应力加载作用引起地下水微温度场变化的研究综述
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摘要
在地震地下流体动态观测中,水温对地震活动的响应非常敏感,井水温度微动态观测越来越受到有关学者的关注。本文收集了相关资料,以引起水温变化的水动力学机制为基础,从应力加载作用下渗流场的变化、渗流场变化引起地下水温度变化以及裂隙介质热量运移三个方面分别阐述了前人研究成果,旨在理清“含水层受力变形→井-含水层系统内水流变化→井水温度变化”的理论模式,探讨应力加载作用引起地下水微温度场变化的理论基础和技术途径。对这一领域研究成果的综合分析将有助于我们深入地研究地震孕育过程中的前兆成因机理。
During the observation of underground water,the response of water temperature to seismic activity is very sensitive,observation of micro changes of the temperature of water in the well has lead to the attention of relevant scholars.Based on data collection and the water dynamics that causes changes of water temperature,the research results obtained up to now are summarized from three aspects: changes of the percolation field,temperature changes of underground water caused by changes of the percolation,heat movement in the cracking media.The aim is putting in order the theoretical model of "deformation of water-bearing layers caused by stresses→changes of water flow in the system of well-water bearing system→changes of temperature of water in the well".Discussion is focused on the theoretical foundation and technical approach for the changes of micro temperature field of underground water caused by stress loading.Comprehensive analysis in this field will help us to deepen understanding of the mechanism of precursors during the process of earthquake generation.
During the observation of underground water,the response of water temperature to seismic activity is very sensitive,observation of micro changes of the temperature of water in the well has lead to the attention of relevant scholars.Based on data collection and the water dynamics that causes changes of water temperature,the research results obtained up to now are summarized from three aspects: changes of the percolation field,temperature changes of underground water caused by changes of the percolation,heat movement in the cracking media.The aim is putting in order the theoretical model of "deformation of water-bearing layers caused by stresses→changes of water flow in the system of well-water bearing system→changes of temperature of water in the well".Discussion is focused on the theoretical foundation and technical approach for the changes of micro temperature field of underground water caused by stress loading.Comprehensive analysis in this field will help us to deepen understanding of the mechanism of precursors during the process of earthquake generation.
引文
[1]蔡永恩,殷有泉,王仁.热状态对地震发生的影响.地球物理学报,1992,35(2):204-212
[2]王琳瑛,朱传镇.唐山地震和海城地震前地温的异常变化.地震研究,1984,7(6):649-656
[3]强祖基,孔令昌,郭满红,等.卫星热红外增温机制的实验研究.地震学报,1997,19(2):197-201
[4]王庆良,王文萍,梁伟锋,等.应力-耗散热地温前兆机理研究.地震,1998,20(5):529-534
[5]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.地震,1997,17(4):389-396
