Derivation of Continuity Equation - Definition, Formula, FAQs

Derivation of Continuity Equation - Definition, Formula, FAQs

Vishal kumarUpdated on 02 Jul 2025, 05:04 PM IST

In physics, Derivation of the continuity equation is one of the most supreme derivations in fluid dynamics. In this article, we will discuss the continuity equation. What is the formula for the continuity equation? What is continuity equation derivation? Derive steady flow energy equation. What is the continuity equation in differential form? What is the continuity equation in semiconductors? What is the equation of continuity in electromagnetism? What is the law of continuity?

Derivation of Continuity Equation - Definition, Formula, FAQs
Derivation of Continuity Equation

What is the continuity equation?

Definition: In physics, the equation of continuity is defined as the mass balance of a fluid flowing via a stationary volume segment. It states that the speed or rate of mass accumulation in this volume element equals the speed of mass in minus the rate of mass out.

Continuity Equation Derivation

The continuity equation shows that the material of the cross-sectional area of the pipe and the fluid rate at any particular point across the pipe is consistently constant. This material is equal to the volume flow per sec. or simply the rate of flow. The continuity eq. is represented as:

$$
\mathrm{R}=\mathrm{A} \vee=\text { constant }
$$


Where,
$R=$ volume flow rate
$A=$ flow area
$v=$ flow velocity

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Assumptions in the continuity equation:

The below keys are the assumptions of continuity equation:

  • The tube, which is taken into contemplation, has a single entry and a single exit.

  • The fluid that influx (flows) in the tube is non-viscous fluid.

  • The fluid is close or in-compressible.

  • Fluid influx (flow) is steady.

Derivation of Continuity Equation

Let us see the following diagram:
Let us assume that the fluid flows in the tube for a short period $\Delta t$. In the course of this time, the liquid (fluid) will cover a distance of $\Delta x_1$, with a velocity of $v_1$ in the lower fragment of the pipe.

The interval covered by the fluid with rate $v_1$ in time $\Delta t$ will be shown by,

$$
\Delta x_1=v_{1 \Delta} t
$$


So, in the lower part of the pipe, the volume of fluid move (flow) into the pipe is,

$$
\mathrm{V}=\mathrm{A}_1 \Delta \mathrm{x}_1=\mathrm{A}_1 \mathrm{v}_1 \Delta \mathrm{t}
$$


As it is known,

$$
\mathrm{m}=\mathrm{pV}
$$


Where,
$\mathrm{m}=$ Mass
$\mathrm{p}=$ Density
$V=$ Volume

So, the mass of liquid (fluid) in part $\Delta \mathrm{x}_1$ will be:

$$
\begin{aligned}
& \Delta m_1=p \times V \\
& \Delta \mathrm{~m}_1=\mathrm{p}_1 \mathrm{~A}_1 \mathrm{v}_1 \Delta \mathrm{t} \ldots \ldots (1)
\end{aligned}
$$

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Therefore, at the lower region of the pipe, we have to calculate the mass flux. Mass flux is the mass of the fluid that flows through the given cross-sectional area per unit of time. For the lower part of the pipe, with the lower end of the pipe having a cross-sectional area $A_1$, the mass flux is given by:

$$
\frac{\Delta m_1}{\Delta_t}=p_1 A_1 v_1 \ldots . .(2)
$$


Likewise, the mass flux of the liquid (fluid) at the upper end of the pipe will be:

$$
\frac{\Delta m_2}{\Delta t}=p_2 A_2 v_2 \ldots \ldots (3)
$$

Where,

$v_2$ is the velocity of the liquid flowing in the upper end of the pipe
$\Delta \mathrm{x}_2$ is the distance travelled by the fluid
$\Delta t$ is time
$\mathrm{A}_2$ is an area of cross-section of the upper end of the pipe
It is speculated (assumed) that the density of the liquid (fluid) in the lower end of the pipe is the same as that of the upper end. Then the fluid flux (flow) is said to be streamlined.

So the mass flux at the bottom point of the pipe will also be equal to the mass flux at the upper end of the pipe. Then

Equation $2=$ Equation 3
Therefore,

$$
p_1 A_1 v_1=p_2 A_2 v_2 . (4)
$$

From eq. (4) we can write:

$\rho A v=$ constant
This equation proves the law of conservation of mass in liquid (fluid) dynamics. As the liquid (fluid) is taken to be compact, the density of the liquid (fluid) will be constant for steady flow.

