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三峡水库小江回水区春季初级生产力

郭劲松 李伟 李哲 孙志禹 陈永柏 龙曼 陈杰

湖泊科学2011,Vol.23Issue(4):591-596,6.
湖泊科学2011,Vol.23Issue(4):591-596,6.

三峡水库小江回水区春季初级生产力

Spring primary productivity in Xiaojiang River backwater area in the Three Gorges Reservoir

郭劲松 1李伟 1李哲 1孙志禹 2陈永柏 2龙曼 1陈杰3

作者信息

  • 1. 重庆大学城市建设与环境工程学院,重庆400045
  • 2. 中国长江三峡集团公司,宜昌443002
  • 3. 林同棪国际工程咨询(中国)有限公司,重庆401121
  • 折叠

摘要

Abstract

During April and May in 2010, the primary production in the Xiaojiang River backwater area, Three Gorges Reservoir was measured using the black-white-bottle method. The distribution features and relationships with light intensity, chlorophyll-a concentration(Chl. A) , water temperature and partial pressure of carbon dioxide(pCO2 ) were studied. The results showed that the gross primary productivities(GPP) were 1927.5 mg O2/( m2 ? D) and 1325.0 mg O2/( m2 ? D) in April and May, respectively, the average value was 1626.3 mg O2/(m2 ? D). The gross respirations(GR) in the two months were 1037.5 mg O2/( m2 ? D) and 1062.5 mg O2/m2 ? D, respectively, and the average value was 1050.0 mg O2/(m2 ? D). The gross net productivities (GNP) in the two months were 890.0 mg O2/( m2 ? D) and 262.5 mg O2/(m2 ? D) , and the average value was 576.3 mg O2/ ( m2 ? D). Ratio of GPP/GR were 1.86 and 1.25. These indexes suggested that the Xiaojiang River was autotrophic in the spring season. Primary productivity(P) in each depth and the ratio of productivity to respiration(P/R) had similar vertical distribution feature, showing that the maximum values occurred near the surface and they decreased with depth. Correlation analysis showed that light intensity(I) and Chl. A were significantly positive correlation with the P. Equations of the linear regression model P with Chl. A and with /were respectively: P =0.154 Chi. A -0.278, with coefficient R2 =0.570, and P =0.001 /-0.013, with coefficient R2 =0.942.

关键词

三峡水库/小江/浮游植物/初级生产力

Key words

Three Gorges Reservoir/ Xiaojiang River/ phytoplankton/ primary productivity

引用本文复制引用

郭劲松,李伟,李哲,孙志禹,陈永柏,龙曼,陈杰..三峡水库小江回水区春季初级生产力[J].湖泊科学,2011,23(4):591-596,6.

基金项目

国家自然科学基金项目(51009155)、国家“973”计划项目(2010CB955904-02)、中国长江三峡集团公司项目(CT-09-08-03)和中央高校基本科研业务费科研专项“研究生科技创新基金”(CDJXS10211153)联合资助 (51009155)

湖泊科学

OA北大核心CSCDCSTPCD

1003-5427

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