科学大洋钻探中的新技术

doi:10.11867/j.issn.1001-8166.2003.05.0789

地球科学进展 ›› 2003, Vol. 18 ›› Issue (5): 789 -794. doi: 10.11867/j.issn.1001-8166.2003.05.0789

科学大洋钻探中的新技术

孙连浦,周祖翼

同济大学海洋地质教育部重点实验室，上海 200092

收稿日期:2003-05-23 修回日期:2003-07-27 出版日期:2003-12-20
通讯作者: 孙连浦 E-mail:sunlianpu@hotmail.com
基金资助:
国家重点基础研究发展规划项目“暖池形成和演变的构造控制及其沉积证据”（编号：G2000078501）资助.

APPLICATIONS OF NEW TECHNOLOGIES IN THE SCIENTIFIC OCEAN DRILLING

Sun Lianpu, Zhou Zuyi

Laboratory of Marine Geology, Tongji University , Shanghai 200092 , China

Received:2003-05-23 Revised:2003-07-27 Online:2003-12-20 Published:2003-10-01

大洋钻探诸多科学目标的实现与包括钻探、取芯、测试和海底观测技术在内的各种新技术的开发和革新密不可分。即将开展的IODP计划，将对各种技术提出新的要求。在钻探技术上，将联合使用多平台，以实现区域更广深度更大的钻探作业；在取芯技术上，取样范围更广，从各种岩石取样到地下流体的取样，并要求样品保持原始状态，同时确保获得更高的岩芯采收率；在测试上，要求采用随钻测试技术，以适时地获得地下真实信息；在观测技术上，要求开发各种工具，去除由于钻探造成的扰动，使得各种观测仪器能够进行长期的跟踪观测。

关键词: IODP, 科学大洋钻探, 新技术, ODP

Achievements of the scientific ocean drilling are closely related to the developments and renovations of new technologies in drilling ,coring ,measurement and observation. Scientific objectives of IODP require new technologies. The use of multiple drilling platforms will permit operations in wider and deeper water areas. By use of new coring technologies, scientists can obtain a wide range of samples from rocks to fluids, while at the same time maintaining the in situ situation and enhancing core recovery. LWD will be used to acquire real information in subseafloor. Many new measuring tools are being developed to satisfy the demands of downhole measurements. Tools for long-term observation are to be developed that are able to obviate drilling perturbations.

Key words: ODP, IODP., Scientific ocean drilling, New technology

中图分类号:

[1] STA/JAMSTEC. Ocean Drilling in the 21st Century[R]. Tokyo: STA/JAMSTEC,1994.

[2] JOI. Understanding Our Dynamic Earth Through Ocean Drilling:ODP Long Range Plan [R]. Washington DC:JOI,1996.

[3] IWG. Earth,Oceans and Life:Scientific Investigation of the Earth System Using Multiple Drilling Platform and New Technology:IODP Initial Science Plan[R]. Washington DC: International Work Group Support Office,2001.

[4] Jin Xingchun,Zhou Zuyi,Wang Pinxian. Ocean Drilling & Chinese Earth Sciences[M]. Shanghai:Tongji University Press,1995. [ 金性春,周祖翼,汪品先. 大洋钻探与中国地球科学[M].上海:同济大学出版社,1995.]

[5] Shipboard Scientific Party. Controls on Microbial Communities in Deeply Buried Sediments,Eastern Equatorial Pacific and Peru Margin:ODP Leg 201 Preliminary Report[R]. Texas:Texas A & M University,2002.

[6] Tamaki K, Tanaka T. Status Report of the Japanese OD-21 Program [A]. In:Planning for a New Era of Scientific Ocean Drilling:Report of ODP Technical & Operations Workshop[C].Texas:IWG,1998.

[7] Takagawa S. Plans and Specifications for the Riser Drillship[A]. In:Planning for a New Era of Scientific Ocean Drilling: Report of ODP Technical Operations Workshop[C]. Texas:IWG,1998.

[8] CDC. The Non-Riser Drilling Vessel for the Integrated Ocean Drilling Program:A Report to the US National Science Foundation[R]. Washington DC:USSAC,2000.

[9] Mike S. Overview of Coring Tools and Sampling Technology [A]. iPPSP Meeting#2-Minutes[C]. Texas: ChevronTexaco, 2002.

