5. Estimate numerically the change in carbonate-rock
porosity caused by a complete dolomitization
of calcite, accounting to the chemical reaction, 2CaCO3+Mg2+
=CaMg(CO3)2+Ca2+, will yield a carbonate rock’s porosity of 13%
.
Porosity in any material is the voidage or fraction of empty space (void) in the material
Let V denote volume
For this case of carbonate rock before dolomization
V[rock]= V[calcite] + V[void]
After dolomization
V[rock] = V[calcite] + V[dolomite] + V[void]
Since the process is complete dolomization V[calcite] is 0 here
Given after dolomization:
V[void]/V[rock] = 0.13
So V[dolomite] = 1 - V[void]/V[rock] =1- 0.13 = 0.87
V[dolomite]=0.87*V[rock]
It is evident from reaction stiochiometry that 2 moles of calcite form 1 mole of dolomite.
Assuming no difference in the molar density of dolomite and calcite
V[calcite] = 0.5*V[dolomite] = 0.5^0.87*V[rock] = 0.435*V[rock]
Thus, the initial porosity of rock
V[void]/V[rock]= 1- V[calcite]/V[rock] = 1- 0.435 = 0.565 = 56.5%
A net decrease of (56.5-13)% = 43.5% change in porosity
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