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Continuous flow analysis of dissolved total phosphorus in seawater by UVK_(2)S_(2)O_(8) online digestion method 被引量:1
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作者 YUZhigang RAABEThomas +1 位作者 HEMKENGitta BROCKMANNUwe 《Acta Oceanologica Sinica》 SCIE CAS CSCD 2004年第4期637-645,共9页
Several methods for analysis of dissolved total phosphorus in seawater were reviewed. Discussions were focused on UVirradiation and persulphate oxidation methods which are the most popular dissolved organic phosphorus... Several methods for analysis of dissolved total phosphorus in seawater were reviewed. Discussions were focused on UVirradiation and persulphate oxidation methods which are the most popular dissolved organic phosphorus determinationmethods presently. The compounds used for the phosphorus recovery test were categorized into three groups accordingto their chemical structure. It was found that low power UV irradiation can decompose POC or PC bonds efficientlybut may be inefficient for POP bonds. Heating-bath in acid condition is useful for decomposing POP bonds. Usingthe continuous flow analysis system (Auto-analyzer II), UV digestion and heating-bath, series experiments were carriedout based on the above analysis. Eleven model compounds were employed for the phosphorus recovery test and thefactors influencing the decomposition efficiency of dissolved compounds containing phosphorus were clarified. Finally,the optimal design for determination of dissolved total phosphorus in seawater based on the routine continuous flowanalysis system was presented. For the organic mono-phosphate, the recovery is more than 90% and a recovery of33%~51% was obtained for inorganic or organic polyphosphates. Up to now, this is the highest decompositionefficiency for dissolved phosphorus based on the continuous flow analysis system. 展开更多
关键词 dissolved total phosphorus organic phosphorus ultraviolt persulfate potassium continuous flow analysis
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LATE QUATERNARY SEISMIC SEQUENCES AND SEDIMENTATION ALONG THE COAST OFF TAISHAN,GUANGDONG,AS REVEALED BY HIGH RESOLUTION SEISMIC DATA
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作者 吴时国 黄孝健 《Chinese Journal of Oceanology and Limnology》 SCIE CAS CSCD 2002年第3期270-276,共7页
Seismic stratigraphic analysis of 150 km of high resolution seismic profiles (GEOPULSE and 3.5 kHz) obtained along the muddy coast off Taishan, Guangdong provided valuable information on the offshore Quaternary strati... Seismic stratigraphic analysis of 150 km of high resolution seismic profiles (GEOPULSE and 3.5 kHz) obtained along the muddy coast off Taishan, Guangdong provided valuable information on the offshore Quaternary stratigraphy, tectonics, sedimentary evolution, and environmental and engineering geology of this area.The following late Quaternary stratigraphic sequences were mapped. (1) Pleistocene alluvial silty sand and shallow marine clay; (2) coarse fluvial channel sand; (3) nearshore and bay clayey sediments. The incision of fluvial channels occurred in two stages: during the Late Pleistocene and at the beginning of the Holocene. The Pleistocene fluvial channels have been filled by coarse sand overlain by more than 10 m of late Pleistocene clay and 20-30 m of Holocene clay.The coastal area is dissected by two major fault systems: the first group strikes ENE-WSW and controls the evolution of the adjacent Quaternary basin, while the second one trends NNE-SSW. These fault systems must be taken into account in any coastal engineering considerations. In addition, both granitic and metamorphic basements were recognized. 展开更多
关键词 地震序列 沉降 地震资料 台山 广东
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基于沉积物捕获器的南海表层初级生产力及输出生产力估算 被引量:29
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作者 陈建芳 郑连福 +3 位作者 M.G.Wiesner 陈荣华 郑玉龙 H.K.Wong 《科学通报》 EI CAS CSCD 北大核心 1998年第6期639-642,共4页
南海时间系列沉积物捕获器研究结果初步表明 ,南海颗粒有机碳通量受季风影响 ,其中北部的高生产力主要与东北季风有关 ,而南海中部除受东北季风影响之外 ,则更体现受西南季风的影响 .据颗粒有机碳通量估算的初级生产力和表层输出生产力... 南海时间系列沉积物捕获器研究结果初步表明 ,南海颗粒有机碳通量受季风影响 ,其中北部的高生产力主要与东北季风有关 ,而南海中部除受东北季风影响之外 ,则更体现受西南季风的影响 .据颗粒有机碳通量估算的初级生产力和表层输出生产力分别为 53.0~ 6 3.4 gC·m- 2 ·a- 1和 10 .32~ 12 .93gC·m- 2 ·a- 1.季风期间生产力与颗粒有机碳通量的增高在某种程度上说明了南海盛冰期时古生产力的增高可能是由于当时季风加强的结果 . 展开更多
关键词 南海 沉积物捕获器 初级生产力 输出生产力
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南海颗粒有机碳通量的垂向变化及早期降解作用的标志物 被引量:15
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作者 陈建芳 M.G.Wiesner +3 位作者 H.K.Wong 郑连福 郑士龙 徐鲁强 《中国科学(D辑)》 CSCD 1999年第4期372-378,共7页
南海不同水层的颗粒有机碳通量与表层沉积物有机碳积累率的对比 ,以及氨基酸、氨基糖、糖类物质的组成变化表明 ,南海水柱中的颗粒有机碳主要来源于近期生长的海洋浮游生物 ,仅有 1.4%~ 1.6 %初级生产力产生的有机碳进入深海水柱 ,而... 南海不同水层的颗粒有机碳通量与表层沉积物有机碳积累率的对比 ,以及氨基酸、氨基糖、糖类物质的组成变化表明 ,南海水柱中的颗粒有机碳主要来源于近期生长的海洋浮游生物 ,仅有 1.4%~ 1.6 %初级生产力产生的有机碳进入深海水柱 ,而在深海盆地沉积物中积累的有机碳仅占初级生产力的 0 .2 2 %以下 .颗粒有机物通量与组成改变主要发生在表层数百米以及底层海水与沉积物界面之间 ,而在中下水层变化较小 . (TAA+TSUG)OC ,AA/AS ,Gluam/Galam ,Arom .AA/Non Prot.AA ,ASP/b ALA ,GLU/g ABA等指标在颗粒物沉积过程中逐渐减少 。 展开更多
关键词 颗粒有机碳 南海 海洋 早期降解作用 南海
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