[10] Shipboard Scientific Party. Drilling Gas Hydrates on Hydrate Ridge,Cascadia Continental Margin:ODP Leg 204 Preliminary Report[R]. Texas:Texas A & M University,2002.

[11] Shipboard Scientific Party. Anatomy of an Active Felsic-Hosted HydrothermalSystem, Eastern Manus Basin:ODP Leg 193 Preliminary Report[R]. Texas:Texas A & M University,2001.

[12] Mottl M, Gieskes J. Chemistry of waters sampled from oceanic boreholes, 1979 and 1988[J]. Geophysical Research, 1990,95:9 327-9 342.

[13] Davis E E, Becker K. Borehole observatories record driving forces for hydrothermal circulation in young oceanic crust[J]. EOS, 1998.79:369.

[14] Shipboard Scientific Party. Leg 186 Summary[A]. In: Sacks I S, Suyehiro K, Acton G D, et al. Proceedings of ODP Initial Reports186[C]. Texas :Texas A & M University,2000.

[1]	汪品先. 未雨绸缪——迎接大洋钻探学术新计划的制定[J]. 地球科学进展, 2017, 32(12): 1229-1235.
[2]	赵玉龙, 刘志飞. 等积体在全球大洋中的空间分布及其古环境意义——国际大洋钻探计划对全球等深流沉积研究的贡献[J]. 地球科学进展, 2017, 32(12): 1287-1296.
[3]	张虎才. 参加国际大洋发现计划IODP 361的启示[J]. 地球科学进展, 2016, 31(4): 422-427.
[4]	李永祥，鄢全树，赵西西，全体船上科学家. 剥蚀型汇聚板块边缘大地震成因机理研究：来自国际综合大洋钻探344航次的报告[J]. 地球科学进展, 2013, 28(6): 728-736.
[5]	胡正莹，王汝建，李文宝. 南塔斯曼海隆2 Ma以来碳酸钙沉积记录及其对环流系统和轨道周期的响应[J]. 地球科学进展, 2013, 28(2): 269-281.
[6]	张介霞, 詹力扬, 陈立奇. 南大洋N ₂O研究进展及测量新技术展望 ^*[J]. 地球科学进展, 2013, 28(11): 1201-1208.
[7]	汪鹏，钟广法. 南海ODP1144站深海沉积牵引体的岩石物理模型研究[J]. 地球科学进展, 2012, 27(3): 359-366.
[8]	杨守业，王权. 冲绳海槽中部热液活动与IODP 331航次初步成果[J]. 地球科学进展, 2011, 26(12): 1282-1289.
[9]	朱俊江. 哥斯达黎加地震起源计划——IODP 334航次介绍[J]. 地球科学进展, 2011, 26(12): 1300-1305.
[10]	吴婷婷,李三忠,庞洁红,王健,戴黎明，IODP Expedition 324 Scientific Party. IODP 324航次FMS成像测井资料处理及其在Shatsky海隆构造研究中的应用[J]. 地球科学进展, 2010, 25(7): 753-765.
[11]	李春峰,苏新,姜涛,Ujiie K, Fabbri O, Yamaguchi A,Chester F M,Kimura G. 日本南海海槽俯冲增生楔前缘的构造变形特征[J]. 地球科学进展, 2010, 25(2): 203-211.
[12]	陈木宏. 国际综合大洋钻探计划IODP323白令海航次介绍[J]. 地球科学进展, 2009, 24(12): 1352-1356.
[13]	田军. 新生代的气候节律：赤道太平洋IODP-320、321航次[J]. 地球科学进展, 2009, 24(12): 1357-1361.
[14]	刘志飞，拓守廷. IODP计划的新进展[J]. 地球科学进展, 2009, 24(12): 1318-1324.
[15]	郑洪波,汪品先,刘志飞,杨守业,王家林,李前裕,周祖翼,贾军涛,李上卿,贾健宜,JohnChappell,YoshikiSaito,TakahiroInoue. 东亚东倾地形格局的形成与季风系统演化历史寻踪——综合大洋钻探计划683号航次建议书简介[J]. 地球科学进展, 2008, 23(11): 1150-1160.

阅读次数

全文

摘要