基于剖面声呐的海底微地貌观测研究<sup>&#x0002A;</sup>

doi:10.7605/gdlxb.2022.01.014

古地理学报 ›› 2022, Vol. 24 ›› Issue (1): 180-190. doi: 10.7605/gdlxb.2022.01.014

• 海洋古地理专辑 • 上一篇

基于剖面声呐的海底微地貌观测研究^*

田壮才^1,2,4, 彭子奇³, 贾永刚^2,4, 张明伟¹

1 中国矿业大学深部岩土力学与地下工程国家重点实验室, 江苏徐州 221116;
2 中国海洋大学山东省海洋环境地质工程重点实验室, 山东青岛 266100;
3 广东省海洋发展规划研究中心, 广东广州 510220;
4 青岛海洋科学与技术国家实验室海洋地质过程与环境功能实验室,山东青岛 266061

收稿日期:2021-07-20 修回日期:2021-08-03 出版日期:2022-01-01 发布日期:2022-01-24
通讯作者: 贾永刚,男,1965年生,毕业于中国海洋大学,获博士学位,现为中国海洋大学教授,主要从事海洋工程地质与原位观测研究。E-mail: yonggang@ouc.edu.cn。
作者简介:田壮才,男,1991年生,毕业于中国海洋大学,获博士学位,现为中国矿业大学深部岩土力学与地下工程国家重点实验室助理研究员,主要从事海洋工程地质与海洋岩土工程研究。E-mail: zhuangcaitian@163.com。
基金资助:
*国家自然科学基金青年项目(编号: 42107158)和重点项目(编号: 41831280)、江苏省自然科学基金青年项目(编号: BK20210527)和中央高校基本科研业务费项目(编号: 2021QN1096)联合资助

In-situ observation of seabed micro-landform based on profiling sonar

Tian Zhuang-Cai^1,2,4, Peng Zi-Qi³, Jia Yong-Gang^2,4, Zhang Ming-Wei¹

1 State Key Laboratory for Geomechanics and Deep Underground Engineering,China University of Mining and Technology, Jiangsu Xuzhou 221116,China;
2 Shandong Provincial Key Laboratory of Marine Environment and Geological Engineering,Ocean University of China, Shandong Qingdao 266100,China;
3 Guangdong Center for Marine Research and Development,Guangzhou 510220,China;
4 Laboratory for Marine Geology,Qingdao National Laboratory for Marine Science and Technology,Shandong Qingdao 266061,China

Received:2021-07-20 Revised:2021-08-03 Online:2022-01-01 Published:2022-01-24
Contact: Jia Yong-Gang,born in 1965,is a professor of Ocean University of China,with a Ph.D. degree obtained from Ocean University of China. He is mainly engaged in researches on ocean engineering geology and in-situ observation. E-mail: yonggang@ouc.edu.cn.
About author:Tian Zhuang-Cai,born in 1991,is a research assistant of State Key Laboratory for Geomechanics and Deep Underground Engineering of China University of Mining and Tech nology,with a Ph.D. degree obtained from Ocean University of China. He is mainly engaged in researches on ocean engineering geology and marine geotechnical engineering. E-mail: zhuangcaitian@163.com.
Supported by:
Co-funded by the National Natural Science Fund for Distinguished Young Scholars(No.42107158),the Major Program of National Natural Science Foundation of China(No.41831280),the Natural Science Foundation of Jiangsu Province (No. BK20210527)and the Fundamental Research Funds for the Central Universities(No.2021QN1096)

摘要/Abstract

摘要： 海底地貌是海水覆盖下的固体地球表面形态的总称。海底地貌巨变往往与海底地质灾害息息相关,会对海底管线和海上平台等海洋工程设施造成危害,因而对海底地貌进行原位观测具有重要意义。本研究基于前人研究成果和团队常年自主研发仪器经验,研制出了剖面声呐海底微地貌原位观测系统,详细介绍了观测系统的组成、功能、工作原理和工作模式,并提出了观测数据的处理分析方法;然后,使用观测系统进行了标志物检验实验,通过将观测系统测量数据与其他设备测量数据相对比,验证了观测系统的可行性和数据准确性;最后,使用观测系统在舟山海域朱家尖滑坡区进行原位观测,进一步验证了观测系统的可行性。观测结果进一步表明剖面声呐观测系统可以用于海底微地貌的观测研究。

关键词: 海底, 微地貌, 原位观测, 剖面声呐

Abstract: Seabed geomorphology is a general term for the surface morphology of solid earth covered by seawater. Submarine geomorphic changes are often closely related to submarine geological disasters,which will cause damage to submarine pipelines,offshore platforms and other offshore engineering facilities. Therefore,in-situ observation for submarine landform is of great significance. We develop the in-situ observation system of profiling sonar for seabed micro-landform based on previous studies and the team’s years of experiments in independent research and development of instrument. The composition,function,working principle and working mode of the observation system are introduced in detail,and the processing and analysis methods of the observation data are proposed;then,the observation system is used to carry out the marker inspection experiment. By comparing the measurement data of the observation system with the measurement data of other equipment,the feasibility and data accuracy of the observation system are verified. Finally,the observation system is used to observe on the Zhujiajian landslide in Zhoushan sea area, which verified the feasibility of the observation system and showed that the observation system of profile sonar can be used for micro-landform.

