104 citations
Counting papers with at most 25 authors, so collaboration author lists do not stand in for the people here.
- Second Institute of OceanographyCN17 papers
- Zhejiang UniversityCN14 papers
- ETH ZurichCH4 papers
- Texas A&M UniversityUS4 papers
- Universidade Federal do CearáBR4 papers
- Institute for Building MaterialsCH3 papers
- University of California, Los AngelesUS3 papers
- Friedrich-Alexander-Universität Erlangen-NürnbergDE2 papers
- Ningbo UniversityCN2 papers
- State Oceanic AdministrationCN2 papers
- Anhui Provincial Meteorological BureauCN1 paper
- Centre National de la Recherche ScientifiqueFR1 paper
5 papers · 1 filter
Unification of Aeolian and Fluvial Sediment Transport Rate from Granular Physics
Thomas Pähtz, Orencio Durán
One of the physically least understood characteristics of geophysical transport of sediments along sediment surfaces is the well known experimental observation that the sediment tr…
Local Rheology Relation with Variable Yield Stress Ratio across Dry, Wet, Dense, and Dilute Granular Flows
Thomas Pähtz, Orencio Durán, David N. de Klerk +2
Dry, wet, dense, and dilute granular flows have been previously considered fundamentally different and thus described by distinct, and in many cases incompatible, rheologies. We ca…
Universal friction law at granular solid-gas transition explains scaling of sediment transport load with excess fluid shear stress
Thomas Pähtz, Orencio Durán
A key interest in geomorphology is to predict how the shear stress exerted by a turbulent flow of air or liquid onto an erodible sediment bed affects the transport load $M\tild…
Flux saturation length of sediment transport
Thomas Pähtz, Jasper F. Kok, Eric J. R. Parteli +1
Sediment transport along the surface drives geophysical phenomena as diverse as wind erosion and dune formation. The main length-scale controlling the dynamics of sediment erosion…
Analytical model for flux saturation in sediment transport
Thomas Pähtz, Eric J. R. Parteli, Jasper F. Kok +1
The transport of sediment by a fluid along the surface is responsible for dune formation, dust entrainment and for a rich diversity of patterns on the bottom of oceans, rivers, and…