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The chemical formula for copper ore can vary depending on the specific mineral composition. However, a common mineral form of copper ore is copper pyrite, which has the chemical formula CuFeS2.
Copper sulfate dissolving in water is a physical change because the chemical composition of copper sulfate remains the same. Physical changes do not alter the chemical structure of a substance.
Adding water to heated copper sulfate crystals is a chemical change. When water is added to heated copper sulfate crystals, the copper sulfate undergoes a chemical reaction where it dissolves in the water to form a solution. This is a chemical change because the chemical composition of the copper sulfate is altered during the process.
The chemical formula of copper matte is typically not fixed and can vary depending on the specific composition of the mixture. In general, copper matte is a combination of copper sulfides and other metal sulfides that result from the smelting of copper ores.
EC grade copper typically contains a minimum of 99.9% copper with trace amounts of impurities such as oxygen, silver, and phosphorus. It is a high-purity form of copper commonly used in electrical applications due to its excellent conductivity and low levels of contaminants.
CuCl2 has 52,632 % chlorine and 47,368 % copper.
Pounding a sheet of copper into a bowl is a physical change because the copper is still the same substance before and after the change. The change in shape does not alter the chemical composition of the copper.
Bacteria plants extract copper by absorbing its chemical properties. The same goes along with fungi but they absorb the copper and use that as a reproduction synthetic. Bacteria plants can also repel the copper if the chemical properties to them is not suffice or sufficient. First, bacteria will explore the copper and its chemical properties and search for the right chemical composition to support the plant. Then, once the pathogen/virus finds the right chemical composition, they absorb the chemical composition in the copper and return to the plant. Finally, they repel the composition from their bodies into the plant which makes it suffice to create glucose.
Yes, hammered copper is a physical change. When copper is hammered, its shape and size change, but its chemical composition remains the same.
The chemical formula for copper ore can vary depending on the specific mineral composition. However, a common mineral form of copper ore is copper pyrite, which has the chemical formula CuFeS2.
When copper ore is heated in a furnace, it undergoes a chemical reaction that separates the copper from the other elements in the ore. This process of extracting the pure copper from its ore through smelting is a chemical change because the chemical composition of the copper is altered.
Copper sulfate dissolving in water is a physical change because the chemical composition of copper sulfate remains the same. Physical changes do not alter the chemical structure of a substance.
Examples: iron sulfide and some copper alloys.
Adding water to heated copper sulfate crystals is a chemical change. When water is added to heated copper sulfate crystals, the copper sulfate undergoes a chemical reaction where it dissolves in the water to form a solution. This is a chemical change because the chemical composition of the copper sulfate is altered during the process.
The chemical formula of copper matte is typically not fixed and can vary depending on the specific composition of the mixture. In general, copper matte is a combination of copper sulfides and other metal sulfides that result from the smelting of copper ores.
EC grade copper typically contains a minimum of 99.9% copper with trace amounts of impurities such as oxygen, silver, and phosphorus. It is a high-purity form of copper commonly used in electrical applications due to its excellent conductivity and low levels of contaminants.
Using a Bunsen burner to heat copper is a physical change. The copper undergoes a change in its physical state from solid to liquid without changing its chemical composition.