2023年2月6日土耳其两次7.8级地震引起的井水位同震响应对比分析

doi:10.12196/j.issn.1000-3274.2024.03.007

Abstract

Abstract: The two M7.8 earthquakes in Türkiye on February 6, 2023, caused coseismic responses in Xin 04 well, Xin 10 well, and Xin 11 well in Urumqi, Xinjiang, but their coseismic variation patterns were different. In this paper, we compare and analyze the coseismic response characteristics of water levels in the three observation wells, and discuss the earthquake-induced changes in well water levels and their coseismic response mechanisms. The results illustrate three types of coseismic responses: oscillation at Xin 10 well, coseismic decrease at Xin 04 well, and coseismic increase at Xin 11 well, which indicates the complexity of the mechanisms of coseismic changes in well water levels. Two M7 earthquakes caused the same type of coseismic response at the same well, and the coseismic changes of water levels of different observation wells are related to changes in the permeability structure where the well boreholes are located.

Key words: Well water level, Coseismic response mechanism, Tidal factor, Phase lag, The 2023 Türkiye M7.8 earthquake

CLC Number:

P315.7

LIANG Hui, GAO Xiao-qi, YAN Long. Comparison and Analysis of Coseismic Response of Well Water Level Caused by Two M7.8 Earthquakes in Türkiye on February 6, 2023[J]. EARTHQUAKE, 2024, 44(3): 96-107.

