A new equipment for deep-sea geothermal gradient measurement (FY2)

LI Jiawei; CHEN Jie; XU Xing; PAN Feiru; LUO Xianhu; YU Xinqin; LUO Xinheng

doi:10.16562/j.cnki.0256-1492.2020092702

2021 Vol. 41, No. 3

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Article navigation > Marine Geology & Quaternary Geology > 2021 > 41(3): 203-211

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LI Jiawei, CHEN Jie, XU Xing, PAN Feiru, LUO Xianhu, YU Xinqin, LUO Xinheng. A new equipment for deep-sea geothermal gradient measurement (FY2)[J]. Marine Geology & Quaternary Geology, 2021, 41(3): 203-211. doi: 10.16562/j.cnki.0256-1492.2020092702

Citation:

LI Jiawei, CHEN Jie, XU Xing, PAN Feiru, LUO Xianhu, YU Xinqin, LUO Xinheng. A new equipment for deep-sea geothermal gradient measurement (FY2)[J]. Marine Geology & Quaternary Geology, 2021, 41(3): 203-211. doi: 10.16562/j.cnki.0256-1492.2020092702

A new equipment for deep-sea geothermal gradient measurement (FY2)

1.
Guangzhou Marine Geological Survey, Guangzhou 51076, China
2.
Zhuhai Taide Enterprise Co.Ltd., Zhuhai 519082, China

More Information

Corresponding author: XU Xing, gz_xuxing@163.com

Received Date: 27 September 2020

Revised Date: 31 March 2021

Publish Date: 28 June 2021

Abstract

Abstract

The seabed geothermal research has become a common component of integrated marine geological survey nowadays and high requirements are raised to the technical performance of instruments for seabed measurement. Based on the FY1, the self-contained miniature temperature measurement recorder independently developed by Guangzhou Marine Geological Survey, a new type of self-contained miniature temperature measurement recorder, FY2 in abbreviation, was developed after summarization of previous practicce data and survey experiences. In order to verify the performance of the FY2, efforts have been devoted to the instrument calibration and the comparison of the FY2 to the FY1 in laboratories under a constant temperature flume as well as in the deep water area on the northern slope of the South China Sea. Results show that the resolution of the FY2 is higher than 0.0001 ℃, and the precision is higher than ±0.0015 ℃. The seabed geothermal flow value of the measuring point is 78 mW/m²; indicating an excellent performance of the new equipment. The new equipment also has high efficiency, and may provide strong technical support for the research of seabed geothermal flow.
- geothermal gradient /
- deep sea sediments /
- seabed geothermal flow /
- temperature data logger

