Calculate The Solubility Of Mgoh2 In Water Using Ksp






Calculate the Solubility of Mg(OH)2 in Water Using Ksp | Solubility Calculator


Calculate the Solubility of Mg(OH)2 in Water Using Ksp

Determine the molar and mass solubility of Magnesium Hydroxide quickly and accurately.


Standard Ksp for Mg(OH)₂ is approximately 1.8 × 10⁻¹¹. Use scientific notation (e.g., 1.8e-11).
Please enter a valid positive number for Ksp.


Ksp values are temperature-dependent. This calculator uses the Ksp value provided.


Molar Solubility (s)

0.000165 mol/L

The quantity of Mg(OH)₂ that dissolves to form a saturated solution.

Mass Solubility (g/L):
0.00962 g/L
[Mg²⁺] Concentration:
1.65e-4 mol/L
[OH⁻] Concentration:
3.30e-4 mol/L
Theoretical pH:
10.52

Formula used: Ksp = [Mg²⁺][OH⁻]² = (s)(2s)² = 4s³

Solubility vs. Ksp Logarithmic Curve

Illustration of how molar solubility increases as the Solubility Product Constant rises.

What is the Calculation of Solubility of Mg(OH)2 in Water Using Ksp?

To calculate the solubility of mgoh2 in water using ksp is a fundamental exercise in analytical chemistry and equilibrium thermodynamics. Magnesium hydroxide, commonly known as milk of magnesia in aqueous suspension, is a sparsely soluble ionic compound. When it is introduced to water, a dynamic equilibrium is established between the solid phase and its constituent ions in the solution.

Who should use this? Chemistry students, laboratory technicians, and environmental engineers often need to calculate the solubility of mgoh2 in water using ksp to predict precipitation in industrial boilers, understand mineral bioavailability, or design wastewater treatment protocols. A common misconception is that solubility is a fixed constant; however, it is highly sensitive to temperature, pH, and the presence of other ions (the common ion effect).

Formula and Mathematical Explanation

The dissociation equation for Magnesium Hydroxide is:

Mg(OH)₂(s) ⇌ Mg²⁺(aq) + 2OH⁻(aq)

The equilibrium expression is defined by the solubility product constant ($K_{sp}$):

$K_{sp} = [Mg^{2+}][OH^-]^2$

If we let ‘$s$’ represent the molar solubility (the moles of $Mg(OH)_2$ that dissolve per liter of water), then at equilibrium:

  • $[Mg^{2+}] = s$
  • $[OH^-] = 2s$

Substituting these into the $K_{sp}$ expression gives: $K_{sp} = (s)(2s)^2 = 4s^3$. Therefore, to calculate the solubility of mgoh2 in water using ksp, we rearrange the formula to solve for $s$: $s = \sqrt[3]{K_{sp} / 4}$.

Variable Meaning Unit Typical Range (at 25°C)
Ksp Solubility Product Constant Dimensionless 1.5 × 10⁻¹¹ to 5.6 × 10⁻¹²
s Molar Solubility mol/L (M) 1.1 × 10⁻⁴ to 1.7 × 10⁻⁴
Molar Mass Mass of 1 mole Mg(OH)₂ g/mol 58.3197
pH Acidity/Alkalinity pH Scale 10.3 – 10.6

Practical Examples (Real-World Use Cases)

Example 1: Pure Water at 25°C

Given $K_{sp} = 1.8 \times 10^{-11}$. To calculate the solubility of mgoh2 in water using ksp, we use the formula $s = (1.8 \times 10^{-11} / 4)^{1/3}$. The result is approximately $1.65 \times 10^{-4}$ mol/L. To convert this to grams per liter, multiply by the molar mass (58.32 g/mol), resulting in 0.0096 g/L.

Example 2: Industrial Cooling Systems

In a cooling tower where the $K_{sp}$ might effectively change due to temperature increases (e.g., $K_{sp}$ becoming $5.0 \times 10^{-11}$), the solubility increases. Applying the same logic, $s = (5.0 \times 10^{-11} / 4)^{1/3} \approx 2.32 \times 10^{-4}$ mol/L. This shows how slight temperature shifts can lead to significantly more dissolved mineral content, affecting scale formation.

How to Use This Solubility Calculator

  1. Enter the Ksp: Locate the solubility product constant for your specific temperature. The default is $1.8 \times 10^{-11}$.
  2. Check Real-Time Updates: As you type, the tool will automatically calculate the solubility of mgoh2 in water using ksp.
  3. Analyze the Results: Look at the Molar Solubility (mol/L) for chemical equations and Mass Solubility (g/L) for physical measurements.
  4. Review the pH: Since $Mg(OH)_2$ releases hydroxide ions, the solution will be basic. The calculator provides the theoretical pH.
  5. Copy for Reports: Use the “Copy Results” button to quickly export your data to a lab report or spreadsheet.

Key Factors That Affect Mg(OH)2 Solubility

  • Temperature: Dissolution is typically endothermic; as temperature rises, $K_{sp}$ increases, causing higher solubility.
  • Common Ion Effect: If $Mg^{2+}$ or $OH^-$ ions are already present (e.g., from $MgCl_2$ or $NaOH$), the equilibrium shifts left, significantly reducing solubility.
  • pH Levels: Lowering the pH (adding acid) removes $OH^-$ ions, shifting the equilibrium right and increasing the amount of $Mg(OH)_2$ that dissolves.
  • Ionic Strength: High concentrations of “spectator ions” can slightly increase solubility by shielding the $Mg^{2+}$ and $OH^-$ ions from each other.
  • Complex Ion Formation: If ligands are present that bind with $Mg^{2+}$, the effective solubility can increase.
  • Particle Size: While it doesn’t change $K_{sp}$ itself, very small nanoparticles can show higher kinetic solubility compared to bulk material.

Frequently Asked Questions (FAQ)

1. Why is the solubility of Mg(OH)2 so low?

The lattice energy of the $Mg(OH)_2$ crystal structure is very high compared to the hydration energy released when the ions dissolve, leading to a small $K_{sp}$.

2. How does temperature specifically change the result?

When you calculate the solubility of mgoh2 in water using ksp at higher temperatures, you must use a higher $K_{sp}$ value. For example, at 100°C, the solubility is roughly 10 times higher than at 25°C.

3. Can I use this for milk of magnesia?

Yes, milk of magnesia is a suspension. This calculator tells you the maximum amount that is actually dissolved in the liquid phase of that suspension.

4. What is the pH of a saturated Mg(OH)2 solution?

Typically around 10.5. This mild alkalinity is why it is used as an antacid; it neutralizes stomach acid without being caustic.

5. Does pressure affect the calculation?

For solids and liquids, pressure has a negligible effect on solubility compared to temperature and chemical environment.

6. What if there is already MgCl2 in the water?

This is the common ion effect. The $[Mg^{2+}]$ from $MgCl_2$ will force the equilibrium to the left, drastically lowering the solubility of $Mg(OH)_2$.

7. Is molar solubility the same as Ksp?

No. $K_{sp}$ is a constant at a given temperature, while molar solubility ($s$) is the amount that dissolves. For $Mg(OH)_2$, $K_{sp} = 4s^3$.

8. Why do different sources list different Ksp values?

$K_{sp}$ measurements are sensitive to experimental conditions and the purity of the sample. Values typically range between $1.5 \times 10^{-11}$ and $5.6 \times 10^{-12}$.

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