Tremor[J].Rockburst and Seismicity in Mines,Young(ed).Rotterdan,1993:87-89
    [15]佩图霍夫等著,段克信译《冲击地压和突出的力学计算方法》[M].北京:煤炭工业出版社,1994
    [16]章梦涛,徐曾和,潘一山.冲击地压和突出统一失稳理论[J].煤炭学报,1991(4):48-53
    [17]章梦涛.冲击地压失稳理论与数值模拟计算[J].岩石力学与工程学报,1987(3):197-204
    [18]潘一山,章梦涛.冲击地压失稳理论的解析分析[J],岩石力学与工程学报1996(15):504-510
    [19]齐庆新,史元伟,刘天泉.冲击地压粘滑失稳机理的实验研究[J].煤炭学报,1997,vol.29(6):633-636
    [20]谢和平,Pariseau W G.岩爆的分形特征及机理[J].岩石力学与工程学报,1993,12(1):28-37
    [21]李延介等.岩石裂纹的分形特征及岩爆机理研究[J].岩石力学与工程学报,2000(1):6-10
    [22]伊光志,李贺等.煤岩体失稳的突变理论模型[J],重庆大学学报1994(1):23-28
    [23]潘一山,章梦涛.用突变理论分析冲击地压发生的物理过程[J].阜新矿业学院学报,1992,11(1):12-18
    [24]张晓春等.三河尖煤矿冲击矿压发生机理分析[J]岩石力学与工程学报,1998(5):508-513
    [25]张晓春等.冲击矿压的层裂板模型及实验研究[J].岩石力学与工程学报,1999(5):497-502
    [26]张晓春,杨挺青等.冲击矿压的模拟实验研究[J].岩土工程学报,1999(1):66-70
    [27]缪协兴.岩(煤)壁中滑移裂纹扩展的冲击矿压模型[J].中国矿业大学学报,1999 Vol.28(2):113-117
    [28]宋维源,潘一山.冲击地压的混沌学模型及预测预报[J].煤炭学报,2001,26(1):26-30
    [29]谈云亮.岩层运动非线性动力学预测基本框架[J].中国地质灾害与防治学报,2002,(2)
    [30]潘立友.冲击地压前兆信息的可识别性研究及应用[J].岩石力学与工程学报,2004,23(8):1411-1415
    [31]谭云亮等.冲击地压声发射前兆式初步研究[J].岩石力学与工程学报,2000,19(4):425-428
    [32]纪洪广,王金安,蔡美峰.冲击地压事件物理特征与几何特性的相关性与统一性[J].煤炭学报,2003,28(1):31-36
    [33]杨正华,吴兴荣,井顺泉.煤层卸载爆破在冲击矿压防治中的应用[J].江苏煤炭,2000,(4),7-8
    [34]潘一山等.煤体振动方法防治冲击地压的机理研究[J].岩石力学与工程学报,1999,18(4):432-436
    [35]潘一山,李中华,章梦涛.我国冲击地压的分布、类型、机理及防治研究[J].岩石力学与工程学报,2003,22(11):1844-1851
    [36]关杰,孙可明,朱月明.急倾斜煤层开采解放层防治冲击地压数值模拟[J].辽宁工程技术大学学报,2002,21(4):411-413
    [37]李国宏等.利用卸压钻孔防治冲击矿地压的实践[J].煤矿安全,2004,35(11):8-10
    [38]章梦涛.我国冲击地压预测和防治[J].辽宁工程技术大学学报,2001,20(4):434-435
    [39]陈绍杰,郭惟嘉等.煤层冲击倾向性试验研究[J].矿业安全与环保,2007,34(2):10-14
    [40]孙成栋.岩石声学测试[M].北京:地质出版社,1981年
    [41] ke W.Microseismic applications for mining-a practical guide[R] U S:Bureau of Mines,l982
    [42]腾山邦久.声发射(AE)技术的应用[M].冯夏庭译.北京:冶金工业出版社,1996
    [43] Mogi K. Study of elastic shocks caused by the fracture of betterogeneous material and its relation to earthquake phenomena[J]. Bull.of the Earthquake Res. Inst.,1962,40:168–180
    [44] Holcomb D J. Using acoustic emissions to determine in-situstress:problems and promise[J]. Geomechanics,ASME,1983,57:11–21
    [45] Holcomb D J,Costin L S.Detecting damage surfaces in brittlematerials using acoustic emissions[J].Transactions of the ASME,1986,53:536–544
    [46] Mu Y H,Yang Q,Yao Y X,et al. Monitoring of grinding process with acoustic emission signals[J].Journal of Harbin Institute ofTechnology,1994,1(2):48–51
    [47] Chang S H,Lee C I.Estimation of cracking and damage mechanismsin rock under triaxial compression by moment tensor analysis of acoustic emission[J]. International Journal of Rock Mechanics andMining Sciences,2004,41:1 069–1086
    [48] Mansurov V A. Acoustic emission from failing rock behavior[J]. RockEngng.,1994,27(3):173–182
    [49]张晖辉,颜玉定,余怀忠,等.循环载荷下大试件岩石破坏声发射实验—岩石破坏前兆的研究[J].岩石力学与工程学报,2004,23(21):3621-3628
    [50]余贤斌,谢强,李心一等.直接拉伸、劈裂及单轴压缩试验下岩石的声发射特性[J].岩石力学与工程学报,2007,26(1):137-142.:137-142.
