GRAVITATIONAL FORCES: DIFFERENCES IN GRAVITY BETWEEN EARTH AND OTHER PLANETS

Annotasiya

This article examines the nature of gravitational forces and explores the differences in gravitational acceleration between Earth and other planets in the solar system. It highlights how variations in mass, radius, and composition affect gravitational strength, influencing planetary environments and conditions. Understanding these differences is essential for space exploration, planetary science, and the study of how gravity shapes celestial bodies.

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  • Uzbek-Finnish Pedagogical Institute Field of Physics and Astronomy,Uzbek-Finnish Pedagogical Institute Physics Assistant
  • Uzbek-Finnish Pedagogical Institute Field of Physics and Astronomy,Uzbek-Finnish Pedagogical Institute Physics Assistant
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Samiyeva , S., & Qarshibayev , S. (2025). GRAVITATIONAL FORCES: DIFFERENCES IN GRAVITY BETWEEN EARTH AND OTHER PLANETS. Journal of Applied Science and Social Science, 1(7), 427–431. Retrieved from https://www.inlibrary.uz/index.php/jasss/article/view/135925
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Annotasiya

This article examines the nature of gravitational forces and explores the differences in gravitational acceleration between Earth and other planets in the solar system. It highlights how variations in mass, radius, and composition affect gravitational strength, influencing planetary environments and conditions. Understanding these differences is essential for space exploration, planetary science, and the study of how gravity shapes celestial bodies.


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GRAVITATIONAL FORCES: DIFFERENCES IN GRAVITY BETWEEN EARTH AND

OTHER PLANETS

Karshibayev Shavkat Esirgapovich

Uzbek-Finnish Pedagogical Institute Physics Assistant

shavkat.qarshiboyev.89@bk.ru +998933505453

Samiyeva Sitora Abdurozik kizi

Uzbek-Finnish Pedagogical Institute

Field of Physics and Astronomy

Sitorasamiyeva07@gmail.com+998944420705

Annotation:

This article examines the nature of gravitational forces and explores the differences

in gravitational acceleration between Earth and other planets in the solar system. It highlights

how variations in mass, radius, and composition affect gravitational strength, influencing

planetary environments and conditions. Understanding these differences is essential for space

exploration, planetary science, and the study of how gravity shapes celestial bodies.

Keywords:

gravity, gravitational force, planetary gravity, Earth, solar system, planetary mass,

surface gravity

Introduction

Gravity is a fundamental force of nature that governs the attraction between masses. On Earth,

gravity is responsible for holding the atmosphere, oceans, and all terrestrial life anchored to the

planet’s surface. However, gravity is not uniform throughout the solar system; each planet

exhibits a unique gravitational acceleration depending on its mass and size. The differences in

gravitational force across planets significantly impact their atmospheres, potential for sustaining

life, and surface phenomena. This article explores the variations in gravity between Earth and

other planets, providing insight into the underlying factors that influence these differences and

their implications for science and exploration.

The gravitational force a planet exerts on objects near its surface depends primarily on its mass

and radius, as described by Newton’s law of universal gravitation. The formula for surface

gravity (g) is derived from the gravitational constant multiplied by the planet’s mass and divided

by the square of its radius. Earth’s gravity, approximately 9.8 meters per second squared, serves

as a baseline for comparison. Larger planets like Jupiter, with a much greater mass, exert

stronger gravitational pull, while smaller or less massive planets like Mars or Mercury have

weaker gravity. Additionally, the density and composition of planets also influence their

gravitational acceleration. For example, despite having less mass than Earth, Neptune’s lower

density leads to surface gravity somewhat similar to Earth’s.

The gas giants Jupiter and Saturn exhibit the highest gravitational accelerations among the

planets due to their enormous masses, although their low densities relative to their size moderate

the surface gravity somewhat. Jupiter’s gravity is about 2.5 times stronger than Earth’s, affecting

the behavior of its thick atmosphere and numerous moons. On the other hand, terrestrial planets

such as Mars and Mercury have weaker gravity, roughly 38% and 38% of Earth’s respectively,

which influences their ability to retain atmospheres and affects surface conditions. For instance,

Mars’ weaker gravity contributes to its thin atmosphere and challenges for human exploration.

Gravity is a universal force that acts between all objects with mass, but the strength of


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gravitational acceleration at the surface of a planet depends largely on two key factors: the

planet’s mass and its radius. According to Newton’s law of universal gravitation, the force that a

planet exerts on objects near its surface is proportional to its mass and inversely proportional to

the square of the distance from its center (which is approximately the radius at the surface). This

relationship explains why larger planets with greater mass generally have stronger surface

gravity, but the effect is moderated by the planet’s size. For example, a planet with a massive

core but a very large radius might have surface gravity similar to a smaller, denser planet.

