Long-Term Impact of Wind Erosion on the Particle Size Distribution of Soils in the Eastern Part of the European Union
Status PubMed-not-MEDLINE Jazyk angličtina Země Švýcarsko Médium electronic
Typ dokumentu časopisecké články
Grantová podpora
ITMS2014+ 313011W580
Operational Programme Integrated Infrastructure
09-GASPU-2021
SUA
CEP - Centrální evidence projektů
PubMed
34441075
PubMed Central
PMC8391434
DOI
10.3390/e23080935
PII: e23080935
Knihovny.cz E-zdroje
- Klíčová slova
- GIS, aeolian erosion, decision-making processes, land degradation, landscape entropy and stability, soil protection, sustainable agroecosystems, wind erosion indicators,
- Publikační typ
- časopisecké články MeSH
Wind erosion is the leading cause of soil degradation and air pollution in many regions of the world. As wind erosion is controlled by climatic factors, research on this phenomenon is urgently needed in soil and land management in order to better adapt to climate change. In this paper, the impact of wind erosion on the soil surface in relation to particle size distribution was investigated. Changes in percentage of sand, silt and clay fractions based on historical KPP data (1961-1970), LUCAS data base (2009), and field measurements (2016) were analysed in five cadastral areas impacted by wind erosion (Záhorie Lowlands, Slovakia). With the use of GIS tools, models of spatial distribution of sand, silt, clay and erodible fraction (EF) content were developed based on those measurements. Our findings proved that soil texture change driven by wind erosion could happen relatively quickly, and a significant proportion of soil fine particles may be carried away within a few years. The results indicate that the soil surface became much rougher over the period of more than 50 years, but also that the accumulation of fraction of the silt particles occurred in most of the areas affected by the erosive effect.
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