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汉江上游全新世特大古洪水事件光释光测年研究

王恒松 黄春长 周亚利 熊康宁

王恒松, 黄春长, 周亚利, 熊康宁. 汉江上游全新世特大古洪水事件光释光测年研究[J]. 沉积学报, 2014, 32(6): 1100-1112.
引用本文: 王恒松, 黄春长, 周亚利, 熊康宁. 汉江上游全新世特大古洪水事件光释光测年研究[J]. 沉积学报, 2014, 32(6): 1100-1112.
WANG Heng-song, HUANG Chun-chang, ZHOU Ya-li, XIONG Kang-ning. OSL Dating and Climatic Change Record of the Holocene Paleoflood Events in the Upper Reaches of Hanjiang River, China[J]. Acta Sedimentologica Sinica, 2014, 32(6): 1100-1112.
Citation: WANG Heng-song, HUANG Chun-chang, ZHOU Ya-li, XIONG Kang-ning. OSL Dating and Climatic Change Record of the Holocene Paleoflood Events in the Upper Reaches of Hanjiang River, China[J]. Acta Sedimentologica Sinica, 2014, 32(6): 1100-1112.

汉江上游全新世特大古洪水事件光释光测年研究

基金项目: 国家自然科学基金重点项目(批准号:41030637)、教育部博士点基金项目(批准号: 20110202130002)、国家重大科技支撑项目(编号:2011BAC09B01)与中央高校基本科研业务费专项基金项目(编号: GK200902020,GK200901007)联合资助
详细信息
    作者简介:

    王恒松 男 1967年出生 教授 资源开发与全球变化、喀斯特地貌与洞穴、石漠化综合治理 E-mail: wanghengsong796@163.com

    通讯作者:

    黄春长 男 教授 E-mail: cchuang@snnu.edu.cn

  • 中图分类号: P532

OSL Dating and Climatic Change Record of the Holocene Paleoflood Events in the Upper Reaches of Hanjiang River, China

  • 摘要: 古洪水事件对中国古代文明的演变进程产生过重大影响,古洪水水文学研究是全球变化研究的前沿课题.通过野外深入考察,在汉江上游河谷阶地上,发现典型的全新世剖面中赋存古洪水滞流沉积层,记录了古洪水事件的气候水文信息.选择三个剖面系统采样,应用SAR法的Post-IR OSL技术对样品进行测年研究,获得了14个OSL年龄数据.结合样品的粒度成分和磁化率等气候替代指标测定分析,获得了全新世洪水事件与气候变化关系的记录.证明在距今9.5~8.5 ka和3.2~2.8 ka前,汉江上游经历了2个特大洪水期.该流域黄土—古土壤剖面记录了全新世早期气温回升增湿的气候,由于大气波动失稳,出现了9~8 ka前的全球降温事件;中期土壤成壤强烈,记录了温暖湿润的气候;晚期形成的现代黄土和表土层,记录了相对干旱的气候.由此揭示了在全新世早期气候波动失稳和中期向晚期过渡的气候转折时期,气候变化剧烈,降水变率增大,是导致特大古洪水事件频发的主要原因,这也是该区域气候水文事件对全球气候变化响应规律的具体表现.
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  • 收稿日期:  2013-08-27
  • 修回日期:  2013-11-24
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目录

    汉江上游全新世特大古洪水事件光释光测年研究

      基金项目:  国家自然科学基金重点项目(批准号:41030637)、教育部博士点基金项目(批准号: 20110202130002)、国家重大科技支撑项目(编号:2011BAC09B01)与中央高校基本科研业务费专项基金项目(编号: GK200902020,GK200901007)联合资助
      作者简介:

      王恒松 男 1967年出生 教授 资源开发与全球变化、喀斯特地貌与洞穴、石漠化综合治理 E-mail: wanghengsong796@163.com

      通讯作者: 黄春长 男 教授 E-mail: cchuang@snnu.edu.cn
    • 中图分类号: P532

    摘要: 古洪水事件对中国古代文明的演变进程产生过重大影响,古洪水水文学研究是全球变化研究的前沿课题.通过野外深入考察,在汉江上游河谷阶地上,发现典型的全新世剖面中赋存古洪水滞流沉积层,记录了古洪水事件的气候水文信息.选择三个剖面系统采样,应用SAR法的Post-IR OSL技术对样品进行测年研究,获得了14个OSL年龄数据.结合样品的粒度成分和磁化率等气候替代指标测定分析,获得了全新世洪水事件与气候变化关系的记录.证明在距今9.5~8.5 ka和3.2~2.8 ka前,汉江上游经历了2个特大洪水期.该流域黄土—古土壤剖面记录了全新世早期气温回升增湿的气候,由于大气波动失稳,出现了9~8 ka前的全球降温事件;中期土壤成壤强烈,记录了温暖湿润的气候;晚期形成的现代黄土和表土层,记录了相对干旱的气候.由此揭示了在全新世早期气候波动失稳和中期向晚期过渡的气候转折时期,气候变化剧烈,降水变率增大,是导致特大古洪水事件频发的主要原因,这也是该区域气候水文事件对全球气候变化响应规律的具体表现.

    English Abstract

    王恒松, 黄春长, 周亚利, 熊康宁. 汉江上游全新世特大古洪水事件光释光测年研究[J]. 沉积学报, 2014, 32(6): 1100-1112.
    引用本文: 王恒松, 黄春长, 周亚利, 熊康宁. 汉江上游全新世特大古洪水事件光释光测年研究[J]. 沉积学报, 2014, 32(6): 1100-1112.
    WANG Heng-song, HUANG Chun-chang, ZHOU Ya-li, XIONG Kang-ning. OSL Dating and Climatic Change Record of the Holocene Paleoflood Events in the Upper Reaches of Hanjiang River, China[J]. Acta Sedimentologica Sinica, 2014, 32(6): 1100-1112.
    Citation: WANG Heng-song, HUANG Chun-chang, ZHOU Ya-li, XIONG Kang-ning. OSL Dating and Climatic Change Record of the Holocene Paleoflood Events in the Upper Reaches of Hanjiang River, China[J]. Acta Sedimentologica Sinica, 2014, 32(6): 1100-1112.
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