Key words: seabed, micro-landform, in-situ observation, profiling sonar

中图分类号:

P737

田壮才, 彭子奇, 贾永刚, 张明伟. 基于剖面声呐的海底微地貌观测研究^*[J]. 古地理学报, 2022, 24(1): 180-190.

Tian Zhuang-Cai, Peng Zi-Qi, Jia Yong-Gang, Zhang Ming-Wei. In-situ observation of seabed micro-landform based on profiling sonar[J]. JOPC, 2022, 24(1): 180-190.

http://www.gdlxb.cn/CN/Y2022/V24/I1/180

参考文献

[1]柏秀芳. 2008. 海床原位监测及其动力特性研究. 中国科学院研究生院(海洋研究所)博士学位论文. [Bai X F. 2008. In-situ monitoring of seabed and dynamic characteristics research. Doctoral dissertation of Institute of Oceanology,Chinese Academy of Sciences]
[2]陈景东,汪亚平,朱庆光,黄蓓,吴自银,高建华. 2014. 潮滩微地貌的声学观测与分析. 南京大学学报(自然科学), 50(5): 611-620.
[Chen J D,Wang Y P,Zhu Q G,Huang B,Wu Z Y,Gao J H.2014. Acoustic observations and analysis of microrelief on tidal flats. Journal of Nanjing University(Natural Sciences), 50(5): 611-620]
[3]李勇航,牟泽霖,刘文涛,温明明,倪玉根,单晨晨,潘冬阳. 2021a. 海南海棠湾海底微地貌多源声学特征、成因及其指示意义. 地球物理学进展, 36(4): 1694-1701.
[Li Y H,Mou Z L,Liu W T,Wen M M,Ni Y G,Shan C C,Pan D Y.2021a. Multi-source acoustic characteristics,genesis and indicative significance of submarine micro-geomorphology in Haitang Bay,Hainan. Progress in Geo physics, 36(4): 1694-1701]
[4]李勇航,牟泽霖,倪玉根,苏明,潘冬阳,蔡鹏捷,陈志坚. 2021b. 海南东方近岸海底活动沙波的地球物理特征及其迁移机制. 海洋地质与第四纪地质, 41(4): 27-35.
[Li Y H,Mou Z L,Ni Y G,Su M,Pan D Y,Cai P J,Chen Z J.2021b. Geophysical characteristics and migration mechanism of active submarine sand waves off the coast of Dongfang,Hainan. Marine Geology & Quaternary Geology, 41(4): 27-35]
[5]李泽文,阎军,栾振东,王小红. 2010. 海南岛西南海底沙波形态和活动性的空间差异分析. 海洋地质动态, 26(7): 24-32.
[Li Z W,Yan J,Luan Z D,Wang X H.2010. Analysis on spatial dif ferences of morphology and mobility of the submarine sand waves in southwest Hainan island. Marine Geology Letters, 26(7): 24-32]
[6]马廷英. 1941. 亚洲第四纪中叶气候变迁与冰川的原因. 地质论评,(Z2): 220-230.
[Ma T Y.1941. Reasons of climate change and glaciers in the Asian Quaternary. Geological Review,(Z2): 220-230]
[7]马小川. 2013. 海南岛西南海域海底沙波沙脊形成演化及其工程意义. 中国科学院研究生院(海洋研究所)博士学位论文. [Ma X C. 2013. Formation,evolution and engineering significance of submarine sand waves and sand ridges,southeast of Hainan Island. Doctoral dissertation of Institute of Oceanology,Chinese Academy of Sciences]
[8]彭子奇,贾永刚,田壮才,程升,单红仙. 2020. 基于剖面声呐的海底沙纹演变规律试验研究. 科学技术与工程, 20(31): 12753-12758.
[Peng Z Q,Jia Y G,Tian Z C,Cheng S,Shan H X.2020. Experimental study on evolution of wave ripples by using profiling sonar. Science Technology and Engineering, 20(31): 12753-12758]
[9]孙永福,王琮,周其坤,刘振纹. 2018. 海底沙波地貌演变及其对管道工程影响研究进展. 海洋科学进展, 36(4): 489-498.
[Sun Y F,Wang C,Zhou Q K,Liu Z W.2018. A review on sand waves evolution and its influence on pipeline engineering. Advances in Marine Science, 36(4): 489-498]
[10]张朝阳. 2013. 朱家尖岛近岸海域潮流和泥沙特性研究. 华东师范大学硕士学位论文. [Zhang C Y. 2013. Study on tidal current and sediment characteristics of Zhujiajian island offshore area. Masteral dissertation of East China Normal University]
[11]赵晓明,刘丽,谭程鹏,范廷恩,胡光义,张迎春,张文彪,宋来明. 2018. 海底水道体系沉积构型样式及控制因素: 以尼日尔三角洲盆地陆坡区为例. 古地理学报, 20(5): 825-840.
[Zhao X M,Liu L,Tan C P,Fan T N,Hu G Y,Zhang Y C,Zhang W B,Song L M.2018. Styles of submarine-channel architecture and its controlling factors: a case study from the Niger Delta Basin slope. Journal of Palaeogeography(Chinese Edition), 20(5): 825-840]
[12]郑勇玲,吴承强,蔡锋,鲍晶晶,许艳. 2012. 中国海底地貌研究进展及其在东海近海的新发现、新认识. 地球科学进展, 27(9): 1026-1034.
[Zheng Y L,Wu C Q,Cai F,Bao J J,Xu Y.2012. The present research trend of China’s submarine geomorphology and new discoveries of the East China Sea offshore. Advances in Earth Science, 27(9): 1026-1034]
[13]Blondeaux P,Vittori G.2016. A model to predict the migration of sand waves in shallow tidal seas. Continental Shelf Research, 112: 31-45.
[14]Favali P,Beranzoli L.2006. Seafloor observatory science: a review. Annals of Geophysics, 49(2-3): 515-567.
[15]Langhorne D.1982. A study of the dynamics of a marine sandwave. Sedimentology, 29(4): 571-594.
[16]Németh A A,Hulscher S J M H,Van Damme R M J.2006. Simulating offshore sand waves. Coastal Engineering, 53(2-3): 265-275.
[17]Rubin D M,Mcculloch D S,Hill H R.1983. Sea-floor-mounted rotating side-scan sonar for making time-lapse sonographs. Continental Shelf Research, 1(3): 295-301.

