Skydrol Thermal Expansion Coefficient Calculator

Skydrol Volumetric Thermal Expansion Coefficient (β)

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β = −(1/ρ)(dρ/dT), computed piecewise from the digitized density curves on the Skydrol Density page.

Skydrol PE-5 is not shown — it has no published density-vs-temperature curve, so no slope (and therefore no β) can be derived for it.

Dashed lines represent segments where the underlying density is extrapolated (below 7.65 °F for Skydrol 7000, the floor of its digitized curve).

Toggle data sets by clicking the legend.

Skydrol Percent Volume Change Relative to 77 °F (25 °C)

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ΔV/V₀ = (ρ₀ − ρ) / ρ × 100%, referenced to each grade's own density at 77 °F (25 °C), matching the brochure's own reference temperature. Negative values mean the fluid is denser (contracted) relative to 77 °F.

Toggle data sets by clicking the legend.

Skydrol Thermal Expansion Calculator
Grade:
Degrees (°F):
Degrees (°C):
β × 10⁻⁴ (1/K):  
β × 10⁻⁵ (1/K):  
β × 10⁻⁶ (ppm/K):  
β (1/K):  
β (1/°R):  
% Vol. Change from 77°F:  
Density used (kg/m³):  
Thermal Expansion of Skydrol Phosphate Ester Hydraulic Fluid
Volumetric Thermal Expansion Coefficient — β

The volumetric thermal expansion coefficient β describes how much a fluid expands per degree of temperature rise at constant pressure:

β = −(1/ρ)(dρ/dT)

β is a derivative, and differentiating digitized data amplifies its noise. Each grade's density points lie on a straight line to R² ≥ 0.9998, with a worst-case departure of 0.78 kg/m³ — 0.075% of ρ. But consecutive anchor points sit only 45–75 °F apart, so that 0.05% wiggle becomes a 3.6–12.2% swing in the slope measured between one pair of points and the next. Taking β from those local slopes produced a sawtooth that rose, fell, and rose again — something a fluid whose density decreases monotonically cannot physically do.

So β here comes from a single least-squares straight line fitted to each grade's digitized points, the same approach the MIL-PRF-23699 page uses. With ρ = b + mT, that gives β = −m/(b + mT): a smooth curve that rises gently with temperature, because the same absolute density loss per degree is a progressively larger fraction of a shrinking density. That gentle rise is real; the steps were not.

Percent Volume Change

For a fixed mass of fluid, volume is inversely proportional to density. The percent volume change relative to 77 °F (25 °C, Eastman's own reference temperature for density) is:

ΔV/V₀ = (ρ₀ − ρ(T)) / ρ(T) × 100%

Negative values indicate that the fluid is denser than at 77 °F (volume contracted). This is useful for sizing hydraulic reservoirs and accumulators across the full service temperature range.

Data Source and Coverage

β and ΔV/V₀ are derived entirely from the density curves already digitized on the Skydrol Density page — real measured curves for LD-4, 500B-4, and the obsolete Skydrol 7000 (the last extrapolated below its 7.65 °F digitized floor, shown dashed).

Skydrol PE-5 and Skydrol 5 are deliberately absent. Each has only a single published density value, at 25 °C, and β is a slope — one point cannot produce one. Substituting another grade's curve would mean publishing that grade's β under a different name, so this page shows only grades whose β is actually measured. The Prandtl and thermal diffusivity pages do estimate density for those two grades, because there density is one input among several rather than the answer itself; both state the assumption explicitly.

Skydrol — Thermal Expansion vs. Temperature
Temp
(°F)
Temp
(°C)
500B-4 LD-4 Skydrol 7000*
β×10⁻⁴ (1/K) ΔV/V₀ (%) β×10⁻⁴ (1/K) ΔV/V₀ (%) β×10⁻⁴ (1/K) ΔV/V₀ (%)

ρ₀ is each grade's own density at 77 °F (25 °C). *Values marked with an asterisk are extrapolated below Skydrol 7000's 7.65 °F digitized floor. Skydrol PE-5 and Skydrol 5 are omitted — each has only a single published 25 °C density, and β cannot be derived from one point.

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