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References

[1]	汪集暘. 地热学及其应用[M]. 北京: 科学出版社, 2015. Google Scholar WANG Jiyang. Geothermics and its Applications[M]. Beijing: Science Press, 2015. Google Scholar
[2]	O卡普迈耶 O, 海涅尔 R. 地热学及其应用[M]. 北京: 科学出版社, 1981. Google Scholar Kappelmeyer O, Haenel R. Geotherks with Special Reference to Application[M]. Beijing: Science Press, 1981. Google Scholar
[3]	徐行, 罗贤虎, 肖波. 海洋地热流测量技术及其方法研究[J]. 海洋技术, 2005, 24(1):77-81 doi: 10.3969/j.issn.1003-2029.2005.01.019 CrossRef Google Scholar XU Xing, LUO Xianhu, XIAO Bo. Research on the methods & technique of marine heat flow measurement [J]. Ocean Technology, 2005, 24(1): 77-81. doi: 10.3969/j.issn.1003-2029.2005.01.019 CrossRef Google Scholar
[4]	徐行, 陆敬安, 罗贤虎, 等. 南海北部海底热流测量及分析[J]. 地球物理学进展, 2005, 20(2):562-565 doi: 10.3969/j.issn.1004-2903.2005.02.057 CrossRef Google Scholar XU Xing, LU Jing’an, LUO Xianhu, et al. The marine heat flow survey and the result discussion in the northern part of South China Sea [J]. Progress in Geophysics, 2005, 20(2): 562-565. doi: 10.3969/j.issn.1004-2903.2005.02.057 CrossRef Google Scholar
[5]	罗贤虎, 徐行, 张志刚, 等. XXG-T型海底地温梯度探测系统的研发及技术特点[J]. 南海地质研究, 2007(1):102-110 Google Scholar LUO Xianhu, XU Xing, ZHANG Zhigang, et al. Development and technical character of XXG-T marine geothermal gradient measurement system [J]. Gresearch of Eological South China Sea, 2007(1): 102-110. Google Scholar
[6]	Bullard E C. The flow of heat through the floor of the Atlantic ocean [J]. Proceedings of the Royal Society of A: Mathematical, Physical and Engineering Sciences, 1954, 222(1150): 408-429. Google Scholar
[7]	Von Herzen R, Maxwell A E. The measurement of thermal conductivity of deep-sea sediments by a needle-probe method [J]. Journal of Geophysical Research, 1959, 64(10): 1557-1563. doi: 10.1029/JZ064i010p01557 CrossRef Google Scholar
[8]	Sclater J G, Corry C E, Vacquier V. In situ measurement of the thermal conductivity of ocean‐floor sediments [J]. Journal of Geophysical Research, 1969, 74(4): 1070-1081. doi: 10.1029/JB074i004p01070 CrossRef Google Scholar
[9]	Hyndman R D, Erickson A J, Von Herzen R P. Geothermal measurement on DSDP Leg 26[M]//Davies T A, Luyendyk B P. Initial Reports of the Deep Sea Drilling Project 26. Washington: US Government Printing Office, 1974: 675-742. Google Scholar
[10]	Lister C R B. The pulse-probe method of conductivity measurement [J]. Geophysical Journal of the Royal Astronomical Society, 1979, 57(2): 451-461. doi: 10.1111/j.1365-246X.1979.tb04788.x CrossRef Google Scholar
[11]	Pfender M, Villinger H. Miniaturized data loggers for deep sea sediment temperature gradient measurements [J]. Marine Geology, 2002, 186(3-4): 557-570. doi: 10.1016/S0025-3227(02)00213-X CrossRef Google Scholar
[12]	Chang H I, Shyu C T. Compact high-resolution temperature loggers for measuring the thermal gradients of marine sediments [J]. Marine Geophysical Research, 2011, 32(4): 465-479. doi: 10.1007/s11001-011-9136-y CrossRef Google Scholar
[13]	钱翼鹏. 南海北部地热流测量及其成果[J]. 海洋地质与第四纪地质, 1982, 2(4):104-109 Google Scholar QIAN Yipeng. Terrestrial heat flow measurements and the results in the north of South China Sea [J]. Marine Geological Research, 1982, 2(4): 104-109. Google Scholar
[14]	姚伯初. 中美合作调研南海地质专报[M]. 武汉: 中国地质大学出版社, 1994. Google Scholar YAO Bochu. The Geological Memoir of South China Sea Surveyed Jointly by China & USA[M]. Wuhan: China University of Geosciences Press, 1994. Google Scholar
[15]	Nissen S S, Hayes D E, Yao B C, et al. Gravity heat flow, and seismic constraints on the processes of crustal extension: Northern margin of the South China Sea [J]. Journal of Geophysical Research, 1995, 100(B11): 22447-22483. doi: 10.1029/95JB01868 CrossRef Google Scholar
[16]	Qian Y P, Niu X P, Yao B C, et al. Geothermal Pattern Beneath the continental margin in the northern part of the South China Sea[C]//CCOP/TB, 1995, 25: 89-104. Google Scholar
[17]	徐行, 罗贤虎, 许鹤华, 等. 南海地热流探测、研究与展望[J]. 南海地质研究, 2015:1-18 Google Scholar XU Xing, LUO Xianhu, XU Hehua, et al. The measurement, review and prospect on geothermal studies of the South China Sea [J]. Geological Research of South China Sea, 2015: 1-18. Google Scholar
[18]	徐行, 罗贤虎, 彭登, 等. 系列化的海洋地热流探测技术获得突破[J]. 中国地质, 2017, 44(3):621-622 Google Scholar XU Xing, LUO Xianhu, PENG Deng, et al. Marine geothermal flow detection technology gains breakthrough [J]. Geology in China, 2017, 44(3): 621-622. Google Scholar
[19]	彭登, 徐行, 罗贤虎. 海底沉积物地温梯度测量系统设计[J]. 电子设计工程, 2014, 22(6):1-3 doi: 10.3969/j.issn.1674-6236.2014.06.001 CrossRef Google Scholar PENG Deng, XU Xing, LUO Xianhu. Design of marine sediment geothermal gradient measurement system [J]. Electronic Design Engineering, 2014, 22(6): 1-3. doi: 10.3969/j.issn.1674-6236.2014.06.001 CrossRef Google Scholar
[20]	张东风, 片秀红. 热工测量及仪表[M]. 3版. 北京: 中国电力出版社, 2015. Google Scholar ZHANG Dongfeng, PIAN Xiuhong. Thermal Measurement and Instrumentation[M]. 3rd ed. Beijing: China Electric Power Press, 2015. Google Scholar