摘要
１９９７ 年７ 月份（ 汛期） 和１１ 月份（ 平水期） 对北江河口站和西江马口站水体有机碳含量进行了两次采样分析。结果表明：两江水体的颗粒有机碳含量在不同季节均高于溶解有机碳含量（ 本文用近似值ＤＯＣ＋ 代替ＤＯＣ） ，这与全球河流以溶解有机碳为主的平均格局显著不同。溶解有机碳、颗粒有机碳含量以及总有机碳含量均随水文季节的变化而变化，汛期含量高于平水期。悬浮物中有机碳的含量随悬浮物含量的增加，也即流域土壤机械侵蚀强度的加强而降低，这种现象与全球河流的总体趋势一致。汛期水体颗粒物中自源有机碳的贡献量高于平水期。
Water samples were collected in high water season (July, 1997) and middle water season (October, 1997) from two main lower reach gauge stations of the Pearl River, namely Hekou and Makou, respectively. Content of particulate organic carbon is always higher than that of dissolved organic carbon in both seasons, which is obviously different from the global average pattern, i.e., dissolved organic carbon is the dominate composition of the riverine transported organic carbon. The contents of dissolved and particulate organic carbon change with the water levels in a direct ratio. The percentage of organic carbon in total suspended substance changes with the content of total suspended substance in an inverse ratio. The more intense is the soil erosion in the drainage, the more concentrated is the riverine organic carbon in the river. The contribution of autochthonous organic carbon is larger in high water season than in middle water season.
出处
《地球化学》
CAS
CSCD
北大核心
1999年第3期273-280,共8页
Geochimica
基金
中国科学院资源与生态环境研究重点项目!( 编号:KZ952J1402)
有机地球化学国家重点实验室开放基金
国家自然科学基金
关键词
有机碳通量
季节变化
土壤侵蚀
珠江
水体
organic carbon flux, seasonal variation, soil erosion, Pearl River
