Climate vs. parent material — Which is the key of Stagnosol diversity in Croatia?

Rubinić, Vedran; Galović, Lidija; Husnjak, Stjepan; Durn, Goran

doi:10.1016/j.geoderma.2014.11.029

Cited by 18 publications

(13 citation statements)

References 44 publications

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“…The fact that no progressive increase of the coarse/fine silt ratio was observed across the study region neither in the westerly nor in the easterly direction (Fig. 3c) was interpreted by Rubinić et al (2015) as an indication of loess originating from multiple sources and overlapping in the central Pannonian region of Croatia.…”

Section: Particle Size Distribution Of the Investigated Pseudogley Prmentioning

confidence: 90%

“…Moreover, Rubinić et al (2015) stress modal mineralogy of the investigated Pseudogley parent materials indicates more than one source of loess in the Pannonian region of Croatia. This, along with the uplifts of different loess plateaus in different points of time during the Pleistocene and the Holocene (see Mutić, 1990 and Section 2.1.1), resulted in slightly different particle size distributions of Pseudogley parent materials across the region.…”

Section: Pseudogley Parent Materialsmentioning

confidence: 92%

“…2). Given that parent materials of Croatian Pseudogleys are usually thoroughly altered by pedogenesis, they are morphologically similar to Btg horizons (see Rubinić et al, 2014Rubinić et al, , 2015. Most notably, both Btg horizons and parent materials are usually dominated by RMF (Table 1 and Fig.…”

Section: Morphology Of the Investigated Pseudogley Profiles And Desigmentioning

confidence: 99%

“…Further, the parent materials of Croatian Pseudogleys usually have the same or even slightly increased clay content compared with the Btg horizons above them (see Bašić, 2013;Rubinić et al, 2014Rubinić et al, , 2015. Given the clay coatings observed in thin sections and the depthrelated trends of the weathering indices (Ti/Al and CIA), Rubinić et al (2014) inferred that the vertical increase in clay content from the topsoil towards the parent material in Croatian Pseudogleys is largely due to lessivage.…”

Section: Morphology Of the Investigated Pseudogley Profiles And Desigmentioning

confidence: 99%

“…Additionally, morphology of soil profiles 7, 19, and 28 (see Appendix B) is described in Rubinić et al (2015). Hence, the following text describes only basic morphological characteristics that prevail across the 33 Pseudogleys investigated in this study.…”

Section: Morphology Of the Investigated Pseudogley Profiles And Desigmentioning

confidence: 99%

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Climate and relief influence on particle size distribution and chemical properties of Pseudogley soils in Croatia

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Section: Particle Size Distribution Of the Investigated Pseudogley Prmentioning

confidence: 90%

Section: Pseudogley Parent Materialsmentioning

confidence: 92%

Section: Morphology Of the Investigated Pseudogley Profiles And Desigmentioning

confidence: 99%

Section: Morphology Of the Investigated Pseudogley Profiles And Desigmentioning

confidence: 99%

Section: Morphology Of the Investigated Pseudogley Profiles And Desigmentioning

confidence: 99%

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The dynamics of soil nutrients in cold desert environments in the north-west Himalayas under a variety of forest types using geographical information system

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The effect of weathering on clay mineralogy of Plio-Quaternary sediments and the overlying material on SE slopes of Medvednica Mt., Croatia

et al. 2023

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Clay mineralogy of Plio-Quaternary sediments of SE slopes of Medvednica Mt. was compared to that of the overlying weathering horizons. Three locations of Plio-Quaternary sediments, representing past weathering products, were sampled along with the overlying material, representing more recent weathering cycles.Particle size distribution, pH and cation exchange capacity (CEC) of the samples were analyzed. Bulk mineralogy was determined using X-ray diffraction (XRD). Clay mineralogy was determined, after carbonate cement, organic matter and free Fe oxides removal, on fractions < 2 and < 0.2 µm using XRD and Fouriertransform infrared spectroscopy (FTIR). Average layer charge of the expandable layers was determined using the O-D method. Major elements content was determined using inductively coupled plasma optical emission spectroscopy (ICP-OES). Bulk mineralogy comprises quartz, feldspars, mica, clay minerals and occasional Al and Fe (oxy)hydroxides. Clay mineralogy differs subtly between samples; dioctahedral expandable clay minerals dominate with illite and kaolinite present. Hydroxyl interlayering of expandables is noted in the surface samples, corresponding to lower CEC values. Average absolute layer charge of the expandable layers is higher in the surface samples and decreases with depth on two of the investigated locations. Overall, clay mineralogy of the Plio-Quaternary sediments re ects a more intensive weathering regime, con rmed by the presence of Al (oxy)hydroxides and lower absolute charge of the expandable layers. The weathered material and soil overlying these sediments shows heterogeneity in genesis, but corresponds to less intense weathering regime, con rmed by the formation of hydroxy-interlayered minerals and higher absolute charge of the expandable layers.

show abstract

Climate vs. parent material — Which is the key of Stagnosol diversity in Croatia?

Cited by 18 publications

References 44 publications

Climate and relief influence on particle size distribution and chemical properties of Pseudogley soils in Croatia

Climate and relief influence on particle size distribution and chemical properties of Pseudogley soils in Croatia

The dynamics of soil nutrients in cold desert environments in the north-west Himalayas under a variety of forest types using geographical information system

The effect of weathering on clay mineralogy of Plio-Quaternary sediments and the overlying material on SE slopes of Medvednica Mt., Croatia

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