北京平原区典型混合成因地裂缝成因机理研究
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摘要
近年来,地裂缝危害的发生愈演愈烈,北京平原区位于大华北裂缝带上,区域内地裂缝多以混合成因型为主。地裂缝隐蔽性强,危害大,造成了严重的财产损失,直接影响工农业生产,城镇规划,生命线工程,土地使用等。其发生发展受到了地质灾害研究部门和广大群众的重视和关注。探讨其形成原因及成因机理是一直以来的重点。在初步研究北京平原地区混合成因型地裂缝分布的基础上,选取典型地区为代表进行探讨。认为构造活动及过度采掘地下水资源是引起地裂缝生成的核心因素,据此提出了相应防治建议。
In recent years, the occurrence of ground fissure is becoming more and more serious. Beijing district is in the belt of ground fissures in North China, the ground fissures in the area are mostly mixed and caused. The ground fissures are concealed and harmful, causing serious property losses, directly affecting industrial and agricultural production, town planning, lifeline engineering, land use, etc. Its occurrence and development have received the attention and concern of the geological disaster research department and the general public. It has always been the focus of discussion on the causes and mechanism of ground fissures. Based on the preliminary study of the distribution of mixed genetic ground fissure in the Beijing Plain, typical regions are selected as representatives for discussion. It is believed that excessive extraction of groundwater resources and tectonic activity are the main factors causing the formation of ground fissures, and accordingly corresponding prevention and control recommendations are proposed.
In recent years, the occurrence of ground fissure is becoming more and more serious. Beijing district is in the belt of ground fissures in North China, the ground fissures in the area are mostly mixed and caused. The ground fissures are concealed and harmful, causing serious property losses, directly affecting industrial and agricultural production, town planning, lifeline engineering, land use, etc. Its occurrence and development have received the attention and concern of the geological disaster research department and the general public. It has always been the focus of discussion on the causes and mechanism of ground fissures. Based on the preliminary study of the distribution of mixed genetic ground fissure in the Beijing Plain, typical regions are selected as representatives for discussion. It is believed that excessive extraction of groundwater resources and tectonic activity are the main factors causing the formation of ground fissures, and accordingly corresponding prevention and control recommendations are proposed.
引文
[1]王景明.地裂缝及其灾害的理论与应用[M].西安:陕西科学技术出版社, 2000.
[2]赵忠海.北京地区地裂缝灾害的分布特征及其成因探讨[J].地质灾害与环境保护, 2006, 17(3):75-78.
[3]武强,陈佩佩.地裂缝灾害研究现状与展望[J].中国地质灾害与防治学报, 2003(1):25-30.
[4]王景明.华北区地裂与地震活动周期性分析[J].地震研究,1992(1):53-62.
[5]彭建兵,范文,李喜安,等.汾渭盆地地裂缝成因研究中的若干关键问题[J].工程地质学报, 2007, 15(4):433-440.
[6]刘方翠,祁生文,彭建兵,等.北京市地裂缝分布与发育规律[J].工程地质学报, 2016(6):1269-1277.
[7]蔡向民,栾英波,郭高轩,等.北京平原地区地质系统[J].城市地质, 2009, 4(3):6-12.
[8]蔡向民,栾英波,郭高轩,等.北京平原第四系的三维结构[J].中国地质, 2009, 36(5):1021-1029.
[9]ROJAS E, ARZATE J, ARROYO M. A method to predict the group fissuring and faulting caused by regional groundwater decline[J]. Engineering Geology, 2002, 65(4):245-260.
[10]赵忠海.北京平原区新构造活动及其引发的不良地质现象分析[J].地质灾害与环境保护, 2009, 20(2):66-70.
[11]贾三满,刘明坤,田芳,等.北京地区地裂缝分类及防治措施[J].城市地质, 2011, 6(2):4-7.
[12]赵忠海.北京顺义木林—塔河一带地裂缝成因及防治措施初探[J].中国地质灾害与防治学报, 2001(2):29-32.
[13]董殿伟,林沛,晏婴,等.北京平原区地下水水位监测网优化[J].水文地质工程地质, 2007, 34(1):10-19.
