請用此 Handle URI 來引用此文件:
http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/29418
完整後設資料紀錄
DC 欄位 | 值 | 語言 |
---|---|---|
dc.contributor.advisor | 魏慶琳(Ching-Ling Wei) | |
dc.contributor.author | Yen-Ruei Hou | en |
dc.contributor.author | 侯雁睿 | zh_TW |
dc.date.accessioned | 2021-06-13T01:06:35Z | - |
dc.date.available | 2007-07-25 | |
dc.date.copyright | 2007-07-25 | |
dc.date.issued | 2007 | |
dc.date.submitted | 2007-07-20 | |
dc.identifier.citation | Amiel, D., J. K. Cochran, D. J. Hirschberg. 2002. 234Th/238U disequilibrium as an indicator of the seasonal export flux of particulate organic carbon in the North Water. Deep-Sea Research II, 49, 5191-5209.
Benitez-Nelson, C. R., K. O. Buesseler, G. Crossin. 2000. Upper ocean carbon export, horizontal transport, and vertical eddy diffusivity in the southwestern Gulf of Maine. Continental Shelf Research, 20, 707-736. Buesseler, K. O., M. P. Bacon, J. K. Cochran, H. D. Livingston. 1992. Carbon and nitrogen export during the JGOFS North Atlantic Bloom Experiment estimated from 234Th:238U disequilibria. Deep-sea Research, 39, 1115-1137. Buesseler, K., L. Ball, J. Andrews, C. Benitez-Nelson, R. Belastock, F. Chai, Y. Chao. 1998. Upper ocean export of particulate organic carbon in the Arabian Sea derived from thorium-234. Deep-sea Research II, 45, 2461-2487. Chung, S.-W., S. Jan, K.-K. Liu. 2001. Nutrient fluxes through the Taiwan Strait in Spring and Summer 1999. Journal of Oceanography, 57, 47-53. Coale, K. H., K. W. Bruland. 1985. 234Th:238U disequilibria within the California Current. Limnology and Oceanography, 30, 22-33. Coale, K. H., K. W. Bruland. 1987. Oceanic stratified euphotic zone as elucidated by 234Th:238U disequilibria. Limnology and Oceanography, 32, 189-200. Cochran, J. K., C. Barnes, D. Achman, D. J. Hirschberg. 1995. Thorium-234/Uranium-238 disequilibrium as an indicator of scavenging rates and particulate organic carbon fluxes in the Northeast Water Polynya, Greenland. Journal of Geophysical Research, 100, 4399-4410. Coppola, L., M. Roy-Barman, P. Wassmann, S. Mulsow, C. Jeandel. 2002. Calibration of sediment traps and particulate organic carbon export using 234Th in the Barents Sea. Marine Chemistry, 80, 11-26. Eppley, R. W.. 1989. New Production: history, methods, problems. In: Berger, W. H., V. S. Smetack, G. Wefer, editors, Productivity of the Ocean: Present and Past. Wiley, New York, 85-97. Fan, K.-L.. 1982. A study of water masses in Taiwan Strait. Acta Oceanographica Taiwanica , 13, 140-153. Frignani, M., T. Courp, J. K. Cochran, D. Hirschberg, L. Vitoria i Codina. 2002. Scavenging rates and particle characteristics in and near the Lacaze-Duthiers submarine canyon, northwest Mediterranean. Continental Shelf Research, 22, 2175-2190. Goldberg, E. D.. 1954. Marine geochemistry: Chemical scavengers of the sea. Journal of Geology, 62, 249-265. Guo, L.-D., C.-C. Hung, P. H. Santschi, I. D. Walsh. 2002. 234Th scavenging and its relationship to acid polysaccharide abundance in the Gulf of Mexico. Marine Chemistry, 78, 103-119. Gustafsson, O., K. O. Buesseler, W. R. Geyer, S. B. Moran, P. M. Gschwend. 1998. An assessment of the relative importance of horizontal and vertical transport of particle-reactive chemicals in the coastal ocean. Continental Shelf Research, 18, 805-829. Gustafsson, O., A. Widerlund, P. S. Andersson, J. ingri, P. Roos, A. Ledin. 2000. Colloid dynamics and transport of major element through a boreal river—brackish bay mixing zone. Marine Chemistry, 71, 1-21. Gustafsson, O., P. Andersson, P. Roos, Z. Kukulska, D. Broman, U. Larsson, S. Hajdu, J. Ingri. 