|
|
MicrOBEM: a micro-ocean-bottom electromagnetic receiver |
LUO Xian-Hu1( ), DENG Ming2, QIU Ning3,4, SUN Zhen3,4, WANG Meng2, JING Jian-En2, CHEN Kai2( ) |
1. Institute of Marine Technology Methods, Guangzhou Marine Geological Survey, Guangzhou 510076, China 2. School of Geophysics and Information Technology, China University of Geosciences(Beijing), Beijing 100083, China 3. Key Laboratory of Marginal Sea Geology of CAS, South China Sea Institute of Oceanology, Guangzhou 511458,China 4. Southern Ocean Science and Engineering Guangdong Laboratory (Guangzhou), Nanhai Ocean Institute,Guangzhou 511458,China |
|
|
Abstract Ocean bottom electromagnetic receivers (OBEMs) are mainly used for high-precision observation and measurement of magnetotelluric signals and controlled-source electromagnetic signals at the sea bottom. To overcome the shortcomings of large volume, high power consumption, and high cost of the existing OBEMs (OBEM-Ⅲ type), this study conducted technical research regarding miniaturization, low power consumption, and low cost. As a result, the overall power consumption of the existing OBEMs (OBEM-Ⅲ type) has been reduced from 1 600 mW to 500 mW or less (by equipment of inductive magnetic sensors) due to the development of a low-power control unit and preamplifier, the installation of low-power fluxgate sensors, and adoption of advanced power management technology. Traditional acoustic releasers are expensive and bulky and require more suitable buoyant materials. By integrating the underwater acoustic communication module and being equipped with the external erosion wearing release device, the MicrOBEMs make release and recovery possible using only a 17-inch glass sphere, thus greatly reducing the volume and hardware cost of the instrument and improving the integration and operation efficiency of devices. Compared to the OBEM-Ⅲ type, the volume, power consumption, and cost of the newly developed MicrOBEMs are reduced by 3/4, 2/3, and 1/2, respectively. A deep-water geomagnetic test was conducted in March 2021 in the southern South China Sea, preliminarily verifying the geomagnetic measurement function of the MicrOBEMs and reflecting that the MicrOBEMs have the advantages of small size, low power consumption, and low cost.
|
Received: 27 August 2021
Published: 21 June 2022
|
|
Corresponding Authors:
CHEN Kai
E-mail: luoxianhu@163.com;ck@cugb.edu.cn
|
|
|
|
|
Photo of MicrOBEM
|
|
Structure diagram of data acquisition module
|
|
Diagram of data acquisition module
|
|
Diagram of data acquisition circuit (the reserved channel is not given)
|
|
Diagram of acoustic release deck unit
|
|
Screenshot of the APP menu of acoustic release deck unit
|
|
Work area layout
|
序号 | 站位名 | 水深/m | 仪器编号 | 备注 | 1 | S1 | 1932 | HA | | 2 | S2 | 1975 | HC | | 3 | S3 | 1826 | HA | | 4 | S4 | 1693 | HA | | 5 | S5 | 1400 | HC | 数据无效 | 6 | S5A | 1400 | HA | 补做 |
|
Point coordinates of seafloor MT station
|
|
Fragment of the measured time series (station S3, water depth 1 826 m)
|
|
MT sounding raw data curves of five stations
|
[1] |
Constable S C. Marine electromagnetic induction studies[J]. Surveys in Geophysics, 1990, 11(2/3): 303-327.
|
[2] |
Naif S, Key K, Constable S, et al. Melt-rich channel observed at the lithosphere-asthenosphere boundary[J]. Nature, 2013, 495: 356-359.
|
[3] |
Ichiki M, Baba K, Toh H, et al. An overview of electrical conductivity structures of the crust and upper mantle beneath the northwestern Pacific, the Japanese Islands, and continental East Asia[J]. Gondwana Research, 2009, 16(3/4): 545-562.
|
[4] |
Johansen S E, Panzner M, Mittet R, et al. Deep electrical imaging of the ultraslow-spreading Mohns Ridge[J]. Nature, 2019, 567: 379-383.
|
[5] |
Worzewski T, Jegen M, Kopp H, et al. Magnetotelluric image of the fluid cycle in the Costa Rican subduction zone[J]. Nature Geoscience, 2011, 4(2): 108-111.
|
[6] |
Key K, Constable S, Liu L, et al. Electrical image of passive mantle upwelling beneath the northern East Pacific Rise[J]. Nature, 2013, 495: 499-502.
|
[7] |
魏文博, 邓明, 温珍河, 等. 南黄海海底大地电磁测深试验研究[J]. 地球物理学报, 2009, 52(3):740-749.
|
[7] |
Wei W B, Deng M, Wen Z H, et al. Experimental study of marine magnetotellurics in southern Huanghai[J]. Chinese Journal of Geophysics, 2009, 52(3), 740-749.
|
[8] |
Key K W, Constable S C, Weiss C J. Mapping 3D salt using the 2D marine magnetotelluric method: Case study from Gemini Prospect, Gulf of Mexico[J]. Geophysics, 2006, 71(1): B17-B27.
|
[9] |
Constable S C. Review paper: Instrumentation for marine magnetotelluric and controlled source electromagnetic sounding[J]. Geophysical Prospecting, 2013, 61: 505-532.
|
[10] |
Quasar Federal System, QMax EM3[EB/OL].(2010-06)[2020-09]. http://quasarfs.com/downloads/QuasarGeo-QMax-EM3-Datasheet.pdf
|
[11] |
Ogawa K, Matsuno T, Ichihara H, et al. A new miniaturized magnetometer system for long-term distributed observation on the seafloor[J]. Earth Planets & Space, 2018, 70(1)111-119.
|
[12] |
Chen K, Deng M, Luo X, et al. A micro ocean-bottom E-field receiver[J]. Geophysics, 2017, 82(5): E233-E241.
|
[13] |
陈凯, 景建恩, 赵庆献, 等. 海底可控源电磁接收机及其水合物勘查应用[J]. 地球物理学报, 2017, 60(11):4262-4272.
|
[13] |
Chen K, Jing J E, Zhao Q X, et al. Ocean bottom EM receiver and application for gas-hydrate detection[J]. Chinese Journal of Geophysics, 2017, 60(11):4262-4272.
|
[1] |
ZHAO Bao-Feng, WANG Qi-Nian, GUO Xin, GUAN Da-Wei, CHEN Tong-Gang, FANG Wen. Gravity survey and audio magnetotellurics-based insights into the deep structures and geothermal resource potential of the Rucheng Basin[J]. Geophysical and Geochemical Exploration, 2023, 47(5): 1147-1156. |
[2] |
HE Sheng, WANG Wan-Ping, DONG Gao-Feng, NAN Xiu-Jia, WEI Feng-Feng, BAI Yong-Yong. Application of the opposing-coils transient electromagnetic method in urban geological surveys[J]. Geophysical and Geochemical Exploration, 2023, 47(5): 1379-1386. |
|
|
|
|