Occurrence potential study on submarine Quaternary freshwater resources in the north Zhoushan sea area

Zhang Zhizhong; Zou Liang; Zhou Liangyong

doi:10.3969/j.issn.0253-4193.2018.03.005

Article Contents

Article Navigation > Haiyang Xuebao > 2018 > 40(3): 50-61

Zhang Zhizhong, Zou Liang, Zhou Liangyong. Occurrence potential study on submarine Quaternary freshwater resources in the north Zhoushan sea area[J]. Haiyang Xuebao, 2018, 40(3): 50-61. doi: 10.3969/j.issn.0253-4193.2018.03.005

Citation:

Zhang Zhizhong, Zou Liang, Zhou Liangyong. Occurrence potential study on submarine Quaternary freshwater resources in the north Zhoushan sea area[J]. Haiyang Xuebao, 2018, 40(3): 50-61. doi: 10.3969/j.issn.0253-4193.2018.03.005

Citation:

PDF( 36913 KB)

Occurrence potential study on submarine Quaternary freshwater resources in the north Zhoushan sea area

doi: 10.3969/j.issn.0253-4193.2018.03.005

1.
The Key Laboratory of Marine Hydrocarbon Resources and Environmental Geology, Ministry of Land and Resources, Qingdao Institute of Marine Geology, Qingdao 266071, China;Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266071, China
2.
The Key Laboratory of Marine Hydrocarbon Resources and Environmental Geology, Ministry of Land and Resources, Qingdao Institute of Marine Geology, Qingdao 266071, China

Received Date: 2017-06-12

Abstract

Abstract

To comprehend occurrence potential condition of submarine Quaternary freshwater resources in north Zhoushan sea area, Quaternary stratigraphic texture and sedimentary environment are analyzed based on drilling cores and high-resolution single-channel seismic profiles. Regularities of distribution of submarine loose sediment are elaborated. Extension and distribution of paleo-channels in middle and late Early-Pleistocene and early Early-Pleistocene form Shanghai land area and occurrence status of submarine Quaternary aquifer in the study sea area are discussed. The main exploitable Quaternary aquifers are the 4th confined aquifer in middle and late Early-Pleistocene and the 5th confined aquifer in early Early-Pleistocene. The water-abundance in the area of paleo-channels in the 4th confined aquifer is best, the confined aquifer with thick upper clay confining layer may be prone to reserving freshwater resources. The exploitable potential is classified into three types:better development prospect (type A), good development prospect (type B) and general development prospect (type C). The water-abundance in the area of paleo-channel in the 5th confined aquifer is also good, in which the reserving capacity and prospect of development and utilization are favorable.
- Quaternary,
- submarine paleo-channels,
- occurrence potential of freshwater resources,
- north Zhoushan sea area

FullText(HTML)

References(13)

References

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(2):644-651.

Perrine F, Michel B, Ghislain D M. Submarine springs and coastal karst aquifers:A review[J]. Journal of Hydrology, 2007, 339(3):79-92.

Vassilios K. Submarine groundwater discharge:Effects of hydrogeology and of near shore surface water bodies[J]. Journal of Hydrology, 2006, 325(3):96-117.

刘海龄, 吴世敏, 杨树康. 初谈海底淡水资源的形成条件与开发意义[J]. 海洋科学, 1995, 10(5):32-33. Liu Hailing, Wu Shimin, Yang Shukang. On the formation condition and exploitation significance of seafloor freshwater resources[J]. Marine Sciences, 1995, 10(5):32-33.

刘海龄, 吴世敏, 魏常兴. 论河口海底淡水资源的形成[J]. 自然资源学报, 1998, 13(4):364-367. Liu Hailing, Wu Shimin, Wei Changxing. On the formation of seafloor freshwater resources[J]. Journal of Natural Resources, 1998, 13(4):364-367.

张志忠, 邹亮, 韩月. 舟山北部海域海底淡水资源研究[J]. 地质论评, 2012, 57(1):81-86. Zhang Zhizhong, Zou Liang, Han Yue. Primary study on submarine freshwater resources in north Zhoushan sea area[J]. Geological Review, 2012, 57(1):81-86.

Vincent E A, Jacobus G, Henk K, et al. Offshore fresh groundwater reserves as a global phenomenon[J]. Nature, 2013, 504(12):71-77.

张志忠, 邹亮, 杨振京, 等. 舟山北部海域DZS2钻孔孢粉记录与古环境[J]. 海洋地质与第四纪地质, 2015, 35(4):125-132. Zhang Zhizhong, Zou Liang, Yang Zhenjing, et al. Sporo-pollen records of borehole DZS2 offshore north Zhoushan Islands and paleo-environmental implication[J]. Marine Geology & Quaternary Geology, 2015, 35(4):125-132.

邹亮, 张志忠, 韩月. 长江口外海区DZS2孔第四纪磁性地层[J]. 海洋地质与第四纪地质, 2015, 35(2):43-52. Zou Liang, Zhang Zhizhong, Han Yue. Magneto-stratigraphy of Core DZS2 off the Yangtze River estuary[J]. Marine Geology & Quaternary Geology, 2015, 35(2):43-52.

黎兵, 魏子新, 李晓, 等. 长江三角洲第四纪沉积记录与古环境响应[J]. 第四纪研究, 2011, 31(2):316-325. Li Bing, Wei Zixin, Li Xiao, et al. Records from Quaternary sediment and paleo-environment in the Yangtze River delta[J]. Quaternary Sciences, 2011, 31(2):316-325.

邱金波, 李晓. 上海市第四纪地层与沉积环境[M]. 上海:上海科学技术出版社, 2007. Qiu Jinbo, Li Xiao. Quternary Strata and Depositional Environment of Shanghai[M]. Shanghai:Shanghai Science and Technology Press, 2007.

李珍, 李杰, 李贞, 等. 浙江嵊泗海域第四纪沉积层序及承压水层位特征初探[J]. 上海地质, 2008, 29(1):7-13. Li Zhen, Li Jie, Li Zhen, et al. The primary research on the Quaterrnary stratigraphic sequence and the characteristics of the water bearing stratum in the sea of Shengsi area, Zhajiang province[J]. Shanghai Geology, 2008, 29(1):7-13.

陆志坚. 从上海地区地下淡水古河道含水的分布探讨嵊泗列岛的供水问题[J]. 上海地质, 1989, 10(1):23-26. Lu Zhijian. An approach to the water supply of the Shengsi Islands-from the distribution of the underground paleo-channels aquifer of freshwater in Shanghai area[J]. Shanghai Geology, 1989, 10(1):23-26.

Relative Articles

Supplements(0)

Cited By

Proportional views