Jove
Visualize
Contáctanos
JoVE
x logofacebook logolinkedin logoyoutube logo
ACERCA DE JoVE
Visión GeneralLiderazgoBlogCentro de Ayuda JoVE
AUTORES
Proceso de PublicaciónConsejo EditorialAlcance y PolíticasRevisión por ParesPreguntas FrecuentesEnviar
BIBLIOTECARIOS
TestimoniosSuscripcionesAccesoRecursosConsejo Asesor de BibliotecasPreguntas Frecuentes
INVESTIGACIÓN
JoVE JournalMethods CollectionsJoVE Encyclopedia of ExperimentsArchivo
EDUCACIÓN
JoVE CoreJoVE BusinessJoVE Science EducationJoVE Lab ManualCentro de Recursos para ProfesoresSitio de Profesores
Términos y Condiciones de Uso
Política de Privacidad
Políticas

Videos de Conceptos Relacionados

Kepler's Second Law of Planetary Motion01:29

Kepler's Second Law of Planetary Motion

In the early 17th century, German astronomer and mathematician Johannes Kepler postulated three laws for the motion of planets in the solar system. His first law states that all planets orbit the Sun in an elliptical orbit, with the Sun at one of the ellipse's foci. Therefore, the distance of a planet from the Sun varies throughout its revolution around the Sun.
While in an elliptical orbit, the total energy of the planet is conserved. Therefore, the planet slows down when it is at apogee and...
Kepler's First Law of Planetary Motion01:10

Kepler's First Law of Planetary Motion

In the early 17th century, German astronomer and mathematician Johannes Kepler postulated three laws for the motion of planets in the solar system. He formulated his first two laws based on the observations of his forebears, Nikolaus Copernicus and Tycho Brahe.
Polish astronomer Nikolaus Copernicus put forth a theory that stated a heliocentric model for the solar system. According to this heliocentric theory, all the planets, including Earth, orbit the Sun in circular orbits.
On the other hand,...
Kepler's Third Law of Planetary Motion01:18

Kepler's Third Law of Planetary Motion

In the early 17th century, German astronomer and mathematician Johannes Kepler postulated three laws for the motion of planets in the solar system. In 1909, he formulated his first two laws based on the observations of his forebears, Nikolaus Copernicus and Tycho Brahe. However, in 1918, he published his third law of planetary motion, which gives a precise mathematical relationship between a planet's average distance from the Sun and the amount of time it takes to revolve around the Sun. It...
Thomson's e/m Experiment01:19

Thomson's e/m Experiment

In a beam of charged particles created by a heated cathode, the particles move at different speeds. However, many applications need a beam with uniform particle speeds. An arrangement known as a velocity selector uses electric and magnetic fields to pick particles with a particular speed from the beam.
A particle with charge q, speed v, and mass m enters an area from the top, where the magnetic and electric fields are perpendicular both to the particle's motion and to one another. The magnetic...
Acceleration due to Gravity on Other Planets01:24

Acceleration due to Gravity on Other Planets

The gravitational acceleration of an object near the Earth's surface is called the acceleration due to gravity. It can be measured by conducting simple experiments on Earth. However, such an experiment is impossible to conduct on the surface of other planets.
Astronomical observations are thus used to measure the acceleration due to gravity on other planets. This can be determined by observing the effect of a planet's gravity on objects close to it. The crucial factor that helps in this...
Circular Orbits and Critical Velocity for Satellites01:16

Circular Orbits and Critical Velocity for Satellites

The Moon orbits around the Earth. In turn, the Earth (and other planets) orbit the Sun. The space directly above our atmosphere is filled with artificial satellites in orbit. One can examine the circular orbit, the simplest kind of orbit, to understand the relationship between the speed and the period of planets and satellites with respect to their positions and the bodies that they orbit.
Nicolaus Copernicus (1473-1543) first suggested that the Earth and all other planets orbit the Sun in...

También podría leer

Artículos Relacionados

Artículos vinculados a este trabajo por autores compartidos, revista y gráfico de citas.

