Sublacustrine sedimentary topography detection and analysis of Poyang Lake based on sub-bottom profiler

ZHANG Hong; ZHOU Quanping; JIANG Yuehua; JIN Yang; CHEN Zi; JIA Zhengyang; MEI Shijia

doi:10.16788/j.hddz.32-1865/P.2023.03.007

2023 Vol. 44, No. 3

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Article navigation > East China Geology > 2023 > 44(3): 313-322

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ZHANG Hong, ZHOU Quanping, JIANG Yuehua, JIN Yang, CHEN Zi, JIA Zhengyang, MEI Shijia. 2023. Sublacustrine sedimentary topography detection and analysis of Poyang Lake based on sub-bottom profiler. East China Geology, 44(3): 313-322. doi: 10.16788/j.hddz.32-1865/P.2023.03.007

Citation:

ZHANG Hong, ZHOU Quanping, JIANG Yuehua, JIN Yang, CHEN Zi, JIA Zhengyang, MEI Shijia. 2023. Sublacustrine sedimentary topography detection and analysis of Poyang Lake based on sub-bottom profiler. East China Geology, 44(3): 313-322. doi: 10.16788/j.hddz.32-1865/P.2023.03.007

Sublacustrine sedimentary topography detection and analysis of Poyang Lake based on sub-bottom profiler

1. Nanjing Center, China Geological Survey, Nanjing 210016, Jiangsu, China;
2. Key Laboratory of Watershed Eco-Geological Processes, Ministry of Natural Resources, Nanjing 210016, Jiangsu, China;
3. Chinese Academy of Geological Sciences, Beijing 100037, China

More Information

Corresponding author: JIN Yang, jinyang@mail.cgs.gov.cn

Received Date: 27 April 2023

Revised Date: 05 June 2023

Abstract

Abstract

Poyang Lake is an important freshwater, sand and stone source area in China, where its sublacustrine sedimentary topography has always drawn much attention in academia. This study systematically investigates the underwater topography and sedimentary characteristics of Poyang Lake with sub-bottom profiler. Data analysis of 32 survey lines revealed that the depth of Poyang Lake varies from 0.16 m to 23.71 m, with the water channel into Yangtze River and the northwest part of the main lake area being relatively deeper. The thickness of unconsolidated sediment varies from 0 m to 8.73 m, with thick layers concentrating in the central part of the main lake area, and the estimated volume of the unconsolidated sediments is approximately 3.02 km³. In September 2022, shallow drilling exploration is conducted in the main lake area to verify the reliability of the data from sub-bottom profiler. Comparison with previous studies indicates that large-scale sand mining can significantly impact the bottom topography of Poyang Lake. This study comprehensively reveals the current state of underwater topography and sedimentary characteristics of Poyang Lake, and the conclusion is useful for the relevant research and management.
- Poyang Lake /
- sub-bottom profiler /
- sublacustrine topography /
- thickness and volume of unconsolidated sediments

