Seismic characterisation of gas-rich near surface sediments in the Arkona Basin, Baltic Sea.

Mathys , M., Thießen , Olaf, Theilen , F. and Schmidt, Mark (2005) Seismic characterisation of gas-rich near surface sediments in the Arkona Basin, Baltic Sea. Marine Geophysical Research, 26 . pp. 207-224. DOI 10.1007/s11001-005-3719-4.

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Abstract

Gas in sediments has become an important subject of research for various reasons. It affects large areas of the sea floor where it is
mainly produced. Gas and gas migration have a strong impact on the environmental situation as well as on sea floor stability.
Furthermore, large research programs on gas hydrates have been initiated during the last 10 years in order to investigate their potential
for future energy production and their climatic impact. These activities require the improvement of geophysical methods for reservoir
investigations especially with respect to their physical properties and internal structures. Basic relationships between the physical
properties and seismic parameters can be investigated in shallow marine areas as they are more easily accessible than hydrocarbon
reservoirs. High-resolution seismic profiles from the Arkona Basin (SW Baltic Sea) show distinct ‘acoustic turbidity’ zones which
indicate the presence of free gas in the near surface sediments. Total gas concentrations were determined from cores taken in the study
area with mean concentrations of 46.5 ml/l wet sediment in non-acoustic turbidity zones and up to 106.1 ml/l in the basin centre with
acoustic turbidity. The expression of gas bubbles on reflection seismic profiles has been investigated in two distinct frequency ranges
using a boomer (600–2600 Hz) and an echosounder (38 kHz). A comparison of data from both seismic sources showed strong
differences in displaying reflectors. Different compressional wave velocities were observed in acoustic turbidity zones between boomer
and echosounder profiles. Furthermore, acoustic turbidity zones were differently characterised with respect to scattering and attenuation
of seismic waves. This leads to the conclusion that seismic parameters become strongly frequency dependent due to the dynamic
properties of gas bubbles.

Document Type: Article
Keywords: Geochemistry; Arkona Basin; P-wave velocity; shallow gas; velocity dispersion; ECKERNFORDE BAY; ACOUSTIC TURBIDITY; BEARING SEDIMENTS; MARINE-SEDIMENTS; MUDDY SEDIMENTS; SHALLOW GAS; POS266; AL201; AL214; AL214
Research affiliation: Kiel University
Refereed: Yes
Open Access Journal?: No
Publisher: Springer
Projects: GEOTECHNOLOGIEN, NATLAB-INGGAS
Date Deposited: 07 Apr 2011 07:32
Last Modified: 09 Aug 2017 11:31
URI: https://oceanrep.geomar.de/id/eprint/11634

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