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| LEADER |
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| 001 |
in00001302213 |
| 005 |
20220103113952.0 |
| 007 |
cr unu a |
| 008 |
960528s1994 xx a b 000 0 eng d |
| 035 |
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|9 AHA4786AM
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| 035 |
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|a (OCoLC)34794809
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| 040 |
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|a TXA
|c TXA
|d UtOrBLW
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| 049 |
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|a TXAM
|a TXAR
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| 099 |
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|a 1994
|a Thesis
|a D5836
|
| 100 |
1 |
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|a Dinakaran, Srikanth,
|d 1969-
|
| 245 |
1 |
0 |
|a Detection of gas hydrates by the measurement of instantaneous temperature /
|c by Srikanth Dinakaran.
|
| 264 |
|
1 |
|a [Place of publication not identified] :
|b [publisher not identified] ;
|c 1994.
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| 300 |
|
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|a xvi, 124 leaves :
|b illustrations ;
|c 28 cm.
|
| 336 |
|
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|a text
|b txt
|2 rdacontent
|
| 337 |
|
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|a computer
|b c
|2 rdamedia
|
| 338 |
|
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|a online resource
|b cr
|2 rdacarrier
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| 500 |
|
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|a "Major subject: Civil Engineering".
|
| 500 |
|
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|a Vita.
|
| 502 |
|
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|b M.S.
|c Texas A&M University
|d 1994.
|
| 504 |
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|a Includes bibliographical references.
|
| 520 |
|
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|a "hydrate nodule" layers was tested. The temperature versus
|
| 520 |
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|a be to develop a method to detect hydrates in ocean sediment.
|
| 520 |
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|a cm/sec. Validation tests were performed in the laboratory
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| 520 |
|
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|a Cone Penetrometer. Thus in addition to temperature
|
| 520 |
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|a could be made to aid in the detection of hydrates.
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| 520 |
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|a depth profile indicated the presence of hydrates. The
|
| 520 |
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|a Detection of gas hydrates is possible due to the significant
|
| 520 |
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|a differences in the physical properties of hydrates and the
|
| 520 |
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|a due to the complications faced in recovering insitu samples
|
| 520 |
|
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|a effectiveness of this method to "hydrate nodule" layers was
|
| 520 |
|
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|a for laboratory testing. The presence of hydrates near the
|
| 520 |
|
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|a for the formation of natural gas hydrates in ocean sediments.
|
| 520 |
|
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|a formed by gas molecules trapped in a water lattice. Suitable
|
| 520 |
|
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|a foundation zone of deepwater structures may pose problems to
|
| 520 |
|
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|a involves the measurement of instantaneous temperature as a
|
| 520 |
|
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|a measurements, simultaneous measurements of electrical
|
| 520 |
|
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|a methods used to measure sediment temperature were studied. A
|
| 520 |
|
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|a Natural gas hydrates are icelike crystalline substances
|
| 520 |
|
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|a new method to detect hydrates was developed based on sediment
|
| 520 |
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|a oil exploration in the oceans, the first logical step would
|
| 520 |
|
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|a probe is pushed continuously into the sediment at a rate of 2
|
| 520 |
|
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|a properties of hydrates and ocean sediment and the past
|
| 520 |
|
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|a resistivity, cone penetration resistance and pore pressure
|
| 520 |
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|a sediments. Detailed study of hydrate properties is difficult
|
| 520 |
|
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|a Several major problems are associated with hydratebearing
|
| 520 |
|
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|a surrounding sediments. In this research, the physical
|
| 520 |
|
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|a temperature and its effectiveness was tested. This method
|
| 520 |
|
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|a temperature measuring device could be mounted on a Standard
|
| 520 |
|
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|a tested. effectiveness of this method to detect "hydrate" and
|
| 520 |
|
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|a the presence of gas hydrates could limit the development of
|
| 520 |
|
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|a the stability of the foundations of these structures. Since
|
| 520 |
|
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|a thermodynamic conditions and the presence of gas are required
|
| 520 |
|
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|a using glass marbles as a substitute for gas hydrates. The
|
| 530 |
|
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|a Also available online.
|
| 650 |
|
4 |
|a Major civil engineering.
|
| 856 |
4 |
1 |
|u https://hdl.handle.net/1969.1/ETD-TAMU-1994-THESIS-D5836
|z Link to OAKTrust copy
|t 0
|
| 999 |
|
|
|a MARS
|
| 999 |
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|i 0ee5e242-fcaf-3a85-b4fb-3382ab89c50c
|t 0
|
| 952 |
f |
f |
|p noncirc
|a Texas A&M University
|b J.J. Pickle Campus
|c High Density Repository
|s HDR
|d Remote Storage
|t 0
|e 1994 Thesis D5836
|h Other scheme
|i computer -- online resource
|m A14841059251
|
| 952 |
f |
f |
|a Texas A&M University
|b College Station
|c Electronic Resources
|s www_evans
|d Available Online
|t 0
|e 1994 Thesis D5836
|h Other scheme
|
| 998 |
f |
f |
|a 1994 Thesis D5836
|t 0
|l Remote Storage
|
| 998 |
f |
f |
|a 1994 Thesis D5836
|t 0
|l Available Online
|