raindrop impact
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CATENA ◽  
2021 ◽  
Vol 207 ◽  
pp. 105603
Author(s):  
N. Sadeghian ◽  
A.R. Vaezi ◽  
A. Majnooniheris ◽  
A. Cerdà

2021 ◽  
Vol 1 (1) ◽  
Author(s):  
Moritz Lehmann ◽  
Lisa Marie Oehlschlägel ◽  
Fabian P. Häusl ◽  
Andreas Held ◽  
Stephan Gekle

AbstractRaindrops impacting water surfaces such as lakes or oceans produce myriads of tiny droplets which are ejected into the atmosphere at very high speeds. Here we combine computer simulations and experimental measurements to investigate whether these droplets can serve as transport vehicles for the transition of microplastic particles with diameters of a few tens of μm from ocean water to the atmosphere. Using the Volume-of-Fluid lattice Boltzmann method, extended by the immersed-boundary method, we performed more than 1600 raindrop impact simulations and provide a detailed statistical analysis on the ejected droplets. Using typical sizes and velocities of real-world raindrops – parameter ranges that are very challenging for 3D simulations – we simulate straight impacts with various raindrop diameters as well as oblique impacts. We find that a 4mm diameter raindrop impact on average ejects more than 167 droplets. We show that these droplets indeed contain microplastic concentrations similar to the ocean water within a few millimeters below the surface. To further assess the plausibility of our simulation results, we conduct a series of laboratory experiments, where we find that microplastic particles are indeed contained in the spray. Based on our results and known data – assuming an average microplastic particle concentration of 2.9 particles per liter at the ocean surface – we estimate that, during rainfall, about 4800 microplastic particles transition into the atmosphere per square kilometer per hour for a typical rain rate of $10 \frac {\text {mm}}{\mathrm {h}}$ 10 mm h and vertical updraft velocity of $0.5 \frac {\mathrm {m}}{\mathrm {s}}$ 0.5 m s .


Author(s):  
S. Pulley ◽  
C. Morten ◽  
S. Morgan ◽  
L. M. Cardenas ◽  
A. L. Collins

2021 ◽  
Author(s):  
Weifei Hu ◽  
Weiyi Chen ◽  
Xiaobo Wang ◽  
Yeqing Wang ◽  
Zhenyu Liu ◽  
...  

Author(s):  
Leal K. Lauderbaugh ◽  
Roser M. Ginebra-Solanellas ◽  
Curtis D. Holder ◽  
Rebecca Webb

2021 ◽  
Author(s):  
Peter Kinnell

<p>Raindrop driven erosion – what is in the black box ?</p><p>P.I.A. Kinnell</p><p>Faculty of Science and Technology, University of Canberra, Canberra, Australia</p><p>Many experiments applying rainfall to produce erosion on soil surfaces consider the inputs and outputs in a black box situation where little or no consideration is given to the actual mechanisms controlling erosion. It is well known that rainfall erosion is caused by raindrop impact and flow forces acting singly or together. Raindrops impacting directly or through surface water detaches soil material from where it is held within the soil surface by cohesion and inter-particle friction  and erosion occurs if the detached material is transported away from the site of detachment. The movement of detached material downslope may be in the air by splash or more importantly in surface water flows where raindrop impact may induce coarse sediment may to move when sediment transport normally associated with undisturbed flow does not occur. These transport processes vary in space and time during laboratory and field experiments. How this influences the amounts of soil loss during these experiments is the subject of  this presentation .</p>


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