{"title":"陆相摄影测量技术在土壤粗糙度评估中的应用[j] .遥感学报,2006,26 (2):Böden","authors":"M. Grims, C. Atzberger, Thomas Bauer, P. Strauss","doi":"10.1127/1432-8364/2014/0226","DOIUrl":null,"url":null,"abstract":"as soil surface roughness indices, which are also important for other environmental applications (MARZAHN et al. 2012). A broad range of indices were defined for describing the roughness of soil surfaces, e.g. the roughness indices by TACONET & CIARLETTI (2007), PLANCHON et al. (2002), ALLMARAS et al. (1966) or LINDEN & VAN DOREN (1986). Such indices are needed for the calculation of soil erosion with erosion models (RENARD et al. 1997). To calculate those indices, threedimensional data of the soil surfaces is needed. Additionally, the dynamic of soil surfaces (changes) has to be assessed. It is a big challenge for soil scientists to get significant information on all kinds of soils and their development due to the diversity of soils on local level","PeriodicalId":56096,"journal":{"name":"Photogrammetrie Fernerkundung Geoinformation","volume":null,"pages":null},"PeriodicalIF":0.0000,"publicationDate":"2014-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"3","resultStr":"{\"title\":\"Low-cost Terrestrial Photogrammetry as a Tool for a Sample-Based Assessment of Soil Roughness Preiswerte terrestrische Photogrammetrie als Werkzeug zur Bestimmung der Rauigkeit von Böden\",\"authors\":\"M. Grims, C. Atzberger, Thomas Bauer, P. Strauss\",\"doi\":\"10.1127/1432-8364/2014/0226\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"as soil surface roughness indices, which are also important for other environmental applications (MARZAHN et al. 2012). A broad range of indices were defined for describing the roughness of soil surfaces, e.g. the roughness indices by TACONET & CIARLETTI (2007), PLANCHON et al. (2002), ALLMARAS et al. (1966) or LINDEN & VAN DOREN (1986). Such indices are needed for the calculation of soil erosion with erosion models (RENARD et al. 1997). To calculate those indices, threedimensional data of the soil surfaces is needed. Additionally, the dynamic of soil surfaces (changes) has to be assessed. It is a big challenge for soil scientists to get significant information on all kinds of soils and their development due to the diversity of soils on local level\",\"PeriodicalId\":56096,\"journal\":{\"name\":\"Photogrammetrie Fernerkundung Geoinformation\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2014-10-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"3\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Photogrammetrie Fernerkundung Geoinformation\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1127/1432-8364/2014/0226\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q\",\"JCRName\":\"Social Sciences\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Photogrammetrie Fernerkundung Geoinformation","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1127/1432-8364/2014/0226","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q","JCRName":"Social Sciences","Score":null,"Total":0}
引用次数: 3
摘要
作为土壤表面粗糙度指数,这对其他环境应用也很重要(MARZAHN等,2012)。为了描述土壤表面的粗糙度,定义了一系列广泛的指标,例如TACONET和CIARLETTI (2007), PLANCHON等人(2002),ALLMARAS等人(1966)或LINDEN和VAN DOREN(1986)的粗糙度指数。利用侵蚀模型计算土壤侵蚀需要这些指标(RENARD et al. 1997)。为了计算这些指标,需要土壤表面的三维数据。此外,还必须评估土壤表面(变化)的动态。由于地方土壤的多样性,获取各种土壤及其发展的重要信息对土壤科学家来说是一个巨大的挑战
Low-cost Terrestrial Photogrammetry as a Tool for a Sample-Based Assessment of Soil Roughness Preiswerte terrestrische Photogrammetrie als Werkzeug zur Bestimmung der Rauigkeit von Böden
as soil surface roughness indices, which are also important for other environmental applications (MARZAHN et al. 2012). A broad range of indices were defined for describing the roughness of soil surfaces, e.g. the roughness indices by TACONET & CIARLETTI (2007), PLANCHON et al. (2002), ALLMARAS et al. (1966) or LINDEN & VAN DOREN (1986). Such indices are needed for the calculation of soil erosion with erosion models (RENARD et al. 1997). To calculate those indices, threedimensional data of the soil surfaces is needed. Additionally, the dynamic of soil surfaces (changes) has to be assessed. It is a big challenge for soil scientists to get significant information on all kinds of soils and their development due to the diversity of soils on local level