As Particle size increases the angle is repose decrease. Reason being, smaller particles have dominant cohesive and adhesive forces as compared to particle weight whereas in bigger particles gravity plays a dominant role so less repose angle.
As particle size in increases, capillarity decreases
particle size
with a set of sieves
soil ferility
increases
The angle of repose for fertilizer in bulk can vary depending on factors such as the type of fertilizer, particle size, and moisture content. Generally, it can range from 25 to 45 degrees. Testing is recommended to determine the specific angle of repose for a particular fertilizer product.
The three main factors that affect the angle of repose are particle shape, size distribution, and surface roughness. A particle's shape influences how particles stack together, with angular particles generally forming steeper angles. Smaller particle sizes typically lead to flatter angles, while surface roughness can impact the interlocking and sliding of particles.
No, dry boulders do not support the steepest angle of repose. The steepest angle of repose is supported by finer-grained dry materials such as sand or gravel, which can stack at angles close to the natural angle of repose. Dry boulders are less likely to form stable piles at steep angles due to their size and irregular shapes.
Size, Shape , and Weight Your Welcome :)
the composition ,size ,weight and shape .
Yes, the angle of repose for dry sand is the maximum angle at which sand can remain stable without collapsing. It is influenced by factors such as grain size, shape, and moisture content, and can vary depending on the specific characteristics of the sand material.
The submerged angle of repose of sand refers to the maximum angle at which submerged sand particles can stack up without further movement or slumping. It typically ranges from 25 to 37 degrees depending on factors like grain size and water content.
anung sagot?
Smaller the particle, faster the dissolution. By the way, you spelled dissolution incorrectly.
crystallite is the average size of the particle whereas the particle size denotes the individual size of the particle.
The more a solution is agitated, the faster the rate of the solution The smaller the particle size, the faster it will dissolve The higher the temperature, the faster rate of dissolving
Charles L. Mader has written: 'Numerical modeling of the effect of particle size of explosives on shock initiation properties' -- subject(s): Particle size, Explosives, Shock waves