Detection of gas hydrates by the measurement of instantaneous temperature /

"hydrate nodule" layers was tested. The temperature versus

Bibliographic Details
Main Author: Dinakaran, Srikanth, 1969-
Format: Thesis eBook
Language:English
Published: [Place of publication not identified] : [publisher not identified] ; 1994.
Subjects:
Online Access:Link to OAKTrust copy

MARC

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035 |a (OCoLC)34794809 
040 |a TXA  |c TXA  |d UtOrBLW 
049 |a TXAM  |a TXAR 
099 |a 1994  |a Thesis  |a D5836 
100 1 |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. 
300 |a xvi, 124 leaves :  |b illustrations ;  |c 28 cm. 
336 |a text  |b txt  |2 rdacontent 
337 |a computer  |b c  |2 rdamedia 
338 |a online resource  |b cr  |2 rdacarrier 
500 |a "Major subject: Civil Engineering". 
500 |a Vita. 
502 |b M.S.  |c Texas A&M University  |d 1994. 
504 |a Includes bibliographical references. 
520 |a "hydrate nodule" layers was tested. The temperature versus  
520 |a be to develop a method to detect hydrates in ocean sediment.  
520 |a cm/sec. Validation tests were performed in the laboratory  
520 |a Cone Penetrometer. Thus in addition to temperature  
520 |a could be made to aid in the detection of hydrates. 
520 |a depth profile indicated the presence of hydrates. The  
520 |a Detection of gas hydrates is possible due to the significant  
520 |a differences in the physical properties of hydrates and the  
520 |a due to the complications faced in recovering insitu samples  
520 |a effectiveness of this method to "hydrate nodule" layers was  
520 |a for laboratory testing. The presence of hydrates near the  
520 |a for the formation of natural gas hydrates in ocean sediments.  
520 |a formed by gas molecules trapped in a water lattice. Suitable  
520 |a foundation zone of deepwater structures may pose problems to  
520 |a involves the measurement of instantaneous temperature as a  
520 |a measurements, simultaneous measurements of electrical  
520 |a methods used to measure sediment temperature were studied. A  
520 |a Natural gas hydrates are icelike crystalline substances  
520 |a new method to detect hydrates was developed based on sediment  
520 |a oil exploration in the oceans, the first logical step would  
520 |a probe is pushed continuously into the sediment at a rate of 2  
520 |a properties of hydrates and ocean sediment and the past  
520 |a resistivity, cone penetration resistance and pore pressure  
520 |a sediments. Detailed study of hydrate properties is difficult  
520 |a Several major problems are associated with hydratebearing  
520 |a surrounding sediments. In this research, the physical  
520 |a temperature and its effectiveness was tested. This method  
520 |a temperature measuring device could be mounted on a Standard  
520 |a tested. effectiveness of this method to detect "hydrate" and  
520 |a the presence of gas hydrates could limit the development of  
520 |a the stability of the foundations of these structures. Since  
520 |a thermodynamic conditions and the presence of gas are required  
520 |a using glass marbles as a substitute for gas hydrates. The  
530 |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 
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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