Video Experimental Relacionado
Updated: Dec 6, 2025

06:29
Simulation of Early Earth Hydrothermal Chimneys in a Thermal Gradient Environment
Published on: February 27, 2021
3.9K
Venas de carbonato brillante en el asteroide (101955) Bennu: Implicaciones para la historia de la alteración acuosa
H H Kaplan1,2, D S Lauretta3, A A Simon4
1NASA Goddard Space Flight Center, Greenbelt, MD, USA. hannah.kaplan@nasa.gov.
Resumen
El asteroide Bennu
Área de la Ciencia:
- Ciencias planetarias
- Astrogeología
- La evolución temprana del sistema solar
Sus antecedentes:
- La composición de los asteroides y las conexiones de los meteoritos revelan la geología temprana del Sistema Solar.
- El asteroide cercano a la Tierra Bennu es un asteroide carbonoso.
- Los meteoritos de condrita carbonácea muestran evidencia de alteración acuosa.
Objetivo del estudio:
- Para analizar datos espectrales de la región del cráter Nightingale de Bennu.
- Para investigar la composición de las venas brillantes observadas en las rocas de Bennu.
- Para entender los primeros procesos geológicos en los asteroides.
Principales métodos:
- Análisis espectral de la región del cráter Nightingale en el asteroide Bennu.
- Imágenes de las rocas para identificar las características de la superficie.
- Interpretación de las características de absorción espectral y las características visuales.
Principales resultados:
- Se detectó una característica de absorción infrarroja distinta de alrededor de 3,4 micrómetros en la región del cráter Nightingale.
- Se observaron venas brillantes de un metro de largo y centímetros de espesor en las rocas de Bennu.
- Estas venas se interpretan como depósitos potenciales de carbonato.
Conclusiones:
- La presencia de venas de carbonato sugiere una alteración hidrotermal a gran escala en el cuerpo principal de Bennu.
- El flujo y la deposición de fluidos se produjeron a escalas de kilómetros durante períodos prolongados.
- Esto indica la alteración hidrotermal del sistema abierto de asteroides carbonáceos en el Sistema Solar temprano.
Videos de Conceptos Relacionados
Conditions on Early Earth
99.8K
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.
99.8K
Minerals
849
Minerals are essential nutrients that the human body needs in small amounts to work properly. They play a vital role in many bodily functions, such as building strong bones and transmitting nerve impulses. Some minerals are needed for hormone production or to maintain a normal heartbeat. Major minerals include calcium, phosphorus, potassium, sulfur, sodium, chlorine, and magnesium, while trace minerals include iron, manganese, copper, iodine, zinc, cobalt, fluoride, and selenium.
Major...
Major...
849
Gravimetry: Inorganic And Organic Precipitating Agents
4.4K
In gravimetry, the precipitant is chosen carefully to obtain a pure solid that can be easily filtered. Common inorganic precipitants can be used to determine several cations and anions. In some cases, the formation of the same precipitate can be used to determine the cation and the anion. For example, the reaction of barium and chromate ions to give barium chromate is used to determine both barium and chromate. However, precipitates such as hydroxides, oxalates, and metal ammonium phosphates...
4.4K
Green Algae
523
Green algae, also referred to as chlorophytes, are different from red algae in having the chloroplasts containing chlorophylls a and b, which give them their distinct green hue. However, they lack phycobiliproteins, preventing them from developing the red or blue-green pigmentation seen in red algae. In terms of photosynthetic pigment composition, green algae closely resemble plants and share a close evolutionary relationship with them. Taxonomically Green algae belong to Phylum Chlorophyta in...
523
Water and Mineral Acquisition
34.9K
Specialized tissues in plant roots have evolved to capture water, minerals, and some ions from the soil. Roots exhibit a variety of branching patterns that facilitate this process. The outermost root cells have specialized structures called root hairs that increase the root surface, thus increasing soil contact. Water can passively cross into roots, as the concentration of water in the soil is higher than that of the root tissue. Minerals, in contrast, are actively transported into root cells.
34.9K
Water: A Bronsted-Lowry Acid and Base
56.0K
The reaction between a Brønsted-Lowry acid and water is called acid ionization. For example, when hydrogen fluoride dissolves in water and ionizes, protons are transferred from hydrogen fluoride molecules to water molecules, yielding hydronium ions and fluoride ions:
56.0K

