[1]孙萍萍,张茂省*,程秀娟,等.黄土高原地质灾害发生规律[J].山地学报,2019,(05):737-746.[doi:10.16089/j.cnki.1008-2786.000464]
 SUN Pingping,ZHANG Maosheng*,CHENG Xiujuan,et al.On the Regularity of Geological Hazards on the Loess Plateau in China[J].Mountain Research,2019,(05):737-746.[doi:10.16089/j.cnki.1008-2786.000464]
点击复制

黄土高原地质灾害发生规律()
分享到:

《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2019年05期
页码:
737-746
栏目:
山地灾害
出版日期:
2019-09-30

文章信息/Info

Title:
On the Regularity of Geological Hazards on the Loess Plateau in China
文章编号:
1008-2786-(2019)5-737-10
作者:
孙萍萍12张茂省2*程秀娟2黄玉华2薛 强2刘 洁2
1.西北大学 大陆动力学国家重点实验室,西安 710069; 2.中国地质调查局西安地质调查中心 自然资源部黄土地质灾害重点实验室,西安 710054
Author(s):
SUN Pingping12 ZHANG Maosheng2*CHENG Xiujuan2 HUANG Yuhua2 XUE Qiang2LIU Jie2
1. State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an 710069, China; 2. Key Laboratory for Geo-hazards in Loess Area, of Ministry of Natural Resources, Xi'an Center of Geological Survey, China Geological Survey, Xi'an 710054, China
关键词:
黄土高原 地质灾害 滑坡 发生规律 斜坡结构
Keywords:
loess plateau geohazards landslides distribution pattern slope structure
分类号:
P694~A
DOI:
10.16089/j.cnki.1008-2786.000464
摘要:
我国每年约有30%地质灾害发生在约占国土面积6%黄土高原地区,灾害数量多、危害严重、机理复杂,然而由于对黄土灾害的发生规律仍然不明晰,长期以来制约了区内大型工程建设、移民搬迁选址等工作。依托1:5万黄土高原区地质灾害调查数据,通过专题要素图件编制和数理统计等手段,重点分析11 680处地质灾害,总结了灾害时空分布规律。结果表明,1)在区域地质构造抬升的背景下,黄土高原地形破碎,地貌沟壑纵横,具有滑坡、崩塌、泥石流等地质灾害多发的特点。2)地质灾害具有明显的时空发生规律,在整个黄土高原区域尺度上,地貌演化与斜坡结构控制地质灾害空间分布和斜坡破坏模式; 在流域尺度上,老年期、壮年期、幼年期等沟谷发育期控制着地质灾害变形破坏模式及危害程度; 在具体斜坡点上,坡型、坡度、坡高等坡体几何形态控制地质灾害的类型和失稳概率; 在时间上,降雨及冻融作用控制年内地质灾害的分布。
Abstract:
There are about 30% of the total geological hazards occurring on the Loess plateau of China each year, but they occupy only about 6% of Chinese land area. Although loess geohazard are characterized by diverse types and large occurrences, complicated mechanisms and serious aftermaths, their occurrence regularity are still unclear, which has restricted the construction of large-scale projects, relocation and site selection of immigrants in the region for a long time. In this study, it inspected the catalog data from a report of geohazard survey with the scale of 1:50 000 in the Loess Plateau area, campaigned by China Geological Survey since 2005. 11 680 geological disaster records were scrutinized with reexamination of detailed information. The temporal and spatial distribution of loess geohazards was delineated by statistics analysis and compilations of thematic maps of geohazard survey. The results show that: 1)under the influence of regional tectonic uplift, vertical and horizontal gullies richly developed in broken loess terrain contributed to frequent occurrences of loess geohazard such as landslide, collapse and debris flow. 2)Loess geohazards are characterized by obvious spatio-temporal formation. As viewed from a regional scale of the Loess Plateau, geomorphological evolution and slope structure of loess massif dominated the spatial distribution of loess geohazards and slope failure modes; On the basin scale, the deformation and failure modes of loess slopes, as well as the resulting aftermaths were associated with the evolution phases of loess gullies, such as old-stage, adult-stage and young-stage of a gully; At a given slope site, the morphology of a slope such as geometry, inclination, height, etc. determined the type of loess geohazards and their failure probability; As viewed from time scale, loess geohazards mostly occurred during monsoon, freezing-thawing seasons in a year. This research would provide a scientific insight into loess geohazard regularity in different circumstances.

