2015
DOI: 10.1016/j.catena.2014.12.024
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Climate and relief influence on particle size distribution and chemical properties of Pseudogley soils in Croatia

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Cited by 22 publications
(17 citation statements)
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“…clay eluviation/illuviation) have modified the PSD of soil horizons. The major influence of parent material properties on soil PSD has been reaffirmed in recent studies on Pseudogley soils (IUSS Working Group WRB, 2006) in Croatia (Rubinić et al, 2015), and on Typic Dystrudepts (Soil Survey Staff, 2014) developed from granites in France (Mareschal et al, 2015).…”
Section: Discussionmentioning
confidence: 82%
“…clay eluviation/illuviation) have modified the PSD of soil horizons. The major influence of parent material properties on soil PSD has been reaffirmed in recent studies on Pseudogley soils (IUSS Working Group WRB, 2006) in Croatia (Rubinić et al, 2015), and on Typic Dystrudepts (Soil Survey Staff, 2014) developed from granites in France (Mareschal et al, 2015).…”
Section: Discussionmentioning
confidence: 82%
“…In total, 90 soil horizons were used for the development of the PTF. Some properties of soil horizons covered in this study were previously analyzed by Rubinić et al (2015;2016), as affected by relief, climate, and profile stratigraphy.…”
Section: Study Area Field and Laboratory Workmentioning
confidence: 99%
“…On each location, Pseudogley soils were found. One of the main features of these soils is periodic stagnation of precipitation water on/in their poorly permeable (clayenriched and often massive) subsurface Btg horizon, as well as their low pH (see Rubinić et al, 2015;2016). Most of these soils correlate with Stagnosols, and some with Stagnic Retisols and Stagnic Luvisols (IUSS Working Group WRB, 2014).…”
Section: Study Area Field and Laboratory Workmentioning
confidence: 99%
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“…The surrounding area is mostly a mixture of plains with gentle hills. The parent materials in the area are composed of loamy loess sediments that developed a silty loam Luvic Stagnosols (IUSS Working Group WRB 2006) formed by top down pedogenesis (Rubinić et al 2015). Organic matter ranges from 16 g/kg at the surface to 6 g/kg at a depth of 35-95 cm (Table 1).…”
Section: Methodsmentioning
confidence: 99%