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References

[1]	朱海虹,张本,郑长苏,等.鄱阳湖:水文生物·沉积·湿地·开发整治[M].合肥:中国科学技术大学出版社,1997:1-10. Google Scholar ZHU H H, ZHANG B, ZHENG C S, et al. Poyang lake:hydrology and biology·deposit·wetland·development and rehabilitation[M]. Hefei:Press of University of Science and Technology of China, 1997:1-10. Google Scholar
[2]	马超,顾延生,刘春根,等.鄱阳湖东南部地区全新统植硅体组合特征与古环境分析[J].华东地质, 2018, 39(3):187-193. Google Scholar MA C, GU Y S, LIU C G, et al. Characteristics of Holocene phytolith assemblage in the southeast of Poyang Lake and its paleoenvironmental implications[J]. East China Geology, 2018, 39(3):187-193. Google Scholar
[3]	YE X C, GUO Q, ZHANG Z X, et al. Assessing hydrological and sedimentation effects from bottom topography change in a complex river-lake system of Poyang Lake, China[J]. Water,2019, 11(7):1489. Google Scholar
[4]	姚仕明,胡呈维,渠庚,等.长江通江湖泊演变及其影响效应研究进展[J].长江科学院院报, 2022, 39(9):15-23. Google Scholar YAO S M, HU C W, QU G, et al. Research advances in morphological evolution of lakes connecting the Yangtze river and its influences[J]. Journal of Yangtze River Scientific Research Institute, 2022, 39(9):15-23. Google Scholar
[5]	张龚泉,岳建平,刘胜男,等.基于遥感影像的鄱阳湖地形提取方法[J].测绘通报, 2022(5):62-66. Google Scholar ZHANG G Q, YUE J P, LIU S N, et al. Terrain extraction method of Poyang Lake based on remote sensing image[J]. Bulletin of Surveying and Mapping, 2022(5):62-66. Google Scholar
[6]	邴建平.长江-鄱阳湖江湖关系演变趋势与调控效应研究[D].武汉:武汉大学, 2018. BING J P. The evolution trend and regulation effect of the Yangtze River-Poyang Lake relationship[D]. Wuhan:Wuhan University, 2018. Google Scholar
[7]	FENG L, HU C M, CHEN X L, et al. MODIS observations of the bottom topography and its inter-annual variability of Poyang Lake[J]. Remote Sensing of Environment, 2011, 115(10):2729-2741. Google Scholar
[8]	刘前进,董毓,封林波.九江地区长江沿岸工程地质特征与岸坡稳定性探讨[J].华东地质, 2017, 38(2):147-154. Google Scholar LIU Q J, DONG Y, FENG L B. Engineering geological characteristics and bank slope stability in the Jiujiang region along the Yangtze River[J]. East China Geology, 2017, 38(2):147-154. Google Scholar
[9]	FANG C, LU S L, LI M Y, et al. Lake water storage estimation method based on similar characteristics of above-water and underwater topography[J]. Journal of Hydrology, 2023, 618:129-146. Google Scholar
[10]	许小华,雷声,王小笑,等.基于DEM的鄱阳湖水下地形分析[J].人民长江, 2014, 45(21):30-32. Google Scholar XU X H, LEI S, WANG X X, et al. Underwater topography analysis of Poyang Lake by DEM[J]. Yangtze River, 2014, 45(21):30-32. Google Scholar
[11]	吴桂平,刘元波,范兴旺.近30年来鄱阳湖湖盆地形演变特征与原因探析[J].湖泊科学, 2015, 27(6):1168-1176. Google Scholar WU G P, LIU Y B, FAN X W. Bottom topography change patterns of the Lake Poyang and their influence mechanisms in recent 30 years[J]. Journal of Lake Sciences, 2015, 27(6):1168-1176. Google Scholar
[12]	王淑平,程和琴,郑树伟,等.近期长江与鄱阳湖汇流河段冲淤变化与微地貌特征[J].泥沙研究, 2018, 43(3):15-20. Google Scholar WANG S P, CHENG H Q, ZHENG S W, et al. Fluvial processes and micro-topography characteristics in the Yangtze River and Poyang Lake confluence in recent years[J]. Journal of Sediment Research, 2018, 43(3):15-20. Google Scholar
