Preliminary study on the dissolved and colloidal organic carbon in the Zhujiang River estuary[J]. 海洋湖沼学报(英文), 2000,18(3):265-273.
Min-han, D., Martin, JM., Hua-sheng, H. et al. Preliminary study on the dissolved and colloidal organic carbon in the Zhujiang River estuary., Chin. J. Ocean. Limnol. 18, 265–273 (2000). https://doi.org/10.1007/BF02842674
Preliminary study on the dissolved and colloidal organic carbon in the Zhujiang River estuary[J]. 海洋湖沼学报(英文), 2000,18(3):265-273. DOI: 10.1007/BF02842674.
Min-han, D., Martin, JM., Hua-sheng, H. et al. Preliminary study on the dissolved and colloidal organic carbon in the Zhujiang River estuary., Chin. J. Ocean. Limnol. 18, 265–273 (2000). https://doi.org/10.1007/BF02842674DOI:
Preliminary study on the dissolved and colloidal organic carbon in the Zhujiang River estuary
摘要
Abstract
This paper reports data on the dissolved and colloidal organic carbon in the Zhujiang (Pearl) River estuary. DOC concentration was 142 to 239 μmol/L in the freshwater taken in March 1997 from the four Zhujiang River tributaries flowing into the Lingdingyang estuary. High concentration was observed in the Humen tributary located near Guangzhou. The rapidly increased DOC concentration at low salinities (∼5) may be attributed to the exchange between macroparticulate and dissolved organic matter during the early stage of estuarine mixing. DOC concentration overall followed the mixing line until salinity 25
where the Deep Bay is located and where DOC was elevated. This elevated DOC may suggest a local organic matter source from Shenzhen. Using a cross-flow ultrafiltration (CFF) system equipped with a Millipore Prep-scale CFF 1 kD regenerated cellulose membrane
we also separated the colloidal organic matter from the truly dissolved fraction (<1 kD). CFF membranes were carefully evaluated for their applicability (retention characteristics
blank level and mass balance) to separate colloidal organic matter. COC in the study area ranged from 5 to 85 μmol/L
representing 3%–32% of DOC. The highest COC percentage was found at low salinities (<5) in both winter and summer. Evidence suggests in-situ production of colloidal material at this salinity range. Beyond this point
a very modest removal was observable until high salinities. Again
an increase in COC concentration was shown in the samples taken from the Deep Bay.
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references
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相关作者
Ping XU
Fanxiang KONG
Qingfei ZENG
Min ZHANG
Xiaoli SHI
Yuanfeng CAI
Limei SHI
Yunni GAO
相关机构
The Philips Institute of Oral and Craniofacial Molecular Biology, Virginia Commonwealth University, Richmond, VA 23298-0566, United States of America
State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences
State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences
Australian Rivers Institute, Griffith University, Nathan
Engineering Lab of Henan Province for Aquatic Animal Disease Control, Engineering Technology Research Center of Henan Province for Aquatic Animal Cultivation, College of Fisheries, Henan Normal University