Particulate Phosphorus Input and Burial Efficiency in the Gaoping Coastal Sea

Autor: Yu-ching Yeh, 葉雨青
Rok vydání: 2009
Druh dokumentu: 學位論文 ; thesis
Popis: 97
The purposes of this study are to investigate the sources, distributions, fluxes and phosphorus burial efficiency (PBE) of particulate phosphorus in the Gaoping (GP) coastal sea. The GP River carried about 3.14 × 104 ton yr-1 (1.03 × 109 mol yr-1) particulate P into the GP coastal sea. The total P flux was primarily determined by the river runoff during the May-yu (monsoon) and typhoon seasons. The river P was approximately consisted of 90.8% particulate inorganic-P (PIP), 7.4% particulate organic-P (POP), 1.5% dissolved inorganic-P (DIP) and 0.3% dissolved organic-P (DOP). The particulate-P existed mainly in 10-63 μm particles. In the GP costal sea, particulate P in surface sediments was found to be 80-90% as PIP and 10-20% as POP. The highest distribution of PIP was located on the flanks of GP Canyon at the upper slope (200-600 m) region. This distribution may be caused by plumes of river sediments or turbidity currents overflowing the canyon. The sedimentation rates of sediments ranged from 0.032 to 1.62 g cm-2 yr-1 in the GP coastal sea and the highest rates were also located on both sides of the GP Canyon. The burial fluxes of total phosphorus (TP) ranged from 0.02 to 0.84 g cm-2 yr-1, consisted approximately by 88% PIP and 12% POP. The burial fluxes of this study area were generally similar to those in other continental margins (Bohai Sea, Yellow Sea, Mississippi Delta). The total depositions of sediment and TP were approximately 6.6 × 106 ton yr-1 and 4227 ton yr-1, respectively, in the study area. The burial TP was equivalent to 0.06% of deposited sediments. The buried TP can be proportionate approximately into 15% in the continental shelf (< 200 m), 69% in the continental slope (200-1000 m), and 16% in the slope basin (> 1000 m). The continental shelf
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