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Relevant bibliographies by topics / Maximum spreading

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Journal articles

Academic literature on the topic 'Maximum spreading'

Author: Grafiati

Published: 6 September 2023

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Journal articles on the topic "Maximum spreading"

1

Walsh, B. M., D. T. Welling, Y. Zou, and Y. Nishimura. "A Maximum Spreading Speed for Magnetopause Reconnection." Geophysical Research Letters 45, no. 11 (2018): 5268–73. http://dx.doi.org/10.1029/2018gl078230.

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2

Aksoy, Yunus Tansu, Pinar Eneren, Erin Koos, and Maria Rosaria Vetrano. "Spreading of a droplet impacting on a smooth flat surface: How liquid viscosity influences the maximum spreading time and spreading ratio." Physics of Fluids 34, no. 4 (2022): 042106. http://dx.doi.org/10.1063/5.0086050.

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Existing energy balance models, which estimate maximum droplet spreading, insufficiently capture the droplet spreading from low to high Weber and Reynolds numbers and contact angles. This is mainly due to the simplified definition of the viscous dissipation term and incomplete modeling of the maximum spreading time. In this particular research, droplet impact onto a smooth sapphire surface is studied for seven glycerol concentrations between 0% and 100%, and 294 data points are acquired using high-speed photography. Fluid properties, such as density, surface tension, and viscosity, are also me

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3

Liu, Xiaohua, Kaimin Wang, Yaqin Fang, R. J. Goldstein, and Shengqiang Shen. "Study of the effect of surface wettability on droplet impact on spherical surfaces." International Journal of Low-Carbon Technologies 15, no. 3 (2020): 414–20. http://dx.doi.org/10.1093/ijlct/ctz077.

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Abstract The effect of surface wettability on droplet impact on spherical surfaces is studied with the CLSVOF method. When the impact velocity is constant, with the increase in the contact angle (CA), the maximum spreading factor and time needed to reach the maximum spreading factor (tmax) both decrease; the liquid film is more prone to breakup and rebound. When CA is constant, with the impact velocity increasing, the maximum spreading factor increases while tmax decreases. With the curvature ratio increasing, the maximum spreading factor increases when CA is between 30 and 150°, while it decr

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4

Zhang, Xuan, Bingqiang Ji, Xin Liu, Siyu Ding, Xiaomin Wu, and Jingchun Min. "Maximum spreading and energy analysis of ellipsoidal impact droplets." Physics of Fluids 33, no. 5 (2021): 052108. http://dx.doi.org/10.1063/5.0047583.

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5

Fukai, Jun, Mitsuru Tanaka, and Osamu Miyatake. "Maximum Spreading of Liquid Droplets Colliding with Flat Surfaces." JOURNAL OF CHEMICAL ENGINEERING OF JAPAN 31, no. 3 (1998): 456–61. http://dx.doi.org/10.1252/jcej.31.456.

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6

Liang, Gangtao, Yang Chen, Liuzhu Chen, and Shengqiang Shen. "Maximum Spreading for Liquid Drop Impacting on Solid Surface." Industrial & Engineering Chemistry Research 58, no. 23 (2019): 10053–63. http://dx.doi.org/10.1021/acs.iecr.9b02014.

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7

Börnhorst, Marion, Xuan Cai, Martin Wörner, and Olaf Deutschmann. "Maximum Spreading of Urea Water Solution during Drop Impingement." Chemical Engineering & Technology 42, no. 11 (2019): 2419–27. http://dx.doi.org/10.1002/ceat.201800755.

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8

Ashikhmin, Alexander, Nikita Khomutov, Roman Volkov, Maxim Piskunov, and Pavel Strizhak. "Effect of Monodisperse Coal Particles on the Maximum Drop Spreading after Impact on a Solid Wall." Energies 16, no. 14 (2023): 5291. http://dx.doi.org/10.3390/en16145291.

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The effect of coal hydrophilic particles in water-glycerol drops on the maximum diameter of spreading along a hydrophobic solid surface is experimentally studied by analyzing the velocity of internal flows by Particle Image Velocimetry (PIV). The grinding fineness of coal particles was 45–80 μm and 120–140 μm. Their concentration was 0.06 wt.% and 1 wt.%. The impact of particle-laden drops on a solid surface occurred at Weber numbers (We) from 30 to 120. It revealed the interrelated influence of We and the concentration of coal particles on changes in the maximum absolute velocity of internal

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9

Grevemeyer, Ingo, Nicholas W. Hayman, Dietrich Lange, et al. "Constraining the maximum depth of brittle deformation at slow- and ultraslow-spreading ridges using microseismicity." Geology 47, no. 11 (2019): 1069–73. http://dx.doi.org/10.1130/g46577.1.

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Abstract The depth of earthquakes along mid-ocean ridges is restricted by the relatively thin brittle lithosphere that overlies a hot, upwelling mantle. With decreasing spreading rate, earthquakes may occur deeper in the lithosphere, accommodating strain within a thicker brittle layer. New data from the ultraslow-spreading Mid-Cayman Spreading Center (MCSC) in the Caribbean Sea illustrate that earthquakes occur to 10 km depth below seafloor and, hence, occur deeper than along most other slow-spreading ridges. The MCSC spreads at 15 mm/yr full rate, while a similarly well-studied obliquely open

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10

Li, Siqi, Hourong Yu, and Haisheng Fang. "Experimental study of liquid droplets impact on powder surface: The application of effective dimensionless parameters in analysis." E3S Web of Conferences 341 (2022): 01011. http://dx.doi.org/10.1051/e3sconf/202234101011.

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Spreading dynamics of liquid droplets impacting onto powder bed are experimentally studied using high-speed photography. Dimensionless numbers—We, Re, the modified We* and Re∗ corrected by substrate deformation—are used to analyze the impact behaviors of droplets. The spreading time and the maximum spreading factor are further analyzed. The spreading time is accurately described by a universal scaling law that is obtained from the modified dimensionless time vs. the effective Weber number (We∗), and the maximum spreading factor is found to follow the modified classic scaling law βmax = f(We*,

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