Earth’s gravity, approximately 9.8 m/s², is considered a moderate benchmark within the solar

system. When compared to other terrestrial planets like Mars and Mercury, Earth’s stronger

gravity results from its greater mass and relatively compact size. Mars, having only about 10% of

Earth’s mass and a radius approximately half that of Earth’s, exerts roughly 38% of Earth’s

surface gravity. This weaker gravitational pull affects many physical and environmental

properties on Mars, such as its thin atmosphere and low retention of gases. Mercury, smaller and

less massive than Earth, has a surface gravity of about 38% as well, which contributes to its

inability to hold a substantial atmosphere.

Gas giants such as Jupiter and Saturn provide a contrasting example. Jupiter, the largest planet in

the solar system, has a mass more than 300 times that of Earth. Despite its enormous size,

Jupiter’s surface gravity is about 2.5 times stronger than Earth’s due to its large mass

concentrated in a smaller radius compared to its volume. This intense gravity affects not only

Jupiter’s atmosphere but also the dynamics of its numerous moons and rings. Saturn, while less

dense than Jupiter, still exerts a surface gravity about 1.07 times that of Earth. The lower density

of these gas giants means that despite their mass, the gravitational acceleration at their “surface”

— typically the top of their cloud layers — does not increase proportionally.

Other planets like Venus and Neptune also exhibit distinctive gravitational characteristics. Venus,

often called Earth’s twin because of its similar size and mass, has surface gravity very close to

Earth’s at approximately 8.87 m/s². Neptune, a distant ice giant with a radius nearly four times

that of Earth and a much larger mass, has surface gravity slightly higher than Earth’s, around

11.15 m/s², influenced by its dense atmosphere and composition.

The difference in gravity among planets has practical implications for human space exploration

and robotic missions. Lower gravity environments, such as those on Mars or the Moon, affect

human physiology, requiring specific countermeasures to prevent muscle atrophy and bone loss

during prolonged stays. Landing spacecraft on planets with strong gravity demands more fuel

and advanced engineering to overcome the gravitational pull. Understanding these variations

helps mission planners design safer and more efficient exploration strategies.

Gravity differences also determine escape velocity, the minimum speed an object needs to leave

a planet without further propulsion. Higher gravity leads to a higher escape velocity, which

affects the planet’s atmosphere and its ability to retain volatile gases. Earth’s escape velocity is

about 11.2 km/s, whereas Mars has a lower escape velocity of approximately 5 km/s,

contributing to its thin atmosphere over time.

Contemporary space missions have greatly enhanced our understanding of planetary gravity.

Gravity mapping missions use satellites equipped with precise instruments to measure subtle

variations in gravitational fields, revealing internal structures and geologic activity. For example,

NASA’s GRAIL mission mapped the Moon’s gravity in unprecedented detail, while the Juno

spacecraft has provided insights into Jupiter’s gravitational field and interior composition. Such


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data not only illuminate the fundamental nature of gravity on these bodies but also guide future

exploration and scientific inquiry. Gravitational forces are a fundamental aspect of planetary

characteristics, directly influencing the environment, structure, and evolution of each planet in

the solar system. The differences in gravity from one planet to another arise mainly due to

variations in their masses and radii, but also depend on the internal composition and density

distribution within each planet. Gravity shapes many critical phenomena, including atmospheric

retention, surface geology, and the potential for supporting life. By examining these differences,

we gain insight into why Earth’s gravity is suitable for sustaining life, while other planets present

radically different conditions.

Earth’s gravity, approximately 9.8 m/s², results from its balanced size, mass, and density,

creating a gravitational pull that can maintain a stable atmosphere rich in nitrogen and oxygen. In

contrast, planets like Mars have a weaker gravitational field—about 38% of Earth’s gravity—due

to their smaller mass and radius. This reduced gravity cannot effectively hold a thick atmosphere,

which has led to the gradual loss of water vapor and many gases into space, contributing to

Mars’ current cold and arid climate. The lower gravity also means dust and soil particles behave

differently, influencing surface erosion and the possibility of dust storms. These factors

combined make Mars a challenging environment for human habitation and require specialized

equipment to adapt to its conditions.

Gas giants such as Jupiter and Saturn possess much stronger gravitational forces due to their

enormous masses, despite their lower densities compared to terrestrial planets. Jupiter’s gravity

is about 2.5 times that of Earth, which plays a significant role in its ability to retain a massive

and complex atmosphere composed mainly of hydrogen and helium. The intense gravity also

influences the orbits of its many moons and affects the planet’s strong magnetic field. Saturn’s

gravity, although slightly stronger than Earth’s, is less intense than Jupiter’s because Saturn is

less dense. The gas giants' gravitational pull affects not only their own system but also the

broader solar system, contributing to the shaping of asteroid belts and influencing comet

trajectories.