2004. Evaluation of the collection efficiency of upper ocean sub-photic-layer sediment traps: a 24-mouth in situ calibration in the open Baltic Sea using 234Th. Limnology and Oceanography: Methods, 2, 62-74. Honeyman, B. D., L. S. Balistrieri, J. W. Murray. 1988. Oceanic trace metal scavenging: the importance of particle concentration. Deep-sea Research I, 35, 227-246. Huh, C.-A.. 1995. The Isotopes in the Santa Monica Basin: temporal Variation, Long-Term Mass Balance and Model Rate Constants. Journal of Oceanography, 51, 363-373. Huh, C.-A., C.-C. Su. 1999. Sedimentation dynamics in the East China Sea elucidated from 210Pb, 137Cs and 239,240Pu. Marine Geology, 160, 183-196. Hung, C.-C, C.-L. Wei. 1992. Th-234 scavenging in the water column off southwestern Taiwan. Terrestrial, Atmospheric and Oceanic Sciences, 3, 183-197. Hung, C.-C., L. Guo, K. A. Roberts, P. H. Santschi. 2004. Upper ocean carbon flux determined by the 234Th approach and sediment traps using size-fractionated POC and 234Th data from the Gulf of Mexico. Geochemical Journal, 38, 601-611. Hung, J.-J., P.-L. Lin, K.-K. Liu. 2000. Dissolved and particulate organic carbon in the southern East China Sea. Continental Shelf Research, 20, 545-569. Jan, S., S.-Y. Chao. 2003. Seasonal variation of volume transport in the major inflow region of Taiwan Strait: the Penghu Channel. Deep-sea Research II, 50, 1117-1126. Jan, S., J. Wang, C.-S. Chern, S.-Y. Chao. 2002. Seasonal variation of the circulation in the Taiwan Strait. Journal of Marine Systems, 35, 249-268. Ku, T.-L., K. G. Knauss, G. G. Mathieu. 1977. Uranium in open ocean: concentration and isotopic composition. Deep-sea Research, 24, 1005-1017. Kersten, M.. 1998. Scavenging and particle residence times determined from 234Th/238U disequilibrium in the coastal waters of Mecklenburg Bay. Applied Geochemistry, 13, 339-347. Liang, W.-D., T.-Y. Tang, Y.-J. Yang, M.-T. Ko, W.-S. Chuang. 2003. Upper-ocean currents around Taiwan. Deep-sea Research II, 50, 1085-1105. Liu, C.-S., S.-Y. Liu, S. E. Lallemand, N. Lundberg, D. L. Reed. 1998. Digital Elevation Model Offshore Taiwan and Its Tectonic Implications. Terrestrial, Atmospheric and Oceanic Sciences, 9, 705-738. Liu, K.-K., T.-Y. Tang, G.-G. Gong, L.-Y. Chen, F.-K. Shiah. 2000. Cross-shelf and along-shelf nutrient fluxes derived from flow fields and chemical hydrography observed in the southern East China Sea off northern Taiwan. Continental Shelf Research, 20, 493-523. Mckee, B. A., D. J. DeMaster, C. A. Nittrouer. 1984. The use of 234Th/238U disequilibrium to examine the fate of particle-reactive species on the Yangtze continental shelf. Earth and Planetary Science Letters, 68, 431-442. Mckee, B. A., D. J. DeMaster, C. A. Nittrouer. 1986. Temporal variability in the partitioning of thorium between dissolved and particulate phases on the Amazon shelf: implications for the scavenging of particle-reactive species. Continental Shelf Research, 6, 87-106. Mopper, K., J. Zhou, K. S. Ramana, U. Passow, H. G. Dam, D. T. Drapeau. 1995. The role of surface-active carbohydrates in the flocculation of a diatom bloom in a mesocosm. Deep-sea Research II, 42, 47-73. Moran, S. B., J. N. Smith. 2000. 234Th as a tracer of scavenging and particle export in the Beaufort Sea. Continental Shelf Research, 20, 153-167. Murray, J. W., J. N. Downs, S. Storm, C.-L. Wei, H. W. Jannasch. 1989. Nutrient assimilation, export production and 234Th scavenging in the eastern equatorial Pacific. Deep-Sea Research, 36, 1471-1489. Ochoa-Loza, F. J., J. F. Artiola, R. M. Maier. 