参考文献/References:

[1] 孙建中. 黄土学(上篇)[M]. 香港:香港考古学会,2005:1. [SUN Jianzhong. Loessology(Vol.1)[M]. Hong Kong: Hong Kong Archaeological Society, 2005:1]
[2] 张茂省,李同录,程秀娟,等. 山区城市地下空间资源评价与开发利用模式--以延安市为例[J].山地学报,2019,37(3):303-315. [ZHANG Maosheng, LI Tonglu, CHENG Xiujuan, et al. Evaluation of underground space resources in mountain cities and their development models-taking Yan'an city as a example[J]. Mountain Research, 2019, 37(3): 303-315]
[3] BETTIS E A, MUHS D R, ROBERTS H M, et al. Last glacial loess in the conterminous USA[J]. Quaternary Science Reviews, 2003, 22(18/19): 1907-1946.
[4] SUN Youbin, CLEMENS S C, MORRILL C, et al. Influence of Atlantic meridional overturning circulation on the East Asian winter monsoon[J]. Nature Geoscience, 2012, 5(1): 46-49.
[5] 彭建兵,林鸿州,王启耀,等.黄土地质灾害研究中的关键问题与创新思路[J].工程地质学报,2014,22(4):684-691. [PENG Jianbing, LIN Hongzhou, WANG Qiyao, et al. The critical issues and creative concepts in mitigation research of loess geological hazards [J]. Journal of Engineering Geology, 2014, 22(4): 684-691]
[6] 李媛,孟辉,董颖,等.中国地质灾害类型及其特征--基于全国县市地质灾害调查成果分析[J]. 中国地质灾害与防治学报,2004,15(2):29-34. [LI Yuan, MENG Hui, DONG Ying, et al. Main types and characterisitics of geo-hazard in China-Based on the results of geo-hazard survey in 290 counties [J]. The Chinese Journal of Geological Hazard and Control, 2004, 15(2): 29-34]
[7] 张茂省,胡炜,孙萍萍,等.黄土水敏性及水致黄土滑坡研究现状与展望[J]. 地球环境学报,2016,7(4):323-334. [ZHANG Maosheng, HU Wei, SUN Pingping, et al. Advances and prospects of water sensitivity of loess and the induced loess landslides [J]. Journal of Earth Environment, 2016, 7(4): 323-334]
[8] 徐张建,林再贯,张茂省.中国黄土与黄土滑坡[J]. 岩石力学与工程学报,2007,26(7):1297-1312. [XU Zhangjian, LIN Zaiguan, ZHANG Maosheng. Loess in China and loess landslides [J]. Chinese Journal of Rock Mechanics and Engineering, 2007, 26(7): 1297-1312]
[9] 雷祥义.黄土高原地质灾害与人类活动[M].北京:地质出版社,2001:30-31. [LEI Xiangyi. Geological disasters and human activities on the loess plateau of China[M]. Beijing: Geological Publishing House, 2001:30-31]
[10] 张茂省,孙萍萍,程秀娟,等.西北黄土高原地质灾害综合研究报告[R]. 西安:中国地质调查局西安地质调查中心,2015.12. [ZHANG Maosheng, SUN Pingping, CHENG Xiujuan, et al. Report on the comprehensive research of geohazards at the Loess Plateau, northwest China [R]. Xi'an Center of Geological Survey, CGS, 2015.12]
[11] 刘文红. 黄土高原滑坡发育背景与成灾模式研究[D]. 西安:长安大学,2016:52. [LIU Wenhong. Study on the background and disaster modes of landslide on Loess Plateau [D]. Xi'an: Chang'an University, 2016:52]
[12] 雷祥义.黄土高原河谷阶地黄土地层结构模式[J].海洋地质与第四纪地质,2006,2(2):113-122. [LEI Xiangyi. Models of loess stratigraphical structure on the terraces in the loess plateau of China[J]. Marine Geology & Quaternary Geology, 2006, 26(2): 113-122]
[13] 张茂省,校培喜,魏兴丽,等. 延安宝塔区滑坡崩塌地质灾害[M]. 北京:地质出版社,2008:109-111.[ZHANG Maosheng, XIAO Peixi, WEI Xingli, et al. Landslide and collapse disasters in Baota area of Yan'an [M]. Beijing: Geological Publishing House, 2008:109-111]
[14] ZHANG M, LIU Jie. Controlling factors of loess landslides in western China[J]. Environmental Earth Sciences, 2010, 59(8): 1671-1680.
[15] 李萍.黄土中水分迁移规律研究[D]. 西安:长安大学,2013:1-6. [LI Ping. Study on the regularities of water migration in unsaturated loess [D]. Xi'an: Chang'an University, 2013:1-6]
[16] TU X B, KWONG A K L, DAI F C, et al. Field monitoring of rainfall infiltration in a loess slope and analysis of failure mechanism of rainfall-induced landslides[J]. Engineering Geology, 2009, 105(1/2): 134-150.
[17] WANG Genlong, LI Tonglu, XING Xianli, et al. Research on loess flow-slides induced by rainfall in July 2013 in Yan'an, NW China [J]. Environmental Earth Sciences, 2015, 73(12): 7933-7944.
[18] 李同录,习羽,侯晓坤.水致黄土深层滑坡灾变机理[J]. 工程地质学报,2018,26(5):1113-1120. [LI Tonglu, XI Yu, HOU Xiaokun. Mechanism of surface water infiltration induced deep loess landslide [J]. Journal of Engineering Geology, 2018, 26(5): 1113-1120]
[19] 张珊珊,张茂省,孙萍萍,等.面向黄土地质灾害的优势流研究[J]. 兰州大学学报:自然科学版,2019,55(2):274-280. [ZHANG Shanshan, ZHANG Maosheng, SUN Pingping, et al. Advances in and outlooks of preferential flow study in unsaturated soils [J]. Journal of Lanzhou University: Natural Sciences, 2019, 55(2): 274-280]
[20] 曾磊.季节性冻融过程黄土斜坡水文效应及其稳定性研究[D]. 西安:长安大学,2018:1. [ZENG Lei. Study on the hydrological effect and stability of loess slope on seasonal freezing-thawing process [D]. Xi'an: Chang'an University, 2018:1]
[21] 张茂省,李同录. 黄土滑坡诱发因素及其形成机理研究[J]. 工程地质学报,2011,19(4):530-540. [ZHANG Maosheng, LI Tonglu. Triggering factors and forming mechanism of loess landslides [J]. Journal of Engineering Geology, 2011, 19(4): 530-540]
[22] 张茂省,程秀娟,董英,等.冻结滞水效应及其促滑机理--以甘肃黑方台地区为例[J]. 地质通报,2013,32(6):852-860. [ZHANG Maosheng, CHENG Xiujuan, DONG Ying. The effect of frozen stagnant water and its impact on slope stability: A case study of Heifangtai, Gansu Province [J]. Geological Bulletin of China, 2013, 32(6): 852-860]

