山东蓬莱玄武岩覆盖区高密度电法找水效果分析
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摘要
蓬莱市北沟镇迎口山火山及周围为一新生代玄武岩台地,近年来区域经济发展过程中,周边工业用水量急剧增加,当地居民日常饮水十分困难.高密度电法作为一种有效的地球物理勘探方法在地下水资源调查、活动断裂探测等方面应用广泛.本文依据玄武岩地下水以原生孔洞、节理缝和次生裂隙等组成的裂隙孔洞储水层地质特点,选择高密度电法温纳α装置,在北沟镇迎口火山南侧2 km玄武岩地区寻找地下潜在水资源,通过6条高密度电法测量剖面(P1-P6),发现在P1和P2剖面中存在多段连续性较好的低阻异常区.低阻异常区均分布于一厚度大于30 m玄武岩高阻异常区之下,连续低阻异常在剖面垂直地面向下延伸范围较大,作为良好的地下水资源分布区得到了现有水井的验证.研究表明高密度电法在玄武岩区调查水资源是一种行之有效的技术方法,可为未来玄武岩区找水提供技术支撑.
Beigou town Penglai city Yingkou mountain volcano and the surrounding is a Cenozoic basalt platform.In recent years,with the regional economic process the surrounding industrial water consumption increased dramatically, the local residents of daily drinking water is very difficult. As an effective geophysical prospecting method, high density electrical method is widely used in groundwater resource investigation and active fault detection. In this paper, based on the original groundwater in basalt cavities, joint fissures and secondary cracks are composed of fissures and holes aquifers geological characteristics, the high-density electrical method is selected to find potential underground water in the 2 km basalt area in the south of volcano(P1-P6). It is found that there are many low-resistance anomalies with good continuity in the P1 and P2 profiles, and low resistivity anomaly areas are distributed in a thickness greater than the high resistivity anomaly zone of 30 m basalt under the continuous low resistivity profile in vertical downward range is large. The distribution of the groundwater resources as a good groundwater resource area has been verified by the existing wells,and the study indicats that the high density electrical method is an effective technical method for the future basalt area to provide technical support for water.
Beigou town Penglai city Yingkou mountain volcano and the surrounding is a Cenozoic basalt platform.In recent years,with the regional economic process the surrounding industrial water consumption increased dramatically, the local residents of daily drinking water is very difficult. As an effective geophysical prospecting method, high density electrical method is widely used in groundwater resource investigation and active fault detection. In this paper, based on the original groundwater in basalt cavities, joint fissures and secondary cracks are composed of fissures and holes aquifers geological characteristics, the high-density electrical method is selected to find potential underground water in the 2 km basalt area in the south of volcano(P1-P6). It is found that there are many low-resistance anomalies with good continuity in the P1 and P2 profiles, and low resistivity anomaly areas are distributed in a thickness greater than the high resistivity anomaly zone of 30 m basalt under the continuous low resistivity profile in vertical downward range is large. The distribution of the groundwater resources as a good groundwater resource area has been verified by the existing wells,and the study indicats that the high density electrical method is an effective technical method for the future basalt area to provide technical support for water.
引文
Cao X W, Ma X M, Hu D G, el al. 2017. Application of the resistivity tomography method to detection of active faults Northeast of the Hainan Island [J]. Geology and Exploration (in Chinese), 53(5): 1001-1009.
Chen Z D, Zhang B Z. 1994. Basic characteristics of groundwater in basalt in the Changbai Mount area [J]. Journal of Fuxin Mining Institue(Natural Science) (in Chinese), 13(4): 26-29.
Cheng G G. 2013. The Application of high-density electric method in search of groundwater in the southeast of Chongqin [J]. Underground Water (in Chinese), 35(3): 106-109.
Guo L P, Zhao J. 2007. The volcano landscape of Yingkou Hill in Penglai,Shangdong provience [J]. Journal of Taiyuan Normal University(Natural Science) (inChinese), 6(1): 88-90.
Jia F H.1993.Basalt Groundwater in China[J].BeiJing:Geology Press.
