The General Material-Balance Equation
Material balance treats the reservoir as a tank - cumulative underground withdrawal equals the total expansion of what remains, plus any water influx - and for a volumetric gas reservoir it collapses to the famous p/z straight line.
Treat the reservoir as a tank: every barrel removed underground must be matched by expansion of what remains, plus any water that flows in.
The Reservoir as a Tank
Material balance is the other great reservoir-engineering accounting tool, and it treats the reservoir as a single tank. Its statement is conservation of mass: the cumulative underground withdrawal - the reservoir-barrel equivalent of everything produced so far - must equal the total expansion of everything still in the reservoir, plus any water influx $W_e$ that has entered from a connected aquifer. As fluid is removed, what remains expands to fill the space, and the pressure drops as a direct result. Material balance ties production and pressure together through the physics of expansion.
The Terms of the Equation
The general material-balance equation gathers several expansion terms, each named here qualitatively. Oil and its dissolved gas expand as pressure falls below the bubble point and gas comes out of solution. A gas cap, if one exists, expands as its gas swells. The connate water and the rock pore volume themselves expand slightly as pressure drops (compaction). And water influx $W_e$ from an aquifer adds fluid from outside the original reservoir boundary. Setting cumulative production equal to the sum of these terms is what closes the balance - and once every term but one is known, you solve for that remaining unknown.
For a volumetric dry-gas reservoir - one with no water drive and no gas cap - the general equation collapses to a famous straight line. Because the gas in place is fixed and only pressure falls as gas is produced, the ratio $p/z$ declines linearly with cumulative gas produced $G_p$: $\dfrac{p}{z} = \dfrac{p_i}{z_i}\left(1 - \dfrac{G_p}{G}\right)$. Plot $p/z$ versus $G_p$ and the data should fall on a straight line whose intercept at $p/z = 0$ is the original gas in place $G$. A water-drive reservoir behaves differently: as the aquifer pushes in to support pressure, the $p/z$ line flattens (bends upward) instead of tracking the straight line - the diagnostic shape explored in this module's interactive $p/z$ material-balance plot.
- Initial $p/z$: $p_i/z_i = 4000/0.80 = 5000$ psia.
- Production fraction: $G_p/G = 30/100 = 0.30$.
- Current $p/z = 5000 \times (1 - 0.30) = 5000 \times 0.70 = 3500$ psia.
- If $z \approx 0.85$ at that condition: $p = (p/z) \times z = 3500 \times 0.85 = 2975$ psia.
Check your understanding
- Material balance treats the reservoir as a tank: cumulative underground withdrawal equals the total expansion of what remains plus any water influx - conservation of mass on reservoir volumes.
- The general equation gathers oil + dissolved-gas expansion, gas-cap expansion, connate-water and rock (compaction) expansion, water influx We, and production; once all but one term are known, you solve for the rest.
- For a volumetric dry-gas reservoir the equation collapses to the p/z straight line, p/z = (p_i/z_i)(1 - G_p/G); extrapolating to p/z = 0 gives OGIP, while a water drive bends the line upward.