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春季黄东海颗粒有机碳的时空分布特征
引用本文:程君,石晓勇,张传松,王丽莎,黄爽,刘东生.春季黄东海颗粒有机碳的时空分布特征[J].环境科学,2011,32(9):2505-2511.
作者姓名:程君  石晓勇  张传松  王丽莎  黄爽  刘东生
作者单位:中国海洋大学海洋污染生态化学实验室,青岛 266100;中国海洋大学海洋污染生态化学实验室,青岛 266100;中国海洋大学海洋污染生态化学实验室,青岛 266100;中国海洋大学海洋污染生态化学实验室,青岛 266100;中国海洋大学海洋污染生态化学实验室,青岛 266100;中国海洋大学海洋污染生态化学实验室,青岛 266100
基金项目:国家海洋局公益性项目(200805065); 国家重点基础研究发展规划(973)项目(2010CB428701)
摘    要:根据2009年4~5月对黄东海大面积调查的资料,分析研究了黄东海颗粒有机碳(particulate organic carbon,POC)的浓度和时空分布特征,并结合叶绿素(Chlorophyll a,Chl-a)和C/N摩尔比值探讨了POC的主要来源.结果表明,春季黄东海POC的浓度范围是24.33~2 817.29...

关 键 词:颗粒有机碳  分布特征  周日变化  来源  黄东海
收稿时间:2010/10/22 0:00:00
修稿时间:2010/12/15 0:00:00

Temporal and Spatial Distribution of Particulate Organic Carbon in the Yellow Sea and East China Sea in Spring
CHENG Jun,SHI Xiao-yong,ZHANG Chuan-song,WANG Li-sh,HUANG Shuang and LIU Dong-sheng.Temporal and Spatial Distribution of Particulate Organic Carbon in the Yellow Sea and East China Sea in Spring[J].Chinese Journal of Environmental Science,2011,32(9):2505-2511.
Authors:CHENG Jun  SHI Xiao-yong  ZHANG Chuan-song  WANG Li-sh  HUANG Shuang and LIU Dong-sheng
Institution:CHENG Jun,SHI Xiao-yong,ZHANG Chuan-song,WANG Li-sha,HUANG Shuang,LIU Dong-sheng(Laboratory of Marine Pollution Ecological Chemistry,Ocean University of China,Qingdao 266100,China)
Abstract:Based on the data from cruises that carried out in the Yellow Sea and East China Sea from April to May, 2009, the temporal and spatial distributions of the particulate organic carbon (POC) were analyzed. And the sources of POC were further discussed according to the chlorophyll a (Chl-a) and C/N. The results showed that the concentration of POC in the Yellow Sea and East China Sea ranged from 24.33 microg/L to 2 817.29 microg/L in spring and the average content was 230.76 microg/L. In horizontal distribution, the highest POC content is in the coastal zones and it tends to decrease toward the far shore on the whole. The highest concentration of POC appears at the northern of Jiangsu Province coastal waters both in surface layer and bottom layer in particular, which is mainly affected by resuspension of sediments. And there is also a second highest concentration in the vicinity of the Yangtze River estuary, indicating the primary influence in the Yangtze River is by diluted water. The concentration of POC in shallow sea area is the highest and distributed uniformly and it is primarily from terrestrial inputs and resuspension. Moreover, the resuspension is relatively stronger than terrestrial inputs. However, the POC concentration in far coast deep water area is under 75 microg/L and it reduces gradually with the increase of water depth, which shows ocean water characteristics. And the POC is mainly from the ocean. The diurnal change of POC concentration in the middle of East Sea shows half-cycle variation, as a whole, the concentration value is high both in the afternoon and midnight, while it is relatively low at dusk, which is mainly under the influence of biological activity at the scene.
Keywords:particulate organic carbon (POC)  distribution  diurnal change  source  the Yellow Sea and East China Sea
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