[14]贾三满,赵守生,罗勇,等.北京地面沉降机理研究初探[J].城市地质, 2007, 2(1):20-26.
[15]顺义县人民政府地震办公室.顺义地区地震砂液化浅析[Z].北京:顺义县人民政府地震办公室, 1990.
[16]马超.北京高丽营地裂缝成因研究[D].北京:中国地质大学(北京), 2011.
[17]贾三满,郭萌.从高丽营探槽分析黄庄—高丽营断裂与地裂缝的关系[J].城市地质, 2007(4):24-28.
[18]刘明坤,贾三满,陈柘舟,等.北京平原区高丽营地裂缝带活动性及灾害特征研究[J].上海国土资源, 2014, 35(4):53-57.
[19]罗勇,赵龙,田苗壮,等.北京市通州区宋庄地裂缝补充勘察[Z].北京:北京市水文地质工程地质大队, 2016.
[20]田苗壮,王荣,赵龙,等.高密度电法在北京宋庄地裂缝中的应用[J].上海国土资源, 2017, 38(3):35-38.
[21]赵龙,刘久荣,王荣,等.北京宋庄地裂缝分布特征及成因分析[J].上海国土资源, 2017, 38(2):35-38.
[2]赵忠海.北京地区地裂缝灾害的分布特征及其成因探讨[J].地质灾害与环境保护, 2006, 17(3):75-78.
[3]武强,陈佩佩.地裂缝灾害研究现状与展望[J].中国地质灾害与防治学报, 2003(1):25-30.
[4]王景明.华北区地裂与地震活动周期性分析[J].地震研究,1992(1):53-62.
[5]彭建兵,范文,李喜安,等.汾渭盆地地裂缝成因研究中的若干关键问题[J].工程地质学报, 2007, 15(4):433-440.
[6]刘方翠,祁生文,彭建兵,等.北京市地裂缝分布与发育规律[J].工程地质学报, 2016(6):1269-1277.
[7]蔡向民,栾英波,郭高轩,等.北京平原地区地质系统[J].城市地质, 2009, 4(3):6-12.
[8]蔡向民,栾英波,郭高轩,等.北京平原第四系的三维结构[J].中国地质, 2009, 36(5):1021-1029.
[9]ROJAS E, ARZATE J, ARROYO M. A method to predict the group fissuring and faulting caused by regional groundwater decline[J]. Engineering Geology, 2002, 65(4):245-260.
[10]赵忠海.北京平原区新构造活动及其引发的不良地质现象分析[J].地质灾害与环境保护, 2009, 20(2):66-70.
[11]贾三满,刘明坤,田芳,等.北京地区地裂缝分类及防治措施[J].城市地质, 2011, 6(2):4-7.
[12]赵忠海.北京顺义木林—塔河一带地裂缝成因及防治措施初探[J].中国地质灾害与防治学报, 2001(2):29-32.
[13]董殿伟,林沛,晏婴,等.北京平原区地下水水位监测网优化[J].水文地质工程地质, 2007, 34(1):10-19.
[14]贾三满,赵守生,罗勇,等.北京地面沉降机理研究初探[J].城市地质, 2007, 2(1):20-26.
[15]顺义县人民政府地震办公室.顺义地区地震砂液化浅析[Z].北京:顺义县人民政府地震办公室, 1990.
[16]马超.北京高丽营地裂缝成因研究[D].北京:中国地质大学(北京), 2011.
[17]贾三满,郭萌.从高丽营探槽分析黄庄—高丽营断裂与地裂缝的关系[J].城市地质, 2007(4):24-28.
[18]刘明坤,贾三满,陈柘舟,等.北京平原区高丽营地裂缝带活动性及灾害特征研究[J].上海国土资源, 2014, 35(4):53-57.
[19]罗勇,赵龙,田苗壮,等.北京市通州区宋庄地裂缝补充勘察[Z].北京:北京市水文地质工程地质大队, 2016.
[20]田苗壮,王荣,赵龙,等.高密度电法在北京宋庄地裂缝中的应用[J].上海国土资源, 2017, 38(3):35-38.
[21]赵龙,刘久荣,王荣,等.北京宋庄地裂缝分布特征及成因分析[J].上海国土资源, 2017, 38(2):35-38.
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