Young-Laplace Equation Calculator

Calculate capillary pressure, meniscus radius, and capillary rise height using the Young-Laplace equation for surface tension phenomena.

Results

Step-by-Step Calculation

Meniscus Shape

Capillary Rise Diagram

Reservoir θ h r γ γ Capillary Rise Surface tension (γ) Tube radius (r) Rise height (h) Contact angle (θ)

What is the Young-Laplace Equation?

The Young-Laplace equation is a fundamental relationship in fluid mechanics and surface science that describes the capillary pressure difference across a curved interface between two fluids, such as a liquid and a gas. Named after Thomas Young and Pierre-Simon Laplace, who independently developed the theory in the early 19th century, the equation links the pressure difference to the surface tension of the fluid and the geometry of the interface.

The general form of the equation is:

ΔP = γ × (1/R₁ + 1/R₂)

Where ΔP is the pressure difference across the interface, γ is the surface tension, and R₁ and R₂ are the principal radii of curvature. This equation is the starting point for understanding a wide range of capillary phenomena, from the rise of water in narrow tubes to the behavior of soap bubbles, droplets on surfaces, and fluid flow in porous media.

In the simplest case of a spherical meniscus (where both radii of curvature are equal, R₁ = R₂ = R), the equation simplifies to ΔP = 2γ/R. For a liquid meniscus inside a cylindrical capillary tube, the relationship becomes ΔP = 2γ cos(θ)/r, where θ is the contact angle and r is the tube radius.

Surface Tension Explained

Surface tension is a property of liquid surfaces that arises from the imbalance of intermolecular forces at the interface. Molecules in the bulk of a liquid experience attractive forces equally in all directions from neighboring molecules. However, molecules at the surface have no liquid neighbors above them, so they experience a net inward pull. This creates a "tension" at the surface, causing it to behave like an elastic membrane.

Surface tension is measured in Newtons per meter (N/m) or equivalently Joules per square meter (J/m²), reflecting the energy required to increase the surface area by one unit. Common values include:

Surface tension decreases with increasing temperature because thermal energy disrupts the cohesive forces between molecules. Surfactants (like soap) dramatically reduce surface tension by adsorbing at the interface, which is why soap helps water spread and penetrate fabrics.

Contact Angle

The contact angle (θ) is the angle formed at the three-phase contact line where a liquid, gas, and solid meet. It is measured through the liquid phase and is a fundamental indicator of wettability — how well a liquid spreads on a surface.

The contact angle is determined by the balance of three interfacial tensions: solid-liquid, solid-gas, and liquid-gas. Young's equation describes this balance:

γSG = γSL + γLG cos(θ)

In capillary calculations, the contact angle plays a critical role because cos(θ) determines the direction and magnitude of the capillary effect. When θ < 90°, cos(θ) > 0, and the liquid rises. When θ > 90°, cos(θ) < 0, and the liquid is depressed.

Capillary Pressure

Capillary pressure is the pressure difference across a curved liquid-gas interface confined in a narrow space, such as a capillary tube, pore, or gap between surfaces. It arises directly from the Young-Laplace equation and is the driving force behind capillary phenomena.

For a liquid inside a cylindrical capillary tube with an inner radius r, the meniscus forms a spherical cap with a radius of curvature R = r / cos(θ). Substituting this into the Young-Laplace equation for a spherical interface gives:

ΔP = 2γ / R = 2γ cos(θ) / r

Derivation: The meniscus in a cylindrical tube is a portion of a sphere. The relationship between the tube radius r and the meniscus radius of curvature R depends on the contact angle: r = R cos(θ). Since R₁ = R₂ = R for a spherical surface, the general Young-Laplace equation ΔP = γ(1/R + 1/R) = 2γ/R becomes ΔP = 2γ cos(θ)/r after substitution.

Key observations:

Capillary Rise (Jurin's Law)

When a narrow tube is dipped into a liquid with a contact angle less than 90 degrees, the liquid spontaneously rises inside the tube against gravity. This phenomenon, known as capillary rise, is governed by the balance between capillary pressure (pulling the liquid up) and hydrostatic pressure (pushing it down due to gravity).

At equilibrium, the capillary pressure equals the hydrostatic pressure of the liquid column:

2γ cos(θ) / r = ρ g h Solving for h: h = 2γ cos(θ) / (ρ g r)

This relationship is known as Jurin's Law. It can equivalently be written in terms of the meniscus radius R:

h = 2γ / (ρ g R)

Where:

Jurin's Law reveals that the capillary rise height is inversely proportional to the tube radius. In very thin tubes (micrometers in diameter), liquid can rise to remarkable heights. This principle explains how water is transported in plant xylem, how ink rises in felt-tip pens, and how moisture wicks through fabrics.

Meniscus Shape

The meniscus is the curved surface of a liquid inside a container, and its shape is determined by the contact angle between the liquid and the container wall.

The shape of the meniscus directly affects experimental measurements. When reading a graduated cylinder or burette, the measurement should be taken at the bottom of the meniscus for concave surfaces (like water) and at the top for convex surfaces (like mercury).

The radius of curvature of the meniscus is related to the tube radius by R = r / cos(θ). As the tube becomes narrower, the meniscus curvature increases, leading to higher capillary pressure and greater capillary rise or depression.

How to Calculate Capillary Pressure

Let us work through a practical example to demonstrate the calculation process.

