水库调控下黄河口沉积有机碳的分布、来源与输运特征

党瑶, 刘夙睿, 王厚杰, 卢泰安, 吴晓, 毕乃双, 胡利民. 水库调控下黄河口沉积有机碳的分布、来源与输运特征[J]. 海洋地质与第四纪地质, 2024, 44(2): 120-130. doi: 10.16562/j.cnki.0256-1492.2023012401
引用本文: 党瑶, 刘夙睿, 王厚杰, 卢泰安, 吴晓, 毕乃双, 胡利民. 水库调控下黄河口沉积有机碳的分布、来源与输运特征[J]. 海洋地质与第四纪地质, 2024, 44(2): 120-130. doi: 10.16562/j.cnki.0256-1492.2023012401
DANG Yao, LIU Surui, WANG Houjie, LU Taian, WU Xiao, BI Naishuang, HU Limin. Distribution, source, and transport of particulate organic carbon in the Yellow River estuary as affected by the water-sediment regulation[J]. Marine Geology & Quaternary Geology, 2024, 44(2): 120-130. doi: 10.16562/j.cnki.0256-1492.2023012401
Citation: DANG Yao, LIU Surui, WANG Houjie, LU Taian, WU Xiao, BI Naishuang, HU Limin. Distribution, source, and transport of particulate organic carbon in the Yellow River estuary as affected by the water-sediment regulation[J]. Marine Geology & Quaternary Geology, 2024, 44(2): 120-130. doi: 10.16562/j.cnki.0256-1492.2023012401

水库调控下黄河口沉积有机碳的分布、来源与输运特征

  • 基金项目: 国家自然科学基金“黄河流域生态系统变化与生态屏障效应”(42041005),“黄河口关键过程及物质输运协同效应重大科学考察实验研究”(42149301);山东省泰山学者项目(ZR2018BD028, TSQN202211054);山东省高等学校“青创团队计划”团队项目(2022KJ045);东营市市校合作重点项目“黄河三角洲海岸非均衡演化及应对策略”(SXHZ-2022-02-15);中央高校基本科研业务费专项“人新世河口海岸”(202241007)
详细信息
    作者简介: 党瑶(1998—),女,硕士研究生,地质学专业,E-mail:364906824@qq.com
    通讯作者: 王厚杰(1972—),男,教授,主要从事近海沉积动力学研究,E-mail:hjwang@mail.ouc.edu.cn
  • 中图分类号: P736.21

Distribution, source, and transport of particulate organic carbon in the Yellow River estuary as affected by the water-sediment regulation

More Information
  • 黄河是全球输沙量最大的河流之一,陆源颗粒有机碳通量高。然而,近年来流域水库调控对黄河下游水文格局和颗粒有机碳输送产生了重要影响,小浪底水库调水调沙时期成为黄河水沙和有机碳入海的关键时段。为揭示水库调控对河口水动力和有机碳分布的影响机制,基于2020年7月调水期和调沙期黄河口的水动力观测结果,结合沉积物有机碳测试结果,研究了水库调控不同阶段下河口沉积物粒度参数和表层沉积物有机碳的时空分布。研究结果表明,水库不同阶段下悬浮颗粒物的物源和主要扩散、沉积区域的变化,使得黄河口表层沉积物的粒度组成特征发生明显变化;在高径流量的调水期期间,粗颗粒泥沙携带颗粒有机碳在河口距离口门12 km范围内大量埋藏,河口区域表层沉积物的有机碳含量相较于调沙期明显偏低。调水期黄河口陆源有机碳主要来自下游河床冲刷,颗粒较粗,调沙期则转变为水库释放的细颗粒有机碳和流域C3维管植物碎屑。水库调控的不同阶段使得黄河下游河流水动力格局和泥沙运输机制改变,从而引起黄河口沉积有机碳来源和分布的显著变化。因此,人类活动对调节有机碳向海洋的输送及其在近岸海域的分布具有主导性作用。

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  • 图 1  黄河口概况与调水期(a)和调沙期(b)的调查站位分布

    Figure 1. 

    图 2  利津水文站2020年调水调沙期间流量(Q)和悬浮颗粒物浓度(SSC)(a)及粒度参数变化(b)

    Figure 2. 

    图 3  调水期和调沙期期间黄河口表层沉积物中值粒径(D50)时空分布

    Figure 3. 

    图 4  调水调沙期间黄河口表层沉积物各粒级组分百分含量时空分布

    Figure 4. 

    图 5  调水调沙期间黄河口表层沉积物有机碳含量(TOC)、碳稳定同位素(δ13C)和碳氮比(C/N)时空分布

    Figure 5. 

    图 6  调水期与调沙期表层沉积物TOC与中值粒径分布散点图

    Figure 6. 

    图 7  调水期和调沙期黄河口表层沉积物各组分有机碳贡献分布图

    Figure 7. 

    表 1  TOC含量与各粒级组分含量相关性分析

    Table 1.  Correlations of TOC content and each fractional percentage of sediment

    不同时期黄河口表层沉积物TOC含量砂含量
    粉砂含量
    黏土含量
    调水期−0.540.100.75**
    调沙期−0.90**0.500.94**
    注:*为 p<0.05,** 为p<0.01。
    下载: 导出CSV
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收稿日期:  2023-01-24
修回日期:  2023-03-11
刊出日期:  2024-04-28

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