地球科学进展 ›› 2006, Vol. 21 ›› Issue (4): 417 -423. doi: 10.11867/j.issn.1001-8166.2006.04.0417

学术论文 上一篇    下一篇

衡水地区地裂缝空间发育特征与地下水位降深关系
王秀艳 1,2,王金哲 2,臧逸中 2,韩双平 2,陈江 2,李向全 2   
  1. 1.同济大学土木工程学院,上海 200092; 2.中国地质科学院水文地质环境地质研究所,河北 石家庄 050061
  • 收稿日期:2005-10-26 修回日期:2006-03-14 出版日期:2006-04-15
  • 通讯作者: 王秀艳 E-mail:wxiuyan9948@163.com
  • 基金资助:

    国家自然科学基金项目“华北平原深层地下水超采引起的粘性土再固结效应研究”(编号:40472139)资助.

Exploitation of Deep Groundwater with Relevant Issues of Earth Fissures at Hengshui Area in North China

Wang Xiuyan 1,2,Wang Jinzhe 2,Han Shuangping 2,Zang Yizhong 2,Chen Jiang 2,Li Xiangquan 2   

  1. 1.College of Civil Engineering, Tongji University,Shanghai 200092, China; 2.Instituteof Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences,Shijiazhuang 050061,China
  • Received:2005-10-26 Revised:2006-03-14 Online:2006-04-15 Published:2006-04-15

通过浅层地震法及高密度电阻率法物探对河北衡水地区最近发现的3条地裂缝调查,探明了地裂缝地下发育深度、宽度、倾向等,发现地裂缝在地表与地下发育特征有明显不同:地表以一条地裂缝存在,在地下深处则以裂缝带发育,裂缝带两侧裂缝埋深不同,地下裂缝形态表现为上窄下宽。对该地区深层钻探、水文地质和多年地下水开采等资料分析表明,该地区的地裂缝是地质历史时期地质构造活动产物,开采深层地下水等资源则是促使地裂缝发展的主要原因。通过对不同地点地裂缝发育深度与近36年以来地下水水位降深的关系分析,结果显示:不同地区地裂缝发育深度与相应深层地下水水位降深呈线性关系。研究成果对地裂缝机理研究及预防开采深层地下水对地质环境的影响具有指导作用。

    The earth fissure is one of the geological hazards in North China Plain. It is developing continually in recent years. More than 573 Earth fissures have been found since 1995.From 1995 to 2005 in Hengshui, 4 new fissures were found in one area of North China Plain. Earth fissures directly lead to cultivated land cracking, irrigation system leakage, house and hydraulic facilities damages as well as pollution of groundwater. It not only seriously threatens human being,economy construction in cities and villages,but also brings countless damage and hidden danger to descendants. Therefore, the study of Earth fissure  attracts great attention of concerned experts.
    We found three-Earth fissures that had been developing in recent years around the depression cone of groundwater in Hengshui area:①.Nanzhangjiacun village at Shenxian County in November, 2003;②. Nanqinglin village of Wuyi County —Hanguan village at Fucheng County in June, 1995; ③. Shuipo village of Jianguo town at Gucheng County in May, 2002.The result of geophysical prospecting work shows that Earth fissures are developing obviously in different way on the Earth surface and underground in depth,width,etc. The earth fissure on the Earth surface is wider in the upper part and is narrower with the depth. Reversely, the earth fissures of underground are narrower in the upper part and is wider with depth.Ground fissures are usually developed as a fissure zone underground in the Hengshui area with its width of 10-38m and depth of burial of 60-120m. The geophysical prospecting shows the dip of axes for underground fissure zone to the steep, 75-88 . The terminal fissures of the same fissures zone are different in depth burial. Usually the difference in vertical depth is about 10-30m. The earth fissures that we can see on the earth surface are only the seriously active part in the earth fissure zone. They may be wider and longer with effects on the human activities. Even the other side may become active.
    The investigation shows, on one hand, earth fissures in the Hengshui area is consistent extending along the geotectonic directions. On the other hand, the earth fissures are all distributed close to the juncture between the accumulation at the channel belt and the interchannel zone around subsidence basin of different soil masses. Analysis indicates that the geotectonic movements are the direct reason to form some hidden fissure plane in the soil mass or the hidden earth fissures. The different origins of the soil mass provide the favourable conditions for the ground fissures development.
    Datum of deep layer drilling ,deep groundwater exploration, local hydrogeological condition, drawdown of deep and shallow water exploration in recent 35 years and earth fissures development of different areas proved  better correlation with exploration drawdown of deep groundwater than with exploration drawdown of shallow groundwater and the ground fissures developed are deeper than drawdown of groundwater. This is closely related to the deeper groundwater depression cone, geothermal exploitation and oil exploitation,etc.
    To sum up, the earth fissures are usually developed around the depression cone of groundwater as a fissure zone underground in the Hengshui area. It is the result of geological tectonic activities of different periods, tectonic activity form hidden earth fissures. And exploitation of ground water is also the main reason that caused land subsidence and earth fissures developing in hard soil area in North China. It will be guidance for research mechanism of earth fissure and for preventing the effect that exploiting deep groundwater acted on geological environment.