Ordenar por
Same author

New Measurements of the Deuteron-to-Proton F_{2} Structure-Function Ratio.

Physical review letters·2025
Same author

Determinants of short interpregnancy intervals in high-income countries: a systematic review.

Sexual and reproductive health matters·2025
Same author

Reporting of paediatric osteoporotic vertebral fractures in Duchenne muscular dystrophy and potential impact on clinical management: the need for standardised and structured reporting.

Pediatric radiology·2023
Same author

Endocrine and Bone Monitoring in Boys with Duchenne Muscular Dystrophy; Do we adhere to the standards of care?

Journal of neuromuscular diseases·2023
Same author

Cellular and humoral immunogenicity of the COVID-19 vaccine and COVID-19 disease severity in individuals with immunodeficiency.

Frontiers in immunology·2023
Same author

Determining the gluonic gravitational form factors of the proton.

Nature·2023

Video Experimental Relacionado

Updated: Jul 12, 2026

Bringing the Visible Universe into Focus with Robo-AO
10:35

Bringing the Visible Universe into Focus with Robo-AO

Published on: February 12, 2013

El encuentro de Venus con Galileo.

T V Johnson, C M Yeates, R Young

    Science (New York, N.Y.)
    |September 27, 1991
    PubMed
    Resumen
    Este resumen es generado por máquina.

    La nave espacial Galileo proporcionó nuevos datos sobre el entorno de plasma y los patrones de nubes de Venus durante su sobrevuelo de 1990. Estas observaciones, combinadas con datos terrestres, mejoraron nuestra comprensión de Venus, incluido el rayo potencial.

    Más Videos Relacionados

    Scattering And Absorption of Light in Planetary Regoliths
    11:34

    Scattering And Absorption of Light in Planetary Regoliths

    Published on: July 1, 2019

    Thermocapillary Convection Space Experiment on the SJ-10 Recoverable Satellite
    07:00

    Thermocapillary Convection Space Experiment on the SJ-10 Recoverable Satellite

    Published on: March 11, 2020

    Videos de Experimentos Relacionados

    Last Updated: Jul 12, 2026

    Bringing the Visible Universe into Focus with Robo-AO
    10:35

    Bringing the Visible Universe into Focus with Robo-AO

    Published on: February 12, 2013

    Scattering And Absorption of Light in Planetary Regoliths
    11:34

    Scattering And Absorption of Light in Planetary Regoliths

    Published on: July 1, 2019

    Thermocapillary Convection Space Experiment on the SJ-10 Recoverable Satellite
    07:00

    Thermocapillary Convection Space Experiment on the SJ-10 Recoverable Satellite

    Published on: March 11, 2020

    Área de la Ciencia:

    • Ciencias planetarias Ciencias planetarias.
    • Exploración del espacio Exploración espacial
    • Física de la atmósfera Física de la atmósfera

    Sus antecedentes:

    • La nave espacial Galileo fue lanzada en 1989 para una misión a Júpiter.
    • La trayectoria de Galileo incluyó un sobrevuelo de Venus en febrero de 1990.

    Objetivo del estudio:

    • Para recopilar datos completos sobre Venus durante el sobrevuelo de Galileo.
    • Para mejorar la comprensión del entorno de plasma de Venus, la dinámica de las nubes y los fenómenos atmosféricos.

    Principales métodos:

    • Utilizó los instrumentos científicos de la nave espacial Galileo para mediciones in situ.
    • Datos integrados de naves espaciales con observaciones astronómicas terrestres simultáneas.

    Principales resultados:

    • Adquirió extensas mediciones del entorno de plasma de Venus.
    • Obtuvo observaciones detalladas de los patrones de nubes de Venus.
    • Recopilado evidencia que sugiere la posible existencia de rayos en Venus.

    Conclusiones:

    • El encuentro con Venus de Galileo proporcionó datos valiosos y multifacéticos.
    • Conocimiento científico mejorado de las condiciones atmosféricas y de plasma de Venus.
    • La misión contribuyó a la investigación en curso sobre las atmósferas planetarias y los fenómenos eléctricos.