Jiang Z J, Bian J M, Zha E S, et al. 2010. The Application of electrical resistivty tomography in hydrology: An overview [J]. Hydrogeology & Engineerng Geology (inChinese), 37(2): 21-26.
Kong Z H. 2004. Hydrogeological property and laws of water abundance of the volcanic rocks in LeiZhou Peninsula [J] TROPICAL GEOGRAPHY (inChinese), 24(2):136-139.
Li H J, Zhu Q J, Li W. 2012. Storage rules and electrical characteristics of groundwater in Cenozoic basalt in Linqu county of, ShanDong [J]. South-to-North Water Transfers and Water Science & Technology (inChinese), 10(6): 65-69.
Liu C H. 2008. Hydrogeology engineering and electric prospecting for water [M]. Zhengzhou: The Yellow River Water Conservancy Press.
Mu H B, Zhang X H, Luan C. 2003. Laws of water abundance of the volcanic rock [J], Underground Water (in Chinese), 35(6): 46-47,112.
Ou Y W, Xu X Y. 2013. Application of high density resistivity method in water exploration in limestone [J]. North China Earthquake Sciences (in Chinese), 31(4): 47-49.
Pan S Z, Wang F Y, Zheng Y P, et al. 2015. Crustal velocity structure beneath Jiaodong Peninsula and its tectonic implications [J]. Chinese Journal of Geophys (in Chinese), 58(9): 3251-3263, doi: 10.6038/cjg20150920.
Qin J F. 2012. Application effect of comprehensive electric method in finding emergency water for fighting a drought [J]. Site Investigation Science and Technology (in Chinese), 3: 58-61.
Song H W, Zhang Y L, Xia F, et al. 2011. Analysis of the water investigation by super density electrical method and IP in Hebei [J]. South-to-North Water Transfers and Water Science & Technology (in Chinese), 9(4): 60-62.
Tian Y K, Liu H S, Zhang J, et al. 2008. The application of High-density electrical Methord in Search of Groundwater in Jimo[J]. Chinese Journal of Enginnering Geophysics.5(6):670-674.
Wang S P. 2000. Application of high-density electrical method in hydrogeology and engineering geology [J]. Hydrogeology & Engineerng Geology (in Chinese), 27(1):52-56.
Xian S S. 2015. Application of high-density electrical method in groundwater exploration under complex geologic structural conditions [J]. Geology and Resources (in Chinese), 24(2): 132-136.
Zhang X L, Xu Q, Peng D L, et al. 2017. Application of high density resitivity method to ground water exploration in Hei fang tai [J]. Progress in Geophysics (in Chinese), 32(4): 1862-1867, doi: 10.6038/pg20170462.
Zhang Z Q,Liu W M. 2008. lithostratigraphy of ShangDong Province[M]. Wuhan: China University of Geoscience.
曹新文, 马秀敏, 胡道功. 2017. 电阻率层析成像技术在琼东北活动断裂探测中的应用[J]. 地质与勘探, 53(5): 1001-1009.
陈振东, 张宝柱. 1994. 长白山地区玄武岩地下水基本特征[J]. 阜新矿业学院学报(自然科学版), 13(4): 26-29.
程光贵. 2013. 高密度电法在渝东南地区找水勘查中的应用[J]. 地下水, 35(3): 106-109.
郭柳平, 赵建. 2007. 山东蓬莱迎口山火山地貌景观[J]. 太原师范学院学报(自然科学版), 6(1): 88-90.
贾福海. 1993. 中国玄武岩地下水[M]. 北京: 地质出版社.
姜振蛟, 卞建民, 查恩爽, 等. 2010. 高密度电阻率成像法在水文地质领域的应用[J]. 水文地质工程地质, 37(2): 21-26.
孔中恒. 2004. 雷州半岛火山岩的水文地质特征及富水规律[J]. 热带地理, 24(2): 136-139.
李慧杰, 朱庆俊, 李伟. 2012. 山东临朐新生代玄武岩地下水赋存规律及电性特征[J]. 南水北调与水利科技, 10(6): 65-69.
刘春华.2008.水文地质与电测找水技术[M].郑州:黄河水利出版社.
