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Conditions on Early Earth02:06

Conditions on Early Earth

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Around 4 billion years ago, oceans began to condense on earth while volcanic eruptions released nitrogen, carbon dioxide, methane, ammonia, and hydrogen into the primordial atmosphere. However, organisms with the characteristics of life were not initially present on earth. Scientists have used experimentation to determine how organisms evolved that could grow, reproduce, and maintain an internal environment.
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Nuclear Stability03:18

Nuclear Stability

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Protons and neutrons, collectively called nucleons, are packed together tightly in a nucleus. With a radius of about 10−15 meters, a nucleus is quite small compared to the radius of the entire atom, which is about 10−10 meters. Nuclei are extremely dense compared to bulk matter, averaging 1.8 × 1014 grams per cubic centimeter. If the earth’s density were equal to the average nuclear density, the earth’s radius would be only about 200 meters.
To hold positively charged protons together...
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Nuclear Fusion02:45

Nuclear Fusion

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The process of converting very light nuclei into heavier nuclei is also accompanied by the conversion of mass into large amounts of energy, a process called fusion. The principal source of energy in the sun is a net fusion reaction in which four hydrogen nuclei fuse and ultimately produce one helium nucleus and two positrons.
A helium nucleus has a mass that is 0.7% less than that of four hydrogen nuclei; this lost mass is converted into energy during the fusion. This reaction produces about...
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Nuclear Transmutation03:20

Nuclear Transmutation

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Nuclear transmutation is the conversion of one nuclide into another. It can occur by the radioactive decay of a nucleus, or the reaction of a nucleus with another particle. The first manmade nucleus was produced in Ernest Rutherford’s laboratory in 1919 by a transmutation reaction, the bombardment of one type of nuclei with other nuclei or with neutrons. Rutherford bombarded nitrogen-14 atoms with high-speed α particles from a natural radioactive isotope of radium and observed...
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Nuclear Fission02:50

Nuclear Fission

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Many heavier elements with smaller binding energies per nucleon can decompose into more stable elements that have intermediate mass numbers and larger binding energies per nucleon—that is, mass numbers and binding energies per nucleon that are closer to the “peak” of the binding energy graph near 56. Sometimes neutrons are also produced. This decomposition of a large nucleus into smaller pieces is called fission. The breaking is rather random with the formation of a large...
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Conservation of Mass in Finite Cotrol Volume01:16

Conservation of Mass in Finite Cotrol Volume

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The principle of conservation of mass is a fundamental law in fluid mechanics and is applied using the continuity equation. We apply the concept to a finite control volume to derive the continuity equation.
A system is defined as a collection of unchanging contents, and the conservation of mass states that a system's mass is constant.
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Updated: Sep 9, 2025

Simulation of the Planetary Interior Differentiation Processes in the Laboratory
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Simulation of the Planetary Interior Differentiation Processes in the Laboratory

Published on: November 15, 2013

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Restringir la composición del núcleo de la Tierra desde la nucleación del núcleo interno

Alfred J Wilson1, Christopher J Davies2, Andrew M Walker3

  • 1School of Earth and Environment, University of Leeds, Leeds, UK. a.j.wilson1@leeds.ac.uk.

Nature communications
|September 4, 2025
PubMed
Resumen
Este resumen es generado por máquina.

La composición del núcleo de la Tierra es clave para su evolución. Las nuevas simulaciones muestran que los núcleos de hierro y carbono son compatibles con la nucleación interna del núcleo, lo que limita sus posibles elementos.

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Área de la Ciencia:

  • La geofísica
  • Ciencias de la Tierra
  • Ciencias planetarias

Sus antecedentes:

  • La composición del núcleo de la Tierra es crucial para comprender la estructura profunda de la Tierra, la evolución térmica y la generación de campos magnéticos.
  • Los modelos actuales enfrentan desafíos en la conciliación de datos cosmoquímicos, de formación y sismológicos con la composición del núcleo.
  • El papel del súper enfriamiento en la formación del núcleo interno ha sido un tema de debate, ya que algunas composiciones de núcleos binarios son incompatibles con la nucleación.

Objetivo del estudio:

  • Investigar la compatibilidad de las composiciones específicas del núcleo de hierro-carbono (Fe-C) con la nucleación interna del núcleo.
  • Determinar si las aleaciones de Fe-C pueden nuclearse en condiciones geofísicas realistas, cumpliendo los requisitos de sobreenfriamiento.
  • Para refinar las restricciones en la composición del núcleo de la Tierra mediante la evaluación del comportamiento de la nucleación.

Principales métodos:

  • Utilizó simulaciones de dinámica molecular para modelar el proceso de nucleación del núcleo interno.
  • Se ha simulado una composición hierro-carbono (Fe1-xC x=0,1-0,15) en condiciones de presión y temperatura pertinentes.
  • Resultados de simulación comparados con las restricciones geofísicas existentes en la formación y las propiedades del núcleo.

Principales resultados:

  • Se ha demostrado que una composición Fe-C (Fe1-xC x=0,1-0,15) es compatible con la nucleación del núcleo interno.
  • Demostró que esta composición específica puede nuclear sin requerir un súper enfriamiento extremo, alineándose con las observaciones geofísicas.
  • Identificó la nucleación interna como un factor significativo para discriminar entre las posibles composiciones del núcleo.

Conclusiones:

  • La nucleación del núcleo interno proporciona una fuerte restricción en la posible composición química del núcleo de la Tierra.
  • Las aleaciones de hierro y carbono son candidatos plausibles para la composición del núcleo de la Tierra, consistentes con la dinámica de la nucleación.
  • Este estudio avanza en nuestra comprensión de la formación y composición del núcleo, ayudando a resolver enigmas geofísicos de larga data.