Problem: Calculate the capillary pressure for water in a glass tube with an inner radius of 2 mm and a contact angle of 20 degrees at 20°C.

Given:

Step 1: Convert the contact angle to radians for the cosine function:

θ = 20° → cos(20°) = 0.9397

Step 2: Apply the capillary pressure formula:

ΔP = 2γ cos(θ) / r ΔP = 2 × 0.07275 × 0.9397 / 0.002 ΔP = 0.13672 / 0.002 ΔP = 68.36 Pa

Step 3: Calculate the meniscus radius of curvature:

R = r / cos(θ) = 0.002 / 0.9397 = 0.002128 m = 2.128 mm

Result: The capillary pressure is approximately 68.36 Pa and the meniscus radius is 2.128 mm.

For a 1 mm radius tube with the same parameters, the pressure would double to approximately 136.72 Pa, illustrating the inverse relationship between tube radius and capillary pressure.

Applications

The Young-Laplace equation and capillary phenomena have wide-ranging applications across science, engineering, and nature:

Mercury in Capillary Tubes

Mercury provides a striking contrast to water in capillary experiments. While water rises in glass tubes, mercury is depressed below the external liquid level. This difference is entirely explained by the contact angle.

Mercury on glass has a contact angle of approximately 140°. Since cos(140°) = -0.766, the capillary pressure becomes negative:

ΔP = 2γ cos(θ) / r ΔP = 2 × 0.487 × cos(140°) / r ΔP = 2 × 0.487 × (-0.766) / r ΔP = -0.746 / r

For a tube with r = 1 mm (0.001 m): ΔP = -746 Pa. The negative sign indicates that the pressure inside the meniscus is greater than outside, pushing the mercury down.

The capillary depression height is calculated the same way as capillary rise:

h = 2γ cos(θ) / (ρ g r) h = 2 × 0.487 × (-0.766) / (13534 × 9.81 × 0.001) h = -0.746 / 132.829 h = -0.00562 m = -5.62 mm

The negative value means the mercury is depressed 5.62 mm below the external mercury level. Mercury's convex meniscus (bulging upward in the center) is immediately recognizable and is the reason mercury thermometers and barometers are read at the top of the meniscus rather than the bottom.

Mercury's extremely high surface tension (0.487 N/m, about 6.7 times that of water) combined with its very high density (13,534 kg/m³) results in relatively small capillary depression compared to water's capillary rise in the same tube, despite the much larger surface tension.

Frequently Asked Questions

What is the difference between the Young-Laplace equation and Jurin's Law?
The Young-Laplace equation (ΔP = γ(1/R₁ + 1/R₂)) is the general relationship describing pressure difference across any curved interface. Jurin's Law (h = 2γ cos(θ)/(ρgr)) is a specific application of the Young-Laplace equation to capillary rise, where the capillary pressure is balanced against the hydrostatic pressure of the liquid column. Jurin's Law can be derived directly from the Young-Laplace equation by setting the capillary pressure equal to ρgh.
How is capillary pressure used in petroleum engineering?
In petroleum engineering, capillary pressure determines how oil, water, and gas distribute themselves within reservoir rock pore spaces. The capillary pressure curve (a plot of capillary pressure versus water saturation) is essential for reservoir characterization, determining the height of the oil-water transition zone, estimating initial water saturation, and planning enhanced oil recovery strategies. Engineers use the Young-Laplace equation with measured pore throat radii to predict capillary behavior in reservoir simulations.
Why does water rise in thin tubes but mercury goes down?
The key difference is the contact angle. Water wets glass (contact angle near 0°, making cos(θ) > 0), so capillary pressure is positive and pulls water upward. Mercury does not wet glass (contact angle approximately 140°, making cos(θ) < 0), so capillary pressure is negative and pushes mercury downward. The contact angle reflects the relative strength of adhesion (liquid-solid attraction) versus cohesion (liquid-liquid attraction).
What happens when the contact angle is exactly 90 degrees?
When θ = 90°, cos(90°) = 0, which means the capillary pressure is zero and there is no capillary rise or depression. The meniscus is flat. This represents the transition point between wetting and non-wetting behavior. In practice, perfectly flat menisci are rare, but some liquid-solid combinations approach this condition.
How does temperature affect capillary rise?
Temperature affects capillary rise primarily through changes in surface tension and liquid density. As temperature increases, surface tension generally decreases (weakening the capillary driving force), and density typically decreases slightly (reducing the weight of the liquid column). The net effect is usually a decrease in capillary rise height with increasing temperature. For water, the surface tension drops from 0.07275 N/m at 20°C to about 0.0589 N/m at 100°C.
Can the Young-Laplace equation be applied to non-cylindrical geometries?
Yes. The general form of the Young-Laplace equation uses two independent radii of curvature (R₁ and R₂) to describe any curved surface. For cylindrical interfaces, one radius is infinite. For saddle-shaped surfaces, the radii have opposite signs. This generality makes the equation applicable to droplets on surfaces, bubbles, menisci in irregular pores, and the shape analysis of pendant drops used to measure surface tension.
What role does capillary pressure play in soil moisture and agriculture?
In soil science, capillary pressure (often called matric potential or soil suction) determines how tightly water is held within the pore spaces between soil particles. Fine-grained soils like clay have smaller pores and thus higher capillary pressures, retaining water more strongly. Sandy soils with larger pores have lower capillary pressure and drain more freely. Understanding these relationships helps in irrigation planning, drainage design, and predicting water availability for plant roots.