References

[1] Rojstaczer S, Wolf S, Michel R. Permeability enhancement in the shallow crust as a cause of earthquake-induced hydrological changes[J]. Nature, 1995, 373(6511): 237-239.
[2] Shi Z M, Wang G C. Relationship between the Earth tidal factor and phase lag of groundwater levels in confined aquifers and the Wenchuan M_S8.0 earthquake of 2008[J]. Science China Earth Sciences, 2013, 56(10): 1722-1730.
[3] Wang C Y, Barbour A J. Influence of pore pressure change on coseismic volumetric strain[J]. Earth and Planetary Science Letters, 2017, 475: 152-159.
[4] Sun X, Xiang Y, Shi Z. Estimating the hydraulic parameters of a confined aquifer based on the response of groundwater levels to seismic Rayleigh waves[J]. Geophysical Journal International, 2018, 213(2): 919-930.
[5] 向阳. 地震引起的井水位动态响应及其机理研究[D]. 北京: 中国地震局地壳应力研究所, 2020.
XIANG Yang. Study on well water level response and mechanism induced by earthquake[D]. Beijing: Institute of Crustal Dynamics, China Earthquake Administration, 2020 (in Chinese).
[6] 晏锐. 影响井水位变化的几种因素研究[D]. 北京: 中国地震局地震预测研究所, 2008.
YAN Rui. Study of several influence factor of well water level change[D]. Beijing: Institute of Earthquake Forecasting, China Earthquake Administration, 2008 (in Chinese).
[7] Hsieh P A, Bredehoeft J D, Rojstaczer S A. Response of well aquifer systems to Earth tides: Problem revisited[J]. Water Resources Research, 1988, 24(3): 468-472.
[8] Rojstaczer S. Determination of fluid flow properties from the response of water levels in wells to atmospheric loading[J]. Water Resources Research, 1988, 24(11): 1927-1938.
[9] Eaton J P, Takasaki K J. Seismological interpretation of earthquake-induced water-level fluctuations in wells[J]. Bulletin of the Seismological Society of America, 1959, 49(3): 227-245.
[10] Cooper Jr H H, Bredehoeft J D, Papadopulos I S, et al. The response of well-aquifer systems to seismic waves[J]. Journal of Geophysical Research, 1965, 70(16): 3915-3926.
[11] 汪成民, 卓明葆, 郭一新, 等. 地震引起的深井水位振荡现象[J]. 地震, 1983, 3(2): 36-40.
WANG Cheng-min, ZHUO Ming-bao, GUO Yi-xin, et al. The oscillation phenomenon of deep well water level caused by earthquakes[J]. Earthquake, 1983, 3(2): 36-40 (in Chinese).
[12] 车用太, 王铁城, 鱼金子. 我国水震波研究的现状与动向[J]. 地震, 1989, 9(1): 70-72.
CHE Yong-tai, WANG Tie-cheng, YU Jin-zi. The current status and trends of water shock wave research in China[J]. Earthquake, 1989, 9(1): 70-72 (in Chinese).
[13] 鱼金子, 车用太, 王爱英, 等. 水震波异常与中期强震危险性关系初探[J]. 地震, 1993, 12(4): 30-37.
YU Jin-zi, CHE Yong-tai, WANG Ai-ying, et al. Preliminary study on relations between the anomalies of seismic wave of water level and the earthquake risk[J]. Earthquake, 1993, 12(4): 30-37 (in Chinese).
[14] 张昭栋, 迟镇乐, 陈会民, 等. 水井的频率特性试验和对地震波的响应[J]. 地震学报, 1999, 21(3): 329-331.
ZHANG Zhao-dong, CHI Zhen-le, CHEN Hui-min, et al. Test of frequency characteristic for well and its response to seismic waves[J]. Acta Seismologica Sinica, 1999, 21(3): 329-331 (in Chinese).
[15] Jónsson S, Segall P, Pedersen R, et al. Post-earthquake ground movements correlated to pore-pressure transients[J]. Nature, 2003, 424(6945): 179-183.
[16] Roeloffs E A. Persistent water level changes in a well near Parkfield, California, due to local and distant earthquakes[J]. Journal of Geophysical Research: Solid Earth, 1998, 103(B1): 869-889.
[17] Elkhoury J E, Brodsky E E, Agnew D C. Seismic waves increase permeability[J]. Nature, 2006, 441(7097): 1135-1138.
[18] Montgomery D R, Manga M. Streamflow and water well responses to earthquakes[J]. Science, 2003, 300(5628): 2047-2049.
[19] Mays L W. Water resources engineering[M]. USA: John Wiley & Sons, 2010.
[20] Barbosa N D, Solazzi S G, Lupi M. Seismically induced unclogging in fluid-saturated faults[J]. Journal of Geophysical Research: Solid Earth, 2020, 125(8): e2020JB020152.
[21] 王道. 天山地震活动区地下水同震、震后效应的研究[J]. 内陆地震, 2000, 14(3): 252-259.
WANG Dao. Study on coseismic, postseismic effects of groundwater parameters in Tianshan seismically active area[J]. Inland Earthquake, 2000, 14(3): 252-259 (in Chinese).
[22] 陈玲, 高小其, 朱成英, 等. 新疆地区地下水位同震及震后效应的研究[J]. 华南地震, 2009, 29(3): 43-55.
CHEN Ling, GAO Xiao-qi, ZHU Cheng-ying, et al. Study on coseismic effect and post-seismic effect of groundwater level in Xinjiang[J]. South China Journal of Seismology, 2009, 29(3): 43-55 (in Chinese).
[23] 杨竹转, 邓志辉, 高小其, 等. 新疆乌鲁木齐04号井数字化水位同震阶变的研究[J]. 中国地震, 2010, 26(3): 329-339.
YANG Zhu-zhuan, DENG Zhi-hui, GAO Xiao-qi, et al. Study on coseismic drop steps of water level based on the digital observation from Xin-04 well, Urumqi, Xinjiang[J]. Earthquake Research in China, 2010, 26(3): 329-339 (in Chinese).
[24] 张涛, 杨晓芳, 朱成英. 日本9.0级、苏门答腊8.6级地震新疆地区水位、水温同震响应特征分析[J]. 内陆地震, 2013, 27(3): 235-241.
ZHANG Tao, YANG Xiao-fang, ZHU Cheng-ying. Co-seismic response of water level, temperature in Xinjiang to Japan earthquake with M_S9.0 and Sumatera earthquake with M_S8.6[J]. Inland Earthquake, 2013, 27(3): 235-241 (in Chinese).
