CAJ | 학술논문

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问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.
기후변화대활파적영향관계연구시근년래활파재해연구적열점문제지일.본연구이아국중경신세조중기이래황하상유화삼협고구적활파위연구대상,분석료기발육기여기후변화적대응관계이급기후연변대활파발육적작용궤리.연구인위:1)대형고활파재시공분포상구유명현적다기성화시단성,대구역활파적엄범발육여전구고배경변화적난습문빙기지간정현량호적대응관계.2)황하상유룡양협-류가협단간류구내공발육유3기활파,기중조기활파다피복우황하Ⅲ～Ⅳ급계지,광석광년령현시기발생우MIS 3시기;만기활파다피복우황하Ⅱ급계지,발육우MIS 1시기;현대활파피복우황하Ⅰ급계지,다위조기활파전연인인류공정활동유발적차급활파.3)삼협고구중경신세조중기이래주요발육료3기고활파,병이심해양동위소적MIS 5화MIS 3위최다,우기시중경신세만기이래,활파수량명현증가,연속시간명현증장.
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 modem 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 Holoeene 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.