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黄河故道区晚全新世沉积记录及其对洪水灾害事件的响应

杨劲松, 刘林敬, 赵华, 刘哲, 宋磊, 张鹏, 唐亮. 2023. 黄河故道区晚全新世沉积记录及其对洪水灾害事件的响应[J]. 中国地质, 50(4): 1004-1015. doi: 10.12029/gc20220323001
引用本文: 杨劲松, 刘林敬, 赵华, 刘哲, 宋磊, 张鹏, 唐亮. 2023. 黄河故道区晚全新世沉积记录及其对洪水灾害事件的响应[J]. 中国地质, 50(4): 1004-1015. doi: 10.12029/gc20220323001
YANG Jinsong, LIU Linjing, ZHAO Hua, LIU Zhe, SONG Lei, ZHANG Peng, TANG Liang. 2023. Late Holocene sedimentary records along the abandoned channel areas of the Yellow River and their response to flood hazards[J]. Geology in China, 50(4): 1004-1015. doi: 10.12029/gc20220323001
Citation: YANG Jinsong, LIU Linjing, ZHAO Hua, LIU Zhe, SONG Lei, ZHANG Peng, TANG Liang. 2023. Late Holocene sedimentary records along the abandoned channel areas of the Yellow River and their response to flood hazards[J]. Geology in China, 50(4): 1004-1015. doi: 10.12029/gc20220323001

黄河故道区晚全新世沉积记录及其对洪水灾害事件的响应

  • 基金项目:
    国家自然科学基金项目(41807428)、河北省自然科学基金(D2020504008)和中国地质科学院基本科研业务费项目(YK202308)共同资助
详细信息
    作者简介: 杨劲松,男,1987年生,副研究员,从事第四纪地质调查与环境演变研究;E-mail:yangjinsong@mail.cgs.gov.cn
    通讯作者: 刘林敬,男,1982年生,高级工程师,从事第四纪地质调查与环境演变研究;E-mail:liulinjing@mail.cgs.gov.cn
  • 中图分类号: P512.2;TV122.2

Late Holocene sedimentary records along the abandoned channel areas of the Yellow River and their response to flood hazards

  • Fund Project: Supported by the National Natural Science Foundation of China (No. 41807428), the Natural Science Foundation of Hebei Province (No. D2020504008), and the Basic Research Program of Chinese Academy of Geological Sciences (No.YK202308)
More Information
    Author Bio: YANG Jinsong, male, born in 1987, associate researcher, engaged in environmental evolution research; E-mail: yangjinsong@mail.cgs.gov.cn .
    Corresponding author: LIU Linjing, male, born in 1982, senior engineer, engaged in Quaternary research; E- mail: liulinjing@mail.cgs.gov.cn
  • 研究目的

    黄河故道区蕴藏了丰富的古洪水灾害信息,深入挖掘地层中相应的沉积记录,有助于扩展黄河流域洪水记录的时空范围,增进对洪水灾害的科学认识。

    研究方法

    本文选取河北大名龙王庙剖面作为黄河故道区的典型代表剖面,利用光释光、14C、粒度和地球化学元素等测试手段,综合对比洪水史料记载与区域研究成果。

    研究结果

    研究认为:(1)古土壤、湖沼相沉积、泛滥沉积与平流沉积物之间存在一定的继承性与相关性;(2)晚全新世以来研究区内4次主要的洪水沉积单元,分别对应了周、西汉、北宋和明朝的异常洪水事件;(3)人类活动对流域洪水灾害产生了一定的影响,由高频低能的季节性洪水转变为低频高能的异常洪水事件。

    结论

    该项研究基本查明了黄河故道区不同沉积相的岩性特征及环境代用指标特征,探讨了人类活动对洪水特征的影响,为黄河故道区洪水灾害沉积记录的判别与重建提供了理论参考和示范,同时有助于进一步深入认识黄河流域洪水灾害的过程及演化机制。

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  • 图 1  研究区区域位置图

    Figure 1. 

    图 2  LWM剖面粒度参数及不同粒级含量变化曲线(灰色阴影部分表示异常洪水单元下部的古洪水平流沉积层)

    Figure 2. 

    图 3  LWM剖面常量元素及主成分变化曲线(图例同图 2

    Figure 3. 

    图 4  LWM剖面各沉积相粒度C-M图

    Figure 4. 

    图 5  LWM剖面各沉积相的主成分聚点分析图

    Figure 5. 

    图 6  黄河故道区古洪水沉积剖面对比图

    Figure 6. 

    表 1  LWM地层划分及岩性描述

    Table 1.  Stratigraphic descriptions and subdivision units of the LWM profile

    下载: 导出CSV

    表 2  LWM剖面主量元素指标PC1和PC2与元素变量的相关系数

    Table 2.  Correlations between the first two principal components and major elements in LWM profile

    下载: 导出CSV

    表 3  LWM剖面AMS-14C和OSL测年结果

    Table 3.  AMS-14C and OSL dating results in LWM profile

    下载: 导出CSV
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出版历程
收稿日期:  2022-03-23
修回日期:  2022-05-28
刊出日期:  2023-08-25

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