{"title":"岩石材料位移的岩性指数作为边坡敏感性评估的一部分","authors":"M. Wódka","doi":"10.7306/2022.23","DOIUrl":null,"url":null,"abstract":"The use of multi-temporal LIDAR data in the study of landslides gives many possibilities. The increasing-over-timeavailabilityofALSdataencouragedresearchondevelopmentoflandslidesusingDifferentialDigital Terrain Models. An important passive factor that determines the development of landslides (especially in the Carpathians) is lithology. The author propose a new lithological displacement index, that dscribes the volume of displaced ground (m3) per area of 1 m2 of a given lithological unit. The example of the test area of Ro¿nowskie Lake has shown that lithological displacement index can assess the landslide susceptibility, which is variable and depends on the amount of rainfall. During periods of heavy rainfall, large volumes of displaced rock masses were recorded in the thick-bedded formations. In dry periods, the trend is reversed.","PeriodicalId":35787,"journal":{"name":"Przeglad Geologiczny","volume":"1 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2022-10-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Litologiczny wskaźnik przemieszczeń materiału skalnego jako element oceny podatności stoków na osuwanie\",\"authors\":\"M. Wódka\",\"doi\":\"10.7306/2022.23\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The use of multi-temporal LIDAR data in the study of landslides gives many possibilities. The increasing-over-timeavailabilityofALSdataencouragedresearchondevelopmentoflandslidesusingDifferentialDigital Terrain Models. An important passive factor that determines the development of landslides (especially in the Carpathians) is lithology. The author propose a new lithological displacement index, that dscribes the volume of displaced ground (m3) per area of 1 m2 of a given lithological unit. The example of the test area of Ro¿nowskie Lake has shown that lithological displacement index can assess the landslide susceptibility, which is variable and depends on the amount of rainfall. During periods of heavy rainfall, large volumes of displaced rock masses were recorded in the thick-bedded formations. In dry periods, the trend is reversed.\",\"PeriodicalId\":35787,\"journal\":{\"name\":\"Przeglad Geologiczny\",\"volume\":\"1 1\",\"pages\":\"\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2022-10-10\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Przeglad Geologiczny\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.7306/2022.23\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q4\",\"JCRName\":\"Earth and Planetary Sciences\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Przeglad Geologiczny","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.7306/2022.23","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"Earth and Planetary Sciences","Score":null,"Total":0}
Litologiczny wskaźnik przemieszczeń materiału skalnego jako element oceny podatności stoków na osuwanie
The use of multi-temporal LIDAR data in the study of landslides gives many possibilities. The increasing-over-timeavailabilityofALSdataencouragedresearchondevelopmentoflandslidesusingDifferentialDigital Terrain Models. An important passive factor that determines the development of landslides (especially in the Carpathians) is lithology. The author propose a new lithological displacement index, that dscribes the volume of displaced ground (m3) per area of 1 m2 of a given lithological unit. The example of the test area of Ro¿nowskie Lake has shown that lithological displacement index can assess the landslide susceptibility, which is variable and depends on the amount of rainfall. During periods of heavy rainfall, large volumes of displaced rock masses were recorded in the thick-bedded formations. In dry periods, the trend is reversed.