Pape, Thomas; Bahr, André; Klapp, Stephan A; Abegg, Friedrich; Bohrmann, Gerhard (2011): (Table 5) Unit-specific lengths (LsUx), pore fluid volumes (VpfUx), pore fluid masses (mpfUx), and methane masses (mCH4Ux) calculated for pressure cores from the Batumi seep area [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.763862, In supplement to: Pape, T et al. (2011): High-intensity gas seepage causes rafting of shallow gas hydrates in the southeastern Black Sea. Earth and Planetary Science Letters, 307, 35-46, https://doi.org/10.1016/j.epsl.2011.04.030
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Project(s):
Coverage:
Median Latitude: 41.957998 * Median Longitude: 41.290298 * South-bound Latitude: 41.956833 * West-bound Longitude: 41.287833 * North-bound Latitude: 41.959117 * East-bound Longitude: 41.292417
Date/Time Start: 2007-03-19T18:44:00 * Date/Time End: 2007-04-11T13:09:00
Minimum Elevation: -851.0 m * Maximum Elevation: -840.0 m
Event(s):
GeoB11901 (DAPC-1) * Latitude: 41.956833 * Longitude: 41.289067 * Date/Time: 2007-03-19T18:44:00 * Elevation: -851.0 m * Recovery: 2.6 m * Location: Batumi Seep * Campaign: M72/3a * Basis: Meteor (1986) * Method/Device: Dynamic autoclave piston corer (DAPC) * Comment: DAPC (I), USBL
GeoB11906 (DAPC-3) * Latitude: 41.957750 * Longitude: 41.287833 * Date/Time: 2007-03-22T07:58:00 * Elevation: -843.0 m * Recovery: 0.83 m * Location: Batumi Seep * Campaign: M72/3a * Basis: Meteor (1986) * Method/Device: Dynamic autoclave piston corer (DAPC) * Comment: DAPC (I), USBL
GeoB11918 (DAPC-8) * Latitude: 41.959117 * Longitude: 41.290450 * Date/Time: 2007-03-30T10:30:00 * Elevation: -840.0 m * Recovery: 2.33 m * Location: Batumi Seep * Campaign: M72/3a * Basis: Meteor (1986) * Method/Device: Dynamic autoclave piston corer (DAPC) * Comment: DAPC (II), USBL, first time DAPC-II used
Comment:
a assuming average sediment porosities Ø of 0.85 (Unit 1), 0.72 (Unit 2), and 0.61 (Unit 3), respectively, according to data provided by Haeckel et al. (2008) and Reitz et al. (2011).
b assuming average pore fluid salinities of 23.07 (Unit 1); 22.27 (Unit 2), and 21.15 (Unit 3), respectively, based on pore water salinities provided by Leonov (2005). Those values were converted into pore fluid in situ densities (?pfUx) of 1021.63 (Unit 1), 1021.01 (Unit 2), and 1020.14 kg L**-1 (Unit 3) using the algorithm provided at http://www.phys.ocean.dal.ca/~kelley/seawater/density.html.
c nominal CH4 in situ concentrations (nCCH4Ux) in sediments belonging to Unit 1 (26.6 mmol L**-1) and Unit 2 (430.9 mmol L**-1) calculated from data obtained for cores DAPC 09 and 12. CH4 in situ solubilities calculated with regard to absence (sgp = 108.5 mmol L**-1; Unit 1) or presence (shpU2 = 93.9 mmol L**-1 and shpU3 = 94.7 mmol L**-1) of gas hydrates according to Duan and Mao (2006) and Tishchenko et al. (2005).
d mass of residual CH4 [mCH4U3 = mCH4t – (mCH4U1 + mCH4U2)]
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Sample code/label | Sample label | Pape, Thomas | |||
| 3 | Length | l | mm | Pape, Thomas | ||
| 4 | Length | l | mm | Pape, Thomas | ||
| 5 | Length | l | mm | Pape, Thomas | ||
| 6 | Volume | Vol | ml | Pape, Thomas | Calculated | a |
| 7 | Volume | Vol | ml | Pape, Thomas | Calculated | a |
| 8 | Volume | Vol | ml | Pape, Thomas | Calculated | a |
| 9 | Mass | Mass | kg | Pape, Thomas | Calculated | b |
| 10 | Mass | Mass | kg | Pape, Thomas | Calculated | b |
| 11 | Mass | Mass | kg | Pape, Thomas | Calculated | b |
| 12 | Methane, mass | CH4 | mol | Pape, Thomas | Calculated | |
| 13 | Methane, mass | CH4 | mol | Pape, Thomas | Calculated | c |
| 14 | Methane, mass | CH4 | mol | Pape, Thomas | Calculated | c |
| 15 | Methane, mass | CH4 | mol | Pape, Thomas | Calculated | d |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
86 data points