Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Stanisław Maciejewski"'
Publikováno v:
Geological Quarterly.
Autor:
Wioletta Gorczewska-Langner, Danuta Leśniewska, Rafał Ossowski, Witold Tisler, Adam Szymkiewicz, Stanisław Maciejewski
Publikováno v:
Computational Geosciences. 23:325-337
Flow in flood dikes, earth dams, and embankments occurs in variably saturated conditions, with pores of the earth material filled partly with water and partly with air. In routine engineering analysis, the influence of pore air is neglected and the a
Publikováno v:
Journal of Hydrology. 375:566-577
Summary In this paper, five model approaches with different physical and mathematical concepts varying in their model complexity and requirements were applied to identify the transport processes in the unsaturated zone. The applicability of these mod
Autor:
Stanisław Maciejewski
Publikováno v:
Journal of Contaminant Hydrology. 14:193-206
The results of a study on the hydrodynamic dispersion of ionic solutes in unsaturated porous media are presented. This study concerns the description of solute transport in moving coordinates, the application of the radiometric method to measure the
Autor:
Willibald Stichler, Piotr Małoszewski, Stanisław Maciejewski, Christine Stumpp, Peter Trimborn, Dietmar Klotz
Publikováno v:
Hydrol. Sci. J. 51, 298-313 (2006)
Seven experimental lysimeters were filled with different soil materials and used to study water flow and tracer transport through the unsaturated zone under natural atmospheric conditions during an eight year period (1984–1991). The study of soil c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::298eb05999f24a81db46dad32974c899
https://push-zb.helmholtz-muenchen.de/frontdoor.php?source_opus=5362
https://push-zb.helmholtz-muenchen.de/frontdoor.php?source_opus=5362
Publikováno v:
Hydrol. Sci. J. 51, 285-297 (2006)
Over an eight-year period (1984–1991), seven experimental lysimeters filled with different soil materials from the State of Bavaria (quartz and tertiary sands, quartz and fluvioglacial gravels) were used to study water flow and tracer transport thr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::78c4290b49308905a98c16ed58438222
https://push-zb.helmholtz-muenchen.de/frontdoor.php?source_opus=5145
https://push-zb.helmholtz-muenchen.de/frontdoor.php?source_opus=5145