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The dominant form of breakage for sulfur is cleavage, where the sulfur atoms break along distinct planes due to its molecular structure.
For sulfur, the dominant form of breakage is the cleavage of S-S bonds, resulting in the formation of smaller sulfur molecules or atoms. This process is typically seen in the breakdown of sulfur compounds such as elemental sulfur or disulfides.
The dominant form of breakage for sulfur is cleavage, where the mineral breaks along its natural planes of weakness. This results in the formation of smooth and flat surfaces.
The dominant form of breakage for sulfur is brittle fracture, where the material breaks without significant deformation. This is due to the atomic structure of sulfur, which consists of weak van der Waals forces between the molecules, leading to easy cleavage and fracture.
The main components of coal are carbon, hydrogen, oxygen, nitrogen, and sulfur. The composition and amount of each component vary depending on the type of coal, with carbon being the dominant element in coal.
The dominant form of breakage for sulfur is cleavage, where the sulfur atoms break along distinct planes due to its molecular structure.
For sulfur, the dominant form of breakage is the cleavage of S-S bonds, resulting in the formation of smaller sulfur molecules or atoms. This process is typically seen in the breakdown of sulfur compounds such as elemental sulfur or disulfides.
The dominant form of breakage for sulfur is cleavage, where the mineral breaks along its natural planes of weakness. This results in the formation of smooth and flat surfaces.
The dominant form of breakage for sulfur is brittle fracture, where the material breaks without significant deformation. This is due to the atomic structure of sulfur, which consists of weak van der Waals forces between the molecules, leading to easy cleavage and fracture.
Muscovite mica's dominant type of breakage is perfect basal cleavage, which means it breaks easily along flat planes parallel to its basal structure. This results in thin, flexible sheets of mica being formed when it breaks.
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The dominant type of breakage for muscovite mica is basal cleavage, which means it breaks easily along its cleavage planes into thin sheets. This property is due to the crystal structure of muscovite mica, which consists of layers that are weakly bonded and easily separated.
Muscovite mica has perfect cleavage in one direction. It splits into thin sheets.
Sulfur is a nonmetal.
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frature
Sulfur has covalent bonds with nonmetals.