scholarly article | Q13442814 |
P819 | ADS bibcode | 2018JGRB..123.3747W |
P356 | DOI | 10.1029/2018JB015530 |
P50 | author | Michael Manga | Q6832487 |
Olivier Roche | Q58460927 | ||
P2093 | author name string | T. Dubois | |
A. Weit | |||
P2860 | cites work | Effect of particle volume fraction on the settling velocity of volcanic ash particles: insights from joint experimental and numerical simulations | Q30833592 |
Saharan dust storms: nature and consequences | Q56531638 | ||
Eine neue Bestimmung der Moleküldimensionen | Q56555256 | ||
The Viscosity of Concentrated Suspensions and Solutions | Q56555259 | ||
Role of pore pressure gradients in sustaining frontal particle entrainment in eruption currents: The case of powder snow avalanches | Q57872178 | ||
Multiphase-flow numerical modeling of the 18 May 1980 lateral blast at Mount St. Helens, USA | Q58080986 | ||
The role of gravitational instabilities in deposition of volcanic ash | Q58081817 | ||
Addressing complexity in laboratory experiments: the scaling of dilute multiphase flows in magmatic systems | Q59765283 | ||
Experimental study of turbulence, sedimentation, and coignimbrite mass partitioning in dilute pyroclastic density currents | Q59794958 | ||
Heavy Particle Concentration in Turbulence at Dissipative and Inertial Scales | Q60557468 | ||
Emplacement of massive turbidites linked to extinction of turbulence in turbidity currents | Q61042135 | ||
The rheology of hard sphere suspensions at arbitrary volume fractions: An improved differential viscosity model | Q83292115 | ||
P433 | issue | 5 | |
P304 | page(s) | 3747-3761 | |
P577 | publication date | 2018-05-01 | |
P1433 | published in | Journal of Geophysical Research: Solid Earth | Q27726642 |
P1476 | title | Experimental Measurement of the Solid Particle Concentration in Geophysical Turbulent Gas-Particle Mixtures | |
P478 | volume | 123 |
Q100464418 | Acoustic probing of the particle concentration in turbulent granular suspensions in air |
Q104495299 | Dynamics of large pyroclastic currents inferred by the internal architecture of the Campanian Ignimbrite |
Search more.