2001. Stability Constants for the Complexation of Various Metals with a Rhamnolipid Biosurfactant. Journal of Environment Quality, 30, 479-485. Passow, U.. 2000. Formation of transparent exopolymer particles, TEP, from dissolved precursor material. Marine ecology-progress series, 192, 1-11. Poecelli, D., P. S. Andersson, M. Baskaran, G. J. Wasserburg. 2001. Transport of U- and Th-series nuclides in a Baltic Shield watershed and the Baltic Sea. Geochimica et Cosmochimica Acta, 65, 2439-2459. Radakovitch , O., M. Frignani, S. Giuliani, R. Montanari. 2003. Temporal variations of dissolved and particulate 234Th at a coastal station of the north Adriatic Sea. Estuarine, Coastal and Shelf Science, 58, 813-824. Savoye, N., C. Benitez-Nelson, A. B. Burd, J. K. Cochran, M. Charette, K. O. Buesseler, G. A. Jackson, M. Roy-Barman, S. Schmidt, M. Elskens. 2006. 234Th sorption and export models in the water column: A review. Marine Chemistry, 100, 234-249. Schmidt, S., V. Andersen, S. Belviso, J. Marty. 2002. Strong seasonality in particle dynamics of north-western Mediterranean surface waters as revealed by 234Th/238U. Deep-Sea Research I, 49, 1507-1518. Waples, J. T., K. A. Orlandini, D. N. Edgington, J. V. Klump. 2004. Seasonal and spatial dynamics of 234Th/238U disequilibria in southern Lake Michigan. Journal of Geophysical Research, 109, 1-30. Waples, J. T., C. Benitez-Nelson, N. Savoye, M. R. van der Loeff, M. Baskaran, O. Gustafsson. 2006. An introduction to the application and future use of 234Th in aquatic systems. Marine Chemistry, 100, 166-189. Wei, C.-L., C.-C. Hung. 1992. Spatial variation of 234Th scavenging in the surface water of Bashi Channel and the Luzon Strait. Journal of Oceanography, 48, 427-437. Wei, C.-L., J. W. Murray. 1992. Temporal variations of 234Th activity in the water column of Dabob Bay: Particle scavenging. Limnology and Oceanography, 37, 296-314. Wei, C.-L., C.-C. Hung. 1993. The effect of isotopic equilibration time on the determination of 234Th in seawater. Journal of Radioanalytical and Nuclear Chemistry, 175, 155-159. Wei, C.-L., K.-L. Jen, K. Chu. 1994. Sediment trap experiments in the water column of southwestern Taiwan: 234Th fluxes. Journal of Oceanography, 50, 403-414. Wyrtki, K.. 1961. Physical oceanography of the southeast Asia waters. Scientific results of marine investigations of the South China Sea and Gulf of Thailand. 1959-1961, Naga Report, 195pp. 蔡靜如. 2006. 台灣西部近岸水體清除現象:釷-234與鈾-238不平衡的應用. 國立臺灣大學海洋研究所碩士論文. 董淳禾. 2007. 台灣周遭海域表水浮游植物色素分佈初探. 國立臺灣大學海洋研究所碩士論文. | |
dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/29418 | - |
dc.description.abstract | 本研究利用釷-234/鈾-238不平衡探討臺灣海峽表層水體的顆粒清除現象,於2006年5月20~27日聯合水文探測期間,首度在臺灣海峽海域內大範圍地進行234Th採樣工作,船上同時測量基本的水文參數(溫度、鹽度、螢光和透光度)、總懸浮顆粒濃度和顆粒有機碳濃度,利用不可逆清除模式與周遭物理流速資料來估算顆粒的清除、沉降速率和滯留時間。
依據水文特徵和234Th分佈等資料,臺灣海峽的清除環境可劃分為五個區域:(Ⅰ)臺灣海峽南部;(Ⅱ)臺灣灘一帶;(Ⅲ)濁水溪口;(Ⅳ)臺灣海峽中部;(Ⅴ)閩江口。由模式計算結果,清除速率介於57~520 dpm/m3/d,以濁水溪口最高,其次依高至低順序為臺灣海峽中、南部、臺灣灘一帶、閩江口;顆粒沉降速率介於24~381 dpm/m3/d,以濁水溪口最高,依序為臺灣海峽中、南部、閩江口、臺灣灘一帶。大致上,全區的溶解態、顆粒態234Th滯留時間分別為0~6和1~3天,只有臺灣海峽南部的溶解態234Th滯留時間及臺灣灘一帶的顆粒態234Th滯留時間例外,其值高達16及18天。另一方面,濁水溪口、臺灣海峽中部及閩江口的顆粒有機碳平均移除速率分別為7.2、6.6及5.0 mmole/m3/d;平均滯留時間分別為1.3、1.5及2.7天。 | zh_TW |
dc.description.abstract | This study aims at the investigation of scavenging phenomenon by 234Th/238U disequilibria in the surface water of Taiwan Strait. Spatial sampling of 234Th was carried out by the Joint Hydrographic Survey during May 20~27, 2006. Along with 234Th measurement, basic hydrographic parameters (temperature, salinity, fluorescence and light transmission), total suspended matter concentration and particulate organic carbon concentration were also measured. The scavenging model incorporating the physical transport effect was used to estimate 234Th scavenging and removal rates in the region.