相似文献/References:

[1]王晓慧,陈永富,陈尔学,等.基于遥感和GIS的黄土高原中阳县土壤侵蚀评价[J].山地学报,2011,(04):442.
 Xiaohui,CHEN Yongfu,CHEN Erxue,et al.Quantified Evaluation of Soil Erosion in Zhongyang County, the Loess PlateauWANG[J].Mountain Research,2011,(05):442.
[2]李少龙,苏春江,白立新,等.小流域泥沙来源的~(226)Ra分析法[J].山地学报,1995,(03):199.
[3]王占礼,邵明安.黄土高原典型地区土壤侵蚀共性与特点[J].山地学报,2001,(01):87.
[4]雷会珠,武春龙.黄土高原分形沟网研究[J].山地学报,2001,(05):474.
[5]姜永清,邵明安,李占斌,等.黄土高原流域水系的HORTON级比数和分形特性[J].山地学报,2002,(02):206.
[6]宋述军,李辉霞,张建国.黄土高原坡地单株植物下的微地形研究[J].山地学报,2003,(01):106.
[7]陈燕,齐清文,杨志平,等.数学形态学在黄土地貌单元分类学上的应用[J].山地学报,2005,(01):96.
[8]张金屯,李斌.黄土高原森林植被景观的特征分析[J].山地学报,2006,(01):1.
[9]刘贤赵,宿庆.黄土高原水土流失区生态退耕对粮食安全的影响[J].山地学报,2006,(01):7.
[10]信忠保,许炯心,马元旭,等.黄土高原面积-高程分析及其侵蚀地貌学意义[J].山地学报,2008,(03):356.

备注/Memo

备注/Memo:
收稿日期(Received date):2019-07-13; 改回日期(Accepted date):2019-09-27
基金项目(Foundation item):国家重点研发计划项目(2018YFC1504700); 国家自然科学基金项目(41530640); 中国地质调查项目(DD20189270)。[National Key Research Planning Program(2018YFC1504700); National Natural Science Foundation of China(41530640); Project of China Geological Survey(DD20189270)]
作者简介(Biography):孙萍萍(1983-),女,辽宁阜新人,博士生,高级工程师,从事黄土地质灾害调查与研究。[SUN Pingping(1983-), female, born in Fuxin City of Liaoning Province, Ph.D. candidate, senior engineer, specialized in investigation and research on loess landslides] E-mail: sunpingping203@gmail.com
更新日期/Last Update: 2019-09-30