[13]	向诗月.近期鄱阳湖侵蚀基准面变化及其对水情与湖床演变的影响[D].上海:华东师范大学, 2021. XIANG S Y. Recent changes of erosion datum in Poyang Lake and their effects on hydrological regime and lake bed evolution[D]. Shanghai:East China Normal University, 2021. Google Scholar
[14]	王毛兰.鄱阳湖流域氮磷时空分布及其地球化学模拟[D].南昌:南昌大学, 2007. WANG M L. Spatio-temporal distribution of nitrogen and phosphorus and its geochemical modeling in Poyang Lake catchments[D]. Nanchang:Nanchang University, 2007. Google Scholar
[15]	霍雨.鄱阳湖形态特征及其对流域水沙变化响应研究[D].南京:南京大学, 2011. HUO Y. Poyang Lake morphological characteristics and its response to runoff and sediment of Poyang Lake Basin[D]. Nanjing:Nanjing University, 2011. Google Scholar
[16]	李平,杜军.浅地层剖面探测综述[J].海洋通报, 2011, 30(3):344-350. Google Scholar LI P, DU J. Review on the probing of sub-bottom profiler[J]. Marine Science Bulletin, 2011, 30(3):344-350. Google Scholar
[17]	武传鹏,佟弢.浅地层剖面探测在水域工程中的应用及问题分析[J].港工技术, 2022, 59(5):117-120. Google Scholar WU C P, TONG T. Analysis for application of shallow stratigraphic profiler in marine engineering[J]. Port Engineering Technology, 2022, 59(5):117-120. Google Scholar
[18]	LAFFERTY B, QUINN R, BREEN C. A side-scan sonar and high-resolution Chirp sub-bottom profile study of the natural and anthropogenic sedimentary record of Lower Lough Erne, northwestern Ireland[J]. Journal of Archaeological Science, 2006, 33:756-766. Google Scholar
[19]	ZHENG S W, CHENG H Q, TANG M, et al. Sand mining impact on Poyang Lake:A case study based on high-resolution bathymetry and sub-bottom data[J]. Journal of Oceanology and Limnology, 2022, 40(4):1404-1416. Google Scholar
[20]	武彬,林丰增,张艺武,等.福建宁德近岸海域海底浅层气分布特征及成因分析[J].华东地质, 2022, 43(1):87-93. Google Scholar WU B, LIN F Z, ZHANG Y W, et al. Distribution characteristics and genesis analysis of submarine shallow gas in Ningde coastal area, Fujian Provice[J]. East China Geology, 2022, 43(1):87-93. Google Scholar
[21]	朱诚,张奇,陈星,等.江西鄱阳湖老爷庙水域环境特征与沉船事件的成因研究[J].自然灾害学报, 2021, 30(6):198-208. Google Scholar ZHU C, ZHANG Q, CHEN X, et al. Environmental characteristics of Laoyemiao water area and causes of shipwreck in Poyang Lake[J]. Journal of Natural Disasters, 2021, 30(6):198-208. Google Scholar
[22]	马振兴,蒋玉珍,魏源,等.鄱阳湖组(第四系)的修订及特征[J].地层学杂志, 2003, 27(3):212-215. Google Scholar MA Z X, JIANG Y Z, WEI Y, et al. Revision and characters of the Poyang Formation (quaternary)[J]. Journal of Stratigraphy, 2003, 27(3):212-215. Google Scholar
[23]	李燕,金振奎,高白水,等.汊口滩沉积特征及沉积模式--以鄱阳湖赣江三角洲汊口滩为例[J].吉林大学学报(地球科学版), 2021, 51(6):1678-1688. Google Scholar LI Y, JIN Z K, GAO B S, et al. Sedimentary characteristics and model of branch mouth bar:A case study of branch mouth bar in Ganjiang Delta of Poyang Lake[J]. Journal of Jilin University (Earth Science Edition), 2021, 51(6):1678-1688. Google Scholar
[24]	向诗月,程和琴,滕立志.鄱阳湖流域侵蚀基准面近期变化及其影响[J].泥沙研究, 2021, 46(5):48-54. Google Scholar XIANG S Y, CHENG H Q, TENG L Z. Recent processes of the base level by scour and their impacts on the Poyang Lake Basin[J]. Journal of Sediment Research, 2021, 46(5):48-54. Google Scholar
[25]	欧阳千林.鄱阳湖近10年来冲淤变化特征及成因分析[J].江西水利科技, 2021, 47(5):335-340. Google Scholar OUYANG Q L. Characteristics and causes of scouring and deposit in Poyang Lake[J]. Jiangxi Hydraulic science and Technology, 2021, 47(5):335-340. Google Scholar
