Evolution of rock cover, surface roughness, and flow velocity on stony soil under simulated rainfall

2020 ◽  
Vol 75 (5) ◽  
pp. 651-668
Author(s):  
L. Li ◽  
M.A. Nearing ◽  
V.O. Polyakov ◽  
M.H. Nichols ◽  
M.L. Cavanaugh
Geoderma ◽  
2020 ◽  
Vol 379 ◽  
pp. 114622
Author(s):  
Li Li ◽  
Mark A. Nearing ◽  
Viktor O. Polyakov ◽  
Mary H. Nichols ◽  
Frederick B. Pierson ◽  
...  

2013 ◽  
Vol 56 (2) ◽  
pp. 505-514 ◽  
Author(s):  
Jan Vermang ◽  
L. Darrell Norton ◽  
Jan M. Baetens ◽  
Chi-hua Huang ◽  
Wim M. Cornelis ◽  
...  

2008 ◽  
Vol 348 (1-2) ◽  
pp. 1-12 ◽  
Author(s):  
L. Tatard ◽  
O. Planchon ◽  
J. Wainwright ◽  
G. Nord ◽  
D. Favis-Mortlock ◽  
...  

2021 ◽  
Vol 287 ◽  
pp. 03003
Author(s):  
Sampath Emani ◽  
M. Ramasamy ◽  
Ku Zilati Ku Shaari

One of the major concerns in petroleum refinery preheat trains is identified as fouling. Fouling impacts the refinery economics and environment heavily. Various approaches to mitigate fouling have not yielded the desired results. This is due to lack of understanding on the effect of influencing forces on crude oil fouling in heat exchangers. Therefore, this study attempts to investigate the effects of various forces such as gravity, Saffman Lift, drag and thermophoretic on crude oil fouling in heat exchangers through Computational Fluid Dynamics (CFD) simulations. From the simulations, it is observed that the higher particle size and particle concentration resulted in higher deposition of particles. Deposition velocities increase for larger sized particles and decrease for small and medium sized particles. The Increased flow velocities and surface roughness increases wall shear and mitigate fouling. Lower temperature gradients at the heat exchanger surface decreases deposition rates due to high thermophoretic forces. The mass deposition rate is reduced by 10.3 and 16.9% with 0.03 and 0.05 Pa, respectively, for 0.14 m/s flow velocity. Also, the mass deposition rate is reduced by 15.6 and 25.1% with 0.03 and 0.05 Pa, respectively, for 0.47 m/s flow velocity. With increased surface roughness from 0.03 to 0.05 mm, the mass deposition rate is reduced by 11.48 and 19.18%, respectively, for 0.14 m/s flow velocity. Also, for 0.47 m/s flow velocity, the mass deposition rate is reduced by 18.84 and 32.92% for 0.03- and 0.05-mm surface roughness, respectively.


Author(s):  
Franz Ramstorfer ◽  
Bernd Breitscha¨del ◽  
Helfried Steiner ◽  
Gu¨nter Brenn

The subject of the present work is the modelling of the liquid streamwise flow velocity in the two-phase boundary layer in subcooled boiling flow under the influence of the vapor bubbles. Subcooled boiling flow experiments were carried out in a horizontal test channel in order to investigate the interaction between the bubbles and the liquid phase. The heater surface was located at the bottom of the test channel. The near-wall liquid flow velocity was measured using a two-component laser-Doppler anemometer. Based on the experimental data a model is proposed to describe the impact of the gaseous phase on the motion of the liquid in the subcooled boiling regime. It was observed that the axial velocity profiles near the wall follow a logarithmic law similar to that used in turbulent single-phase flow over rough surfaces. Based on this finding it is suggested to model the influence of the bubbles on the liquid flow analogously to the effect of a surface roughness. The correlation developed for an equivalent surface roughness associated with the bubbles yields good agreement of the modeled axial velocity profiles with the experimental data.


Geoderma ◽  
2018 ◽  
Vol 321 ◽  
pp. 1-7 ◽  
Author(s):  
Xiaohui Zhuang ◽  
Wei Wang ◽  
Yuying Ma ◽  
Xingfa Huang ◽  
Tingwu Lei

Bragantia ◽  
2010 ◽  
Vol 69 (suppl) ◽  
pp. 141-152 ◽  
Author(s):  
Eva Vidal Vázquez ◽  
Ildegardis Bertol ◽  
Glécio Machado Siqueira ◽  
Jorge Paz-Ferreiro ◽  
Jorge Dafonte Dafonte

The objective of this work was to investigate the decay of initial surface roughness induced by simulated rainfall under different soil residue cover and to compare classical statistical indices with geostatistical parameters. A conventionally tilled loamy soil with low structure stability, thus prone to crusting was placed at 1 m² microplots. Each microplot received three successive rainfall events which bring about cumulative 25 mm, 50 mm and 75 mm at 65 mm h-1 intensity. Five treatments without replication were tested with different corn straw quantities (0, 1, 2, 3 and 4 Mg ha"1). Soil surface microrelief was measured at the initial stage and after each simulated rainfall event. Five treatments and four surface stages were monitored, resulting in 20 data sets. Point elevation data were taken at 0.03 m intervals using a pinmeter. Digital elevation models were generated and analysed using semivariograms. All data sets showed spatial dependence and spherical models were fitted to experimental semivariograms. A very significant relationship was found between the random roughness index, RR, and the sill of the semivariogram (C0+C1). All the treatments showed a clear trend to sill value reduction with increasing precipitation. However, roughness decay was lower in treatments with higher straw cover (3 and 4 Mg ha-1). Therefore, residue cover limited soil surface roughness decline. The control treatment, without straw, showed the lowest nugget effect (C0), which means the lowest spatial discontinuity of all treatments in this study. The range of spatial dependence (a) also showed a trend to decrease with increased cumulative rain, which was most apparent in treatments without or with relatively low straw cover (0, 1 and 2 Mg ha-1). The suitability of using sill variance and range for describing patterns of soil surface microrelief decline is discussed.


2012 ◽  
Vol 26 (24) ◽  
pp. 3779-3787 ◽  
Author(s):  
Guanhua Zhang ◽  
Guobin Liu ◽  
Guoliang Wang ◽  
Yuxia Wang

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