Articles

Organic Carbon Distribution in the Yangtze River Estuary-Hangzhou Bay and Its Adjacent Sea Area

Expand
  • 1.Second Institute of Oceangraphy of SOA, Hangzhou310012, China;2.Laboratory of Submarine Geosciences, SOA, Hangzhou310012, China;3.Laboratory of Marine Ecosystem and Biogeochemistry of SOA, Hangzhou310012,China;4.Water Conservancy and Hydropower Survey and Design Institute of Zhejiang Province, Hangzhou310002,China

Received date: 2009-06-12

  Revised date: 2009-08-28

  Online published: 2009-11-10

Abstract

A study of environmentally sensitive grain-size population was used by the grain size class vs standard deviation values of the surface sediment samples in the Yangtze River Estuary, Hangzhou Bay, Zhoushan archipelago sea area and the East China Sea shelf. Results indicated that there were three similar grain size populations between the East China Sea shelf and the Yangtze River estuary and two similar populations between the Hangzhou Bay and the Zhoushan archipelago sea area. According to the environmentally sensitive grain-size population, wet sieving was performed to separate the four area sediments into six size fractions (>0.250 mm, 0.125~0.250 mm, 0.063~0.125 mm, 0.025~0.063 mm, 0.004~0.025 mm, and <0.004 mm). Each of these size fractions and the bulk samples were analyzed for the total organic carbon(TOC) and stable organic carbon isotopic ratios(δ13C org). The further quantitative analysis of TOC and δ13C org for each fraction indicated that there was the highest TOC content in the <0.004 mm fraction except the coarse size fractions of the Hangzhou bay where they were rich in the organic matter from the terrestrial source plant debris, and the particle size and type of the sediment component played important role in the organic matter distribution.

Cite this article

ZHANG Weiyan, JIN Haiyan,ZHANG Fuyuan, ZHAO Guojun,YANG Kehong, LI Hongli . Organic Carbon Distribution in the Yangtze River Estuary-Hangzhou Bay and Its Adjacent Sea Area[J]. Advances in Earth Science, 2009 , 24(11) : 1202 -1209 . DOI: 10.11867/j.issn.1001-8166.2009.11.1202

References


[1] Lu Longfei, Cai Jingong, Bao Yujin,et al. Summary of processes and significance of clay minerals in marine sedimentary organic matter preservation and in global carbon cycle
[J].Advances in Earth Science,2006,21(9):931-937.
[卢龙飞,蔡进功,包于进,等.粘土矿物保存海洋沉积有机质研究进展及其碳循环意义
[J].地球科学进展,2006,21(9):931-937.]

[2] Lin S W, Hsieh I-Jy, Huang K M,et al. Influence of the Yangtze River and grain size on the spatial variations of heavy metals and organic carbon in the East China Sea continental shelf sediments
[J].Chemical Geology,2002, 182:377-394.

[3] Milliman J D,Xie Q C,Yang Z S.Transfer of particulate organic carbon and nitrogen from the Yangtze River to ocean
[J].American Journal of Science,1984,284:824-834.

[4] Edmond J M,Spivack A,Grant B C, et al. Chemical dynamics of the Changjiang Estuary
[J].Continental Shelf Research,1985,4:17-36.

[5] Tan F C,Cai D L,Edmond J M.Carbon isotope geochemistry of the Changjiang Estuary
[J].Estuary Coastal and Shelf Science,1991,32:395-403.

[6] Cai D L,Han Y B.Carbon isotopic composition and flux of particulate organic matter in the Changjiang
[J].Acta Oceanology Sinica,1998,17:337-342.

[7] Wu Y, Zhang J, Liu S M, et al. Sources and distribution of carbon within the Yangtze River system
[J].Estuarine Coastal and Shelf Science,2007,71:13-25.

[8] Wu Y, Dittmar T, Ludwichowski K U, et al. Tracing suspended organic nitrogen from the Yangtze River catchments into the East China Sea
[J].Marine Chemistry,2007,107:367-377.

[9] Zhang J,Wu Y,Jennerjahn,T C, et al. Distribution of organic matter in the Changjiang (Yangtze River) Estuary and their stable carbon and nitrogen isotopic ratios: Implications for source discrimination and sedimentary dynamics
[J].Marine Chemistry, 2007, 106:111-126.

[10] Gao Jianhua,Wang Yaping,Pan Shaoming,et al. Source and Distribution of organic matter in seabed sediments of the Changjiang River estuary and its adjacent sea area
[J].Acta Geographica Sinica,2007,62(9):981-991.
[高建华,汪亚平,潘少明,等.长江口外海域沉积物中有机物的来源及分布
[J].地理学报,2007,62(9): 981-991.]

[11] Lü Xiaoxia,Zhai Shikui,Niu Lifeng.Study on the C/N ratios of orgaic matters in the core sediments of the Yangtze River Estuary
[J].Environmental Chemistry,2005,24(3):255-259.
[吕晓霞,翟世奎,牛丽凤.长江口柱状沉积物中有机质C/N比的研究
[J].环境化学,2005,24(3):255-259.]

[12] Chen Qingqiang, Meng Yi, Zhou Juzhen,et al. Constraints for distribution of soil organic carbon with depth due to evolution of the salt marsh in the Yangtze River Estuary
[J].Advances in Earth Science,2007,22(1):26-32.
[陈庆强,孟翊,周菊珍,等.长江口盐沼滩面发育对有机碳深度分布的制约
[J].地球科学进展,2007,22(1):26-32.]

[13] Zhao Yiyang,Yan Mingcai. Geochemistry of Sediments of the China Shelf Sea
[M].Beijing:Science Press,1994:203.
[赵一阳,鄢明才.中国浅海沉积物地球化学
[M].北京:科学出版社,1994:203.]

[14] Fan Dejiang,Yang Zuosheng,Sun Xiaogong,et al. Quantitative evaluation of sediment provenance on the north area of the East China Sea Shelf
[J].Journal of Ocean University of Qingdao,2002:748-756.
[范德江,杨作升,孙效功,等.东海陆架北部长江、黄河沉积物影响范围的定量估算
[J].青岛海洋大学学报,2002:748-756.]

[15] Wu Ying, Zhang Jing, Zhang Zaifeng, et al. Seasonal variability of stable carbon and nitrogen isotope of suspended particulate matter in the Changjiang River
[J].Oceanologia et Limnologia Sinica,2002,33(5):546-552.
[吴莹,张经,张再峰,等.长江悬浮颗粒物中稳定碳、氮同位素的季节分布
[J].海洋与湖沼,2002,33(5):546-552.]

[16] Cai Deling, Tan F C, Edmond J M. Organic carbon isotope geochemistry of the Changjiang (Yangtze River) estuary
[J].Geochimica,1992,(3):305-312.
[蔡德陵,Tan F C,Edmond J M.长江口区有机碳同位素地球化学
[J].地球化学,1992,(3):305-312.]

[17] Minoura K, Hoshino K, Nakamura T, et al. Late Pleistocene—Holocene paleoproductivity circulation in the Japan Sea: Sea-level control on δ13C and δ15N records of sediment organic material
[J].Palaeogeography, Palaeoclimatology Palaeoecology,1997,135:41-50.

Outlines

/