Determination of Eaton's Exponent in the Gulf of Thailand (Record no. 27987)

MARC details
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fixed length control field 04262nas a2200421 a 4500
005 - DATE AND TIME OF LATEST TRANSACTION
control field 20260818090414.0
008 - FIXED-LENGTH DATA ELEMENTS--GENERAL INFORMATION
fixed length control field 090907s2009 th uu|m rtt 0| a1eng d
035 ## - SYSTEM CONTROL NUMBER
System control number .b12067192
099 #9 - LOCAL FREE-TEXT CALL NUMBER (OCLC)
Classification number AIT Thesis no.OTM-09-04
100 0# - MAIN ENTRY--PERSONAL NAME
Personal name Prairaya Somanandana
245 10 - TITLE STATEMENT
Title Determination of Eaton's Exponent in the Gulf of Thailand
260 ## - PUBLICATION, DISTRIBUTION, ETC.
Place of publication, distribution, etc. Pathum Thani, Thailand :
Name of publisher, distributor, etc. Asian Institute of Technology,
Date of publication, distribution, etc. 2009
300 ## - PHYSICAL DESCRIPTION
Extent 84 leaves :
Other physical details ill.
490 1# - SERIES STATEMENT
Series statement Thesis ;
Volume/sequential designation no. OTM-09-04
500 ## - GENERAL NOTE
General note A thesis submitted in partial fulfillment of the requirements for the degree of Master of Engineering Offshore Technology and Management, School of Engineering and Technology
502 ## - DISSERTATION NOTE
Dissertation note Thesis (M.Eng.) - Asian Institute of Technology, 2009
520 ## - SUMMARY, ETC.
Summary, etc. Eaton's model, a pore pressure prediction equation utilizing porosity to stress relation, has one of the governed factors known as Eaton's Exponent "EE", acting as enhancing factor of overpressure zones. Via his model this factor obtained empirically and suggests that it should be estimated by region due to differences in area's characteristics, leading to the study of specific EE within the Gulf of Thailand. In Eaton's model overpressure sections buried in deep portion of thick sediments with small heterogeneity. In contrast to the study areas locate in the Gulf of Thailand within Pattani Basin to Northern portion of Malay Basin, abnormal pressure zones are in much shallower portion, in heavy faulting system, with thin sequences of sand/shale interbeded, and influenced by high heat flow. In this paper, EE determination method utilizes actual formation pressure measurements under three major controlling factors of overburden stress, shale normal compaction, and temperature. Most study wells are at normal hydrostatic condition, instead of pore pressure gradient in P/Z now use calculated fluid gradient from RFT/MDT comprises with fluid sample report. The most suitable EE is calculated from fluid gradient in hydrocarbon interval. This resulted from a difficulty in estimating pressure in shale section due to shaly ambiguity and non-linear relation of formation pressure. Furthermore, by calculating using all fluid gradients instead of only hydrocarbon zone will lessen the effect of abnormal pressure. Eaton's exponent is directly affected by temperature but inverses to overburden stress. The calculated EE is estimated according to region where EE in North region (North Pattani Basin) is 0.7, then decreasing to 0.4 in Southern regions (South Pattani Basin and Uppermost portion of North Malay Basin), and then jump to approximately 1 or above in Northwestern flank Malay Basin where well locations lie in close proximity to high heat flow zone (Central Malay Basin). In water wells, EE is approaching o. Predicted pore pressure from Eaton's equation using conventional sonic Eaton's exponent in sonic technique or "3", and using calculated EE, shows 38% and 9% deviation from actual fonnation test pressure, respectively. This evidently proves that predicted EE improves accuracy in the Gulf of Thailand region.
650 #0 - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical term or geographic name entry element Hydrostatics
Geographic subdivision Thailand, Gulf of
650 #0 - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical term or geographic name entry element Hydrostatic pressure
Geographic subdivision Thailand, Gulf of
651 #0 - SUBJECT ADDED ENTRY--GEOGRAPHIC NAME
Geographic name Thailand, Gulf of
700 1# - ADDED ENTRY--PERSONAL NAME
Personal name Chiu, Gregory L.F.,
Relator term Chairperson
700 0# - ADDED ENTRY--PERSONAL NAME
Personal name Jirawat Chewaroungroaj,
Relator term Co-chairperson
700 0# - ADDED ENTRY--PERSONAL NAME
Personal name Worsak Kanok-Nukulchai,
Relator term Examination Committee
700 1# - ADDED ENTRY--PERSONAL NAME
Personal name Widjaja, Joko Harsono,
Relator term Examination Committee
710 2# - ADDED ENTRY--CORPORATE NAME
Corporate name or jurisdiction name as entry element Pearl Oil (Thailand) Limited,
Relator term Scholarship donor
810 2# - SERIES ADDED ENTRY--CORPORATE NAME
Corporate name or jurisdiction name as entry element Asian Institute of Technology.
Title of a work Thesis ;
Volume/sequential designation no. OTM-09-04
856 ## - ELECTRONIC LOCATION AND ACCESS
Materials specified Full-Text
Uniform Resource Identifier <a href="http://203.159.5.9/ait-thesis/detail.php?q=B03589 ">http://203.159.5.9/ait-thesis/detail.php?q=B03589 </a>
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998 ## - LOCAL CONTROL INFORMATION (RLIN)
Operator's initials, OID (RLIN) 0
Cataloger's initials, CIN (RLIN) 090907
First date, FD (RLIN) m
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945 ## - LOCAL PROCESSING INFORMATION (OCLC)
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942 ## - ADDED ENTRY ELEMENTS (KOHA)
Koha item type 22-AIT Thesis (Replacement)
942 ## - ADDED ENTRY ELEMENTS (KOHA)
Koha item type 40-Archives
909 ## - LOCAL ITEMS USED
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CREATED CREATED : 2014-05-19
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Holdings
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      Available for Loans Asian Institute of Technology Library Asian Institute of Technology Library AIT Publications 18/08/2026 50.00   AIT Thesis no.OTM-09-04 30050120685705 18/08/2026 3 18/08/2026 22-AIT Thesis (Replacement)
      Available for Loans Asian Institute of Technology Library Asian Institute of Technology Library Archives 18/08/2026     AIT Thesis no.OTM-09-04 30050160006408 18/08/2026 1 18/08/2026 40-Archives
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