龙凡. 2014. 干旱缺水地区地下水勘察技术[M]. 沈阳: 辽宁科学技术出版社.
穆洪波, 张晓红, 栾城. 2013. 火山岩地下水分布规律的探讨[J]. 地下水, 35(6): 46-47,112.
欧阳伟, 徐晓英. 2013. 高密度电法在灰岩找水中的应用[J]. 华北地震科学, 31(4): 47-49.
潘素珍, 王夫运, 郑彦鹏, 等. 2015. 胶东半岛地壳速度结构及其构造意义[J]. 地球物理学报, 58(9): 3251-3263, doi: 10.6038/cjg20150920.
秦军付. 2012. 多种电法在抗旱应急找水中的应用效果[J]. 勘查科学技术, 3: 58-61.
宋洪伟, 张翼龙, 夏凡. 2011. 超高密度电法和激电法在河北某地找水实例分析[J]. 南水北调与水利科技, 9(4): 60-62.
田玉昆,刘怀山,张晶,等.2008.高密度找水在即墨地区的应用[J]. 工程地球物理学报,5(6):670-674.
王士鹏. 2000. 高密度电法在水文地质和工程地质中的应用 [J]. 水文地质工程地质, 27(1): 52-56.
冼诗盛. 2015. 高密度电法在复杂地质构造条件下的找水效果[J]. 地质与资源, 24(2): 132-136.
张先林, 许强, 彭大雷, 等. 2017. 高密度电法在黑方台地下水探测中的应用[J]. 地球物理学进展, 32(4): 1862-1867, doi: 10.6038/pg20170462.
张增奇,刘明渭. 2008. 山东省岩石地层[M].武汉:中国地质大学出版社.
Chen Z D, Zhang B Z. 1994. Basic characteristics of groundwater in basalt in the Changbai Mount area [J]. Journal of Fuxin Mining Institue(Natural Science) (in Chinese), 13(4): 26-29.
Cheng G G. 2013. The Application of high-density electric method in search of groundwater in the southeast of Chongqin [J]. Underground Water (in Chinese), 35(3): 106-109.
Guo L P, Zhao J. 2007. The volcano landscape of Yingkou Hill in Penglai,Shangdong provience [J]. Journal of Taiyuan Normal University(Natural Science) (inChinese), 6(1): 88-90.
Jia F H.1993.Basalt Groundwater in China[J].BeiJing:Geology Press.
Jiang Z J, Bian J M, Zha E S, et al. 2010. The Application of electrical resistivty tomography in hydrology: An overview [J]. Hydrogeology & Engineerng Geology (inChinese), 37(2): 21-26.
Kong Z H. 2004. Hydrogeological property and laws of water abundance of the volcanic rocks in LeiZhou Peninsula [J] TROPICAL GEOGRAPHY (inChinese), 24(2):136-139.
Li H J, Zhu Q J, Li W. 2012. Storage rules and electrical characteristics of groundwater in Cenozoic basalt in Linqu county of, ShanDong [J]. South-to-North Water Transfers and Water Science & Technology (inChinese), 10(6): 65-69.
Liu C H. 2008. Hydrogeology engineering and electric prospecting for water [M]. Zhengzhou: The Yellow River Water Conservancy Press.
Mu H B, Zhang X H, Luan C. 2003. Laws of water abundance of the volcanic rock [J], Underground Water (in Chinese), 35(6): 46-47,112.
Ou Y W, Xu X Y. 2013. Application of high density resistivity method in water exploration in limestone [J]. North China Earthquake Sciences (in Chinese), 31(4): 47-49.
Pan S Z, Wang F Y, Zheng Y P, et al. 2015. Crustal velocity structure beneath Jiaodong Peninsula and its tectonic implications [J]. Chinese Journal of Geophys (in Chinese), 58(9): 3251-3263, doi: 10.6038/cjg20150920.
Qin J F. 2012. Application effect of comprehensive electric method in finding emergency water for fighting a drought [J]. Site Investigation Science and Technology (in Chinese), 3: 58-61.
