陇东黄土高原典型地质灾害发育特征及成灾模式研究——以甘肃庆阳正宁县为例
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本文为甘肃省陇原青年英才资助资金项目的成果


Development characteristics and disaster models of typical geological disasters on loess plateau in Eastern Gansu:A case study of Zhengning County of Qingyang City
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    摘要:

    笔者等对甘肃省正宁县1∶1万地质灾害精细调查灾害点、斜坡单元、遥感解译点等调查数据进行梳理,研究分析典型灾害点孕灾条件、形成机理和成灾模式等。旨在掌握研究区滑坡、崩塌等灾害变形破坏特征和发展趋势,为当地生态移民避险搬迁、防灾减灾、后续风险双控等提供可借鉴的依据。结果表明:开挖型滑坡、降雨型滑坡、河流侧蚀型滑坡、黄土—基岩滑坡为研究区主要的滑坡类型,成灾模式依次为“牵引—拉裂式”、“蠕滑—推移式”、“蠕变式”和“岩土复合式”;“倾倒式崩塌”和“滑移式崩塌”为该区主要的崩塌类型,成灾模式依次为“坠落+砸毁+掩埋”和“击毁+冲毁+掩埋”;研究区地面塌陷主要表现为窑洞坍塌,沟谷发育崩塌/滑坡—碎屑流/泥流水源型黄土地质灾害链成灾过程:人类不合理活动降雨入渗黄土湿陷、裂缝、落水洞等黄土斜坡塌陷、崩滑沟谷泥流冲毁、掩埋承灾体。研究结果厘清了滑坡、崩塌、窑洞塌陷和沟谷灾害链的变形破坏机制,有利于今后快速识别隐患风险、精准实施监测预警和合理规划撤离路线等。

    Abstract:

    Based on the refined 1∶10,000- scale geological hazard survey data for Zhenning County, Gansu Province, including hazard points, slope units, and remote sensing interpretation points, the study systematically analyzes the predisposing conditions, formation mechanisms, and disaster patterns of typical hazards, aiming to elucidate the deformation characteristics and evolutionary trends of landslides, collapses, and other geohazards within the study area, thereby providing a scientific basis for local ecological migration and hazard- avoidance relocation, disaster prevention and mitigation, and the subsequent implementation of dual- control measures for hazard and risk.As a result, the primary landslide types identified in the study area include excavation- induced landslides, rainfall- triggered landslides, river lateral erosion- induced landslides, and loess—bedrock composite landslides, exhibiting characteristic failure patterns of “retrogressive tensile- cracking”, “creep- pushing”, “creep deformation”, and “soil—rock composite”, respectively. The predominant collapse types are “toppling rockfalls” and “sliding rockfalls”, with their associated failure patterns characterized as “falling + impact destruction + burial” and “impact- scouring destruction + burial”, respectively.Ground subsidence in the study area primarily manifests as cave dwelling collapse, while valleys exhibit a water- triggered loess geological hazard chain characterized by rockfall/landslide debris flow/mudflow. The disaster formation process progresses through the following sequence: human improper activities rainfall infiltration loess collapse, cracking, and sinkhole development loess slope subsidence/collapse or landsliding valley mudflow destruction and burial of hazard bearing body.The findings elucidate the deformation and failure mechanisms governing landslides, collapse, cave dwelling collapses, and valley hazard chains, thereby facilitating future rapid identification of potential hazards, precision- based implementation of monitoring and early warning systems, and rational planning of evacuation routes.

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引用本文

包维斌,张凌鹏,李成云.2025.陇东黄土高原典型地质灾害发育特征及成灾模式研究——以甘肃庆阳正宁县为例[J].地质论评,71(6):2025060001,[DOI].
BAO Weibin, ZHANG Linpeng, LI Chengyun.2025. Development characteristics and disaster models of typical geological disasters on loess plateau in Eastern Gansu:A case study of Zhengning County of Qingyang City[J]. Geological Review,71(6):2025060001.

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  • 收稿日期:2025-07-11
  • 最后修改日期:2025-10-17
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  • 在线发布日期: 2025-11-18
  • 出版日期: 2025-11-15