Therefore, $\mathbf{p}_1=\mathbf{p}_2$
Put it this to Eq. 4; it can be written as:

$$
\mathrm{A}_1 \mathrm{v}_1=\mathrm{A}_2 \mathrm{v}_2
$$


The general form of this eq. is:

$$
A v=\text { constant }
$$


Now, let's assume R as the volume flow rate, consequently the eq. can be stated as:

$$
\mathrm{R}=\mathrm{A} \vee=\text { constant }
$$

Hence, it is the derivation of the continuity equation.

Commonly Asked Questions

Q: What is the continuity equation in fluid dynamics?
A:
The continuity equation in fluid dynamics is a fundamental principle that describes the conservation of mass in a flowing fluid. It states that the rate at which mass enters a system is equal to the rate at which mass leaves the system plus the rate of change of mass within the system.
Q: Why is the continuity equation important in studying fluid flow?
A:
The continuity equation is crucial because it helps us understand how the velocity, density, and cross-sectional area of a fluid change as it flows through different regions. This principle is essential for analyzing and predicting fluid behavior in various applications, from pipe systems to aerodynamics.
Q: How does the continuity equation relate to the conservation of mass?
A:
The continuity equation is a direct application of the conservation of mass principle. It ensures that mass is neither created nor destroyed during fluid flow, maintaining a balance between the mass entering and leaving a system, accounting for any changes in density or volume.
Q: How does the continuity equation apply to a varying cross-sectional area, like in a nozzle?
A:
In a nozzle or any varying cross-sectional area, the continuity equation shows that as the area decreases, the velocity must increase to maintain the same mass flow rate. This relationship is expressed as A₁v₁ = A₂v₂, where the subscripts represent two different points along the flow.
Q: What is the significance of the equation A₁v₁ = A₂v₂ in fluid dynamics?
A:
This equation, derived from the continuity principle for incompressible fluids, shows the inverse relationship between cross-sectional area and fluid velocity. It's crucial for understanding how fluids behave in pipes, nozzles, and other systems with varying cross-sections, helping to predict velocity changes.

What is the continuity equation in differential form?

By the divergence theorem, a common continuity equation can also be expressed as in a "differential form":

$$
\frac{\partial p}{\partial t}+\nabla \cdot j=\sigma
$$


Where,
$\nabla=$ divergence
$\rho=a m t$. of quantity as per unit volume
$j=$ flux of $q$.
$\mathrm{t}=$ time
$\sigma=$ generation of q per unit volume per unit time

This common equation is used to derive any continuity equation, varying from as uncomplicated as the volume continuity equation to as complex as the Navier–Stokes equations. This eqn. also generalizes the parameterization equation.

In the condition that $q$ is a conserved quantity that cannot be created or destroyed (like energy), $\sigma=0$ and the equation become

$$
\frac{\partial \rho}{\partial t}+\nabla \cdot \mathbf{j}=0
$$


What is the equation of continuity in electromagnetism?

In electromagnetism, the continuity equation is an empirical law demonstrating charge conservation. Mathematically it is an automatic necessity of Maxwell's equations, even though charge conservation is more elemental than Maxwell's equations. It expresses that the divergence of the current density J (amperes per square meter) is equal to the negative speed of change of the charge density $\rho$ (coulombs per cubic meter),

$$
\nabla \cdot j=-\frac{\partial p}{\partial t}
$$

Current is the flow of charge. The continuity equation says that if a charge discharges out of a differential volume (i.e., a divergence of current density is positive) then the number of charges within that volume decreases. So, the rate of modification of charge density is negative. Therefore, the continuity equation accounts for the conservation of charge.

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What is the continuity equation in semiconductors?

The entire current flow in the semiconductor embraces the drift current and diffusion current of both the electrons in the conduction band and holes in the valence band. Generalize form for electrons in 1 (one) dimension:

$$
\frac{\partial n}{\partial t}=n \mu_n \frac{\partial E}{\partial x}+\mu_n E \frac{\partial n}{\partial x}+D_n \frac{\partial^2 n}{\partial x^2}+\left(G_n-R_n\right)
$$


Where:
$\mathrm{n}=$ local concentration of electrons
$\mu_n=$ electron mobility
$E=$ electric field across the depletion part
$D_n=$ diffusion coefficient for electrons
$\mathrm{G}_{\mathrm{n}}=$ rate of generation of electrons
$R_n=$ rate of recombination of electrons

