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Research of Cambisols in Western Balkan Mountains [PDF]
, 2021 The research deals with Cambisols soil classification and parameters in the area of Western Balkan Mountains. The studied soils are spread in the Lower altitude area of oak forests (0 to 600 m a.s.l.) and in the Middle mountain area of beech and coniferous forests (600 to 2000 ma.s.l.). The gradient of the slopes varied from flat to steep.
Hristov, Biser +4 more
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Resilience of Dystric Cambisols Under Liming and Fertilization
Novenytermeles, 2010Effects of liming and fertilization on improvement of soil chemical properties were studied in a field trial set up on Dystric Cambisol near Gospic, mountain part of Croatia. The two-year investigations revealed significant increases in pH value in treatment with higher rate of limestone.
Jurisic, Aleksandra +3 more
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Effects of mussel shell addition on the chemical and biological properties of a Cambisol
Chemosphere, 2012The use of a by-product of the fisheries industry (mussel shell) combined with cattle slurry was evaluated as soil amendment, with special attention to the biological component of soil. A wide number of properties related to soil quality were measured: microbial biomass, soil respiration, net N mineralization, dissolved organic carbon, dissolved ...
J, Paz-Ferreiro +3 more
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Impact of tillage on maize rooting in a Cambisol and Luvisol in Switzerland
Soil and Tillage Research, 2006Abstract Soil conditions under no-tillage (NT) are often unfavorable for the growth of maize roots in comparison to conventional tillage (CT). In 1997 and 1999, the impacts of tillage on the morphology and spatial distribution of maize ( Zea mays L.) roots at anthesis were investigated in a 5-year field trial at two sites (loamy silt and sandy loam ...
Ruijun Qin, Peter Stamp, Walter Richner
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Effect of acid mine drainage on the mineralogy of a dystric cambisol
Geoderma, 2002Abstract Two natural soil profiles non-acidified and acidified with acid mine drainage (AMD) were selected for study. Interactions between acid mine drainage and the soil were evaluated by the changes in the mineral composition applying XRD, transmission electron microscopy (TEM), analytical electron microscopy (AEM), and selective area electron ...
V Šucha +4 more
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Monosaccharide composition of four humus fractions in an Andosol and a Cambisol
Soil Science and Plant Nutrition, 2007Abstract The composition of seven neutral monosaccharides (glucose, galactose, mannose, xylose, arabinose, fucose and rhamnose) released by acid hydrolysis with 0.5 mol L−1 H2SO4 was compared among four humus fractions, including humic acids (HAs), fulvic acids (FAs), water-soluble non-humic substances (WS-NHS; XAD-8-non-adsorbed fraction of the FA ...
Kazuhito Itoh +3 more
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Humic substances of Cambisols of the southern Vitim Plateau
Агрохимия / Agricultural ChemistryAs a result of cryogenic processes in pockets, carbon sequestration occurs, the initially formed humus in the upper soil layers, mechanically entering the illuvial horizon, is deposited at depth, preserving information about its main components. Therefore, we consider it relevant to determine the scale of carbon conservation in humus pocket reservoirs.
E. O. Chimitdorzhieva +1 more
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The occurrence of terrestrial algae on two beech sites on a Cambisol
Zeitschrift für Pflanzenernährung und Bodenkunde, 1998AbstractThe occurrence of terrestrial algae on two beech sites was determined qualitatively and quantitatively in the litter, organic and mineral layer. Both sites are beech stands of different age and the soil type is a Cambisol. On the site with young beech the maximal value determined was 1.0 · 108 algae g−1 dw in the litter layer.
Ingo Wöhler +5 more
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An Andosol–Cambisol toposequence on granite in the Austrian Bohemian Massif
CATENA, 2004In Europe, non-allophanic Andosols are linked with Hercynian basic and metabasic rocks in smoothed highlands with a cool and humid climate. We describe an Andosol-Cambisol toposequence derived from Variscan coarse-grained granite in Northern Austria (Bohemian Massif), where Andosols have formed on plateaus and Cambisols on steep slopes.
Bruno Delvaux +5 more
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Controlling factors for the stability of subsoil carbon in a Dystric Cambisol
Geoderma, 2017Abstract Subsoils store > 50 % of the total global soil organic carbon (SOC), and low SOC content and high mean residence times indicate that subsoils have the potential to sequester additional C on the long-term. Nevertheless, the mechanisms controlling the turnover of SOC in subsoils are poorly understood.
Patrick Wordell-Dietrich +2 more
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