{"title":"喀尔巴阡山脉东部Gemenea山区集水区土壤表面侵蚀的定量估算","authors":"Florentina Livarciuc, C. Patriche","doi":"10.4316/GEOREVIEW.2016.26.1.315","DOIUrl":null,"url":null,"abstract":"This study aims to estimate soil removal via sheet erosion in a mountain catchment and highlight the stabilizing role of vegetation on sloping land. Spatial representation of the results was performed through the implementation of GIS techniques. The estimation method used is ROMSEM, which is based on six factors that can be separated into two groups, i.e. i) factors that trigger erosion (rainfall erosivity, topography, soils) and ii) factors controlling erosion (vegetation, anti-erosion measures). These factors constitute the database which generated the maps of potential and effective soil erosion. Based on our results, mean potential erosion is very high, 99.64 t ha -1 yr -1 respectively, and thereby falls into the severe erosion class. Mean effective erosion indicates current soil loss and falls within the insignificant erosion class, with 0.98 t ha -1 yr -1 , which suggests that at the catchment scale, soil is eroded at a rate of 7620 t yr -1","PeriodicalId":30470,"journal":{"name":"GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series","volume":"26 1","pages":"49-84"},"PeriodicalIF":0.0000,"publicationDate":"2016-08-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"2","resultStr":"{\"title\":\"Quantitative estimation of soil surface erosion in a mountain catchment (Gemenea, Eastern Carpathians)\",\"authors\":\"Florentina Livarciuc, C. Patriche\",\"doi\":\"10.4316/GEOREVIEW.2016.26.1.315\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"This study aims to estimate soil removal via sheet erosion in a mountain catchment and highlight the stabilizing role of vegetation on sloping land. Spatial representation of the results was performed through the implementation of GIS techniques. The estimation method used is ROMSEM, which is based on six factors that can be separated into two groups, i.e. i) factors that trigger erosion (rainfall erosivity, topography, soils) and ii) factors controlling erosion (vegetation, anti-erosion measures). These factors constitute the database which generated the maps of potential and effective soil erosion. Based on our results, mean potential erosion is very high, 99.64 t ha -1 yr -1 respectively, and thereby falls into the severe erosion class. Mean effective erosion indicates current soil loss and falls within the insignificant erosion class, with 0.98 t ha -1 yr -1 , which suggests that at the catchment scale, soil is eroded at a rate of 7620 t yr -1\",\"PeriodicalId\":30470,\"journal\":{\"name\":\"GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series\",\"volume\":\"26 1\",\"pages\":\"49-84\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2016-08-19\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"2\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.4316/GEOREVIEW.2016.26.1.315\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.4316/GEOREVIEW.2016.26.1.315","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 2
摘要
本研究的目的是估算山区集水区通过薄片侵蚀产生的土壤流失,并强调植被在坡地上的稳定作用。通过实施GIS技术对结果进行空间表示。所使用的估算方法是ROMSEM,该方法基于六个因素,可分为两组,即i)触发侵蚀的因素(降雨侵蚀力、地形、土壤)和ii)控制侵蚀的因素(植被、抗侵蚀措施)。这些因素构成了生成潜在和有效土壤侵蚀图的数据库。根据我们的结果,平均潜在侵蚀非常高,分别为99.64 t / h -1 yr -1,因此属于严重侵蚀级别。平均有效侵蚀是指当前的土壤流失量,属于微不足道的侵蚀类,为0.98 t / h -1 yr -1,这表明在流域尺度上,土壤被侵蚀的速度为7620t / h -1
Quantitative estimation of soil surface erosion in a mountain catchment (Gemenea, Eastern Carpathians)
This study aims to estimate soil removal via sheet erosion in a mountain catchment and highlight the stabilizing role of vegetation on sloping land. Spatial representation of the results was performed through the implementation of GIS techniques. The estimation method used is ROMSEM, which is based on six factors that can be separated into two groups, i.e. i) factors that trigger erosion (rainfall erosivity, topography, soils) and ii) factors controlling erosion (vegetation, anti-erosion measures). These factors constitute the database which generated the maps of potential and effective soil erosion. Based on our results, mean potential erosion is very high, 99.64 t ha -1 yr -1 respectively, and thereby falls into the severe erosion class. Mean effective erosion indicates current soil loss and falls within the insignificant erosion class, with 0.98 t ha -1 yr -1 , which suggests that at the catchment scale, soil is eroded at a rate of 7620 t yr -1