海洋沉积有机物质的降解及其模式

蒋宇轩, 邢磊, 张海龙, 姜一晴, 赵美训. 海洋沉积有机物质的降解及其模式[J]. 海洋地质与第四纪地质, 2014, 34(4): 173-180. doi: 10.3724/SP.J.1140.2014.04173
引用本文: 蒋宇轩, 邢磊, 张海龙, 姜一晴, 赵美训. 海洋沉积有机物质的降解及其模式[J]. 海洋地质与第四纪地质, 2014, 34(4): 173-180. doi: 10.3724/SP.J.1140.2014.04173
JIANG Yuxuan, XING Lei, ZHANG Hailong, JIANG Yiqing, ZHAO Meixun. STUDY ON THE DEGRADATION OF MARINE SEDIMENTARY ORGANIC MATTER AND MODEL DEVELOPMENT[J]. Marine Geology & Quaternary Geology, 2014, 34(4): 173-180. doi: 10.3724/SP.J.1140.2014.04173
Citation: JIANG Yuxuan, XING Lei, ZHANG Hailong, JIANG Yiqing, ZHAO Meixun. STUDY ON THE DEGRADATION OF MARINE SEDIMENTARY ORGANIC MATTER AND MODEL DEVELOPMENT[J]. Marine Geology & Quaternary Geology, 2014, 34(4): 173-180. doi: 10.3724/SP.J.1140.2014.04173

海洋沉积有机物质的降解及其模式

  • 基金项目:

    国家自然科学基金项目(41276068,41020164005)

    国家重点基础研究发展规划项目(2010CB428901)

详细信息
    作者简介: 蒋宇轩(1987-),男,硕士生,海洋化学专业,Email:moonrisegw@163.com
  • 中图分类号: P736.4

STUDY ON THE DEGRADATION OF MARINE SEDIMENTARY ORGANIC MATTER AND MODEL DEVELOPMENT

  • 作为长期碳汇,海洋沉积物中埋藏的大量有机碳对全球碳循环和气候变化有重要影响。有机碳从海洋输出到沉积物中后,在沉积物中还要经历有氧降解和无氧降解。有机物降解是一个十分复杂的过程,影响这一过程的因素有很多,包括有机物本身的分子结构和组成种类;氧化还原状态;有机物所附着的基质;温度、压力、盐度等物理环境因素以及生物因素。研究沉积有机碳的含量及埋藏量变化首先需要校正降解对沉积有机碳含量的影响。降解模式是定量估算降解对沉积有机碳的影响的一个主要手段。在前人的研究基础上,讨论了影响沉积有机碳降解的因素,对降解模式的研究进展和应用进行了综述,提出了未来降解模式的发展中存在的问题。
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出版历程
收稿日期:  2013-08-29
修回日期:  2013-10-02

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