传感器放置深度对水温动态特征的影响及其机理分析

doi:10.12196/j.issn.1000-3274.2022.01.013

地震 ›› 2022, Vol. 42 ›› Issue (1): 169-180.doi: 10.12196/j.issn.1000-3274.2022.01.013

传感器放置深度对水温动态特征的影响及其机理分析

陈其峰¹, 车用太², 刘允³, 冯恩国¹, 温丽媛¹

1.山东省地震局聊城地震监测中心站, 山东聊城 252000;
2.中国地震局地质研究所, 北京 100029;
3.辽宁省地震局大连地震台, 辽宁大连 116000

收稿日期:2020-03-08 修回日期:2020-09-13 出版日期:2022-01-31 发布日期:2022-09-08
通讯作者: 车用太, 研究员。 E-mail: che@ies.ac.cn
作者简介:陈其峰(1974-), 男, 山东聊城人, 高级工程师, 主要从事地震地下流体研究。

Effect of Sensor Placement Depth on Dynamic Characteristics of Water Temperature and Its Mechanism Analysis

CHEN Qi-feng¹, CHE Yong-tai², LIU Yun³, FENG En-guo¹, WEN Li-yuan¹

1. Liaocheng Earthquake Monitoring Central Station of Shandong Earthquake Agency, Liaocheng 252000, China;
2. Institute of Geology, CEA, Beijing 100029, China;
3. Dalian Earthquake Station, Liaoning Earthquake Agency, Dalian 116000, China

Received:2020-03-08 Revised:2020-09-13 Online:2022-01-31 Published:2022-09-08

摘要/Abstract

摘要： 地热井的观测规范要求尽可能将水温传感器放置在井下深处, 一般放置深度应当大于100 m, 小于200 m。然而, 近几年的观测结果表明, 水温传感器的放置深度对水温动态特征的影响较大。在多数观测井中, 同井水温与水位的时值动态、潮汐效应、同震响应及震后阶变等动态特征的相关性或一致性, 多与水温传感器的放置深度有关。本文主要探讨了传感器放置深度对水温动态特征的影响, 水温传感器放置在观测含水层中, 都受井—含水层间水流运动的影响, 会造成水温动态随井水位变化而变化; 当放置在观测含水层下部时, 水温动态则不受井水位变化的影响, 多表现为动态相对稳定。其原因是水温动态的形成受水热动力学与地热动力学两种不同机制的控制, 此外, 井—含水层系统的条件也会产生影响。

关键词: 水温, 动态特征, 传感器放置深度, 影响机理

Abstract: According to observation specifications of geothermal wells, the water temperature sensors should be placed as deep as possible. Generally, the depth is more than 100 m and less than 200 m. However, it is observed that the placement depth of water temperature sensors has a significant effect on the dynamic characteristics of water temperature observation. In most observation wells, the dynamic characteristics between water temperature and water level in the same well, such as time dynamics, tidal effects, co-seismic responses and post-earthquake step-changes, show high correlations or consistencies, which is usually relevant to the placement depth of water temperature sensors. In this paper, the dynamic characteristics of water temperature affected by sensor placement depth is discussed, when the water temperature sensor is placed in the observation aquifer, it is affected by the flow movement between the well and the aquifer, which will cause the water temperature changes with the change of the well water level; when placed under the observation aquifer, the water temperature is not affected by the change of well water level, and most of the dynamic is relatively stable. This is mainly because the formation of water temperature dynamics is controlled by two different mechanisms, hydrothermal dynamics and geothermal dynamics, and the conditions of the well-aquifer system also play a role.

Key words: Water temperature, Dynamic characteristics, Sensor placement depth, Effect mechanism

中图分类号:

P315.7

陈其峰, 车用太, 刘允, 冯恩国, 温丽媛. 传感器放置深度对水温动态特征的影响及其机理分析[J]. 地震, 2022, 42(1): 169-180.

CHEN Qi-feng, CHE Yong-tai, LIU Yun, FENG En-guo, WEN Li-yuan. Effect of Sensor Placement Depth on Dynamic Characteristics of Water Temperature and Its Mechanism Analysis[J]. EARTHQUAKE, 2022, 42(1): 169-180.

