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长江口-杭州湾及其邻近海域不同粒级沉积有机碳分布特征
引用本文:章伟艳,金海燕,张富元,赵国军,杨克红,李宏亮,白有成,高为利.长江口-杭州湾及其邻近海域不同粒级沉积有机碳分布特征[J].地球科学进展,2009,24(11).
作者姓名:章伟艳  金海燕  张富元  赵国军  杨克红  李宏亮  白有成  高为利
作者单位:1. 国家海洋局第二海洋研究所,浙江,杭州,310012;国家海洋局海底科学重点实验室,浙江,杭州,310012
2. 国家海洋局第二海洋研究所,浙江,杭州,310012;国家海洋局海洋生物地球化学与生态系统重点实验室,浙江,杭州,310012
3. 浙江省水利水电设计研究院,浙江,杭州,310002
4. 国家海洋局第二海洋研究所,浙江,杭州,310012
基金项目:浙江省自然科学基金,国家自然科学基金,国家海洋局第二海洋研究所基本科研业务费专项资金项目,浙江省自然科学基金 
摘    要:通过对长江口、杭州湾、舟山海域及东海陆架4个海区表层沉积物样品的粒度敏感组分分析,发现东海陆架与长江口具有相似的三级组分物质组成,杭州湾与舟山海域具有相似的两级组分物质组成.综合4个区域粒级组分分布特征,采用湿分法将4个海域表层沉积物样品分成6个粒级:<0.004 mm,0.004~0.025 mm,0.025~0.063 mm,0.063~0.125 mm,0.125~0.250 mm和>0.250 mm,分别提取各级组分和全样进行有机碳及同位素测试.定量分析各级组分有机碳含量、来源及物质组分,除杭州湾海域粗粒级外,基本上<0.004 mm的粘土组分有机碳含量最高;富集在杭州湾海域粗颗粒中的有机质主要来源于陆源植物碎屑.沉积物颗粒大小、物质组成类型是不同粒级有机质富集的主要控制因素.

关 键 词:沉积物  粒度敏感组分  有机碳  有机碳同位素

Organic Carbon Distribution in the Yangtze River Estuary-Hangzhou Bay and Its Adjacent Sea Area
ZHANG Weiyan,JIN Haiyan,ZHANG Fuyuan,ZHAO Guojun,YANG Kehong,LI Hongliang,BAI Youcheng,GAO Weili.Organic Carbon Distribution in the Yangtze River Estuary-Hangzhou Bay and Its Adjacent Sea Area[J].Advance in Earth Sciences,2009,24(11).
Authors:ZHANG Weiyan  JIN Haiyan  ZHANG Fuyuan  ZHAO Guojun  YANG Kehong  LI Hongliang  BAI Youcheng  GAO Weili
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 rati-os( δ~(13)C_(org) ). The further quantitative analysis of TOC and δ~(13)C_(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.
Keywords:Sediment  Grain size sensitive compositions  Total organic carbon  Stable carbon isotopes
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