All Stories

  1. Evolution of river planforms downstream of dams: Effect of dam construction or earlier human-induced changes?
  2. The formation of an anabranching planform in a sandy floodplain by increased flows and sediment load
  3. The influence of meander bend evolution on the formation of multiple cutoffs: findings inferred from floodplain architecture and bend geometry
  4. Analysis of fluvial, lacustrine and anthropogenic landforms by means of ground-penetrating radar (GPR): field experiment
  5. Reconstruction of anastomosing river course by means of geophysical and remote sensing surveys (the middle obra valley, western poland)
  6. Holocene evolution of meander bends in lowland river valley formed in complex geological conditions (the obra river, poland)
  7. Transformation of a lowland river from a meandering and multi-channel pattern into an artificial canal: retracing a path of river channel changes (the Middle Obra River, W Poland)
  8. GPR and aerial imageries to identify the recent historical course of the Obra River and spatial extent of Obrzańskie Lake, altered by hydro-technical works
  9. Influence of measurement conditions on depth range and resolution of GPR images: The example of lowland valley alluvial fill (the Obra River, Poland)
  10. Changes of river bed pattern of a lowland river: effect of natural processes or anthropogenic intervention?
  11. Anthropogenic transformation of lowland river pattern and changes of spatial extent of lakes inferred from ground-penetrating radar and remote sensing surveys (the Obra River, Poland)
  12. Reconstructing migration phases of meandering channels by means of ground-penetrating radar (GPR): the case of the Obra River, Poland
  13. Changes of river bed pattern and traces of anthropogenic intervention: The example of using GPR method (the Obra River, western Poland)
  14. Types of sedimentary environment in alluvial sediments distinguished on the basis of its chemical constitution: the example of the lower course of the Obra river (Western Poland)
  15. Changes of chromium concentration in alluvial sediments of the Obra river valley