Sulfate minerals contain the ion SO42- and generally have a vitreous to dull luster.
Sulfide minerals contain the ion S2- and tend to have a metallic luster.
Sulfate minerals include the SO42− anion in their chemical makeup, and they are often deposited hydrothermally, by evaporation, or by oxidation of sulfide minerals.
Sulfide minerals contain the S2- anion in their chemical makeup. Combining with a wide range of metals like iron, nickel, copper, lead and antimony, the sulfides form an economically important class of metal ores.
They both have the element sulfur.
Fluorite is a common mineral that forms in a variety of colors. Galena is a lead sulfide mineral with a metallic luster. Gypsum is a soft sulfate mineral commonly used in construction materials.
Sulfate is a chemical compound containing sulfur and oxygen in the form of SO4^2-, while sulfide is a compound containing sulfur and a metal element in the form of S^2-. Sulfate is commonly found in minerals and salts, while sulfide can be found in minerals and some metal ores. Sulfate is generally more soluble in water compared to sulfide.
No, sodium sulfate (Na2SO4) is a white crystalline solid used in detergents and glass production, while sodium sulfide (Na2S) is a yellow solid used in the manufacturing of rubber and dyes. They are different compounds with distinct chemical properties.
No. The sulfate ion has the formula SO42-, while the sulfide ion has the formula S2-.
Sulfate is SO42- and the sulfide ion is S2-.
A mineral sulfide is a mineral that contains the S2- ion.
The ions are different: chlorate/chloride, sulfate/sulfide, etc.
Galena is a lead sulfide - PbS.
Oxygen is found in all sulfate minerals but not in sulfide minerals. Sulfate minerals contain the sulfate ion (SO4)2-, which includes oxygen atoms, while sulfide minerals contain the sulfide ion (S2-), which does not contain any oxygen atoms.
All minerals in the sulfate and sulfide groups contain sulfur.
Sulfate minerals contain the sulfate ion (SO4)2- and often form in oxidizing environments, while sulfide minerals contain the sulfide ion (S2-) and typically form in reducing environments. Sulfate minerals are more soluble in water compared to sulfide minerals. Additionally, sulfate minerals are more common at the Earth's surface, whereas sulfide minerals are common in deeper, hydrothermal environments.