用高密度电法勘探预判钻孔应变观测点岩石完整性

doi:10.3969/j.issn.0253-4967.2013.04.010

地震地质 ›› 2013, Vol. 35 ›› Issue (4): 805-816.DOI: 10.3969/j.issn.0253-4967.2013.04.010

用高密度电法勘探预判钻孔应变观测点岩石完整性

邱泽华¹, 张国宏¹, 张宝红¹, 唐磊¹, 宋乃波², 郭燕平¹, 周龙寿¹, 赵京轶¹, 苏文浩¹

1 中国地震局地壳应力研究所, 北京 100085;
2 山西省地震局, 太原 030021

收稿日期:2013-07-18 修回日期:2013-07-18 出版日期:2013-12-30 发布日期:2014-01-03
基金资助:
中国地震局地震行业科研专项（201108009）和中国地震局地壳应力研究所基本科研业务专项（ZDJ201109）共同资助

PROSPECTING UNDERGROUND CONDITION FOR BOREHOLE STRAIN-MONITORING LOCATION BY MEANS OF RESISTIVITY IMAGING SURVEY

QIU Ze-hua¹, ZHANG Guo-hong¹, ZHANG Bao-hong¹, TANG Lei¹, SONG Nai-bo², GUO Yan-ping¹, ZHOU Long-shou¹, ZHAO Jing-yi¹, SU Wen-hao¹

1 Institute of Crustal Dynamics, China Earthquake Administration, Beijing 100085, China;
2 Earthquake Administration of Shanxi Province, Taiyuan 030021, China

Received:2013-07-18 Revised:2013-07-18 Online:2013-12-30 Published:2014-01-03

摘要/Abstract

摘要： 钻孔应变观测是一种重要的地球动力学研究手段，具有广泛的用途。但是，建立钻孔应变观测点的费用比较高，而成功率又不够高，限制了这种观测的普遍推广。一些观测点的失败，其主要原因是钻孔条件不理想，即仪器安装深度岩石破碎。因为钻孔费用高，所以即使钻孔后发现岩石条件没有达到要求，往往也只能勉强安装仪器。要解决这个问题，就要事先对场地岩石条件进行预判。岩石裂隙通常都含有裂隙水，会降低其电阻率。高密度电法勘探对地下岩石的电阻率有比较高的分辨率，用这种方法在山西的上皇庄、东马坊和交口3个观测点建设中进行了实验。其中，在上皇庄拉了1条测线，东马坊和交口分别拉了2条互相垂直的测线。在上皇庄打了3个钻孔，其他2个点分别只有1个。5个钻孔和取心的岩石强度实验结果以及仪器安装情况，都与勘探结果相符，这表明高密度电法是一个有效的预判岩石完整性的手段。要防止钻孔打在破碎带上，就要避开电法勘探显示的低阻区。

关键词: 钻孔应变仪, 高密度电法勘探, 岩石完整性, 低阻区

Abstract: Borehole strain monitoring is an important geodetic means with a wide range of use in geodynamics research. One of the main reasons for the slow development of this kind of observation is that the establishment of a borehole strain monitoring site is costly and the success rate is not very high. Some sites fail due to the unfavorable borehole conditions,that is,rocks at the depth where the sensor is embedded are not intact but fractured. Sometimes even if the rocks were found not as good as required,the instrument had to be installed because of the expansive cost in drilling the hole. To solve the problem,it is necessary to prospect the rock condition of the site before drilling. Fractured rocks usually contain ground water in the fractures,which lower the rocks' resistivity. Resistivity imaging survey can be applied to the investigation of underground condition and give local distribution of resistivity with relatively high resolution. Three experiments have been carried out in Shanxi Province,in which single profiling is done at Shanghuangzhuang,cross profilings at Dongmafang and at Jiaokou,respectively. Three boreholes at Shanghuangzhuang and one at Dongmafang and at Jiaokou each were drilled for comparison of different types of instruments. Results of rocks strength experiments and instrument installations for the five boreholes agree well with results of the surveys. It suggests that resistivity imaging survey is an effective method to predict the underground condition of rocks. Instrument installation should avoid low-resistivity zones indicated by the profiling to prevent putting the sensor into fractured rocks.

Key words: borehole strainmeter, resistivity imaging survey, rock condition, low resistivity zone

中图分类号:

P613.3⁺25

邱泽华, 张国宏, 张宝红, 唐磊, 宋乃波, 郭燕平, 周龙寿, 赵京轶, 苏文浩. 用高密度电法勘探预判钻孔应变观测点岩石完整性[J]. 地震地质, 2013, 35(4): 805-816.

