热带海洋学报

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DGS AT1M-11型海洋重力仪在东北印度洋的应用与研究

王星月, 毛华斌*, 戚永锋, 邢焕林, 余凌晖, 李先鹏   

  1. 热带海洋环境与岛礁生态全国重点实验室, 中国科学院南海海洋研究所, 广东 广州 510301

  • 收稿日期:2025-04-18 修回日期:2025-06-10 接受日期:2025-06-11
  • 通讯作者: 毛华斌
  • 基金资助:
    国家自然科学基金面上项目(42276193); 国家自然科学基金委员会共享航次计划项目(42149910)

Application and study of the DGS AT1M-11 marine gravimeter in the northeast Indian Ocean*

WANG Xingyue, MAO Huabin, QI Yongfeng, XING Huanlin, YU Linghui, LI Xianpeng   

  1. State Key Laboratory of Tropical Oceanography and Island Reef Ecology, South China Sea Institute of Oceanology, Chinese Academy of Science, Guangzhou 510301, China

  • Received:2025-04-18 Revised:2025-06-10 Accepted:2025-06-11
  • Supported by:

    National Natural Science Foundation of China (42276193); National Natural Science Foundation of China Shiptime Sharing Project (42149910)

摘要: 在海洋区域,重力场的研究对理解海洋动力过程、海底地质构造及全球气候变化具有重要意义。高精度海洋重力勘探技术成为目前海洋重力场调查的发展趋势。中国科学院南海海洋研究所“实验6”科考船配备了DGS AT1M-11型海洋重力仪,该重力仪具有高精度、高可靠性、能够进行全局动态测量的特点。在该重力仪开始使用之前,对其进行了精度评估,包括静态测试、内符合精度测试,结果均符合海洋调查测量规范的要求。利用2022年在东北印度洋采集的实测数据与重力恢复与气候试验(Gravity Recovery and Climate Experiment, GRACE)重力场数据相对比,其结果呈现出基本一致的趋势,且该航次航前航后基准测试与重力交点差结果分别为-0.73mGal与1.15mGal,表明该仪器数据具有较高准确性,可用于高精度海洋重力测量。10°S以北东经九十度海岭重力场与水深不成比例,说明地壳厚度的均衡补偿存在差异,海岭由非均质性的物质组成。通过对实测数据所获得的自由空间重力异常进行反演,结果表明在东经九十度海岭之下存在与地形起伏载荷补偿相关的增厚地壳。

关键词: DGS AT1M-11型海洋重力仪, 东经九十度海岭, 东北印度洋, 重力模拟, “实验6”科考船

Abstract: In marine areas, the study of gravity field is of great significance for understanding marine dynamic processes, submarine geological structure and global climate change. High-precision marine gravity exploration technology has become the current development trend of marine gravity field investigation. The R/V Shiyan 6 of the South China Sea Institute of Oceanography, Chinese Academy of Sciences, is equipped with a DGS AT1M-11 marine gravimeter, which is characterized by high precision, high reliability, and the ability to conduct global dynamic measurements. Before the gravimeter was put into use, the accuracy was evaluated, including static tests and internal conformity accuracy tests, all of which resulted in compliance with the Marine Survey Measurement Specification. Using the measured data collected in the Northeast Indian Ocean in 2022 to compare with the gravity field data from the Gravity Recovery and Climate Experiment (GRACE), the results show a basically consistent trend, and the results of the pre- and post-cruise benchmark tests of the voyage and the gravity intersection point difference are -0.73mGal and 1.15mGal respectively, indicating that the data of this instrument has high accuracy and can be used for high-precision marine gravity measurements. The gravitational field of the 90°E ridge north of 10°S is not proportional to the water depth, indicating that there are differences in equilibrium compensation for crustal thickness and that the ridge consists of non-homogeneous material. Gravity modeling of the free-space gravity anomalies obtained from the measured data suggests that there is a thickened crust beneath the 90°E Ridge associated with compensation for topographic relief loads.

Key words: DGS AT1M-11 marine gravimeter, 90°E ridge, Northeast Indian Ocean, Gravity modeling, R/V Shiyan 6