[6]王志欣,信荃麟.关于地下断层封闭性的讨论-以东营凹陷为例.高校地质学报,1997,3(3):293-300
[7]张昭栋,郑金涵,冯初刚.一种估算地震引起应力调整的新方法.地震,1988(3):19-27
[8]敬少群,王佳卫.长沙井动水位对台湾集集7.6级地震的震时效应及其机理分析.华南地震,2001,21(1):32-37
[9]孙自明,何发歧.断裂作用与流体流动耦合动力学研究进展.新疆石油地质,2002,23(4):348-350
[10]张伯崇,邬慧敏,刘长义,等.应力对岩石中孔隙流体压力的影响和地下水位震前异常变化机理.地震学报,1991,13(1):88-95
[11]刘建军,刘先贵.有效压力对低渗透多孔介质孔隙度、渗透率的影响.地质力学学报,2001,7(1):41-44
[12]任长吉,黄涛.裂隙岩体渗流场与应力场耦合数学模型的研究.武汉大学学报(工学版),2004,37(2):8-12
[13]孙雄,洪汉净.构造应力场对油气运移的影响.石油勘探与开发,1998,25(1):1-3
[14]张树林,田世澄,陈建渝.断裂构造与成藏动力系统.石油与天然气地质,1997,18(4):261-266
[15]华保钦.构造应力场、地震泵和油气运移.沉积学报,1995,13(2):77-85
[16]Byerlee J.Model for ep isod ic flow of h igh-pressure water in fau lt zones before earthquakes.Geology,1993,21:303-306
[17]Isabelle Moretti.The role of fau lts in hydrocarbon m igration.Petroleum Geosc ience,1993,4:81-94
[18]Pratsch J C.Vertical Hydrocarbon m igration:a m ajor exp loration param eter.Journal of Petroleum Geology,1991,14(4):429-444
[19]Atilla A.Fractures,fau lts,and hydrocarbon entrapm ent,m igration and flow.M arine and Petroleum Geology,2000,17:797-814
[20]Cox S F.Fau lting progresses at h igh flu id pressures:An examp le of fau lt valve behavior from theW attle Gu llyFau lt,V ictoria,Australia.Journal of Geophysical Research,1995,100(B7):12 841-12 859
[21]Steven L,Lorraine E,M artin S,et al.Vertical and lateral flu id flow related to a larger growth fau lt,South Eu-gene Island B lock 330 F ield.O ffshore Lou isiana.AAPF 1999,83(N2):244-276
[22]童亨茂.断层开启与封闭的定量分析.石油与天然气地质,1998,19(3):215-220
[23]邱泽华,石耀霖.观测应变阶在地震应力触发研究中的应用.地震学报,200426(5):481-188
[24]易立新,车用太,王广才.水库诱发地震研究的历史、现状与发展趋势.2003,23(1):28-37
[25]易立新,王广才,李榴芬.水文地质结构与水库诱发地震.水文地质工程地质,2004,31(2):29-32
[26]黄辅琼,陈,白长清,等.八宝山断层的变形行为与降雨及地下水的关系.地震学报,2005,27(6):637-646
[27]孙君秀,刘五洲,车用太.地下水对震源体应力、应变场的影响.地震地质,2000,22(2):179-186
[28]刘五洲,孙君秀.地下水在地震前兆应力场演化过程中的作用.地震,2000,20(4):12-18
[29]熊亮萍,汪集.钻孔地温分布与地下水活动.地质科学,1992,增刊:313-321
[30]邓孝.地下水垂直运动的地温场数值模拟与实例剖析.地质科学,1989(1):77-81
[31]车用太,鱼金子.地震地下流体物理化学动态形成的基础理论问题.国际地震动态,1995(12):6-10
[32]Dom en ico P A,Palc iauskas V V.Therm al Expansion of flu ids and fracture in itiation in compacting sed im ents.Geological Soc iety of Am erica Bu lletin,1979,90(6):518-520
[33]Naoji Koizum i.固体潮引起流量变化的地下水化学组分与温度分析.地震地质译丛,1990(1):29-35
[34]张永仙,石耀霖,张国民.流量与水温关系的模型研究及地震水温前兆机制的探讨.中国地震,1991,7(3):88-94
[35]车用太,刘喜兰,姚宝树,等.首都圈地区井水温度的动态类型及其成因分析.地震地质,2003,25(3):403-420
[36]车用太,鱼金子,刘春国.我国地震地下水温度动态观测与研究.水文地质工程地质,1996(4):34-37
[37]D R Montgom ery&M M anga.Stream flow and waterwell responses to earthquakes.Sc ience,June,2003,300(27):2 047-2 049
[38]Cramp in S,Evans R,Atkm son B K.Earthquake pred iction:a new physical basis.Geophys J R Astr Soc.1984 a,76:174-156
[39]Cramp in S,Chesnokov E M,H ipk in R G.Se ism ic an isotropy the state of artⅡ.Geophys J R Astr Soc.1984b,76:1-16
