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

汉江上游全新世特大古洪水事件光释光测年研究

1.
贵州师范大学中国南方喀斯特研究院贵阳 550001;
2.
贵州省喀斯特山地生态环境国家重点实验室培育基地贵阳 550001;
3.
陕西师范大学旅游与环境学院西安 710062

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

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

1.
Institute of South China Karst, Guizhou Normal University, Guiyang 550001;
2.
State Key Laboratory Incubation Base for Karst Mountain Ecology Environment of Guizhou Province, Guiyang 550001;
3.
College of Tourism and Environment, Shaanxi Normal University, Xi'an 710062

摘要

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.
- 光释光测年 /
- 全新世 /
- 古洪水事件 /
- 气候变化 /
- 汉江上游河谷
Abstract: Field investigation was carried out from Xunyang to Yunxian along the upper Hanjiang River valley, typical palaeoflood slackwater deposit interbedded in loess-like sediments were found in the profile of XTZ, NGK and JJTZ, which indicate these bedded slackwater deposits recorded the information of palaeoflood events. Systematic sampling for optical dating was carried out on these profiles. The Post-IR OSL single aliquot regeneration (SAR) protocol was used to determine equivalent and 14 OSL ages were obtained. The results show that there were two stage extreme palaeofloods occurred 9.5~8.5 ka B.P. and 3.2~2.8 ka B.P, respectively. According to the analysis of grain-size distribution and magnetic susceptibility, the relationship between Holocene palaeoflood events and climate change was established. The transitional loess (L_t) was dated to 11 500~8 500 a B.P. It has recorded the climatic shift from cold and moist to amelioration during the Early Holocene and dust storm activity gradually decreased. The Luvisol (S₀) was dated 8 500~ 3 100 a B.P. It has recorded the warm-humid climate during the mid-Holocene Climatic Optimum. This is a period with more intensified pedogenesis. The loess (L₀) was dated to 3 100 a B.P. that has recorded the climate decline during the Late Holocene and dust storms were obviously intensified to form modern loess. Environment records from all over the world revealed the temperature rising, relative precipitation increasing and climatic fluctuation during the period of 9.5~8.5 ka, which lead to abrupt climate events occured frequently such as cooling, flood and drought; during the period of 3.2~2.8 ka, that is a turning period from the Middle Holocene to the Late Holocene, climate changing to aridity, climate change intensively, atmosphere instability and precipitation variability. Therefore, climate changing and transformation were the main reason of frequent flood occurence. The climatic Hydrography event recorded during 9.5~8.5 ka and 3.2~2.8 ka represents the concrete manifestation of the hydrological system to global climate change. The regional responses of the hydrological system. It is significant to understand the regional responses of the hydrological system to global climate change.
- OSL dating /
- Holocene /
- palaeoflood event /
- weather changes /
- Upper Hanjiang River Valley

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参考文献(72)

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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

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

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

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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

1. 贵州师范大学中国南方喀斯特研究院贵阳 550001;

2. 贵州省喀斯特山地生态环境国家重点实验室培育基地贵阳 550001;

3. 陕西师范大学旅游与环境学院西安 710062

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

English Abstract

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

1. Institute of South China Karst, Guizhou Normal University, Guiyang 550001;

2. State Key Laboratory Incubation Base for Karst Mountain Ecology Environment of Guizhou Province, Guiyang 550001;

3. College of Tourism and Environment, Shaanxi Normal University, Xi'an 710062

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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

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

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

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出版历程

目录

汉江上游全新世特大古洪水事件光释光测年研究

1. 贵州师范大学中国南方喀斯特研究院 贵阳 550001; 2. 贵州省喀斯特山地生态环境国家重点实验室培育基地 贵阳 550001; 3. 陕西师范大学旅游与环境学院 西安 710062

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

English Abstract

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

1. Institute of South China Karst, Guizhou Normal University, Guiyang 550001; 2. State Key Laboratory Incubation Base for Karst Mountain Ecology Environment of Guizhou Province, Guiyang 550001; 3. College of Tourism and Environment, Shaanxi Normal University, Xi'an 710062

全文HTML

目录

友情链接

期刊在线

联系我们

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

1. 贵州师范大学中国南方喀斯特研究院贵阳 550001;

2. 贵州省喀斯特山地生态环境国家重点实验室培育基地贵阳 550001;

3. 陕西师范大学旅游与环境学院西安 710062

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

1. Institute of South China Karst, Guizhou Normal University, Guiyang 550001;

2. State Key Laboratory Incubation Base for Karst Mountain Ecology Environment of Guizhou Province, Guiyang 550001;

3. College of Tourism and Environment, Shaanxi Normal University, Xi'an 710062