Chemical composition and internal arrangement of atoms
Color and streak would be the least useful, because they may be shared by a multitude of other minerals.
You could use properties such as cleavage, streak color, color, density, luster, and crystal habit to differentiate between the two samples. These properties can help determine if the samples are the same mineral or different minerals, even if they have the same hardness.
Two properties of minerals that depend on chemical bonds are hardness, which is determined by the strength of the bonds holding the mineral's atoms together, and cleavage, which is the way a mineral breaks along planes of weakness in its atomic structure.
The two factors that cause differential weathering are variations in rock composition and variations in rock structure. Rocks with different mineral compositions and structures will weather at different rates, leading to differential weathering processes.
Climate and parent material are the two factors that have the greatest influence on soil formation. Climate affects the rate of weathering and the type of vegetation that grows, while parent material plays a role in determining the mineral composition and texture of the soil.
mass and volume
Two main factors that affect the absorption of a mineral are the presence of other nutrients or substances that can enhance or inhibit absorption, and the health and integrity of the digestive system, including factors such as pH levels, enzyme activity, and gut health.
The two variables are the concentration of that mineral in the solution and the solubility of that mineral in water. If the concentration of the mineral is higher than its solubility in water, some of the mineral will precipitate out of solution.
Color and streak would be the least useful, because they may be shared by a multitude of other minerals.
You could use properties such as cleavage, streak color, color, density, luster, and crystal habit to differentiate between the two samples. These properties can help determine if the samples are the same mineral or different minerals, even if they have the same hardness.
Two properties of minerals that depend on chemical bonds are hardness, which is determined by the strength of the bonds holding the mineral's atoms together, and cleavage, which is the way a mineral breaks along planes of weakness in its atomic structure.
chemical composition and crystalline structure
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The properties of reactants (reactivity) and catalytic behaviour
Biomass and temperature, erosion and mineral content.
Mineral silver can be used for making jewelry due to its lustrous appearance and durability. It is also used in the production of photographic film and paper because of its light-sensitive properties.
Temperature and hygiene.