Song H W, Zhang Y L, Xia F, et al. 2011. Analysis of the water investigation by super density electrical method and IP in Hebei [J]. South-to-North Water Transfers and Water Science & Technology (in Chinese), 9(4): 60-62.
Tian Y K, Liu H S, Zhang J, et al. 2008. The application of High-density electrical Methord in Search of Groundwater in Jimo[J]. Chinese Journal of Enginnering Geophysics.5(6):670-674.
Wang S P. 2000. Application of high-density electrical method in hydrogeology and engineering geology [J]. Hydrogeology & Engineerng Geology (in Chinese), 27(1):52-56.
Xian S S. 2015. Application of high-density electrical method in groundwater exploration under complex geologic structural conditions [J]. Geology and Resources (in Chinese), 24(2): 132-136.
Zhang X L, Xu Q, Peng D L, et al. 2017. Application of high density resitivity method to ground water exploration in Hei fang tai [J]. Progress in Geophysics (in Chinese), 32(4): 1862-1867, doi: 10.6038/pg20170462.
Zhang Z Q,Liu W M. 2008. lithostratigraphy of ShangDong Province[M]. Wuhan: China University of Geoscience.
曹新文, 马秀敏, 胡道功. 2017. 电阻率层析成像技术在琼东北活动断裂探测中的应用[J]. 地质与勘探, 53(5): 1001-1009.
陈振东, 张宝柱. 1994. 长白山地区玄武岩地下水基本特征[J]. 阜新矿业学院学报(自然科学版), 13(4): 26-29.
程光贵. 2013. 高密度电法在渝东南地区找水勘查中的应用[J]. 地下水, 35(3): 106-109.
郭柳平, 赵建. 2007. 山东蓬莱迎口山火山地貌景观[J]. 太原师范学院学报(自然科学版), 6(1): 88-90.
贾福海. 1993. 中国玄武岩地下水[M]. 北京: 地质出版社.
姜振蛟, 卞建民, 查恩爽, 等. 2010. 高密度电阻率成像法在水文地质领域的应用[J]. 水文地质工程地质, 37(2): 21-26.
孔中恒. 2004. 雷州半岛火山岩的水文地质特征及富水规律[J]. 热带地理, 24(2): 136-139.
李慧杰, 朱庆俊, 李伟. 2012. 山东临朐新生代玄武岩地下水赋存规律及电性特征[J]. 南水北调与水利科技, 10(6): 65-69.
刘春华.2008.水文地质与电测找水技术[M].郑州:黄河水利出版社.
龙凡. 2014. 干旱缺水地区地下水勘察技术[M]. 沈阳: 辽宁科学技术出版社.
穆洪波, 张晓红, 栾城. 2013. 火山岩地下水分布规律的探讨[J]. 地下水, 35(6): 46-47,112.
欧阳伟, 徐晓英. 2013. 高密度电法在灰岩找水中的应用[J]. 华北地震科学, 31(4): 47-49.
潘素珍, 王夫运, 郑彦鹏, 等. 2015. 胶东半岛地壳速度结构及其构造意义[J]. 地球物理学报, 58(9): 3251-3263, doi: 10.6038/cjg20150920.
秦军付. 2012. 多种电法在抗旱应急找水中的应用效果[J]. 勘查科学技术, 3: 58-61.
宋洪伟, 张翼龙, 夏凡. 2011. 超高密度电法和激电法在河北某地找水实例分析[J]. 南水北调与水利科技, 9(4): 60-62.
田玉昆,刘怀山,张晶,等.2008.高密度找水在即墨地区的应用[J]. 工程地球物理学报,5(6):670-674.
王士鹏. 2000. 高密度电法在水文地质和工程地质中的应用 [J]. 水文地质工程地质, 27(1): 52-56.
冼诗盛. 2015. 高密度电法在复杂地质构造条件下的找水效果[J]. 地质与资源, 24(2): 132-136.
张先林, 许强, 彭大雷, 等. 2017. 高密度电法在黑方台地下水探测中的应用[J]. 地球物理学进展, 32(4): 1862-1867, doi: 10.6038/pg20170462.
张增奇,刘明渭. 2008. 山东省岩石地层[M].武汉:中国地质大学出版社.