AI SearchAnalysis of the extent and the distribution of aquifers in the Chao Phraya Basin, Thailand
Call Number: AIT Thesis no. GT-78-26 Material type:
SeriesSeries: Asian Institute of Technology. Thesis ; no. GT-78-26Publication details: Bangkok : Asian Institute of Technology, 1979Description: vi, 186 pSubject(s): Online resources: Dissertation note: Thesis (M.Eng.) - Asian Institute of Technology, 1979 Summary: A thorough analysis of lithologic logs of ground water wells in Bangkok area was carried out by using a systematic correlation procedure based on matching technique utilizing a series of computer programs in order to delineate the stratigray of Bangkok subsoils. Several east-west and north-south stratigraphic cross sections were established and through a detailed analysis of these cross sections, three partially separated sand layers were identified within first 150 m depth. Trend surfaces were fitted to establish trends associated with top and bottom surfaces and were used to analyze thickness variation of each sand layer. Finally, a table giving a detailed description of sand layers was prepared.
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Asian Institute of Technology Library AIT Publications | AIT Thesis no. GT-78-26 (Browse shelf(Opens below)) | 1 | Available | 30050003048518 | |||||||||||||
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20-AIT Publication
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Asian Institute of Technology Library AIT Publications | AIT Thesis no. GT-78-26 (Browse shelf(Opens below)) | 2 | Available | 30050003048526 | |||||||||||||
40-Archives
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Asian Institute of Technology Library Archives | AIT Thesis no. GT-78-26 (Browse shelf(Opens below)) | 1 | Available | 30050160071287 |
A thesis submitted in partial fulfilment of the requirements for the degree of Master of Engineering, School of Engineering and Technology
Thesis (M.Eng.) - Asian Institute of Technology, 1979
A thorough analysis of lithologic logs of ground water wells in Bangkok area was carried out by using a systematic correlation procedure based on matching technique utilizing a series of computer programs in order to delineate the stratigray of Bangkok subsoils. Several east-west and north-south stratigraphic cross sections were established and through a detailed analysis of these cross sections, three partially separated sand layers were identified within first 150 m depth. Trend surfaces were fitted to establish trends associated with top and bottom surfaces and were used to analyze thickness variation of each sand layer. Finally, a table giving a detailed description of sand layers was prepared.
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