|本期目录/Table of Contents|

[1]王熠煕,邵永新,李 悦,等.天津汉1井水温固体潮畸变增多异常机理研究[J].地震研究,2023,46(04):503-510.[doi:10.20015/j.cnki.ISSN1000-0666.2023.0032]
 WANG Yixi,SHAO Yongxin,LI Yue,et al.Research on the Abnormal Mechanism of Increasing Solid Tide Distortion in Water Temperature of Well Han 1 in Tianjin[J].Journal of Seismological Research,2023,46(04):503-510.[doi:10.20015/j.cnki.ISSN1000-0666.2023.0032]
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天津汉1井水温固体潮畸变增多异常机理研究(PDF/HTML)

《地震研究》[ISSN:1000-0666/CN:53-1062/P]

卷:
46
期数:
2023年04期
页码:
503-510
栏目:
出版日期:
2023-12-01

文章信息/Info

Title:
Research on the Abnormal Mechanism of Increasing Solid Tide Distortion in Water Temperature of Well Han 1 in Tianjin
作者:
王熠煕1邵永新1李 悦1孙小龙2李 赫1刘双庆1
(1.天津市地震局,天津 300201; 2.应急管理部国家自然灾害防治研究院,北京 100085)
Author(s):
WANG Yixi1SHAO Yongxin1LI Yue1SUN Xiaolong2LI He1LIU Shuangqing1
(1.Tianjin Earthquake Agency,Tianjin 300201,China)(2.National Institute of Natural Disaster Prevention and Control,Ministry of Emergency Management,Beijing 100085,China)
关键词:
汉1井 水温 固体潮畸变 油气 异常机理 天津
Keywords:
well Han 1 water temperature continous variation oil and gas abnormal mechanism Tianjin
分类号:
P315.723
DOI:
10.20015/j.cnki.ISSN1000-0666.2023.0032
摘要:
针对天津汉1井水温固体潮畸变连续增多现象,从水温对比实验、气压影响、水化学分析等方面分析了畸变特征和异常机理。结果表明:①水温固体潮畸变的深度位于220~255 m,且水温畸变多发生在水温固体潮低潮期、水位固体潮高潮期; ②当气压出现大幅突变时可能对水温固体潮产生相关影响; ③汉1井水化学组分具有明显的海相沉积特点,且汉1井具有聚集油气的构造条件,观测层位于当地油气层的产气层深度; 综合贝尼奥夫应变结果分析认为,汉1井水温固体潮畸变的连续增多实质是逸出油气增多的表现,是汉1井-含水层系统在区域构造作用力下的一种响应。
Abstract:
In view of the continuous variation of the water temperature in well Han 1 caused by the solid tide,we do experiment to compare the water temperature,analyze the air pressure effect and hydro-chemicals,etc.to find out the variation characteristics and the abnormal mechanism of the water temperature in the well.The results show that:① The depth of water temperature solid tide distortion is located at 220-255 m,and water temperature distortion mostly occurs during the low tide period of water temperature solid tide and the high tide period of water level solid tide; ② The abrupt changes of air pressure may have an influence on the water-temperature variation to some extent; ③ The hydrochemical composition in well Han 1 has marine sedimentary characteristics.Well Han 1 is located in the structural environment which is able to accumulate oil and gas,and the observational span of well Han 1 reaches the depth of the oil and gas layer.The continuous variation of water temperature in well Han 1 is a result from the increase of escaped oil and gas,and it is also a response of the well-aquifer system to the regional tectonic forces.

参考文献/References:


车用太,刘成龙,鱼金子.2008.井水温度动态及其形成机制[J].地震,28(4):20-28.
车用太,鱼金子,刘春国.1996.我国地震地下水温度观测与研究[J].水文地质工程地质,23(4):34-37.
付虹,洪敏,王光明,等.2020.云南区域强震活动中短期异常的共性特征及应用研究[J].地震研究,43(2):241-252.
高锡兴.2004.黄骅坳陷石油天然气地质[M].北京:石油工业出版社,154-159.
李兵岩.2016.天津市汉沽地区地面沉降数值模拟[D].三河:防灾科技学院,108-113.
梁莹,张立丰,李惠.2016.内蒙古赤峰市金厂沟梁镇中学水温上升变化的调查分析[J].华南地震,36(1):108-113.
廖丽霞.2019.福建地下流体典型异常核实及分析应用[M].北京:地震出版社,67-73.
刘元生,刘贵和,佟凤兰.2000.辽河盆地地下流体异常与岫岩MS5.6地震[J].西北地震学报,22(3):241-246.
马玉川,刘耀炜,任宏微,等.2010.自流井水温固体潮效应及其应变响应能力[J].中国地震,26(2):172-182.
邵永新,李一兵,张德元.1993.油井动态观测井映震能力的评价[J].地震,25(4):52-57.
邵永新,李悦,马建英,等.1996.天津汉1井水温异常跟踪结果[C].北京:中国地震学会第五届地震流体专业委员会成立暨2016年学术年会.
邵永新,王熠熙,李悦,等.2020.天津流体异常与河北唐山市古冶区MS5.1地震预测[J].华北地震科学,38(4):92-98.
时振梁,汪良谋,傅征祥,等.1997.中国大陆中长期强震危险性预测方法研究[M].北京:海洋出版社.
王瑞丽,徐守余,孙万华,等.2004.唐山地震前不同区域油水井异常变化及其机理分析[J].华北地震科学,22(3):15-19.
杨马陵,陈大庆,黄元敏,等.2011.汶川地震前后四川中坝气田的气井井口压力异常变化[J].地震学报,33(4):505-514.
于海力.1998.人工地震动增油技术的应用[J].地震工程与工程振动,18(1):120-123.
张德元,刘元生,李一兵,等.1995.油田地震信息监测研究与应用[M].北京:地震出版社.
张德元,赵根模.1985.大地震前后油井压力异常机制和前兆意义[J].地震研究,23(5):559-566.
张小涛,冯向东,张跃刚,等.2011.运用小波变换方法研究华北地区的地震活动性[J].地震研究,34(1):24-29.
Benioff H.1951.Crustal strain characteristics derived from earthquake se-quences[J].Trans Amer Geophy Union,32(4):203-208.
Esipko O A,Rosaev A E.2007.The temperature monitoring in Vorotilovo deep well and global climate warming[J].Geophys Res Abst,9:00533.
Furuya I,Shimamura H.1988.Groundwater microtemperature and strain[J].Geophys J,94(2):345-353.
Kitagawa Y,Koizumi N,Tsuskutta T.1996.Comparison of post-seismic groundwater temperature changes with earthquake-induced volumetric strain release:Yundani hot spring,Japan[J].Geophysical Research Letters,23(22):3147-3150.
Mogi K,Mochizuki H,Kurokawa Y.1989.Temperature changes in an artesian spring at Usami in the Izu Peninsula(Japan)and their relation to earthquakes[J].Tectonophysics,159(1):95-108.
Rosaev A E,Esipko O A.2003.Lithospheric tidal effects from observation in deep wells[J].Celestial Mechanics and Dynamical Astronomy,8:203-207.

备注/Memo

备注/Memo:
收稿日期:2022-03-27.
基金项目:地震预测开放基金(XH23071D); 中国地震局地震科技星火项目(XH20003Y); 中国地震局震情跟踪任务(2023010310); 天津市地震局内科研项目(Zd202204).
第一作者简介:王熠煕(1985-),高级工程师,主要从事地震地下流体预报科研工作.E-mail:wangyx123@163.com.
更新日期/Last Update: 2023-10-01