Without overland flow, soil particle sizes in the range of 110-1,450 mu m were most susceptible to detachment. With overland flow, the susceptible size range was 219-2,034 mu m.doi:10.2136/sssaj1973.03615995003700040042xFarmer, Eugene E
1992. Analysis of soil textural porosity relative to skeleton particle size, using mercury porosimetry. Soil Science Society of America Journal, 56, 1062-1067.Fies, J., 1992. Analysis of soil textural porosity relative to skeleton particle size, using mercury porosimetry. Soil Sci. Soc. Am. J...
To investigate the effect of mean particle size D50 on the sand–steel interface, the soil sample was sieved into three ranges: 2–1.18 mm (sample A), 1.18–0.85 mm (sample B), and 0.85–0.425 mm (sample C), as shown in Fig. 1, with each range of the soil sample ...
In contrast to the success in using field soil data for age differentiation, laboratory data on particle-size distribution, organic matter, and pH were not consistently useful. Both the oldest Polar Desert soils and the Arctic Brown soils are Inceptisols, and for till sequences the progression ...
Influence of rate of hydraulic gradient on washed-out soil mass due to perpendicular contact erosion or poor filter design (accepted) To P, Scheuermann A, Williams DJ (2018) Quick assessment on susceptibility to suffusion of continuously graded soils by curvature of particle size distribution. Acta...
(Supplementary Fig.6). This limited effect might be attributed to the lowSavalues during this observation. Supplementary Fig.7apresents the observed particle size distribution of NR-PM1, showing a significant increase in the number concentration of particles in the size range of 14–200 nm ...
We use a synoptic sampling of stream water to quantify the effect of soil type, rock type, deforestation extent determined by Landsat TM imagery, and urban... TW Biggs,T Dunne,TF Domingues,... - 《Water Resources Research》 被引量: 135发表: 2002年 Diffusion and Partitioning of Solutes in...
In the case of unsaturated soils, in addition to other parameters such as void ratio, void distribution, particle size distribution and initial density the degree of saturation also affects the permeability coefficient of water. The degree of saturation, in unsaturated soil, is directly related to ...
Numerical simulation mostly calculates relative permeability with a pore network model or a water retention curve to explore hydrate growth habits and pore-filling characteristics and the effect of various factors such as particle size, hydrate saturation, wettability, and interface tension and their ...
Numerical simulation mostly calculates relative permeability with a pore network model or a water retention curve to explore hydrate growth habits and pore-filling characteristics and the effect of various factors such as particle size, hydrate saturation, wettability, and interface tension and their ...