Cargando…
Water induced sediment levitation enhances downslope transport on Mars
On Mars, locally warm surface temperatures (~293 K) occur, leading to the possibility of (transient) liquid water on the surface. However, water exposed to the martian atmosphere will boil, and the sediment transport capacity of such unstable water is not well understood. Here, we present laboratory...
Autores principales: | Raack, Jan, Conway, Susan J., Herny, Clémence, Balme, Matthew R., Carpy, Sabrina, Patel, Manish R. |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2017
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5658360/ https://www.ncbi.nlm.nih.gov/pubmed/29075001 http://dx.doi.org/10.1038/s41467-017-01213-z |
Ejemplares similares
-
Critical dependence of morphodynamic models of fluvial and tidal systems on empirical downslope sediment transport
por: Baar, A. W., et al.
Publicado: (2019) -
The influence of stormwater infiltration on downslope groundwater chemistry
por: Arora, Meenakshi, et al.
Publicado: (2023) -
Validation of a simple diagnostic relationship for downslope flows
por: Cuxart, Joan, et al.
Publicado: (2020) -
Behaviour of Acoustically Levitated Drops in Mid-Water
por: Ruiken, Jan-Paul, et al.
Publicado: (2023) -
In Situ Sampling of Relative Dust Devil Particle Loads and Their Vertical Grain Size Distributions
por: Raack, Jan, et al.
Publicado: (2018)