莱州湾海底地下水动态及影响机制研究

侯国华; 高茂生; 郭飞; 孔祥淮; 赵金明; 仇建东; 刘森; 郑懿珉

doi:10.3969/j.issn.0253-4193.2016.05.011

莱州湾海底地下水动态及影响机制研究

doi: 10.3969/j.issn.0253-4193.2016.05.011

1.
中国地质调查局青岛海洋地质研究所国土资源部海洋油气资源和环境地质重点实验室, 山东青岛 266071;青岛海洋科学与技术国家实验室海洋地质过程功能实验室, 山东青岛 266061
2.
中国地质调查局青岛海洋地质研究所国土资源部海洋油气资源和环境地质重点实验室, 山东青岛 266071;中国石油大学地球科学与技术学院, 山东青岛 266555
3.
山东省第四地质矿产勘查院, 山东潍坊 261021
4.
中国地质调查局青岛海洋地质研究所国土资源部海洋油气资源和环境地质重点实验室, 山东青岛 266071

基金项目: 国家自然科学基金(41476051,41306063);国家海洋地质保障工程专项(GZH201200505);科技基础性工作专项(2014FY210600)。

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出版历程
- 收稿日期: 2015-06-08

Research on submarine groundwater dynamics and driving mechanism in the Laizhou Bay

1.
Key Laboratory of Marine Hydrocarbon Resources and Environmental Geology, Ministry of Land and Resources, China Geological Survey, Qingdao Institute of Marine Geology, Qingdao 266071, China;Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266061, China
2.
Key Laboratory of Marine Hydrocarbon Resources and Environmental Geology, Ministry of Land and Resources, China Geological Survey, Qingdao Institute of Marine Geology, Qingdao 266071, China;School of Geosciences, China University of Petroleum, Qingdao 266555, China
3.
Exploration Institute of Geology and Mineral Resources, Weifang 261021, China
4.
Key Laboratory of Marine Hydrocarbon Resources and Environmental Geology, Ministry of Land and Resources, China Geological Survey, Qingdao Institute of Marine Geology, Qingdao 266071, China

摘要

摘要: 地下水监测及数理分析是地下水动态研究的主要方法。但目前海岸带地区多以陆域地下水监测为主,海域部分尤其具有多层含水层系统的海底地下水缺少直接监测数据。本研究通过海域钻孔ZK03与ZK08实时监测不同层位海底地下水动态以及海洋潮汐变化,结合其地层结构和沉积演化背景,分析莱州湾海底地下水动态特征并揭示其影响机制。研究结果表明,莱州湾海底地下水动态具有周期性和分层性特征;全新世含水层与海水关系密切,其海水入侵界面垂向上厚10 m左右。海底地下水分层与沉积地层划分大致相同,其动态特征是在地层结构及沉积演化环境影响下,降水、径流及潮汐驱动不同层深地下水间或地下水与海水间混合作用的结果。本文初步构建了海底地下水分布模式,探讨区域地下水与海水的相互作用关系。莱州湾海底地下水动态研究对于深入分析海(咸)水界面变化机制及探索海底地下水排泄具有推动作用。
- 莱州湾 /
- 海底地下水 /
- 动态特征 /
- 影响机制
Abstract: Groundwater monitoring combined with mathematical analysis is the main method of groundwater dynamics studies. But there is less monitoring data for submarine groundwater than inland groundwater in the most coastal areas. In this study, sea drillings ZK03, ZK08 were designed to real-time monitor dynamics characteristic of submarine groundwater in multi-layers aquifers and ocean tides. Combined with stratum structure and sedimentary evolution setting, the paper analyzed the dynamic characteristics of submarine groundwater in the Laizhou Bay and revealed the driving mechanism. The results showed that submarine groundwater dynamic appeared to be periodic and stratified in the Laizhou Bay, Holocene aquifer were closely associated with the sea, where the vertical thickness of seawater intrusion interface was about 10 m. Submarine groundwater stratification were roughly consistent with sedimentary strata. Controlled by strata structure and sedimentary environment, the mixing process in different aquifer groundwater or between groundwater and seawater drived by precipitation, groundwater runoff and tide was the main driving mechanism of submarine groundwater dynamic. Then the paper constructed a preliminary submarine groundwater distribution pattern to explore the interaction between groundwater and seawater. The study on the dynamics characteristic of submarine groundwater in the Laizhou Bay play a positive role in analyzing saltwater interface change mechanism and exploring the submarine groundwater discharge.
- Laizhou Bay /
- submarine groundwater /
- dynamic characteristic /
- driving mechanism

