Development and application of pressure-core-sampling systems for the investigation of gas- and gas-hydrate-bearing sediments

被引:98
作者
Abegg, F. [1 ]
Hohnberg, H. -J. [1 ]
Pape, T. [1 ]
Bohrmann, G. [1 ]
Freitag, J. [2 ]
机构
[1] Univ Bremen, Fachbereich Geowissensch 5, D-28334 Bremen, Germany
[2] Alfred Wegener Inst Polar & Marine Res, D-27568 Bremerhaven, Germany
关键词
Seafloor sampling; Autoclave technology; Pressurised cores; Free gas; Methane; Gas hydrate; Hydrate ridge; Gulf of Mexico; Black Sea;
D O I
10.1016/j.dsr.2008.06.006
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
Free or hydrate-bound gas in the seafloor has been of scientific, ecologic and economic interest for many years because it predominantly contains high concentrations of low-molecular-weight hydrocarbons. A prerequisite of accurate quantifications of gases in sediments is to preserve pressure and temperature close to the in situ conditions during recovery. Here we introduce two new sediment coring devices that allow for the recovery of near-surface gas- and gas-hydrate-bearing sediments and subsequent investigations using several different techniques such as visualisation by computerized tomography, quantitative degassing, and sediment and porewater analyses. The first coring tool, the Multiple Autoclave Corer (MAC), resembles a standard multiple corer in terms of applications, size and core length of about 55 cm. The second tool, the Dynamic Autoclave Piston Corer (DAPC) is similar to a piston corer in application and size and enables one to take cores of up to 2.5 m length. Both focus on the investigation of near-surface sediments, which are most strongly affected by changes in bottom-water temperature and hydrostatic pressure, which in turn influence continental slope stability. Some results from recent offshore applications show the potential of these tools. (C) 2008 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1590 / 1599
页数:10
相关论文
共 33 条
  • [21] Co-existence of gas hydrate, free gas, and brine within the regional gas hydrate stability zone at Hydrate Ridge (Oregon margin):: evidence from prolonged degassing of a pressurized core
    Milkov, AV
    Dickens, GR
    Claypool, GE
    Lee, YJ
    Borowski, WS
    Torres, ME
    Xu, WY
    Tomaru, H
    Tréhu, AM
    Schultheiss, P
    [J]. EARTH AND PLANETARY SCIENCE LETTERS, 2004, 222 (3-4) : 829 - 843
  • [22] In situ methane concentrations, at Hydrate Ridge, offshore Oregon: New constraints on the global gas hydrate inventory from an active margin
    Milkov, AV
    Claypool, GE
    Lee, YJ
    Xu, WY
    Dickens, GR
    Borowski, WS
    [J]. GEOLOGY, 2003, 31 (10) : 833 - 836
  • [23] ORSI TH, 1992, P CIVIL ENG OCEANS, V5, P968
  • [24] Paull C.K, 2001, NATURAL GAS HYDRATES, V124, P53, DOI DOI 10.1029/GM124P0053
  • [25] An experiment demonstrating that marine slumping is a mechanism to transfer methane from seafloor gas-hydrate deposits into the upper ocean and atmosphere
    Paull, CK
    Brewer, PG
    Ussler, W
    Peltzer, ET
    Rehder, G
    Clague, D
    [J]. GEO-MARINE LETTERS, 2003, 22 (04) : 198 - 203
  • [26] DIE SCHWEDISCHE TIEFSEE-EXPEDITION 1947/48
    PETTERSSON, H
    [J]. NATURWISSENSCHAFTEN, 1951, 38 (06) : 125 - 128
  • [27] Reinelt R., 1997, DTSCH WISS GES ERDGA, V9706, P37
  • [28] Origin of salt-enriched pore fluids in the northern Gulf of Mexico
    Reitz, Anja
    Haeckel, Matthias
    Wallmann, Klaus
    Hensen, Christian
    Heeschen, Katja
    [J]. EARTH AND PLANETARY SCIENCE LETTERS, 2007, 259 (3-4) : 266 - 282
  • [29] Macrofaunal community structure and sulfide flux at gas hydrate deposits from the Cascadia convergent margin, NE Pacific
    Sahling, H
    Rickert, D
    Lee, RW
    Linke, P
    Suess, E
    [J]. MARINE ECOLOGY PROGRESS SERIES, 2002, 231 : 121 - 138
  • [30] Schroeder D, 2003, Proc Ocean Drill Program, Initial Reports, V201, P1, DOI DOI 10.2973/0DP.PR0C.IR.201.103.2003