[40]Cramp in S,Zatsep in S V.Production se ismology,the use of shearwaves to mon itor and model production in aporo-reactive and interactive reservoir.Expanded Abstracts.65 tb Anu Int SEG M eeting,Houston,1995,199-202
[41]Zatsep in S V,Cramp in S.Modelling the comp liance of crustal rock—Ⅰ:response of shear-wave sp litting tod ifferential stress.R A S G JI,1997,129:477-494
[42]Cramp in S,Zatsep in S V.Modelling the comp liance of crustal rock—Ⅱ:response to temporal changes beforeearthquakes.Geophys J Int,1997,129:495-506
[43]周志芳,王锦国.裂隙介质水动力学.北京:中国水利水电出版社,2004:47-88
[44]薛禹群,张幼宽.双重介质渗流模型及其里兹有限元解在矿坑涌水量预测中的应用.水文地质工程地质,1984,12(2):33-39
[45]毛昶煦,陈平,李祖贻,等.裂隙岩体计算方法研究.岩土工程学报,1991,13(6):1-10
[46]王恩志.剖面二维裂隙网络渗流计算方法.水文地质工程地质,1993,20(4):27-29
[47]成建梅,陈崇希.广西北山岩溶管道-裂隙-孔隙地下水流数值模拟初探.水文地质工程地质,1998,25(4):50-54
[48]Buscheck T A,C Doughty and C-F Tsang.Pred iction and analysis of a field experim ent on a mu ltilayered aqu i-fer therm al energy storage system w ith strong buoyancy flow.W aterResources Res,1983,19(5):1 307-1 315
[49]Molson JW,E O Frind,C D.Palm er,Therm al energy storage in an unconfined aqu ifer,2.Model develop-m ent,validation and app lication.W ater Resour.Res.,1992,28(10):2 857-2 867
[50]谢春红,赵文良,丁家平.地下水不稳定渗流达西速度计算新方法.岩土工程学报,1996,18(1):68-74
[51]张志辉,吴吉春.含水层热量输运中自然热对流和水-岩热交换作用的研究.工程地质学报,1997,5(3):269-275
[2]王琳瑛,朱传镇.唐山地震和海城地震前地温的异常变化.地震研究,1984,7(6):649-656
[3]强祖基,孔令昌,郭满红,等.卫星热红外增温机制的实验研究.地震学报,1997,19(2):197-201
[4]王庆良,王文萍,梁伟锋,等.应力-耗散热地温前兆机理研究.地震,1998,20(5):529-534
[5]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.地震,1997,17(4):389-396
[6]王志欣,信荃麟.关于地下断层封闭性的讨论-以东营凹陷为例.高校地质学报,1997,3(3):293-300
[7]张昭栋,郑金涵,冯初刚.一种估算地震引起应力调整的新方法.地震,1988(3):19-27
[8]敬少群,王佳卫.长沙井动水位对台湾集集7.6级地震的震时效应及其机理分析.华南地震,2001,21(1):32-37
[9]孙自明,何发歧.断裂作用与流体流动耦合动力学研究进展.新疆石油地质,2002,23(4):348-350
[10]张伯崇,邬慧敏,刘长义,等.应力对岩石中孔隙流体压力的影响和地下水位震前异常变化机理.地震学报,1991,13(1):88-95
[11]刘建军,刘先贵.有效压力对低渗透多孔介质孔隙度、渗透率的影响.地质力学学报,2001,7(1):41-44
[12]任长吉,黄涛.裂隙岩体渗流场与应力场耦合数学模型的研究.武汉大学学报(工学版),2004,37(2):8-12
[13]孙雄,洪汉净.构造应力场对油气运移的影响.石油勘探与开发,1998,25(1):1-3
[14]张树林,田世澄,陈建渝.断裂构造与成藏动力系统.石油与天然气地质,1997,18(4):261-266
[15]华保钦.构造应力场、地震泵和油气运移.沉积学报,1995,13(2):77-85
[16]Byerlee J.Model for ep isod ic flow of h igh-pressure water in fau lt zones before earthquakes.Geology,1993,21:303-306
[17]Isabelle Moretti.The role of fau lts in hydrocarbon m igration.Petroleum Geosc ience,1993,4:81-94
[18]Pratsch J C.Vertical Hydrocarbon m igration:a m ajor exp loration param eter.Journal of Petroleum Geology,1991,14(4):429-444
[19]Atilla A.Fractures,fau lts,and hydrocarbon entrapm ent,m igration and flow.M arine and Petroleum Geology,2000,17:797-814
[20]Cox S F.Fau lting progresses at h igh flu id pressures:An examp le of fau lt valve behavior from theW attle Gu llyFau lt,V ictoria,Australia.Journal of Geophysical Research,1995,100(B7):12 841-12 859
