My guess is that the answer would vary depending on the concentration of the nitric acid.
Marble chemical symbol.
Limestone crystals are much smaller than that of marble and limestone is much more porous.
A chemical formula is a way of presenting information about the chemical proportions of atoms that constitute a particular chemical compound or molecule using chemical element symbols numbers and sometimes also other symbols such as parentheses dashes brackets commas and plus and minus signs.
What is the chemical formula for marble.
Heat and pressure applied to limestone creates.
It s a metamorphic rock which means that it was formed from other rocks.
Marble is a metamorphic rock composed of recrystallized carbonate minerals most commonly calcite or dolomite marble is typically not foliated although there are exceptions in geology the term marble refers to metamorphosed limestone but its use in stonemasonry more broadly encompasses unmetamorphosed limestone.
Marble is commonly used for sculpture and as a building material.
It is one of the most effective acid neutralization materials.
One for concentrated hno3 has no2 nasty nitrogen dioxide as a product while the other for dilute hno3 has not.
Being composed of calcium carbonate marble will react in contact with many acids neutralizing the acid.
The only difference between limestone and marble is the crystalline structure.
The marble chip is calcium carbonate caco3.
Typically marble is composed of the following major constituents.
Chemical formula for marble is caco3.
Marble is often crushed and used for acid neutralization in streams lakes and soils.
They also call marble as calcium carbonate.
It is used for acid neutralization in the chemical industry as well.
The reason i think it would vary is that you get different reactions when one puts pure copper in either concentrated or dilute nitric acid.
Here it means 1 calcium 1 carbon and 3 oxygen.
The exact chemical composition of marble will greatly vary dependong on the location and the minerals or impurities present in the limestone during recrystallization.