[26]	胡振鹏,王仕刚.鄱阳湖冲淤演变及水文生态效应[J].水利水电技术, 2022, 53(6):66-78. Google Scholar HU Z P, WANG S G. Evolution of scour and sedimentation and its hydrological and ecological effects in Poyang Lake[J]. Water Resources and Hydropower Engineering, 2022, 53(6):66-78. Google Scholar
[27]	马逸麟,熊彩云,易文萍.鄱阳湖泥沙淤积特征及发展趋势[J].资源调查与环境, 2003, 24(1):29-37. Google Scholar MA Y L, XIONG C Y, YI W P. Sedimentary characteristics and developing trend of sediments in Poyang Lake, Jiangxi Province[J]. Resources Survey and Environment, 2003, 24(1):29-37. Google Scholar
[28]	刘娟,李晓云,李权,等.卫星直击长江流域旱情[EB/OL].(2022-08-24)[2023-05-08] .http://www.xinhuanet.com/multimediapro/20220824/06c6ea1e0c514851aeb052b9e9bd890e/c.html. Google Scholar LIU J, LI X Y, LI Q, et al. Drought situations in the Yangtze River Basin observed by satellite imagery[EB/OL].(2022-08-24)[2023-05-08] .http://www.xinhuanet.com/multimediapro/20220824/06c6ea1e0c514851aeb052b9e9bd890e/c.html. Google Scholar
[29]	李云良,许秀丽,赵贵章,等.鄱阳湖典型洲滩湿地土壤质地与水分特征参数研究[J].长江流域资源与环境, 2016, 25(8):1200-1208. Google Scholar LI Y L, XU X L, ZHAO G Z, et al. Research of soil textures and soil-water characteristic parameters in a typical wetland of Poyang Lake[J]. Resources and Environment in the Yangtze Basin, 2016, 25(8):1200-1208. Google Scholar
[30]	DE LEEUW J, SHANKMAN D, WU G F, et al. Strategic assessment of the magnitude and impacts of sand mining in Poyang Lake, China[J]. Regional Environmental Change, 2010, 10(2):95-102. Google Scholar
[31]	中华人民共和国水利部. SL42-2010河流泥沙颗粒分析规程[S].北京:中国水利水电出版社, 2010:10-65. Google Scholar Ministry of Water Resources of the People's Republic of China. SL42-2010 Technical standard for determination of sediment particle size in open channels[S]. Beijing:China Water and Power Press, 2010:10-65. Google Scholar
[32]	YUAN S Y, TANG H W, LI K, et al. Hydrodynamics, sediment transport and morphological features at the confluence between the Yangtze River and the Poyang Lake[J]. Water Resources Research, 2021, 57(3):e2020WR028284. Google Scholar
[33]	马水山,徐勤勤.长江采砂管理中的若干关键技术问题[J].中国水利, 2013(10):15-18. Google Scholar MA S S, XU Q Q. Key technical issues in sand excavation management in Yangtze River Basin[J]. China Water Resources, 2013(10):15-18. Google Scholar
[34]	江丰,齐述华,廖富强,等. 2001-2010年鄱阳湖采砂规模及其水文泥沙效应[J].地理学报, 2015, 70(5):837-845. Google Scholar JIANG F, QI S H, LIAO F Q, et al. Hydrological and sediment effects from sand mining in Poyang Lake during 2001-2010[J]. Acta Geographica Sinica, 2015, 70(5):837-845. Google Scholar
[35]	YAO J, ZHANG D, LI Y L, et al. Quantifying the hydrodynamic impacts of cumulative sand mining on a large river-connected floodplain lake:Poyang Lake[J]. Journal of Hydrology, 2019, 579:124156. Google Scholar
[36]	DENG M M, LI Q Y, LI W Y, et al. Impacts of sand mining activities on the wetland ecosystem of Poyang Lake (China)[J]. Land, 2022, 11(8):1364. Google Scholar
[37]	姜月华,陈立德,向芳,等.长江演化及其对洪涝灾害防治的启示[J].中国地质, 2022:1-34. Google Scholar JIANG Y H, CHEN L D, XIANG F, et al. Evolution of the Yangtze River and its implications for prevention and control to flood disaster[J]. Geology in China, 2022:1-34. Google Scholar