[21]Steven L,Lorraine E,M artin S,et al.Vertical and lateral flu id flow related to a larger growth fau lt,South Eu-gene Island B lock 330 F ield.O ffshore Lou isiana.AAPF 1999,83(N2):244-276
[22]童亨茂.断层开启与封闭的定量分析.石油与天然气地质,1998,19(3):215-220
[23]邱泽华,石耀霖.观测应变阶在地震应力触发研究中的应用.地震学报,200426(5):481-188
[24]易立新,车用太,王广才.水库诱发地震研究的历史、现状与发展趋势.2003,23(1):28-37
[25]易立新,王广才,李榴芬.水文地质结构与水库诱发地震.水文地质工程地质,2004,31(2):29-32
[26]黄辅琼,陈,白长清,等.八宝山断层的变形行为与降雨及地下水的关系.地震学报,2005,27(6):637-646
[27]孙君秀,刘五洲,车用太.地下水对震源体应力、应变场的影响.地震地质,2000,22(2):179-186
[28]刘五洲,孙君秀.地下水在地震前兆应力场演化过程中的作用.地震,2000,20(4):12-18
[29]熊亮萍,汪集.钻孔地温分布与地下水活动.地质科学,1992,增刊:313-321
[30]邓孝.地下水垂直运动的地温场数值模拟与实例剖析.地质科学,1989(1):77-81
[31]车用太,鱼金子.地震地下流体物理化学动态形成的基础理论问题.国际地震动态,1995(12):6-10
[32]Dom en ico P A,Palc iauskas V V.Therm al Expansion of flu ids and fracture in itiation in compacting sed im ents.Geological Soc iety of Am erica Bu lletin,1979,90(6):518-520
[33]Naoji Koizum i.固体潮引起流量变化的地下水化学组分与温度分析.地震地质译丛,1990(1):29-35
[34]张永仙,石耀霖,张国民.流量与水温关系的模型研究及地震水温前兆机制的探讨.中国地震,1991,7(3):88-94
[35]车用太,刘喜兰,姚宝树,等.首都圈地区井水温度的动态类型及其成因分析.地震地质,2003,25(3):403-420
[36]车用太,鱼金子,刘春国.我国地震地下水温度动态观测与研究.水文地质工程地质,1996(4):34-37
[37]D R Montgom ery&M M anga.Stream flow and waterwell responses to earthquakes.Sc ience,June,2003,300(27):2 047-2 049
[38]Cramp in S,Evans R,Atkm son B K.Earthquake pred iction:a new physical basis.Geophys J R Astr Soc.1984 a,76:174-156
[39]Cramp in S,Chesnokov E M,H ipk in R G.Se ism ic an isotropy the state of artⅡ.Geophys J R Astr Soc.1984b,76:1-16
[40]Cramp in S,Zatsep in S V.Production se ismology,the use of shearwaves to mon itor and model production in aporo-reactive and interactive reservoir.Expanded Abstracts.65 tb Anu Int SEG M eeting,Houston,1995,199-202
[41]Zatsep in S V,Cramp in S.Modelling the comp liance of crustal rock—Ⅰ:response of shear-wave sp litting tod ifferential stress.R A S G JI,1997,129:477-494
[42]Cramp in S,Zatsep in S V.Modelling the comp liance of crustal rock—Ⅱ:response to temporal changes beforeearthquakes.Geophys J Int,1997,129:495-506
[43]周志芳,王锦国.裂隙介质水动力学.北京:中国水利水电出版社,2004:47-88
[44]薛禹群,张幼宽.双重介质渗流模型及其里兹有限元解在矿坑涌水量预测中的应用.水文地质工程地质,1984,12(2):33-39
[45]毛昶煦,陈平,李祖贻,等.裂隙岩体计算方法研究.岩土工程学报,1991,13(6):1-10
[46]王恩志.剖面二维裂隙网络渗流计算方法.水文地质工程地质,1993,20(4):27-29
[47]成建梅,陈崇希.广西北山岩溶管道-裂隙-孔隙地下水流数值模拟初探.水文地质工程地质,1998,25(4):50-54
[48]Buscheck T A,C Doughty and C-F Tsang.Pred iction and analysis of a field experim ent on a mu ltilayered aqu i-fer therm al energy storage system w ith strong buoyancy flow.W aterResources Res,1983,19(5):1 307-1 315
[49]Molson JW,E O Frind,C D.Palm er,Therm al energy storage in an unconfined aqu ifer,2.Model develop-m ent,validation and app lication.W ater Resour.Res.,1992,28(10):2 857-2 867
[50]谢春红,赵文良,丁家平.地下水不稳定渗流达西速度计算新方法.岩土工程学报,1996,18(1):68-74
[51]张志辉,吴吉春.含水层热量输运中自然热对流和水-岩热交换作用的研究.工程地质学报,1997,5(3):269-275
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