参考文献

[1] 何案华. 我国井水温度潮汐效应的调查与分析[R]. 北京: 中国地震局地壳应力研究所, 2015.
HE An-hua. Investigation and analysis of tidal effects of well water temperature in China[R]. Beijing: Institute of Crustal Dynamics, China Earthquake Administration, 2015 (in Chinese).
[2] 赵刚, 王军, 何案华, 等. 地热对汶川8.0级地震的同震响应及震后调整[J]. 大地测量与地球动力学, 2009, 29(2): 29-32.
ZHAO Gang, WANG Jun, HE An-hua, et al. Co-seismic response and postseismic effect of geotherm on Wenchuan M_S8.0 earthquake[J]. Journal of Geodesy and Geodynamics, 2009, 29(2): 29-32 (in Chinese).
[3] 邓卫平, 何案华, 车用太, 等. 全国水温台网井水温度2008年动态及其汶川地震前后的异常变化[J]. 大地测量与地球动力学, 2019, 39(7): 751-755.
DENG Wei-ping, HE An-hua, CHE Yong-tai, et al. Dynamics of water temperature in China geothermal network: Anomalous changes before and after Wenchuan M_S8.0 earthquake in 2008[J]. Journal of Geodesy and Geodynamics, 2019, 39(7): 751-755 (in Chinese).
[4] 杨竹转, 邓志辉, 杨贤和, 等. 井孔水温动态变化的影响因素探讨[J]. 地震, 2010, 30(2): 71-79.
YANG Zhu-zhuan, DENG Zhi-hui, YANG Xian-he, et al. Study on the influencing factors of well water-temperature changes[J]. Earthquake, 2010, 30(2): 71-79 (in Chinese).
[5] 刘耀炜. 动力加载作用与地下水物理动态过程研究[D]. 北京: 中国地质大学(北京), 2009.
LIU Yao-wei. Dynamic loading and physical dynamics process of groundwater[D]. Beijing: China University of Geosciences (Beijing), 2009 (in Chinese).
[6] He A H, Zhao G, Sun Z H, et al. Co-seismic multilayer water temperature and water level changes associated with Wenchuan and Tohoku-Oki earthquakes in the Chuan No.03 well, China[J]. Journal of Seismology, 2017, 21: 719-734.
[7] 汪成国, 赵刚, 高守权, 等. 新30井不同深度下的水温观测试验及其结果[J]. 地震, 2012, 32(3): 37-46.
WANG Cheng-guo, ZHAO Gang, GAO Shou-quan, et al. Water temperature observation test and results at different depths of the new 30 well [J]. Earthquake, 2012, 32(3): 37-46 (in Chinese).
[8] 张慧, 顾申宜, 李志雄, 等. 单井多层位水温微动态初步研究[J]. 地震, 2013, 33(1): 101-110.
ZHANG Hui, GU Shen-yi, LI Zhi-xiong, et al. Preliminary study on micro-behaviors of water temperature at different layers in the same well[J]. Earthquake, 2012, 33(1): 101-110 (in Chinese).
[9] 杨明波, 郑轶文, 邢成起, 等. 水温传感器放置深度研究现状[J]. 地震地磁观测与研究, 2015, 36(3): 83-89.
YANG Ming-bo, ZHENG Yi-wen, XING Cheng-qi, et al. Reflections on the water temperature sensor placement problems to precursor observation[J]. Seismological and Geomagnetic Observation and Research, 2015, 36(3): 83-89 (in Chinese).
[10] 杨明波, 杨竹转, 郑轶文, 等. 冷水源井水温固体潮现象及其机理研究以黄村井为例[J]. 地震学报, 2017, 39(3): 420-428.
YANG Ming-bo, YANG Zhu-zhuan, ZHENG Yi-wen, et al. Solid tide phenomenon of cold water source well temperature and its mechanism: Taking Huangcun well as an example[J]. Acta Seismologica Sinica, 2017, 39(3): 420-428 (in Chinese).
[11] 鱼金子, 车用太, 刘五洲. 井水温度微动态形成的水动力学机制研究[J]. 地震, 1997, 17(4): 389-396.
YU Jin-zi, CHE Yong-tai, LIU Wu-zhou, et al. Preliminary study on hydrodynamic mechanism of microbehavior of water temperature in well[J]. Earthquake, 1997, 17(4): 389-396 (in Chinese).
[12] 石耀霖, 曹建玲, 马丽, 等. 唐山井水温的同震变化及其物理解释[J]. 地震学报, 2007, 29(3): 265-273.
SHI Yao-lin, CAO Jian-ling, MA Li, et al. Tele-seismic coseismic well temperature changes and their interpretation[J]. Acta Seismologica Sinica, 2007, 29(3): 265-273 (in Chinese).
[13] 车用太, 何案华, 鱼金子. 水温微动态形成的水热动力学与地热动力学机制[J]. 地震学报, 2014, 36(1): 106-107.
CHE Yong-tai, HE An-hua, YU Jin-zi, et al. Mechanisms of water-heat dynamics and earth-heat dynamics of well water temperature micro-behavior[J]. Acta Seismologica Sinica, 2014, 36(1): 106-107 (in Chinese).

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[12]	汪成国, 赵刚, 高守权, 邹广陈大柱, 张新成, 常想德. 新30井不同深度下的水温观测试验及其结果[J]. 地震, 2012, 32(3): 37-46.
[13]	江在森, 武艳强. 地壳形变与强震地点预测问题与认识[J]. 地震, 2012, 32(2): 8-21.
[14]	鱼金子, 车用太, 刘成龙, 李万明. 金沙江水网对日本9.0级地震的同震响应及其特征与机理[J]. 地震, 2012, 32(1): 59-69.
[15]	杨竹转, 邓志辉, 杨贤和, 张子广, 宋健. 井孔水温动态变化的影响因素探讨[J]. 地震, 2010, 30(2): 71-79.

传感器放置深度对水温动态特征的影响及其机理分析

Effect of Sensor Placement Depth on Dynamic Characteristics of Water Temperature and Its Mechanism Analysis

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