Percolation is the amount of water that enters soil during a given timeframe. Different soil types have different rates and the size of the particle affect how quickly the water will penetrate the water.
The particle size,temperature and agitation affect the rate at which a substance will disolve in a solution.
Mean particle size=0.94*Lambda/(FWHM*cos(theta)
If you were to graph particle size and porosity, it would be a constant slope (horizontal line).Porosity is not affected by particle size.
1cm
As particle size in increases, capillarity decreases
As long as the spaces between the particles are connected, the smaller the particles, the higher the capillarity. The larger the particles, the lower the capillarity.Particle size and capillarity are inversely, or negatively related.
capillarity
Percolation is the amount of water that enters soil during a given timeframe. Different soil types have different rates and the size of the particle affect how quickly the water will penetrate the water.
Particle size affects solubility. When particle size is small, the surface area per unit volume is larger, thus the solubility is increased.
The bigger the particle size, the more drainage the soil would have. The smaller the particle sizer, the less drainage the soil would have. ITS EASY
Size matters
The higher the wind speed, the bigger the particle size.
The bigger the particle the lesser the dissolution.
crystallite is the average size of the particle whereas the particle size denotes the individual size of the particle.
the deepest will be at the very bottom
Smaller particle sizes generally result in faster percolation rates because there is less resistance to the flow of liquids through the smaller spaces between the particles. Larger particles create more void spaces and can slow down the percolation rate as the liquid has to travel through these larger spaces. Therefore, finer particles allow liquid to flow more quickly compared to coarser particles.