[25] 颜龙, 梁卉, 向阳, 等. 新疆北天山地区井水位同震响应特征分析研究[J]. 内陆地震, 2019, 33(1): 59-67.
YAN Long, LIANG Hui, XIANG Yang, et al. Analysis on co-seismic response characteristics of well water level in northern Tianshan area, Xinjiang[J]. Inland Earthquake, 2019, 33(1): 59-67 (in Chinese).
[26] 高小其, 陈华静, 杨又陵, 等. 2004年12月26日印尼8.7级强震新疆地区的同震效应[J]. 地震地磁观测与研究, 2006, 27(3): 40-46.
GAO Xiao-qi, CHEN Hua-jing, YANG You-ling, et al. Coseismal effect of Indonesia M8.7 earthquake on Dec. 26, 2004 in Xinjiang region[J]. Seismological and Geomagnetic Observation and Research, 2006, 27(3): 40-46 (in Chinese).
[27] 舒优良, 张世民, 黄辅琼. 汶川8.0级地震周至深井水震波的记录特征[J]. 震灾防御技术, 2014, 9(S1): 572-580.
SHU You-liang, ZHANG Shi-min, HUANG Fu-qiong. Characteristics of water level depth vibration of Zhouzhi deep well during Wenchuan M8.0 earthquake[J]. Technology for Earthquake Disaster Prevention, 2014, 9(S1): 572-580 (in Chinese).
[28] He A, Fan X, Zhao G, et al. Co-seismic response of water level in the Jingle well (China) associated with the Gorkha Nepal (M_W7.8) earthquake[J]. Tectonophysics, 2017, 714-715: 82-89.
[29] 向阳, 孙小龙, 杨朋涛. 新疆阿克陶M_S6.7地震引起的新10井水位同震响应研究[J]. 地震学报, 2017, 39(6): 899-909.
XIANG Yang, SUN Xiao-long, YANG Peng-tao. Coseismic response of water level in Xin10 well caused by M_S6.7 Akto, Xinjiang, earthquake[J]. Acta Seismologica Sinica, 2017, 39(6): 899-909 (in Chinese).
[30] 孙小龙, 向阳. 基于同震水震波的水文地质参数求取方法探讨[J]. 水文地质工程地质, 2018, 45(3): 22-29.
SUN Xiao-long, XIANG Yang. A discussion of the method of estimating hydraulic parameters based on groundwater responses to seismic waves[J]. Hydrogeology & Engineering Geology, 2018, 45(3): 22-29 (in Chinese).
[31] Sun X, Xiang Y, Shi Z. Changes in permeability caused by two consecutive earthquakes—Insights from the responses of a well-aquifer system to seismic waves[J]. Geophysical Research Letters, 2019, 46(17-18): 10367-10374.
[32] Xiang Y, Sun X, Gao X. Different coseismic groundwater level changes in two adjacent wells in a fault-intersected aquifer system[J]. Journal of Hydrology, 2019, 578: 124123.
[33] Sun X, Xiang Y. Aquifer permeability decreases before local earthquakes inferred from water level response to period loading[J]. Geophysical Research Letters, 2021, 48(15): e2021GL093856.
[34] Byerly P, Blanchard F B. Well gauges as seismographs[J]. Nature, 1935, 135(3408): 303-304.
[35] Chia Y, Wang Y S, Chiu J J, et al. Changes of groundwater level due to the 1999 Chi-Chi earthquake in the Choshui River alluvial fan in Taiwan[J]. Bulletin of the Seismological Society of America, 2001, 91(5): 1062-1068.
[36] Zhang Y, Fu L Y, Huang F, et al. Coseismic water-level changes in a well induced by teleseismic waves from three large earthquakes[J]. Tectonophysics, 2015, 651-652: 232-241.
[37] Yan R, Wang G, Shi Z. Sensitivity of hydraulic properties to dynamic strain within a fault damage zone[J]. Journal of Hydrology, 2016, 543: 721-728.
[38] 曹梦涵, 薛莲. 井水位同震响应特征与机理研究进展[J]. 地震研究, 2022, 45(2): 173-186.
CAO Meng-han, XUE Lian. Advances in groundwater coseismic response characteristics and mechanisms[J]. Journal of Seismological Research, 2022, 45(2): 173-186 (in Chinese).
[39] 向阳, 孙小龙, 梁卉. 2016年12月8日呼图壁M_S6.2地震引起的新10、新11井水位同震响应对比分析[J]. 内陆地震, 2017, 31(3): 259-269.
XIANG Yang, SUN Xiao-long, LIANG Hui. Comparative analysis of coseismic response of No.10 and No.11 well induced by Hutubi earthquake with M_S6.2 on December 8^th, 2016[J]. Inland Earthquake, 2017, 31(3): 259-269 (in Chinese).
[40] 史浙明, 王广才, 刘春国. 基于汶川地震同震地下水位变化反演含水层体应变[J]. 地震学报, 2012, 34(2): 215-223.
SHI Zhe-ming, WANG Guang-cai, LIU Chun-guo. Estimating aquifer volumetric strain caused by the 2008 Wenchuan earthquake from tidal effect of groundwater[J]. Acta Seismologica Sinica, 2012, 34(2): 215-223 (in Chinese).
[41] 史浙明, 王广才. 承压含水层地下水位固体潮潮汐因子和相位滞后与汶川地震的关系[J]. 中国科学: 地球科学, 2013, 43(7): 1132-1140.
SHI Zhe-ming, WANG Guang-cai. Relationship between the Earth tidal factor and phase lag of groundwater levels in confined aquifers and the Wenchuan M_S8.0 earthquake of 2008[J]. Science China: Earth Sciences, 2013, 43(7): 1132-1140 (in Chinese).
[42] Shi Z, Wang G. Aquifers switched from confined to semiconfined by earthquakes[J]. Geophysical Research Letters, 2016, 43(21): 11166-11172.
[43] Sun X, Wang G, Yang X. Coseismic response of water level in Changping well, China, to the M_W9.0 Tohoku earthquake[J]. Journal of Hydrology, 2015, 531: 1028-1039.
[44] 向阳, 孙小龙, 高小其, 等. 新10井水位对九寨沟M_S7.0、精河M_S6.6地震同震响应[J]. 中国地震, 2017, 33(4): 563-574.
XIANG Yang, SUN Xiao-long, GAO Xiao-qi, et al. Co-seismic response of water level caused by the Jiuzhaigou M_S7.0 earthquake and the Jinghe M_S6.6 earthquake in Xin Well 10, Xinjiang[J]. Earthquake Research in China, 2017, 33(4): 563-574 (in Chinese).

Comparison and Analysis of Coseismic Response of Well Water Level Caused by Two M7.8 Earthquakes in Türkiye on February 6, 2023

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