Materials Map

Discover the materials research landscape. Find experts, partners, networks.

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The Materials Map is an open tool for improving networking and interdisciplinary exchange within materials research. It enables cross-database search for cooperation and network partners and discovering of the research landscape.

The dashboard provides detailed information about the selected scientist, e.g. publications. The dashboard can be filtered and shows the relationship to co-authors in different diagrams. In addition, a link is provided to find contact information.

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The Materials Map is still under development. In its current state, it is only based on one single data source and, thus, incomplete and contains duplicates. We are working on incorporating new open data sources like ORCID to improve the quality and the timeliness of our data. We will update Materials Map as soon as possible and kindly ask for your patience.

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in Cooperation with on an Cooperation-Score of 37%

Topics

Publications (1/1 displayed)

  • 2017The differences in crown formation during the splash on the thin water layers formed on the saturated soil surface and model surface.23citations

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Chart of shared publication
Sochan, Agata
1 / 1 shared
Ryżak, Magdalena
1 / 1 shared
Polakowski, Cezary
1 / 2 shared
Bieganowski, Andrzej
1 / 1 shared
Mazur, Rafał
1 / 4 shared
Chart of publication period
2017

Co-Authors (by relevance)

  • Sochan, Agata
  • Ryżak, Magdalena
  • Polakowski, Cezary
  • Bieganowski, Andrzej
  • Mazur, Rafał
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article

The differences in crown formation during the splash on the thin water layers formed on the saturated soil surface and model surface.

  • Sochan, Agata
  • Ryżak, Magdalena
  • Polakowski, Cezary
  • Bieganowski, Andrzej
  • Beczek, Michał
  • Mazur, Rafał
Abstract

Splash is the first stage of a negative phenomenon-soil erosion. The aim of this work was to describe the crown formation quantitatively (as part of the splash erosion) and compare the course of this phenomenon on the thin water film formed on a smooth glass surface and on the surface of saturated soil. The height of the falling water drop was 1.5 m. The observation of the crowns was carried out by high-speed cameras. The static and dynamic parameters of crown formation were analysed. It was found that the crowns formed on the water film covering the saturated soil surface were smaller and the time intervals of their existence were shorter. In addition, the shapes of the crowns were different from those created on the water layer covering the glass surface. These differences can be explained by the slightly different values of surface tension and viscosity of the soil solution, the greater roughness of the soil surface and the lower thickness of the water film on the soil surface.

Topics
  • impedance spectroscopy
  • surface
  • glass
  • glass
  • viscosity