选择文件类型/文献管理软件名称

选择包含的内容

基于剖面声呐的海底微地貌观测研究^*

In-situ observation of seabed micro-landform based on profiling sonar

RichHTML

PDF

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 12

编辑推荐

Metrics

本文评价

[1]	时志强, 彭深远, 赵子腾. 上奥陶统五峰组海底麻坑沉积的首次识别及其地质意义^*[J]. 古地理学报, 2024, 26(2): 255-268.
[2]	张佳佳, 吴胜和, 王瑞峰, 王敏, 陈梅, 王晓丰, 徐庆岩, 熊绮聪, 余季陶, 王黎. 东非鲁伍马盆地深水X气藏海底扇储层构型研究:重力流—底流交互作用的指示意义^*[J]. 古地理学报, 2023, 25(1): 163-179.
[3]	李亚茹, 李华, 杨朝强, 周伟, 王玉, 刘圣乾, 何幼斌. 南海莺歌海盆地黄流组海底扇储层构型特征^*[J]. 古地理学报, 2022, 24(3): 556-567.
[4]	吴孟亭, 方浩, 孙龙飞, 史晓颖, 汤冬杰. 华北中元古代浅海碳酸盐沉淀方式变化:海水氧化还原条件波动的响应?^*[J]. 古地理学报, 2021, 23(4): 703-722.
[5]	屈红军, 李文厚, 姚天星, 武龙发, 王妍心, 胡佳森, 成倚山. 陕西洛南县蓟县系洛南群层控玉化硅质岩特征、成因及意义^*[J]. 古地理学报, 2021, 23(4): 651-667.
[6]	吴波, 邓克勇, 刘应忠, 徐安全. 贵州龙里地区早石炭世杜内期铝土矿微地貌及其对铝土矿的控制作用^*[J]. 古地理学报, 2020, 22(5): 977-988.
[7]	黄建松, 郭玮, 杨萍, 易纲. 唐王陵砾岩的形成时代及其构造与沉积环境探讨^*[J]. 古地理学报, 2019, 21(4): 557-576.
[8]	赵晓明, 刘丽, 谭程鹏, 范廷恩, 胡光义, 张迎春, 张文彪, 宋来明. 海底水道体系沉积构型样式及控制因素:以尼日尔三角洲盆地陆坡区为例^*[J]. 古地理学报, 2018, 20(5): 825-840.
[9]	于兴河, 梁金强, 方竞男, 丛晓荣, 姜龙燕, 王建忠. 珠江口盆地深水区晚中新世以来构造沉降与似海底反射（BSR）分布的关系^*[J]. 古地理学报, 2012, 14(6): 787-800.
[10]	田洪水, 张邦花, 祝介旺, 张增奇, 李洪奎. 早寒武世初期沂沭断裂带地震效应^*[J]. 古地理学报, 2011, 13(6): 645-656.
[11]	汤冬杰, 史晓颖, 裴云鹏, 蒋干清, 赵贵生. 华北中元古代陆表海氧化还原条件^*[J]. 古地理学报, 2011, 13(5): 563-580.
[12]	牛新生　王成善. 异地碳酸盐岩块体与碳酸盐岩重力流沉积研究及展望[J]. 古地理学报, 2010, 12(1): 17-30.

模态框（Modal）标题

选择文件类型/文献管理软件名称

选择包含的内容

基于剖面声呐的海底微地貌观测研究*

In-situ observation of seabed micro-landform based on profiling sonar

RichHTML

PDF

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 12

编辑推荐

Metrics

本文评价

基于剖面声呐的海底微地貌观测研究^*