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22o is the angle of repose.

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22o is the angle of repose.

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yes, angle of friction is equal to angle of repose.

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Angle of repose is equal to angle of friction.

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Q. What is angle of repose for lime stone?

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It is the Emptying Angle of Repose that is greater than the Filling Angle of Repose.

It is always the greater of the two Angles of Repose.

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The angle of repose for dry shelled corn is 23 degrees or a tangent of .42

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Angle of Repose - novel - was created in 1971.

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it is as like as viscous liquid so the angle of repose for it under 30 deg

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The angle of repose is the angle on the sides of a substance, like sand, when it is poured out and forms a heap. The angle of repose of desert sand is the same as the angle of the sides of a pyramid.

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The angle of repose for salt is typically around 30 to 40 degrees, which means that salt will naturally form a pile with this angle when poured onto a flat surface before sliding or spilling.

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linear relationship because as the cars index is increased angle of repose also increases.

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The angle of friction refers to the maximum angle at which an object can rest on a surface without sliding, while the angle of repose is the maximum angle at which a pile of granular material remains stable without collapsing or sliding. The angle of friction is specific to an object on a surface, while the angle of repose is more related to the stability of a pile of material.

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The angle of repose for steel chips can vary depending on factors such as the size, shape, and surface characteristics of the chips. Generally, the angle of repose for steel chips is between 30 to 45 degrees. Experimental testing may be needed to determine the specific angle of repose for a particular type of steel chip.

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The angle of repose of iron ore can vary depending on factors such as particle size, shape, and moisture content. In general, the angle of repose for iron ore is typically around 35-45 degrees.

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The angle of repose of rice grains typically ranges from 30 to 40 degrees. This angle represents the maximum angle at which a pile of rice grains can remain stable without sliding. The angle of repose can vary depending on factors such as grain size, shape, and moisture content.

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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.

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The angle of repose is the maximum angle at which a granular material can be piled without slumping. The shape, size, density, and moisture content of the material all influence the angle of repose. Factors such as interparticle friction, cohesion, and particle shape affect the angle at which the material will naturally settle.

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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.

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I believe about 20 degrees.

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lentils ange of respose

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The three characteristics of a material that affect its angle of repose are particle size, shape, and surface roughness. Finer particles tend to have a lower angle of repose than coarser particles. Irregularly shaped particles may have a higher angle of repose compared to spherical particles. Lastly, materials with rough surfaces tend to have a higher angle of repose due to increased interlocking between particles.

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Yes, they do. And this angle of repose will be different for different materials, the particle sizes and the moisture content.

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Smaller particle sizes tend to have a lower angle of repose, meaning they can form steeper piles before slumping. Larger particle sizes typically result in a higher angle of repose, indicating a shallower pile angle before slumping occurs. This relationship is due to factors such as interparticle friction and cohesion.

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The density of a material can influence its size of repose by affecting how closely packed the particles are. Higher density materials tend to have smaller size of repose because their particles can fit more tightly together, leading to a steeper angle of repose. Conversely, lower density materials have a larger size of repose due to their looser particle arrangement, resulting in a shallower angle of repose.

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It is a beautiful heavenly female at rest.

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Movement of a material will occur if the angle of repose is increased by the addition of material, or if friction is decreased by oversaturation of the material, or in the event of a ground moving event.

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Movement of a material will occur if the angle of repose is increased by the addition of material, or if friction is decreased by oversaturation of the material, or in the event of a ground moving event.

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The angle of repose of pumpkin seeds would be different depending on whether they are freshly removed from the pumpkin, whether they have been cleaned, whether they have been dried, and whether they have been "roasted."

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I believe you mean the angle of repose and it differs slightly depending on the type of sand.

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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.

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The angle of repose of iron ore typically ranges from 30 to 45 degrees. This angle represents the steepest angle at which unconsolidated material can remain stable without sliding or collapsing. However, the exact angle can vary depending on factors such as the particle size and shape of the iron ore.

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An increase in moisture content typically results in a decrease in the angle of repose of chalk. This is because moisture lubricates the particles, reducing friction between them and causing them to slide more easily past each other. As a result, the chalk particles are less able to stack compactly, leading to a lower angle of repose.

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the composition ,size ,weight and shape .

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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.

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The angle at which loose material will not slide down a slope is called the angle of repose. It is the maximum angle at which an inclined surface formed of a particular loose material can remain stable without sliding. The angle of repose varies depending on the size, shape, and friction of the particles making up the material.

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The angle of repose of coal can vary depending on the specific type and size of coal particles, but typically ranges from 30 to 45 degrees. This angle represents the steepest angle at which coal can be piled up without further material sliding or cascading down.

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Θ = tan-1 2h

d

Where:

Θ = Angle of repose.

h = Height of the particles pile.

d = Distance from the center of the pile to the edge.

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Water can decrease the angle of repose of soil by reducing the friction between soil particles, making them more likely to slide over one another. This can lead to soil instability and increased risk of landslides or erosion.

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The angle of repose is the steepest angle at which a material remains stable without sliding or flowing. It is important in fields like geology, civil engineering, and agriculture to understand how materials such as soil, rocks, and grains behave under gravitational forces. It helps in designing structures, predicting landslides, and ensuring the stability of slopes.

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