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Acid dissolving power

How much calcite or dolomite a cubic metre of acid dissolves: the gravimetric (β) and volumetric (X) dissolving power from the reaction stoichiometry, the mass of rock dissolved and the CO₂ released.

Formula
β₁₀₀ = ν_m · M_m / (ν_a · M_a)β = C · β₁₀₀X = β · ρ_a / ρ_m

Stoichiometry: 2 moles of a monoprotic acid per mole of calcite, 4 per mole of dolomite, the reaction going to completion. Formic and acetic acids are weak: at reservoir CO₂ pressure the reaction stops at equilibrium, and the real dissolving power is lower. Mineral densities: calcite 2 710, dolomite 2 870 kg/m³. The CO₂ volume is at standard conditions; in the reservoir most of it dissolves in the spent acid.

Source: Economides, Hill, Ehlig-Economides, Petroleum Production Systems (1994): acid dissolving power table; Schechter, Oil Well Stimulation (1992)

Inputs

You can change a field's unit: the value is converted to the formula's units automatically.

HA
MCO₃
C

Usually 10–15 % for sandstones, up to 24–28 % in carbonates.

ρ_a

HCl at 20 °C: 10 % — 1 047, 15 % — 1 073, 20 % — 1 098, 28 % — 1 139 kg/m³.

Unit converter for this formulaDensity and °API · Gas-oil ratio · Fraction and percent
Metric
  • kg/m³850
  • g/cm³0.85
  • t/m³0.85
  • rel. (water 4 °C)0.850024
US field units
  • lb/ft³53.0638
  • lb/gal (ppg)7.09359
  • SG (60/60 °F)0.850837
  • °API34.8068

°API and SG refer to the density at 60 °F (15.6 °C) relative to water at 60 °F, relative density to water at 4 °C. The oil's thermal expansion between the measurement temperatures is not included. °API = 141.5 / SG − 131.5.

All units
Result
XVolumetric dissolving power
Fill in all fields
  • βGravimetric dissolving power
    kg rock / kg solution
  • mRock dissolved by 1 m³ of acid
    kg/m³
  • V_CO₂CO₂ released per m³ of acid (standard conditions)

More in Fracturing and acidizing

Results are engineering estimates from standard formulas; for design decisions check them against the codes, project documents and specialists' calculations. The formulas carried over from the original set are unchanged, and their errors are described in the notes.