QIU Ze-hua, ZHANG Guo-hong, ZHANG Bao-hong, TANG Lei, SONG Nai-bo, GUO Yan-ping, ZHOU Long-shou, ZHAO Jing-yi, SU Wen-hao. PROSPECTING UNDERGROUND CONDITION FOR BOREHOLE STRAIN-MONITORING LOCATION BY MEANS OF RESISTIVITY IMAGING SURVEY[J]. SEISMOLOGY AND GEOLOGY, 2013, 35(4): 805-816.

参考文献

蔡晶晶, 阎长虹, 王宁, 等.2011.高密度电法在地铁岩溶勘察中的应用［J］.工程地质学报, 19(6): 935—940.
CAI Jing-jing, YAN Chang-hong, WANG Ning, et al.2011.Application of high-density resistivity method to karst investigation of metro engineering［J］.Journal of Engineering Geology, 19(6): 935—940(in Chinese).
池顺良, 池毅, 邓涛, 等.2009.从5.12汶川地震前后分量应变仪观测到的应变异常看建设密集应变观测网络的必要性［J］.国际地震动态, 1: 1—13.
CHI Shun-liang, CHI Yi, DENG Tao, et al.2009.The necessity of building national strain-observation network from the strain abnormality before Wenchuan earthquake［J］.Recent Developments in World Seismology, 1: 1—13(in Chinese).
邓凯, 沈云发, 张玉池.2O12.综合物探方法在高速公路岩溶塌陷探测中的应用分析［J］.工程地球物理学报, 9(1): 54—57.
DENG Kai, SHEN Yun-fa, ZHANG Yu-chi.2012.Application of integrated geophysical exploration method to detecting karst collapse of the highway［J］.Chinese Journal of Engineering Geophysics, 9(1): 54—57(in Chinese).
董浩斌, 王传雷.2003.高密度电法的发展与应用［J］.地学前缘, 10(1): 171—176.
DONG Hao-bin, WANG Chuan-lei.2003.Development and application of 2D resistivity imaging surveys［J］.Earth Science Frontiers, 10(1): 171—176(in Chinese).
杜良, 葛宝, 朱丽丽, 等.2012.综合物探技术在隐伏断层探测中的研究与应用［J］.工程勘察, 40(1): 81—85.
DU Liang, GE Bao, ZHU Li-li, et al.2012.The research and application of comprehensive geophysical exploration technique to buried fault detection［J］.Geotechnical Investigation & Surveying, 40(1): 81—85(in Chinese).
顾功叙.1990.地球物理勘探基础［M］.北京: 地质出版社.63—73.
GU Gong-xu.1990.Introduction to Geophysical Prospecting［M］.Geological Publishing House, Beijing.63—73(in Chinese).
马德锡, 赵玉锁, 陈孝强, 等.2004.在金矿勘探中应用STING-SWIFT高密度电法［J］.黄金地质, 4: 70—74.
MA De-xi, ZHAO Yu-suo, CHEN Xiao-qiang, et al.2004.Application of STING-SWIFT high-density resistivity method in gold deposit prospecting［J］.Gold Geology, 4: 70—74(in Chinese).
邱泽华, 马瑾, 池顺良, 等.2007.钻孔差应变仪观测的苏门答腊大地震激发的地球环型自由振荡［J］.地球物理学报, 50(3): 797—805.
QIU Ze-hua, MA Jin, CHI Shun-liang, et al. 2007.Earth's free torsional oscillations of the great Sumatra earthquake observed with borehole shear strainmeter［J］.Chinese J Geophys, 50(3): 797—805(in Chinese).
邱泽华, 石耀霖. 2004.观测应变阶在地震应力触发研究中的应用［J］.地震学报, 26(5): 481—488.
QIU Ze-hua, SHI Yao-lin.2004.Application of observed strain steps to the study of remote earthquake stress triggering［J］.Acta Seismologica Sinica, 17(5): 534—541.

邱泽华, 唐磊, 张宝红, 等.2012.用小波一超限率分析提取宁陕台汶川地震体应变异常［J］.地球物理学报, 55(2): 538—546.
QIU Ze-hua, TANG Lei, ZHANG Bao-hong, et al.2012.Extracting anomaly of the Wenchuan earthquake from the dilatometer recording at NSH by means of Wavelet-Overrun Rate Analysis［J］.Chinese J Geophys, 55(2): 538—546(in Chinese).
邱泽华, 张宝红, 池顺良, 等.2010.汶川地震前姑咱台观测的异常应变变化［J］.中国科学(D辑), 40(8): 1040—1047.
QIU Ze-hua, ZHANG Bao-hong, CHI Shun-liang, et al.2011.Abnormal strain changes observed at Guza before the Wenchuan earthquake［J］.Science in China(Ser D), 54(2): 157—314.

