Renata Kołodyńska‐Gawrysiak
Biographic Data
| ID | 6571866 |
|---|---|
| NAME | Renata Kołodyńska‐Gawrysiak |
| GIVEN NAMES | Renata |
| FAMILY NAME | Kołodyńska‐Gawrysiak |
| SIGNATURE | GAWRYSIAK R K |
| AFFILIATIONS | Maria Curie-Skłodowska University |
| ORCID | 0000-0003-0360-7556 |
| VERIFIED | Yes |
| TOTAL WORKS | 4 |
| TOTAL CITATIONS | 1 |
| WORKS AS AUTHOR | 4 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2016 |
| LATEST PUBLICATION YEAR | 2026 |
| H-INDEX | 1 |
Land Use and Topographical Factors Controlling Collapsed Pipes and Piping‐Related Features Development in the Landscapes of Thick Loess Covers From Eastern Poland
Piping is subsurface water erosion that resulted in the formation of collapsed pipes and piping‐related features in the landscape. Although it is an important and globally widespread land degradation process it is still poorly understood and data is scarce. Loess landscapes with varied topography and long‐term agricultural use of silty soils are particularly susceptible to water surface and subsurface (piping) erosion, resulting in gully network …
The impact of natural closed depressions on soil organic carbon storage in eroded loess landscapes of East Poland
Soil erosion in loess landscapes results in soil organic carbon (SOC) redistribution and storage in SOC pools. Understanding the SOC dynamics is important because changes in the SOC stocks may have impacts on global climate change. However, the topographic‐related patterns controlling SOC storage are not well understood. Closed depressions are natural landforms in loess landscapes and preserve buried Holocene soils and SOC‐rich colluvia resulting…
Holocene evolution of closed depressions and its relation to landscape dynamics in the loess areas of Poland
Past Pleistocene topography of the loess uplands is rich in local sinks (closed depressions (CDs)) influencing sediment fluxes. Soil-sediment sequences from CDs constituting geoarchives where landscape changes under natural and anthropogenic conditions have been recorded. Pedo-sedimentary archives from 10 CDs in the Polish loess belt and human settlements were analysed. Phases of the Holocene evolution of the CDs were correlated with landscape dy…
Geotourist values of loess geoheritage within the planned Geopark Małopolska Vistula River Gap, E Poland
Holocene evolution of closed depressions and its relation to landscape dynamics in the loess areas of Poland
Past Pleistocene topography of the loess uplands is rich in local sinks (closed depressions (CDs)) influencing sediment fluxes. Soil-sediment sequences from CDs constituting geoarchives where landscape changes under natural and anthropogenic conditions have been recorded. Pedo-sedimentary archives from 10 CDs in the Polish loess belt and human settlements were analysed. Phases of the Holocene evolution of the CDs were correlated with landscape dy…
Geotourist values of loess geoheritage within the planned Geopark Małopolska Vistula River Gap, E Poland
Holocene evolution of closed depressions and its relation to landscape dynamics in the loess areas of Poland
Past Pleistocene topography of the loess uplands is rich in local sinks (closed depressions (CDs)) influencing sediment fluxes. Soil-sediment sequences from CDs constituting geoarchives where landscape changes under natural and anthropogenic conditions have been recorded. Pedo-sedimentary archives from 10 CDs in the Polish loess belt and human settlements were analysed. Phases of the Holocene evolution of the CDs were correlated with landscape dy…
The impact of natural closed depressions on soil organic carbon storage in eroded loess landscapes of East Poland
Soil erosion in loess landscapes results in soil organic carbon (SOC) redistribution and storage in SOC pools. Understanding the SOC dynamics is important because changes in the SOC stocks may have impacts on global climate change. However, the topographic‐related patterns controlling SOC storage are not well understood. Closed depressions are natural landforms in loess landscapes and preserve buried Holocene soils and SOC‐rich colluvia resulting…
Land Use and Topographical Factors Controlling Collapsed Pipes and Piping‐Related Features Development in the Landscapes of Thick Loess Covers From Eastern Poland
Piping is subsurface water erosion that resulted in the formation of collapsed pipes and piping‐related features in the landscape. Although it is an important and globally widespread land degradation process it is still poorly understood and data is scarce. Loess landscapes with varied topography and long‐term agricultural use of silty soils are particularly susceptible to water surface and subsurface (piping) erosion, resulting in gully network …
Loess (4 works) · Erosion (3 works) · Geology (3 works) · Geomorphology (3 works) · Soil erosion and sediment transport (3 works) · Archaeology (2 works) · Environmental Science (2 works) · Geography (2 works) · Landform (2 works) · Physical geography (2 works)