Thermocapillary Marangoni convection in gas-bearing bottom sediments of Lake Baikal induced by their heating during in situ thermal conductivity measurements

2014 ◽  
Vol 459 (2) ◽  
pp. 1598-1602
Author(s):  
V. A. Golubev
Keyword(s):  
Thermal Conductivity ◽  
Lake Baikal ◽  
Bottom Sediments ◽  
Marangoni Convection ◽  
Conductivity Measurements ◽  
Gas Bearing

scholarly journals Draft Genome Sequence of Thermaerobacter sp. Strain PB12/4term, a Thermophilic Facultative Anaerobic Bacterium from Bottom Sediments of Lake Baikal, Russia

2018 ◽  
Vol 7 (20) ◽  
Author(s):  
Olga A. Baturina ◽  
Olga N. Pavlova ◽  
Angelina S. Novikova ◽  
Marsel R. Kabilov ◽  
Tamara I. Zemskaya
Keyword(s):  
Lake Baikal ◽  
Genome Sequence ◽  
Bottom Sediments ◽  
Anaerobic Bacterium ◽  
Draft Genome ◽  
Draft Genome Sequence ◽  
Discharge Zone ◽  
Content Type ◽  
Facultative Anaerobic ◽  
Gas Bearing

Here, we report the draft genome sequence of Thermaerobacter sp. strain PB12/4term, a thermophilic facultative anaerobic bacterium from the bottom sediments of Lake Baikal, Russia, associated with the discharge zone of gas-bearing fluids.

scholarly journals In situ thermal conductivity measurements of Titan's lower atmosphere

Icarus ◽  
2008 ◽  
Vol 197 (2) ◽  
pp. 579-584 ◽  
Author(s):  
B. Hathi ◽  
A.J. Ball ◽  
M. Banaszkiewicz ◽  
P.M. Daniell ◽  
J.R.C. Garry ◽  
...  
Keyword(s):  
Thermal Conductivity ◽  
Lower Atmosphere ◽  
Conductivity Measurements

In Situ Thermal Conductivity Measurements of Building Materials with a Thermal Probe

2010 ◽  
Vol 38 (3) ◽  
pp. 102636
Author(s):  
M. R. Mitchell ◽  
R. E. Link ◽  
B. Pilkington ◽  
S. Goodhew ◽  
P. deWilde
Keyword(s):  
Thermal Conductivity ◽  
Building Materials ◽  
Conductivity Measurements ◽  
Thermal Probe

Analysis of Heat Flow Data—in situ Thermal Conductivity Measurements

1971 ◽  
Vol 8 (1) ◽  
pp. 1-19 ◽  
Author(s):  
A. E. Beck ◽  
F. M. Anglin ◽  
J. H. Sass
Keyword(s):  
Thermal Conductivity ◽  
Field Experiments ◽  
Contact Layer ◽  
Design Parameters ◽  
Probe Design ◽  
Thermal Mass ◽  
Flow Data ◽  
Conductivity Measurements ◽  
The Many

The electrically heated cylindrical probe has often been used to measure the thermal conductivity of materials which allow the contact layer to be small enough to have negligible thermal resistance and negligible thermal mass. The probe method is not widely used in boreholes, mainly because the increased complexity of the theory required by the boundary conditions encountered in typical field situations makes it difficult to design appropriate probes and to interpret the data.This paper deals with the results of a comprehensive series of laboratory and field experiments, using cased and uncased boreholes, to investigate the importance of various design parameters and to compare the relative merits of the many proposed methods of reducing the data.It has been found that there is a surprising degree of latitude in probe design provided an uncertainty of 10% in conductivity values can be tolerated.

Diversity of Archaea in Bottom Sediments of the Discharge Areas With Oil- and Gas-Bearing Fluids in Lake Baikal

2017 ◽  
Vol 35 (1) ◽  
pp. 50-63 ◽  
Author(s):  
Anna V. Lomakina ◽  
Elena V. Mamaeva ◽  
Yuri P. Galachyants ◽  
Darya P. Petrova ◽  
Tatyana V. Pogodaeva ◽  
...  
Keyword(s):  
Lake Baikal ◽  
Bottom Sediments ◽  
Oil And Gas ◽  
Gas Bearing

scholarly journals Occurrence of Tankhoy field coals in South Baikal bottom sediments

2021 ◽  
Vol 44 (3) ◽  
pp. 285-292
Author(s):  
O. M. Khlystov ◽  
A. V. Vainer-Krotov ◽  
A. V. Kitaev ◽  
T. V. Pogodaeva
Keyword(s):  
Lake Baikal ◽  
Bottom Sediments ◽  
Distribution Area ◽  
Palynological Analysis ◽  
Southern Basin ◽  
Significant Area ◽  
Lithological Composition ◽  
Bearing Part ◽  
South Baikal

The purpose of the study is to describe the first finds of coal-bearing clays and coals in the bottom sediments of the southern basin of Lake Baikal and compare them with terrestrial coal-bearing deposits of the Tankhoy field. Comparative analysis of the lithological composition and colour of bottom sediments and terrestrial sections, as well as the concentration of organic carbon and conducted palynological analysis allowed their correlation. At the lake’s depth of 900 m the authors discovered a coal-bearing strata in situ (st 56), which later was stratigraphically correlated with the terrestrial coalbearing part of the Tankhoy suite. The fragments of coal found in bottom sediments basically along the entire Tankhoy field, especially bedrock coals on the underwater slope in South Baikal up to 1300 m deep prove the distribution of the coal-bearing part of the Tankhoy suite in the sublacustrine part of the lake throughout the entire slope (from 5 to 10 km offshore) and confirm the distribution area of the Tankhoy paleolake over a significant area of the contour of modern southern basin of Lake Baikal. The finds of coal-bearing strata on these and other various sub-bottom depths, i.e. under various pressure and temperature conditions, suggest that coals themselves and coal-bearing mudstones may be a generation facility of secondary microbial methane. This should be taken into account when searching for gas hydrocarbon and gas hydrate accumulations as well as assessing methane cycles in Lake Baikal.

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