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Calculate The Acceleration Of Gravity

Gravitational Acceleration Formula:

\[ g = \frac{G M}{r^2} = 9.81 \, \text{m/s}^2 \]

m³ kg⁻¹ s⁻²
kg
m

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1. What is Gravitational Acceleration?

Gravitational acceleration (g) is the acceleration of an object due to the force of gravity. On Earth's surface, it is approximately 9.81 m/s² and represents the rate at which objects accelerate when falling freely under gravity's influence.

2. How Does the Calculator Work?

The calculator uses Newton's law of universal gravitation formula:

\[ g = \frac{G M}{r^2} \]

Where:

Explanation: This formula calculates the acceleration due to gravity at a specific distance from the center of a celestial body, based on its mass and the universal gravitational constant.

3. Importance of Gravitational Acceleration

Details: Gravitational acceleration is fundamental in physics, engineering, and astronomy. It affects everything from planetary motion to structural design, satellite orbits, and everyday phenomena like falling objects and fluid dynamics.

4. Using the Calculator

Tips: Enter the gravitational constant (typically 6.674×10⁻¹¹), the mass of the celestial body in kilograms, and the radius from the center in meters. All values must be positive numbers.

5. Frequently Asked Questions (FAQ)

Q1: Why is Earth's gravity approximately 9.81 m/s²?
A: This value results from Earth's mass (5.972×10²⁴ kg) and radius (6.371×10⁶ m) using the gravitational formula.

Q2: How does gravity vary with altitude?
A: Gravity decreases with the square of the distance from Earth's center, so it's slightly less at higher altitudes.

Q3: What is g on other planets?
A: Mars: 3.71 m/s², Moon: 1.62 m/s², Jupiter: 24.79 m/s². Each planet's gravity depends on its mass and radius.

Q4: Is gravitational constant truly constant?
A: Yes, G is a fundamental physical constant that appears to be the same throughout the universe.

Q5: How accurate is this calculation for real-world applications?
A: Very accurate for ideal spherical bodies. For precise Earth calculations, factors like rotation and non-spherical shape cause minor variations.

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