Measure calcite balance from pH, hardness, alkalinity, temperature, and dissolved solids. See scaling risk instantly. Model water stability with charts, exports, and guided interpretation.
| Scenario | pH | Temp (°C) | TDS (mg/L) | Ca Hardness | Alkalinity | CSI | Interpretation |
|---|---|---|---|---|---|---|---|
| Cooling tower loop | 8.40 | 32 | 900 | 240 | 180 | 0.33 | Moderate scaling |
| Drinking water line | 7.50 | 20 | 220 | 95 | 90 | -0.24 | Slightly undersaturated |
| Process rinse water | 6.90 | 28 | 120 | 45 | 50 | -0.73 | Corrosive tendency |
| Membrane concentrate | 8.70 | 30 | 1400 | 310 | 220 | 0.64 | Heavy scale risk |
These rows are example operating conditions for comparing water stability, not laboratory-certified results.
This calculator provides two layers of analysis. The default estimate uses a practical calcite saturation balance. The optional direct method uses user-supplied ion concentrations and an activity correction.
Here, TDSadj equals dissolved solids multiplied by the salinity correction factor. A positive index means supersaturation and likely scaling. A negative index means undersaturation and possible deposit dissolution.
The direct method is useful when you have measured ion concentrations and want an activity-based verification. The Davies equation is a reasonable approximation at low to moderate ionic strength.
A positive value means water is supersaturated with respect to calcium carbonate. That usually indicates scale can form on heat exchangers, membranes, piping, and instrument surfaces.
A negative value means water is undersaturated. It tends to dissolve calcium carbonate deposits and may show a more corrosive or aggressive behavior toward carbonate-based protective films.
pH shifts carbonate equilibria and directly changes how close the water is to calcite saturation. Small pH changes can move the system from stable to scale-forming quickly.
The estimated method uses the same practical balance style often used for calcite saturation screening. Here it is presented as a carbonate saturation calculator for water chemistry decisions.
Use it when you have measured calcium and carbonate ion concentrations and want a thermodynamic check using activities instead of only practical water-treatment approximations.
Yes. Temperature changes equilibrium behavior and the saturation pH term. In many systems, higher temperature increases the tendency for carbonate precipitation and deposit growth.
It helps you model concentrated loops, recycle streams, or operating conditions where effective dissolved solids are higher than the raw sample value used during screening.
It is useful for screening, comparison, and process monitoring. Final design or treatment selection should still consider full speciation, kinetics, materials, and laboratory validation.
Important Note: All the Calculators listed in this site are for educational purpose only and we do not guarentee the accuracy of results. Please do consult with other sources as well.