Video Experimental Relacionado
Updated: Jul 12, 2026

11:50
Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
Published on: June 13, 2015
Gases nobles en el meteorito Murchison: Posibles reliquias del proceso s de nucleosíntesis
Resumen
Los meteoritos primitivos contienen granos de polvo presolar de gigantes rojas, evidenciados por patrones únicos de isótopos de xenón. Estos hallazgos sugieren que los procesos nucleares específicos ocurrieron en las estrellas evolucionadas antes de la formación del sistema solar.
Área de la Ciencia:
- Cosmoquímica es la cosmoquímica.
- La astrofísica nuclear es una astrofísica nuclear.
- Ciencias planetarias Ciencias planetarias.
Sus antecedentes:
- Las condritas carbonáceas, como el meteorito Murchison, son materiales primitivos del sistema solar.
- Las anomalías del isótopo de xenón en los meteoritos pueden proporcionar información sobre la nucleosíntesis presolar.
- Estudios anteriores han identificado varios componentes presolares en los meteoritos.
Objetivo del estudio:
- Para identificar y caracterizar un nuevo componente isotópico de xenón en el meteorito Murchison.
- Para investigar el origen de los enriquecimientos anómalos de isótopos de gases nobles.
- Para vincular estas anomalías a procesos específicos de nucleosíntesis estelar.
Principales métodos:
- Análisis de gases nobles de una fracción mineral específica del meteorito Murchison.
- Experimentos de calentamiento escalonado a alta temperatura para liberar gases atrapados.
- Análisis isotópico de xenón, criptón, neón y helio.
Principales resultados:
- Descubrimiento de un nuevo componente de xenón enriquecido en los isótopos 128-132.
- Identificación de enriquecimientos similares, aunque más pequeños, en los isótopos de criptón 80 y 82.
- Enriquecimientos anómalos observados en el neón-22 y el helio-3, liberados simultáneamente.
Conclusiones:
- Los patrones isotópicos observados sugieren fuertemente orígenes de la nucleosíntesis estelar, específicamente el proceso s y la quema de la cáscara de helio/hidrógeno en las gigantes rojas.
- Esto indica la presencia de granos de polvo presolar expulsados de estrellas gigantes rojas dentro de meteoritos primitivos.
- Estos hallazgos contribuyen a comprender la diversidad de los materiales presolares y la evolución química temprana del sistema solar.
Videos de Conceptos Relacionados
Noble Gases
The elements in group 18 are noble gases (helium, neon, argon, krypton, xenon, and radon). They earned the name “noble” because they were assumed to be nonreactive since they have filled valence shells. In 1962, Dr. Neil Bartlett at the University of British Columbia proved this assumption to be false.
Nuclear Transmutation
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 protons being...
Elements: Chemical Symbols and Isotopes
A chemical symbol is an abbreviation used to indicate an element or an atom of an element. For example, the symbol for mercury is Hg. The same symbol is used to indicate one atom of mercury (microscopic domain) or to label a container of many atoms of the element mercury (macroscopic domain).
Some symbols are derived from the common English name of the element; others are abbreviations of the name in another language — Latin, Greek or German. For example, the symbol for aluminum (common name)...
Some symbols are derived from the common English name of the element; others are abbreviations of the name in another language — Latin, Greek or German. For example, the symbol for aluminum (common name)...
Conditions on Early Earth
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.
Conditions on Early Earth
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.
Nuclear Stability
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 in the...
To hold positively charged protons together in the...

