Limestone
Limestone is formed from particles derived from organic processes, usually in a marine environment. Sandstone particles are derived from the weathering and erosion of silicate bearing rocks, normally.
limestone is a type of ferilizer and some of the particles in limestone had minerals that were in limestones.thats where it got its name
Yes, crushing limestone is a physical change. This is because the chemical composition of limestone remains unchanged during the process of crushing. The size and shape of the limestone particles may change, but the chemical makeup remains the same.
The answer will depend on the size of the limestone!
This is a measure of the effectiveness of agricultural lime at neutralizing soil. It takes into account the mesh size of the particles (if they are too big they don't work) and the purity of the limestone.
This depends on the size of the limestone deposit, the rate of extraction and the economic viability of the deposit.
Limestone
If by particles you mean the size of the crystals, then the crystals in metamorphic rock are often larger than in the sedimentary rock. High heat and pressure can cause the minerals to recrystallize. This would be the case in the metamorphosis of limestone (sedimentary) to marble (metamorphic).
Sandstone is made mostly from sand-sized quartz particles. On the other hand, limestone is made from finer grains of calcite material.
The size of the particles that can be absorbed in Biology are very small sized particles.
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.