A5054052033- Soil erosion and sediment transport
- Integrated Water Resources Management
- Agriculture, Plant Science, Crop Management
- Hydrology and Sediment Transport Processes
- Aeolian processes and effects
- Botany and Plant Ecology Studies
- Peatlands and Wetlands Ecology
- Waste Management and Environmental Impact
- Landslides and related hazards
- Soil and Unsaturated Flow
- Soil Carbon and Nitrogen Dynamics
- Soil Geostatistics and Mapping
- Geology and Environmental Impact Studies
- Mining and Industrial Processes
- Hydrology and Watershed Management Studies
- Agricultural Engineering and Mechanization
- Renewable energy and sustainable power systems
- Building energy efficiency and sustainability
- Tree Root and Stability Studies
- Transboundary Water Resource Management
- Climate change and permafrost
- Granular flow and fluidized beds
- Geotechnical and Mining Engineering
- Crop Yield and Soil Fertility
- Geotechnical and Geomechanical Engineering
Institute of Agrophysics, Polish Academy of Sciences
1998-2017
Agrophysical Research Institute
2017
Polish Academy of Sciences
2001-2014
Polish Academy of Learning
2010
Abstract On the basis of detailed rill surveys carried out on bare plots different lengths at slopes 12 per cent, basic parameters were derived. Rill width and maximum depth increased with plot length, whereas amount cross‐sectional area, expressed unit remained similar. smaller plots, all rills connected in a continuous transport system reaching outlet, whilst larger (10 20 m long) part ended deposition areas inside plots. Amounts erosion, calculated from volume soil bulk density, compared...
Abstract The effect of topsoil reduction on yields cereals soils developed from loess was evaluated the basis a case study and analysis regional data. Differentiation depended climatic conditions, soil erosion class its location in landscape. results showed tendency towards productivity decrease with losses. greatest decreases were found severely eroded (18 per cent), for very calcareous (25 database. On average, decreased by 3–4·3 cent 10 cm reduction. yield partly compensated increase some...
Abstract Results of soil‐loss assessments on loess‐derived silt soils are presented. The studies were conducted plots different length maintained in continuous bare fallow conditions. Analysing runoff events separately, soil losses per unit area varied with plot length. Description the soil‐erosion process terms (1) maximum loss and (2) effective distance transport allows us to overcome problems data interpretation. Smaller values could then be connected impeded development erosion shorter...
The change of primary forest areas into arable land involves the transformation relief and modification soils. In this study, we hypothesized that relatively flat loess area was largely transformed after use due to erosion. modifications in soil pedons distribution properties were studied 185 years use. Structure solum depth measured 128 texture organic carbon 39 points. Results showed soils noneroded eroded profiles occupied 14 50%, respectively, depositional 36% area. As a consequence,...
Annual variations of soil erodibility silt loam developed from loess based on 10-years runoff plot studies Results experiments carried out two sites the Lublin Upland were presented. Despite similar soils and climatic conditions, showed large differences in annual (K factor USLE) between both sites. Experimentally derived values dependent tillage direction time maintaining runoff-plots fallow conditions. On a site cultivated contour direction, 4-year period was insufficient to achieve K...
Despite recognising the role of tillage erosion in landforms evolution, little research has documented its effects prehistoric times. Herein, an interdisciplinary archaeological-geomorphological experiment with reconstructed tools and management was conducted order to measure when a new field grasslands established Bronze Age-Iron Age. Three wooden ards were based on archaeological findings. They tested cross-tillage experiment, consisting pass perpendicular primary slope (6.5-9.7%), second...
Abstract Complexes formed between clay and soil organic matter are important for carbon sequestration physical quality. Here, we use samples of loessial from South-East Poland to explore the phenomenon complexing in loess. Soil were collected a single catchment 8 years after introduction strip tillage their compositions characterized by traditional methods. Complexing was terms content non-complexed which estimated two ways: firstly, measurement readily-dispersible (which assumed be clay);...