Continuity Equation in Cylindrical Coordinates

The continuity equation in cylindrical coordinates is:

$$
\frac{\partial p}{\partial t}+\frac{1}{r} \frac{\partial r p u}{\partial r}+\frac{1}{r} \frac{\partial p v}{\partial \theta}+\frac{\partial p w}{\partial z}=0
$$


Incompressible Flow Continuity Equation/ continuity equation incompressible flow

The continuity equation for incompressible flow as the density, $p=$ constant and is independent of distance and time, the equation is:

$$
\nabla . v=0
$$


Steady Flow Continuity Equation

The continuity equation in cylindrical coordinates is:

$$
\frac{\partial}{\partial x}(p u)+\frac{\partial}{\partial y}(p v)+\frac{\partial}{\partial z}(p w)=0
$$

All these are included in the equation of continuity class 11/continuity equation in three dimensions in fluid mechanics

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Commonly Asked Questions

Q: What are the assumptions made when deriving the continuity equation?
A:
The main assumptions in deriving the continuity equation are:
Q: Can the continuity equation be applied to gases as well as liquids?
A:
Yes, the continuity equation applies to both gases and liquids. However, for gases, which are compressible, the full form of the equation including density changes must be used. For liquids, which are generally treated as incompressible, the simplified form is often sufficient.
Q: What role does the continuity equation play in designing fluid systems like pipelines?
A:
In designing fluid systems, the continuity equation is crucial for:
Q: What is the difference between the differential and integral forms of the continuity equation?
A:
The differential form (∂ρ/∂t + ∇ · (ρv) = 0) describes mass conservation at a point, considering local changes in density and velocity. The integral form applies to a finite control volume, relating the mass flux through the boundaries to the rate of mass change within the volume. Both forms express the same principle but are used in different contexts.
Q: How does the continuity equation relate to the concept of incompressibility in fluids?
A:
For incompressible fluids, the continuity equation simplifies because density remains constant. This allows us to focus solely on the relationship between velocity and cross-sectional area. The assumption of incompressibility is often valid for liquids and gases at low speeds, making the simplified equation widely applicable.

Frequently Asked Questions (FAQs)

Q: What is the role of the continuity equation in studying sediment transport in rivers?
A:
In sediment transport studies, the continuity equation is
Q: How does the continuity equation relate to the concept of streamfunction in 2D flows?
A:
The streamfunction is a mathematical tool that automatically satisfies the continuity equation for 2D incompressible flows. It's defined such that its partial derivatives give the velocity components, ensuring mass conservation. This relationship simplifies the analysis of 2D flow problems by reducing the number of variables needed to describe the flow.
Q: Can you explain how the continuity equation is used in studying planetary atmospheres?
A:
For planetary atmospheres, the continuity equation helps:
Q: How does the continuity equation apply to porous media flow?
A:
In porous media, the continuity equation is modified to account for the porosity of the material. It describes how fluid moves through the interconnected pores, considering both the fluid properties and the characteristics of the porous medium. This is crucial in fields like hydrogeology, petroleum engineering, and filtration systems.
Q: What is the importance of the continuity equation in studying fluid-structure interactions?
A:
In fluid-structure interactions, the continuity equation helps:
Q: Can you explain how the continuity equation is used in studying heat transfer in fluids?
A:
While the continuity equation itself doesn't directly involve heat transfer, it's often used alongside energy equations in heat transfer problems. It ensures mass conservation while energy equations account for heat transfer. Together, they help model how fluid flow and heat transfer interact in systems like heat exchangers or natural convection processes.
Q: How does the continuity equation apply to non-uniform flows?
A:
For non-uniform flows, where fluid properties vary spatially, the full form of the continuity equation must be used. It accounts for changes in velocity, density, and cross-sectional area along the flow path. This is crucial for analyzing complex flow patterns in natural systems or engineered devices with varying geometries.
Q: What is the role of the continuity equation in studying tsunami propagation?
A:
In tsunami studies, the continuity equation is essential for:
Q: How does the continuity equation relate to the concept of fluid compressibility?
A:
The continuity equation accounts for fluid compressibility through the density term. For incompressible fluids, density remains constant, simplifying the equation. For compressible fluids, density changes must be considered, making the equation more complex. This distinction is crucial in analyzing flows where pressure changes significantly affect fluid density.
Q: Can you explain how the continuity equation is used in studying volcanic eruptions?
A:
In volcanology, the continuity equation helps: