ORIGINAL PAPER
The impact of colluvial processes on the properties of organic and organic-mineral soils: a case study of a section of the river valley in the Izerskie Foothills, SW Poland
1
Wrocław University of Environmental and Life Sciences, Institute of Soil Science, Plant Nutrition and Environmental Protection, ul. Grunwaldzka 53, 50-375 Wrocław, Poland
2
Nicolaus Copernicus University in Toruń, Department of Soil Science and Spatial Management, ul. Lwowska 1, 87-100, Toruń, Poland
These authors had equal contribution to this work
Submission date: 2025-07-16
Final revision date: 2026-02-12
Acceptance date: 2026-05-11
Online publication date: 2026-05-11
Publication date: 2026-05-11
Corresponding author
Adam Bogacz
Instytut Nauk o Glebie i Ochrony Środowiska, Uniwersytet Przyrodniczy we Wrocławiu, ul. Grunwaldzka 53, 50-357, Wrocław, Polska
Instytut Nauk o Glebie i Ochrony Środowiska, Uniwersytet Przyrodniczy we Wrocławiu, ul. Grunwaldzka 53, 50-357, Wrocław, Polska
Soil Sci. Ann., 2026, 77(2)221683
KEYWORDS
ABSTRACT
The use of soils in foothill areas and the drying of existing peatlands have, in many cases, led to denudation and degradation of the terrain. Research conducted in the Czarny Potok valley in the Izerskie Foothills examined the impact of colluvial processes on changes in soil structure and properties in extensive meadows, forests, and fallow land. Seven soil profiles were described, and 44 soil samples (including 24 organic samples) were collected for analysis of total organic carbon (TOC), total nitrogen (TN), water-extractable organic carbon (WEOC), and water-extractable total nitrogen (WETN). The soils were classified as Histosols and Gleysols (IUSS Working Group WRB, 2022) and as peat, mursh and gley soils (SPG6, 2019). In the surface layers of some soils, a low MtI and MtII medium mursh formation process was observed. Organic soils consisted of hemic and sapric materials; no fibric material was identified. Colluvial horizons were mainly composed of loam, silt loam and sandy loam. The results indicated that silting reduces the concentration of labile forms of organic matter (WEOC and WETN) in surface horizons compared to unsilted peat horizons. Low TOC/TN ratios and reduced concentrations of labile components in peat suggest increased biological activity and mineralisation of organic matter. In this case soil siltation did not increase their trophic status.
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