Analyses on wave-induced pore pressures in fluidized seabeds
碩士 === 國立成功大學 === 水利及海洋工程學系 === 89 === This thesis primarily investigates the pore pressure responses inside the fluidized non-cohesive seabeds with a wave flume set-up. Analysis on the mean pore pressure build-up and the pressure amplitude were carried out to study interactions of wave and fluidize...
Main Authors: | , |
---|---|
Other Authors: | |
Format: | Others |
Language: | zh-TW |
Published: |
2001
|
Online Access: | http://ndltd.ncl.edu.tw/handle/29872330900626160785 |
id |
ndltd-TW-089NCKU0083003 |
---|---|
record_format |
oai_dc |
spelling |
ndltd-TW-089NCKU00830032016-01-29T04:23:54Z http://ndltd.ncl.edu.tw/handle/29872330900626160785 Analyses on wave-induced pore pressures in fluidized seabeds 液化海床內波引致之孔隙水壓分析 wang chih ming 王智民 碩士 國立成功大學 水利及海洋工程學系 89 This thesis primarily investigates the pore pressure responses inside the fluidized non-cohesive seabeds with a wave flume set-up. Analysis on the mean pore pressure build-up and the pressure amplitude were carried out to study interactions of wave and fluidized seabeds . A fine sand( d50 = 0.085mm) is first used as the test seabed material to investigate the soil responses after internal fluidization. The results show that pressure amplitudes amplify twice during fluidized and the phenomenon is more apparent in the initially-fluidized responses. Besides, pressure amplitudes decrease as mean pressure build-ups reduce in the fluidized stage. Pressure amplitudes is gradually become steady but their magnitudes are still larger then those before fluidization. Comparison with fluidized soil layer and the depth profiles of amplitude in Tzang’ s (1992) and Peng’ s(2000) tests, further illustrate that pore pressure amplitude would amplify after fluidization .Maximum amplitude amplification generally occur close to the bottom of fluidized layer while the depth profile of pressure amplitude is inverse to the pore-elasticity theory. After several wave-induced consecutive soil fluidization, fluidized layer gradually become shallower the pressure amplitude amplifications decrease and revert to non-fluidized mode before fluidization. As a result, this study has preliminary exploded the soil responses after fluidization in the non-cohesive seabed, thus it becomes feasible to further study the characteristics of interactions of waves and fluidized seabeds in the future. Shan-Hwea Ou Shiaw-Yih Tzang 歐善惠 臧效義 2001 學位論文 ; thesis 103 zh-TW |
collection |
NDLTD |
language |
zh-TW |
format |
Others
|
sources |
NDLTD |
description |
碩士 === 國立成功大學 === 水利及海洋工程學系 === 89 === This thesis primarily investigates the pore pressure responses inside the fluidized non-cohesive seabeds with a wave flume set-up. Analysis on the mean pore pressure build-up and the pressure amplitude were carried out to study interactions of wave and fluidized seabeds .
A fine sand( d50 = 0.085mm) is first used as the test seabed material to investigate the soil responses after internal fluidization. The results show that pressure amplitudes amplify twice during fluidized and the phenomenon is more apparent in the initially-fluidized responses. Besides, pressure amplitudes decrease as mean pressure build-ups reduce in the fluidized stage. Pressure amplitudes is gradually become steady but their magnitudes are still larger then those before fluidization.
Comparison with fluidized soil layer and the depth profiles of amplitude in Tzang’ s (1992) and Peng’ s(2000) tests, further illustrate that pore pressure amplitude would amplify after fluidization .Maximum amplitude amplification generally occur close to the bottom of fluidized layer while the depth profile of pressure amplitude is inverse to the pore-elasticity theory. After several wave-induced consecutive soil fluidization, fluidized layer gradually become shallower the pressure amplitude amplifications decrease and revert to non-fluidized mode before fluidization. As a result, this study has preliminary exploded the soil responses after fluidization in the non-cohesive seabed, thus it becomes feasible to further study the characteristics of interactions of waves and fluidized seabeds in the future.
|
author2 |
Shan-Hwea Ou |
author_facet |
Shan-Hwea Ou wang chih ming 王智民 |
author |
wang chih ming 王智民 |
spellingShingle |
wang chih ming 王智民 Analyses on wave-induced pore pressures in fluidized seabeds |
author_sort |
wang chih ming |
title |
Analyses on wave-induced pore pressures in fluidized seabeds |
title_short |
Analyses on wave-induced pore pressures in fluidized seabeds |
title_full |
Analyses on wave-induced pore pressures in fluidized seabeds |
title_fullStr |
Analyses on wave-induced pore pressures in fluidized seabeds |
title_full_unstemmed |
Analyses on wave-induced pore pressures in fluidized seabeds |
title_sort |
analyses on wave-induced pore pressures in fluidized seabeds |
publishDate |
2001 |
url |
http://ndltd.ncl.edu.tw/handle/29872330900626160785 |
work_keys_str_mv |
AT wangchihming analysesonwaveinducedporepressuresinfluidizedseabeds AT wángzhìmín analysesonwaveinducedporepressuresinfluidizedseabeds AT wangchihming yèhuàhǎichuángnèibōyǐnzhìzhīkǒngxìshuǐyāfēnxī AT wángzhìmín yèhuàhǎichuángnèibōyǐnzhìzhīkǒngxìshuǐyāfēnxī |
_version_ |
1718169865800384512 |