王喜迁, 孙明国, 张皓, 等.2011.江玉乐高密度电法在岩溶探测中的应用［J］.煤田地质与勘探, 39(5): 72—75.
WANG Xi-qian, SUN Ming-guo, ZHANG Hao, et al.2011.Application of high-density electrical technique in karst detection［J］.Coal Geology & Exploration, 39(5): 72—75(in Chinese).
王振兴, 李向全, 侯新伟, 等.2012.太行山前严重缺水地区地下水勘查实践: 以灵寿县丘陵区为例［J］.南水北调与水利科技, 10(3): 127—132.
WANG Zhen-xing, LI Xiang-quan, HOU Xin-wei, et al.2012.Groundwater exploration in serious water shortage area of Taihang piedmont: A case study in the hilly area of Lingshou County［J］.South-to-North Water Transfers and Water Science & Technology, 10(3): 127—132(in Chinese).
肖川, 张义平, 缪玉松, 等.2012.高密度电法探测煤矿地下水及溶岩空洞效果［J］.科学技术与工程, 12(17): 4261—4265.
XIAO Chuan, ZHANG Yi-ping, MIAO Yu-song, et al.2012.Application of high-density electrical method to detecting groundwater and cave in coal mine［J］.Science Technology and Engineering, 12(17): 4261—4265.
张建锋, 李国敏, 张元, 等.2012.塔河下游间歇性输水河道附近地下水位动态响应［J］.地球物理学报, 55(2): 622—630.
ZHANG Jian-feng, LI Guo-min, ZHANG Yuan, et al.2012.Responses of groundwater levels to intermittent water transfer in the lower Tarim River［J］.Chinese J Geophys, 55(2): 622—630(in Chinese).
Brace W F.1975. Dilatancy-related electrical resistivity changes in rocks［J］.Pure and Applied Geophysics, 113: 207—217.

Brace W F, Orange A S.1968.Electrical resistivity changes in saturated rocks during fracture and frictional sliding［J］.J Geophys Res, 73: 1433—1445.

Johnston M J S, Borcherdt R D, Linde A T, et al.2006.Continuous borehole strain and pore pressure in the near field of the 28 September 2004 M 6.0 Parkfield, California, earthquake: Implications for nucleation, fault response, earthquake prediction, and tremor［J］.Bull Seism Soc Am, 96: S56—S72.
Ishii H, Yamauchi T, Matsumoto S, et al.2002.Development of multi-component borehole instrument for earthquake prediction study: Some observed examples of precursory and co-seismic phenomena relating to earthquake swarms and application of the instrument for rock mechanics.In: Ogasawara H et al.(eds).Seismic Process Monitoring. Rotterdam: Balkema, 365—377.
Linde A T, Gladwin M T, Johnston M J S, et al.1996.A slow earthquake sequence near San Juan Bautista, California in December 1992［J］.Nature, 383: 65—69.

Mjachkin I, Brace W F, Sobolev G A, et al. 1975. Two models for earthquake forerunners［J］.Pageoph, 113(3-4): 169—181.
QIU Ze-hua, Tang Lei, Zhang Bao-hong, et al.2013.In situ calibration of and algorithm for strain monitoring using four-gauge borehole strainmeters(FGBS)［J］.J Geophys Res-Solid Earth, 118.doi: 10.1002/jgrb.50112.
Sacks I S, Suyehiro S, Linde A T, et al.1978.Slow earthquake and stress distribution［J］.Nature, 275: 599—602.

Scholz C H, Sykes L R, Aggarwal Y P.1973.Earthquake prediction: A physical basis［J］.Science, 181: 8O3—810.

Stefansson R, Sacks I S, Linde A T.1981.The Hekla eruption of 1980-The mechanism of a ridge volcano［J］.Annual Report of the Director, Department of Terrestial Magnetism, Carnegie Inst, 511—514.

用高密度电法勘探预判钻孔应变观测点岩石完整性

PROSPECTING UNDERGROUND CONDITION FOR BOREHOLE STRAIN-MONITORING LOCATION BY MEANS OF RESISTIVITY IMAGING SURVEY

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