中图分类号: 

[1] Wang Jingming,Wang Jiangshuai,Liu Jinfeng,et al. Theory and Applications of Earth Fissures and Hazard[M]. Xi′an: Shaanxi Science and Technology Publishing House,2000:85-135.[王景明,王江帅,刘金峰,.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, 2000:85-135.]

[2] Wang Qingliang,Liu Yuhai,Chen Zhixin,et al. Horizontal strain of aquifer induced by groundwater pumping—A new mechanism for Ground fissure movement [J].Journal of Engineering Geology,2002,10(1):46-50. [王庆良,刘玉海,陈志新,.抽水引起的含水层水平应变——地裂缝活动新机理[J].工程地质学报, 2002,10(1):46-50.]

[3] Helm D C.Hydraulic forces that play a role in generating fissures at depth[J]. Association of Engineering Geologists Bulletin,1994,31(3):293-304.

[4] Khalid A Bankher,Abbas A Al-Harthi. Earth Fissuring and Land Subsidence in Western Saudi Arabia [J]. Natural Hazards,1999,20(1): 21-42.

[5] Duan Yonghou,Luo Yuanhua,Liu Yuan, et al. The Geological Hazards in China[M].Bejing: China Architecture and Building Press,1993:15-18.[段永侯,罗元华,柳源,.中国地质灾害[M].北京:中国建筑工业出版社,1993:15-18.]

[6] Zhang Guanghui,Nie Zhenlong,Wang Jinzhe,et al. Sotopic characteristic and recharge effect of groundwater in the water circul ation of Hehe River basin[J].Advances in Earth Science,2005,20(5):511-519.[张光辉,聂振龙,王金哲,.黑河流域水循环过程中地下水同位素特征及补给效应[J]. 地球科学进展,2005,20(5):511-519.]

[7] Li Jiayang,Chen Panqin,Ge Quansheng,et al. Global change and human activities: Priorities of the global change research in next phase in China[J].Advances in Earth Science,2005,20(4):371-377.[李家洋,陈泮勤,葛全胜,.全球变化与人类活动的相互作用——我国下阶段全球变化研究工作的重点[J].地球科学进展,2005,20(4):371-377.]

[8] Li Jun,Liu Jinfeng,Mo Duowen. Distribution and origin of the rifts in Hebei plain[J].Research of Soil and Water Conservation,2003, 10(3):62-116. [李俊,刘金峰,莫多闻.河北平原地裂缝分布规律及成因初探[J].水土保持研究,2003, 10(3):62-116.]

[9] Zhang Lianjun. Discussion on the settlement caused by over-tapping deep ground water[J]. Journal of North China Institute of Water Conservancy and Hydroelectric Power,1999,20 (2):40-43.[张廉均.超采深层地下水引起地面沉降规律的探讨[J].华北水利水电学院学报, 1999, 20 (2):40-43.]

[10] Wu Fuchun,Fang Wei,Song Lisheng,et al. Analysis of the relationship among geothermal exploitation,ground subsidence and ground fissures in Xi′an city,China[J]. Seismology and Geology,2002,24(2): 234-240. [吴富春,方炜,宋立胜,.西安市地热水开采与地面沉降地裂缝关系的分析[J].地震地质,2002, 24(2): 234-240.]

[11] Helm D C. Hydraulic forces that play a role in generating fissures at depth[J]. Association of Engineering Geologists Bulletin,1994,31(3):293-304.

[12] Wu Qiang,Chen Peipei,Zhang Yu,et al. The problem and countermeasure of ground fracture in city[J]. The Chinese Journal of Geological Hazard and Control,2002,12(2):70-79.[武强,陈佩佩,张宇,.我国裂缝灾害问题与对策[J].中国地质灾害与防治学报, 2002, 12(2):70-79.]

[1] 毛绪美,梁杏,王凤林,韩庆之. 多源 4He及其积累年龄揭示的深层地下水更新能力[J]. 地球科学进展, 2011, 26(4): 417-425.
[2] 熊盛青,于长春,王卫平,范正国,王乃东,万建华,张洪瑞. 直升机大比例尺航空物探在深部找矿中的应用前景[J]. 地球科学进展, 2008, 23(3): 270-275.
[3] 王景明,王春梅,刘科. 地裂缝及其灾害研究的新进展[J]. 地球科学进展, 2001, 16(3): 303-343.
阅读次数
全文


摘要