2009
DOI: 10.4324/9781849774352
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A Handbook of Soil Terminology, Correlation and Classification

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Cited by 91 publications
(62 citation statements)
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“…According to the soil profiles established in the study site, the soil depth varies along a slight topographic gradient (Supplementary Materials 1), deep (250 cm) at the lower elevations and shallow (70 cm) nearer the ridge. In the lower elevation parts of the site, the soil type is brown forest soil with clay illuviation (Luvisol), while in the upper parts it is Rendzic Leptosol [52]. The soils are slightly acidic (pH of the 0-20 cm layer is 4.6 ± 0.2).…”
Section: Study Areamentioning
confidence: 99%
“…According to the soil profiles established in the study site, the soil depth varies along a slight topographic gradient (Supplementary Materials 1), deep (250 cm) at the lower elevations and shallow (70 cm) nearer the ridge. In the lower elevation parts of the site, the soil type is brown forest soil with clay illuviation (Luvisol), while in the upper parts it is Rendzic Leptosol [52]. The soils are slightly acidic (pH of the 0-20 cm layer is 4.6 ± 0.2).…”
Section: Study Areamentioning
confidence: 99%
“…The emphasis of particular soil properties 449 deemed important by the soil expert has remained a common theme for soil classification systems 450 (Krasilnikov and Arnold, 2009). When Dokuchaev's zonal classification gained acceptance, most soil 451 geographers were using agrogeology style classification systems as a guide for creating their medium 452 cartographic scale soil maps.…”
Section: Early Struggles 446mentioning
confidence: 99%
“…Drainage for non-US sites was determined either via contacting individual authors or by soil classification. Soil classification was determined by the referenced literature, and all sites were converted to one of the World Reference Base Group and US Soil Classification Group equivalents using Krasilnikov et al (2009 …”
Section: Studies Published Before December Of 2012mentioning
confidence: 99%