Density of Magnesium HCP Metal Calculator

Calculate theoretical and practical magnesium HCP density using lattice constants, atomic radius, porosity, temperature correction, uncertainty analysis, and flexible scientific units accurately confidently online.

Calculator Inputs

g/mol

Lattice Parameters

Use the selected a unit.
Use the selected c unit.

Atomic Radius Method

HCP Cell Convention

Sample Mass and Volume

Porosity Correction

%
%

Temperature Adjustment

°C
°C
µm/m·K
µm/m·K

Reference and Display Options

Formula Used

Magnesium normally forms a hexagonal close-packed crystal structure. Density equals unit-cell mass divided by unit-cell volume. Correct cell conventions prevent sixfold errors during density calculations.

Crystallographic cell: V = (√3 / 2)a²c
Full HCP prism: V = (3√3 / 2)a²c
Cell mass: m = nM / NA
Theoretical density: ρ = m / V
Measured density: ρ = sample mass / sample volume
Porosity correction: ρbulk = ρtheoretical(1 − P/100)
Thermal expansion: LT = L0[1 + α(T − T0)]

How to Use This Calculator

Select a calculation mode and enter known measurements. Choose matching units before submitting the form. Review all warnings before using results for engineering decisions.

  1. Choose lattice, radius, specimen, porosity, or temperature mode.
  2. Enter values with their matching units and uncertainties.
  3. Select the correct HCP cell convention when required.
  4. Choose output precision and the preferred density unit.
  5. Calculate, compare, copy, print, or export the results.

Worked Magnesium Example

Use the magnesium preset for standard starting values. Replace defaults with laboratory or published measurements. Compare theoretical density with measured density to identify porosity.

Input Example value Purpose
Lattice parameter a3.2094 ÅBasal-plane dimension
Lattice parameter c5.2108 ÅHexagonal-axis dimension
Molar mass24.305 g/molMass per mole of magnesium atoms
Cell conventionCrystallographicUses two atoms and its matching volume
Reference density1.738 g/cm³Comparison benchmark

Theoretical and Bulk Density

Theoretical density assumes a perfect and fully dense crystal. Bulk density includes pores, defects, and manufacturing variations. Their difference helps estimate internal voids and material quality.

Common Assumptions

Results depend on accurate dimensions and consistent unit choices. Thermal expansion is modeled as linear over temperature. Real alloys may require composition-specific data and correction factors.

Density Unit Conversion Table

Starting valueEquivalent value
1 g/cm³1000 kg/m³
1 g/cm³0.0361273 lb/in³
1 g/cm³62.428 lb/ft³
1 kg/m³0.001 g/cm³
1 kg/m³0.001 mg/mm³

Frequently Asked Questions

What does HCP mean?

HCP means hexagonal close-packed. It describes a repeating atomic arrangement. Magnesium commonly adopts this crystal structure near room temperature.

Why are two cell conventions available?

Crystallography often uses a smaller primitive-equivalent hexagonal cell. Textbooks may show a larger full prism. Each volume must use its matching atom count.

Why can atom counts cause large errors?

Density depends directly on mass per selected cell. A mismatched count changes cell mass incorrectly. The calculator warns about common HCP convention mismatches.

What is the ideal HCP c/a ratio?

The geometric ideal is approximately 1.633. Real metals can differ from this value. Magnesium is close but not exactly ideal.

How does porosity change density?

Porosity reduces solid material within the bulk volume. Greater porosity lowers measured bulk density. The correction assumes pores contain negligible solid mass.

Can this calculator handle magnesium alloys?

Yes, by replacing molar mass and structural data. Alloy density may require composition-weighted properties. Phase mixtures can make a single HCP model insufficient.

How is temperature applied?

The calculator expands a and c independently. It uses linear expansion over the entered interval. Large temperature ranges may need nonlinear material data.

How is uncertainty estimated?

Independent relative uncertainties are combined by root-sum-square propagation. The formula changes with the selected mode. Correlated errors require a more detailed analysis.

Why might my result differ from a handbook?

Handbook values depend on temperature, purity, and measurement method. Lattice constants also vary between sources. Use data matching your exact sample conditions.

Disclaimer

This calculator provides educational and preliminary engineering estimates. Verify critical values using traceable laboratory or handbook data. Temperature, purity, alloying, and defects can change actual density.

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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.