Chemical tests can be the only way for identifying and distinguishing minerals with similar physical properties. Here are the three most common chemical tests used in mineral identification.
1. Acid Test: The acid test is performed to identify minerals containing carbonate ions (CO32-). Vinegar will work for many common minerals. Another common acid used for this test is dilute hydrochloric acid (HCl) but is expensive and more dangerous. When the acid is applied to the mineral, it reacts with the carbonate minerals, producing bubbles of carbon dioxide gas (CO2). The presence of effervescence (bubbling) indicates the presence of carbonate minerals.
Hydrochloric Acid can be dangerous, even in diluted form, and should only be used under the supervision of a responsible adult, in a safe environment. A safer alternative is white vinegar, though it is not as strong (that’s why it’s safer), and won’t react with as many minerals.
2. Flame Test: The flame test is used to identify some metals based on the characteristic colors they emit when heated in a flame. To perform the test, a small piece of the mineral is placed on the end of a nichrome (nickel-chromium) wire or a platinum wire loop. The wire is then held in the flame of a Bunsen burner or a torch. The color of the flame observed during the heating process is indicative of specific metal ions present in the mineral.
For instance, copper-bearing minerals, such as malachite (Cu2CO3(OH)2) and azurite (Cu3(CO3)2(OH)2), will produce a green flame. Strontium-bearing minerals, such as celestite (SrSO4), produce a red flame.
Nichrome wire is sometimes used in clay sculpture and may be available at your local hobby store.
It is essential to handle chemicals and open flames with caution when conducting chemical tests. Proper safety measures and laboratory protocols should be followed to ensure safe and accurate mineral identification.
These chemical tests, along with other physical properties such as luster, hardness, cleavage, and crystal form, provide valuable information for mineral identification, contributing to our understanding of Earth’s diverse geological processes and the wide variety of minerals that make up our planet’s crust.