摘要
气候变化对滑坡的影响关系研究是近年来滑坡灾害研究的热点问题之一。本研究以我国中更新世早中期以来黄河上游和三峡库区的滑坡为研究对象,分析了其发育期与气候变化的对应关系以及气候演变对滑坡发育的作用机理。研究认为:1)大型古滑坡在时空分布上具有明显的多期性和时段性,大区域滑坡的广泛发育与全球古环境变化的暖湿间冰期之间呈现良好的对应关系。2)黄河上游龙羊峡-刘家峡段干流区内共发育有3期滑坡,其中早期滑坡多披覆于黄河Ⅲ～Ⅳ级阶地,光释光年龄显示其发生于MIS 3时期;晚期滑坡多披覆于黄河Ⅱ级阶地,发育于MIS 1时期;现代滑坡披覆于黄河Ⅰ级阶地,多为早期滑坡前缘因人类工程活动诱发的次级滑坡。3)三峡库区中更新世早中期以来主要发育了3期古滑坡,并以深海氧同位素的MIS 5和MIS 3为最多,尤其是中更新世晚期以来,滑坡数量明显增加,延续时间明显增长。
The relationships between landslide forming mechanisms and climate changes are one focus in the landslide study in recent years. In the study,paleo-landslides and modern landslides since the early mid-Pleistocene in China were studied and the relationships among the landslide active period, climate change, and the climate change-driven mechanism of landslide were also done. It was found three characteristics. 1 ） Landslide development would be closely related to climate changes. Most landslides developed in warm and wet periods, such as in marine oxygen isotopic odd stages （MIS）. Rapid and continuous climatic fluctuation periods usually were also high-frequency active periods of landslide. 2） There are 3 active periods of paleo-landslide in the region of Longyang Gorge to Liujia Gorge of the upper reaches of Yellow River. Landslides in the first active stage,whose OSL and ESR dating ages are 24 - 35kaB. P. ,developed on the 3^rd -4^th fluvial terraces of Yellow River. Landslides in the 2nd active stage,whose ages are 5kaB. P. ,developed on the 2nd fluvial terraces of Yellow River. Modern landslides in the 3rd active stage developed on the 1st fluvial terraces of Yellow River. The study shows that the Gonghe tectonic movement caused the region uplift and in turn strong down-cutting erosion along the river to form 300 -600m steep slopes. In addition,the rapid climatic fluctuation in the MIS 3 induced landslide development of the first stage. During 5kaB. P. of Holocene Optimal, strong monsoonal rainfall and a large number of melted snow and ice converged into the Yellow River to lead landslides development of the second stage. Modern landslides were mainly trigged by human activities. 3 ） In the Three Gorges Reservoir area, there also were 3 high-frequency periods of landslide since early mid-Pleistocene, which were corresponding to warm and wet climatic periods. Since the later mid-Pleistocene, the amount of landslides obviously increased and the lasting time of landslide active period also lengthened. Particularly, most landslides developed on marine oxygen isotope stages, MIS 5 and MIS 3. During these two landslide active periods, the paleo-climate was warm and wet and a large amount of rainfall in Tibetan Plateau was converged into the Yangtze River to lead strong down-cutting erosion, and in turn to form cliffy slopes with weak slope stability and then a large of landslides.
出处
《第四纪研究》
CAS
CSCD
北大核心
2010年第1期37-45,共9页
Quaternary Sciences
基金
国家自然科学基金面上项目(批准号:40802089)
国土资源大调查项目(批准号:1212010818083)
中国科学院地质与地球物理研究所工程地质力学重点实验室开放课题共同资助
关键词
中更新世
滑坡形成机理
气候变化
黄河上游
三峡库区
mid-Pleistocene, landslide forming mechanism, climate change, the upper reaches of Yellow River, the Three Gorges Reservoir area