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参考文献(29)

丰爱平, 谷东起, 夏东兴. 莱州湾南岸海水入侵发展动态和原因[J]. 海岸工程, 2006, 25(3): 7-13. Feng Aiping, Gu Dongqi, Xia Dongxing. Developments and causes of seawater intrusion in the south coast area of the Laizhou Bay[J]. Coastal Engineering, 2006, 25(3):7-13.

陈广泉. 莱州湾地区海水入侵的影响机制及预警评价研究[D]. 上海: 华东师范大学, 2013. Chen Guangquan. Mechanisms underlying of seawater intrusion and evaluation of early warning systems in the Laizhou Bay area[D]. Shanghai: East China Normal University, 2013.

薛禹群, 吴吉春, 谢春红, 等. 莱州湾沿岸海水入侵与咸水入侵研究[J]. 科学通报, 1997, 42(22): 2360-2368 Xue Yuqun, Wu Jichun, Xie Chunhong, et al. The researches of seawater and saltwater intrusion in the coastal area of Laizhou Bay[J]. Chinese Seience Bulletin, 1997, 42(22): 2360-2368.

Xue Y, Wu J, Ye S, et al. Hydrogeological and hydrogeochemical studies for salt water intrusion on the south coast of Laizhou Bay, China[J]. Ground Water, 2000,38(1):38-45.

Moore W S. Large groundwater inputs to coastal waters revealed by 226Ra enrichments[J]. Nature, 1996, 380(6575): 612-614.

Uchiyama Y, Nadaoka K, Rölke P, et al. Submarine groundwater discharge into the sea and associated nutrient transport in a sandy beach[J]. Water Resources Research, 2000, 36(6): 1467-1479.

李海龙, 万力, 焦赳赳. 海岸带水文地质学研究中的几个热点问题[J]. 地球科学进展, 2011, 26(7): 685-694. Li Hailong, Wan Li,Jiao Jiujiu. Hot issues in the study of coastal hydrogeology[J]. Advances in Earth Science, 2011, 26(7): 685-694.

Porubsky W P, Weston N B, Moore W S, et al. Dynamics of submarine groundwater discharge and associated fluxes of dissolved nutrients, carbon, and trace gases to the coastal zone (Okatee River estuary, South Carolina)[J]. Geochimica et Cosmochimica Acta, 2014,131(5): 81-97.

Li H, Jiao J. Quantifying tidal contribution to submarine groundwater discharges: A review[J]. Chin Sci Bull, 2013, 25(25): 3053-3059.

Rodellas V, Garcia-Orellana J, Tovar-Snchez A, et al. Submarine groundwater discharge as a source of nutrients and trace metals in a Mediterranean bay (Palma Beach, Balearic Islands)[J]. Marine Chemistry, 2014, 160(3): 56-66.

Santos I R, Eyre B D, Huettel M. The driving forces of porewater and groundwater flow in permeable coastal sediments: A review[J]. Estuarine, Coastal and Shelf Science, 2012, 98(1): 1-15.

McCoy C A, Corbett D R. Review of submarine groundwater discharge (SGD) in coastal zones of the Southeast and Gulf Coast regions of the United States with management implications[J]. Journal of Environmental Management, 2009, 90(1): 644-651.

Taniguchi M, Burnett W C, Cable J E, et al. Investigation of submarine groundwater discharge[J]. Hydrological Processes, 2002,16(11):2115-2129.

Wu J, Xue Y, Liu P, et al. Sea-water intrusion in the coastal area of Laizhou Bay, China: 2. sea-water intrusion monitoring[J]. Ground Water, 1993, 31(5): 740-745.