According to the distributions of hydrographic parameters and 234Th, five major domains in the Taiwan Strait can be identified: (Ⅰ) the Southern Taiwan Strait; (Ⅱ) the Taiwan Bank; (Ⅲ) the Cho-shuei River mouth; (Ⅳ) the Middle Taiwan Strait; and (Ⅴ) the Ming River mouth. The 234Th scavenging rates ranged from 57 to 520 dpm/m3/d. The Cho-shuei River mouth showed the highest scavenging rate, and the lowest scavenging rate was found in the Taiwan Bank. The 234Th removal rates ranged from 24 to 381 dpm/m3/d. The highest removal rate appeared in the Cho-shuei River mouth, and the lowest removal rate was found in the Ming River mouth. The residence times of dissolved and particulate 234Th in the Taiwan Strait were short, 0~6 and 1~3 days, respectively. Using 234Th as a proxy of particulate organic carbon, average removal rates of particulate organic carbon in the Cho-shuei River mouth, the Middle Taiwan Strait, and the Ming River mouth were 7.2, 6.6, and 5.0 mmole/m3/d, respectively. | en |
dc.description.provenance | Made available in DSpace on 2021-06-13T01:06:35Z (GMT). No. of bitstreams: 1 ntu-96-R94241406-1.pdf: 4667615 bytes, checksum: 5c0fe2745263c0d154e5116b1e79fd1d (MD5) Previous issue date: 2007 | en |
dc.description.tableofcontents | 論文口試委員審定書﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒Ⅰ
謝誌﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒Ⅱ 中文摘要﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒Ⅲ 英文摘要﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒Ⅳ 目錄﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒Ⅴ 圖目錄﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒Ⅶ 表目錄﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒Ⅸ 第一章 簡介﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒1 第二章 研究方法﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒9 2.1 探針資料﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒9 2.2 水樣分析﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒10 2.2.1 TSM濃度的分析步驟﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒10 2.2.2 DTh活度的分析步驟﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒10 2.2.3 PTh活度的分析步驟﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒12 2.2.4 DTh活度的計算﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒12 2.2.5 PTh活度的計算﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒13 2.2.6 POC濃度的分析步驟﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒14 第三章 結果與討論﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒16 3.1 臺灣海峽的環境特徵﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒16 3.1.1 臺灣海峽的水文型態﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒16 3.1.2 臺灣海峽顆粒成分的空間變化﹒﹒﹒﹒﹒﹒﹒17 3.2 臺灣海峽的清除機制﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒30 3.3 分佈係數﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒35 3.4 臺灣海峽的顆粒清除現象﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒39 3.4.1 二維不可逆清除模式﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒39 3.4.2 臺灣海峽的顆粒滯留時間﹒﹒﹒﹒﹒﹒﹒﹒﹒42 第四章 結論﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒49 參考文獻﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒﹒50 | |
dc.language.iso | zh-TW | |
dc.title | 臺灣海峽表層水體清除作用探討:釷-234/鈾-238不平衡應用 | zh_TW |
dc.title | Scavenging Phenomenon in the Taiwan Strait: 234Th/238U Disequilibria | en |
dc.type | Thesis | |
dc.date.schoolyear | 95-2 | |
dc.description.degree | 碩士 | |
dc.contributor.oralexamcommittee | 簡國童(Kuo-Tung Jiann),溫良碩(Liang-Saw Wen) | |
dc.subject.keyword | 臺灣海峽,清除作用,234Th,滯留時間,顆粒有機碳, | zh_TW |
dc.subject.keyword | Taiwan Strait,scavenging,234Th,residence time,particulate organic carbon, | en |
dc.relation.page | 54 | |
dc.rights.note | 有償授權 | |
dc.date.accepted | 2007-07-23 | |
dc.contributor.author-college | 理學院 | zh_TW |
dc.contributor.author-dept | 海洋研究所 | zh_TW |
顯示於系所單位: | 海洋研究所 |
文件中的檔案:
檔案 | 大小 | 格式 | |
---|---|---|---|
ntu-96-1.pdf 目前未授權公開取用 | 4.56 MB | Adobe PDF |
系統中的文件,除了特別指名其著作權條款之外,均受到著作權保護,並且保留所有的權利。