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∙ 12y agoClose packing basically means that the atoms are so close together, that they can not get any closer to each other. This means that the empty space between the atoms is minimized. Density is weight per volume, so the less empty volume there is, the higher the density will be.
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∙ 12y agoMinerals with close-packing structures have high densities because their atoms are tightly arranged and closely packed together, reducing empty space between them. This arrangement allows for more atoms to be present in a given volume, resulting in a higher mass per unit volume and, thus, a higher density.
Minerals that have a density of around 2.1 include dolomite, pyrite, and galena. These minerals can vary slightly in density based on their specific composition and structure.
Minerals with closest packing have high density because their atoms are arranged in a way that minimizes empty space between them. This close arrangement of atoms allows for more atoms to be packed into a given volume, resulting in higher density. Closest packing is a highly efficient crystalline structure that maximizes atomic packing, leading to increased density.
Close packing basically means that the atoms are so close together, that they can not get any closer to eachother. This means that the empty space between the atoms is minimized. Density is weight per volume, so the less empty volume there is, the higher the density will be.
No, water's density decreases as it cools. Water reaches its maximum density at around 4 degrees Celsius, and as it cools further, the water molecules form a crystalline structure, causing the density to decrease.
Diamond is a crystalline form of carbon which has a density of has a density of 3.51 gm/cm3 compared to 2.26 gm/cm3in the graphite form. Imperfectly formed crystalline forms of diamond are called bort and black diamond.Source: http://hyperphysics.phy-astr.gsu.edu/hbase/minerals/diamond.html
Minerals of a nonsilicate crystal have very high densities because their crystal structures are based on the packing of atoms that are as close together as possible. This structure is called this closest packing.
Minerals with closest packing crystalline structures have high density because the atoms or ions in these structures are closely packed together in an efficient manner, leaving little empty space between them. This results in a higher mass per unit volume, leading to a higher overall density of the mineral.
Density is a physical property of minerals that can be used for identification. It is calculated by dividing the mass of the mineral by its volume. Different minerals have unique densities due to variations in their chemical composition and crystalline structure.
In order to be a mineral, substances need to have fixed internal crystalline structure. Natural glass does not.
Minerals with closest packing have high density because their atoms are arranged in a way that minimizes empty space between them. This close arrangement of atoms allows for more atoms to be packed into a given volume, resulting in higher density. Closest packing is a highly efficient crystalline structure that maximizes atomic packing, leading to increased density.
Some minerals with closely packed atom structure have a high density.
The density of a mineral is determined by its chemical composition and packing of atoms in its crystal structure. Specific gravity, which is the ratio of a mineral's density to the density of water, is a measure of how heavy a mineral is compared to an equal volume of water. Both properties can provide information about a mineral's identity and help distinguish it from other minerals.
Several examples: density, color, refractive index, crystalline structure, melting point.
Several examples: density, color, refractive index, crystalline structure, melting point.
Close packing basically means that the atoms are so close together, that they can not get any closer to eachother. This means that the empty space between the atoms is minimized. Density is weight per volume, so the less empty volume there is, the higher the density will be.
To meet the definition of a mineral, a substance must be an inorganic, naturally occurring solid, with a set parameter of chemical formulas and a crystalline structure. Non-defining physical properties or characteristics of minerals include: hardness, luster, cleavage, crystal structure, chemical formula, streak, radioactivity, refraction, magnetism, and pleochroism.
A mineral's density remains constant unless there is a change in its composition or structure. Factors such as pressure, temperature, and chemical reactions can alter a mineral's density.