Meng Guanglan, Han Yousong, Han Shaoqing, et al. Seawater intrusion types and regional divisions in the southern coast of Laizhou Bay[J]. Chin J Ocean Limnol, 2002, 20(3): 277-284.

Zhou X, Chen M, Ju X, et al. Numerical simulation of sea water intrusion near Beihai, China[J]. Env Geol, 2000, 40(1/2): 223-233.

Kim K Y, Seong H, Kim T, et al. Tidal effects on variations of fresh-saltwater interface and groundwater flow in a multilayered coastal aquifer on a volcanic island (Jeju Island, Korea)[J]. Journal of Hydrology, 2006, 330(3): 525-542.

周训, 阮传侠, 方斌, 等. 海潮及其影响下海岸带地下水位时间序列的周期性和滞后性[J]. 水文地质工程地质, 2006, 5(5): 71-74. Zhou Xun, Ruan Chuanxia, Fang Bin, et al. Period and lag of the time series of tide and groundwater levels affected by the tide in coastal aquifers[J]. Hydrogeology and Engineering Geology, 2006, 5(5): 71-74.

Shalev E, Lazar A, Wollman S, et al. Biased monitoring of fresh water-salt water mixing zone in coastal aquifers[J]. Ground Water, 2009, 47(1): 49-56.

Wang X, Li H, Wan L, et al. Loading effect of water table variation and density effect on tidal head fluctuations in a coastal aquifer system[J]. Water Resources Research, 2012, 48(9): 73-87.

冷莹莹, 李祥虎, 刘蕾. 潍坊市北部天然卤水矿床特征及成因分析[J]. 成都理工大学学报(自然科学版), 2009, 36(2):188-194. Leng Yingying, Li Xianghu, Liu Lei. Characteristics and genesis of the natural brine deposit in the north of Weifang, Shandong, China[J]. Journal of Chengdu University of Technology(Science & Technology Edition), 2009, 36(2):188-194.

秦蕴珊. 渤海地质[M]. 北京: 科学出版社, 1985. Qin Yunshan. Bohai Geology[M]. Beijing: Science Press, 1985.

高茂生, 郑懿珉, 刘森, 等. 莱州湾地下卤水形成的古地理条件分析[J]. 地质论评, 2015, 61(2): 393-400. Gao Maosheng, Zheng Yimin, Liu Sen, et al. Palaeogeographic condition for orign of underground brine in sourthern coast of Laizhou Bay, Bohai Sea[J]. Geological Review, 2015, 61(2): 393-400.

王松涛, 高美霞, 傅俊鹤. 山东潍坊沿海地下卤水矿地质特征及成矿规律[J]. 矿床地质, 2008, 5(5): 631-637. Wang Songtao, Gao Meixia, Fu Junhe. Geological characteristics and metal logenic regularity of underground brine ore in coastal areas of Weifang, Shandong Province[J]. Mineral Deposits, 2008, 5(5): 631-637.

Li H, Jiao J J. Tide-induced groundwater fluctuation in a coastal leaky confined aquifer system extending under the sea[J]. Water Resources Research, 2001, 37(5):1165-1171.

郭巧娜. 滨海多层含水层系统中多组分地下水流及海底地下水排泄[D]. 北京: 中国地质大学, 2010. Guo Qiaona. Multicomponent groundwater flow and submarine groundwater discharge in coastal multilayered aquifer systems[D]. Beijing: China University of Geosciences, 2010.

Austin M J, Masselink G. Swash-groundwater interaction on a steep gravel beach[J]. Continental Shelf Research, 2006, 26(20): 2503-2519.

韩有松, 孟广兰, 王少青. 渤海莱州湾滨海平原晚第四纪地质事件与古环境[D]. 海洋科学集刊, 1994, 35: 87-96. Han Yousong, Meng Guanglan, Wang Shaoqing. The geological events and paleo-environment of the coastal plain of Laizhou Bay in Bohai Sea during late Quaternary[D]. Studia Marina Sinica, 1994, 35: 87-96.

Han D, Kohfahl C, Song X, et al. Geochemical and isotopic evidence for palaeo-seawater intrusion into the south coast aquifer of Laizhou Bay, China[J]. Applied Geochemistry, 2011, 26(5): 863-883.

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