    [51]李庶林,尹贤刚,王泳嘉等.单轴受压岩石破坏全过程声发射特征研究[J].岩石力学与工程学报,2004,23(15):2499–2503.
    [52]张茹,谢和平,刘建锋等.单轴多级加载岩石破坏声发射特性试验研究[J].岩石力学与工程学报,2006,25(12):2584–2588.
    [53]刘保县,赵宝云,姜永东.单轴压缩煤岩变形损伤及声发射特性研究[J].地下空间与工程学报,2007,3(4):647-650
    [54]杨永杰,陈绍杰,韩国栋.煤样压缩破坏过程的声发射试验[J].煤炭学报,2006,31(5): 362-365
    [55]王恩元,何学秋,刘贞堂等.煤体破裂声发射的频谱特征研究[J].煤炭学报,2004,29(3): 289-292.
    [56]窦林名,何学秋.煤岩冲击破坏模型及声电前兆判据研究[J].中国矿业大学学报,2004,33(5): 504-508.
    [57]李元辉,袁瑞甫,赵兴东.不同应力路径对岩石声发射Kaiser效应的影响[J].东北大学学报(自然科学版),2007, 28(4): 476-479
    [58]李俊平,周创兵.岩体的声发射特征试验研究[J].岩土力学,2004,25()3):374-378
    [59]张广清,金衍,陈勉.利用围压下岩石的凯瑟效应测定地应力[J].岩石力学与工程学报,2002, 21(3): 360–363.
    [60]窦林名,何学秋.冲击矿压防治理论与技术[M].徐州:中国矿业大学出版社, 2001 .
    [61]阿维尔申Cr .冲击矿压[M].北京:煤炭工业出版社,1959.
    [62]赵本均.冲击矿压及防治[M].北京:煤炭工业出版社,1995.20(4):434-435.2003
    [63]陈炎光,钱鸣高.中国煤矿采场围岩控制[M].北京:煤炭工业出版社,1994:165 -166.
    [64]窦林名,赵从国,杨思光等.煤矿开采冲击矿压灾害防治[M].徐州:中国矿业大学出版社,2006:1-109.
    [65]钱鸣高,石平五.矿山压力与岩层控制[M].徐州:中国矿业大学出版社,2004:294-330.
    [66]闵长江,卜凡启,周廷振等.煤矿冲击矿压及防治[M].徐州:中国矿业大学出版社,1998: 1-10.
    [67] DUBINSKI J, KONOPKO W. Tapnia-ocena, prog-noza,zwalczanie[M].Katowice:Glowny I nstytut,Gornictwa,2000:1-20.
    [68] KONOPKO W.Doswiadczalne podstawy kwalifikow-ania wyrobisk gorniczych w kopalniach wegla kamien-nego do stopni zagrozenia tapaniami[J].Prace Naukowe GIG,1994,795:81-93.
    [69]王伟,王恩元.岩爆预测技术综述及发展分析[J].矿业安全与环保,2003,30(4):12-15
    [70]窦林名,何学秋.煤矿冲击矿压的分级预测研究[J].中国矿业大学学报,2007,36(6) 717-722
    [71]潘立友,张立俊,刘先贵.冲击地压预测与防治实用技术[M].徐州:中国矿业大学出版社,47-53.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700