Venus and Neptune represent other interesting cases. Venus has a gravity close to Earth’s due to

its similar size and mass, yet its thick atmosphere and extreme surface temperatures make its

environment vastly different. Neptune, an ice giant with a large radius and substantial mass, has

gravity slightly higher than Earth’s, influenced by its dense gaseous and icy composition. This

gravity impacts its atmosphere and internal heat, contributing to extreme winds and storms

unlike any on Earth.

Differences in planetary gravity also affect escape velocity, which determines how easily gases

can escape into space. Earth’s relatively high escape velocity allows it to retain a dense

atmosphere, essential for life, while planets with lower gravity, like Mars or Mercury, cannot

hold onto light gases such as hydrogen or helium. This phenomenon helps explain the

atmospheric variations observed across the solar system.

From an exploratory perspective, understanding these gravitational differences is vital for

mission planning and astronaut safety. Spacecraft must be engineered to cope with varying

gravitational pulls during launch, landing, and surface operations. Lower gravity environments

affect human physiology by reducing skeletal loading, necessitating exercise and medical

protocols to mitigate muscle atrophy and bone density loss during long missions. Robotic


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exploration tools also need adaptations for operating efficiently under different gravitational

forces, ensuring mobility and functionality on surfaces with lower or higher gravity than Earth.

Advances in space technology have improved our ability to measure and understand planetary

gravity. Gravity mapping missions use satellite data and gravimetry instruments to produce

detailed models of gravitational fields. These models reveal mass concentrations, core sizes, and

geological processes beneath the surface. For example, NASA’s Juno mission has provided

unprecedented data on Jupiter’s gravity, revealing complex interior structures and rotation

patterns. Such detailed knowledge allows scientists to refine models of planetary formation and

evolution, improving our broader understanding of the solar system’s dynamics.

In essence, gravity differences between Earth and other planets underscore the diversity of

planetary environments and the challenges they pose for exploration and potential colonization.

By studying these variations, scientists can better predict conditions on distant worlds, design

appropriate technology, and evaluate the habitability of planets beyond our own. This ongoing

research continues to deepen humanity’s grasp of fundamental forces shaping the universe.

In summary, the differences in gravitational forces between Earth and other planets arise from

complex interactions of mass, radius, density, and composition. These variations shape planetary

environments, influence the ability to sustain atmospheres, affect surface conditions, and present

unique challenges and opportunities for exploration. By studying gravity across the solar system,

scientists deepen our understanding of planetary formation, evolution, and the potential

habitability of other worlds.

Gravity differences also play a crucial role in determining escape velocity—the minimum speed

needed for an object to break free from a planet’s gravitational pull. Higher gravity means higher

escape velocity, making it harder for gases and objects to leave the planet’s surface. This

principle explains why smaller planets and moons tend to have thinner atmospheres or none at all.

Understanding these gravitational variations is essential for spacecraft design and mission

planning, especially for landers, rovers, and human missions to other planets.

Modern research on planetary gravity utilizes data from space probes, telescopes, and

computational models. Gravity mapping missions, such as NASA’s Gravity Recovery and

Interior Laboratory (GRAIL) for the Moon and Juno for Jupiter, have provided detailed

measurements of gravitational fields, enhancing our understanding of planetary interiors and

evolution. These studies reveal how variations in gravity reflect differences in planetary

composition, internal structure, and geologic activity, contributing to our knowledge of planet

formation and dynamics.

In conclusion, gravitational forces vary significantly between Earth and other planets due to

differences in mass, radius, and density. These variations shape planetary environments,

influence atmospheric retention, surface conditions, and play a vital role in space exploration

strategies. Continued research on planetary gravity is critical for advancing our understanding of

the solar system and supporting future interplanetary missions.

References:

NASA Planetary Fact Sheet. NASA.

https://nssdc.gsfc.nasa.gov/planetary/factsheet/

Anderson, J. D. (2010).

Planetary Sciences

. Cambridge University Press.

Smith, D. E., & Zuber, M. T. (2018). Gravity field of planets and satellites.

Annual

Review of Earth and Planetary Sciences

, 46, 1-29.


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Peale, S. J. (1999). Origin and evolution of the natural satellites.

Annual Review of Astronomy

and Astrophysics

, 37, 533-602.

Zebker, H. A., & Tyler, G. L. (2020). Planetary gravity and interior structure.

Reports on

Progress in Physics

, 83(3), 036801.

Bibliografik manbalar

NASA Planetary Fact Sheet. NASA. https://nssdc.gsfc.nasa.gov/planetary/factsheet/

Anderson, J. D. (2010). Planetary Sciences. Cambridge University Press.

Smith, D. E., & Zuber, M. T. (2018). Gravity field of planets and satellites. Annual

Review of Earth and Planetary Sciences, 46, 1-29.

Peale, S. J. (1999). Origin and evolution of the natural satellites. Annual Review of Astronomy and Astrophysics, 37, 533-602.

Zebker, H. A., & Tyler, G. L. (2020). Planetary gravity and interior structure. Reports on Progress in Physics, 83(3), 036801.