Jove
Visualize
Contáctanos

Videos de Conceptos Relacionados

Elements and Compounds01:27

Elements and Compounds

Pure substances consist of only one type of matter. A pure substance can be an element or a compound. An element consists of only one type of atom, while a compound consists of two or more types of atoms held together by a chemical bond.ElementsElements are classified as atomic or molecular based on the nature of their basic units. They are unique forms of matter with specific chemical and physical properties that cannot break down into smaller substances by ordinary chemical reactions. There...
The Soil Ecosystem02:23

The Soil Ecosystem

Plants obtain inorganic minerals and water from the soil, which acts as a natural medium for land plants. The composition and quality of soil depend not only on the chemical constituents but also on the presence of living organisms. In general, soils contain three major components:
Network Covalent Solids02:18

Network Covalent Solids

Network covalent solids contain a three-dimensional network of covalently bonded atoms as found in the crystal structures of nonmetals like diamond, graphite, silicon, and some covalent compounds, such as silicon dioxide (sand) and silicon carbide (carborundum, the abrasive on sandpaper). Many minerals have networks of covalent bonds.
To break or to melt a covalent network solid, covalent bonds must be broken. Because covalent bonds are relatively strong, covalent network solids are typically...
Layers of the Epidermis01:21

Layers of the Epidermis

The epidermis, the outermost layer of the skin, is composed of several distinct layers. From deep to superficial, the layers of the epidermis are as follows:
Stratum Basale
Stratum basale, also known as the stratum germinativum, is the deepest layer of the epidermis. It is composed of a single layer of actively dividing cells called basal cells or basal keratinocytes. These cells constantly undergo cell division to replenish the upper layers of the epidermis. Additionally, melanocytes, which...
Gravimetry: Inorganic And Organic Precipitating Agents00:49

Gravimetry: Inorganic And Organic Precipitating Agents

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...
Deep Sea Microbial Ecology01:18

Deep Sea Microbial Ecology

The deep ocean and its underlying sediments represent vast, largely unexplored microbial habitats that extend far beyond the sunlit photic zone. The photic (euphotic) zone typically spans the upper ~100–200 meters of pelagic waters in the open ocean, but its depth varies geographically and seasonally, where sufficient light supports photosynthetic life. Below this lies the deep sea, spanning roughly 1000–6000 meters (bathypelagic to abyssal zones), with deeper hadal trenches extending beyond...

También podría leer

Artículos Relacionados

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

Ordenar por
Same author

Geminal bis-ureas as gelators for organic solvents: gelation properties and structural studies in solution and in the gel state

Chemistry (Weinheim an der Bergstrasse, Germany)·2000
Same author

Dynamics of the silicon (111) surface phase transition

Nature·2000
Same author

Remarkable O(2)-effect in 1,4-additions of diethylzinc to 6-acyloxy-2H-pyran-3(6H)-ones and 6-alkoxy-2H-pyran-3(6H)-ones

Organic letters·2000
Same author

Development of Male Flowers in Zizania aquatica (North American Wild-Rice; Gramineae).

International journal of plant sciences·2000
Same author

Posterior cervical arthrodesis and stabilization: an early report using a novel lateral mass screw and rod technique

Neurosurgery·1999
Same author

Compositional heterogeneity in the bottom 1000 kilometers of Earth's mantle: toward a hybrid convection model

Science (New York, N.Y.)·1999
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

Video Experimental Relacionado

Updated: Jun 30, 2026

Quantification of Hydrogen Concentrations in Surface and Interface Layers and Bulk Materials through Depth Profiling with Nuclear Reaction Analysis
14:11

Quantification of Hydrogen Concentrations in Surface and Interface Layers and Bulk Materials through Depth Profiling with Nuclear Reaction Analysis

Published on: March 29, 2016

La estratificación compositiva en el manto profundo.

Kellogg1, Hager, van der Hilst RD

  • 1Department of Geology, University of California, Davis, CA 95616, USA. Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 01239, USA.

Science (New York, N.Y.)
|March 19, 1999
PubMed
Resumen

Una capa distinta en el manto inferior de la Tierra puede explicar las observaciones sísmicas y las firmas geoquímicas. Esta capa densa y estable influye en la dinámica del manto y el flujo de calor, conciliando las discrepancias en el presupuesto térmico de la Tierra.

Más Videos Relacionados

Combined Size and Density Fractionation of Soils for Investigations of Organo-Mineral Interactions
08:38

Combined Size and Density Fractionation of Soils for Investigations of Organo-Mineral Interactions

Published on: February 15, 2019

3D Depth Profile Reconstruction of Segregated Impurities Using Secondary Ion Mass Spectrometry
07:10

3D Depth Profile Reconstruction of Segregated Impurities Using Secondary Ion Mass Spectrometry

Published on: April 29, 2020

Videos de Experimentos Relacionados

Last Updated: Jun 30, 2026

Quantification of Hydrogen Concentrations in Surface and Interface Layers and Bulk Materials through Depth Profiling with Nuclear Reaction Analysis
14:11

Quantification of Hydrogen Concentrations in Surface and Interface Layers and Bulk Materials through Depth Profiling with Nuclear Reaction Analysis

Published on: March 29, 2016

Combined Size and Density Fractionation of Soils for Investigations of Organo-Mineral Interactions
08:38

Combined Size and Density Fractionation of Soils for Investigations of Organo-Mineral Interactions

Published on: February 15, 2019

3D Depth Profile Reconstruction of Segregated Impurities Using Secondary Ion Mass Spectrometry
07:10

3D Depth Profile Reconstruction of Segregated Impurities Using Secondary Ion Mass Spectrometry

Published on: April 29, 2020

Área de la Ciencia:

  • La geofísica es la geofísica.
  • La geoquímica es la geoquímica.
  • Física mineral Física de los minerales

Sus antecedentes:

  • Las observaciones sísmicas revelan complejidades en el manto inferior de la Tierra.
  • Las firmas isotópicas en los basaltos sugieren depósitos profundos del manto.
  • Existen discrepancias entre el flujo de calor observado y los modelos de producción de calor.

Objetivo del estudio:

  • Para explicar las observaciones sísmológicas y geoquímicas en el manto inferior de la Tierra.
  • Para conciliar las discrepancias en el presupuesto de calor de la región de origen de basalto de la cresta oceánica media.
  • Para investigar la estabilidad y las características de un límite de composición del manto profundo.

Principales métodos:

  • Análisis de datos sismológicos del manto inferior de la Tierra.
  • Modelado de la convección termoquímica utilizando simulaciones numéricas.
  • Investigación de firmas isotópicas en basaltos de cordilleras oceánicas y basaltos de islas oceánicas.

Principales resultados:

  • Se propone un límite de composición a una profundidad de ~ 1600 km.
  • Los modelos numéricos confirman la estabilidad dinámica de una capa más densa del manto profundo.
  • Las propiedades de esta capa concilian las discrepancias entre el flujo de calor y la producción de calor.

Conclusiones:

  • El límite del manto profundo explica los datos sísmicos y geoquímicos.
  • Los modelos de convección termoquímica soportan una capa estable y más densa.
  • Esta capa influye en la dinámica del manto, el flujo de calor y las firmas basálticas.