Video Experimental Relacionado
Updated: Jul 12, 2026

07:58
Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt
Published on: August 7, 2017
Observaciones geoestacionarias por satélite de las erupciones de Soufriere en abril de 1979
Resumen
Las imágenes satelitales infrarrojas analizaron ocho grandes erupciones de Soufriere y St. Vincent en abril de 1979. La erupción más intensa produjo una nube de ceniza de 96.000 km2 en sólo 4 horas.
Área de la Ciencia:
- Volcanología Volcanología.
- La detección remota con sensores.
- La geofísica es la geofísica.
Sus antecedentes:
- El volcán Soufriere, en San Vicente, experimentó una actividad eruptiva significativa en abril de 1979.
- Comprender la dinámica de la nube de ceniza volcánica es crucial para la seguridad de la aviación y la evaluación de riesgos.
Objetivo del estudio:
- Para analizar el crecimiento y la intensidad de las principales erupciones volcánicas de Soufriere utilizando datos satelitales.
- Para comparar las características de diferentes eventos eruptivos durante la secuencia de abril de 1979.
Principales métodos:
- Se utilizaron imágenes infrarrojas (IR) del satélite geoestacionario (SMS-1).
- Dimensiones (área) cuantificadas de la nube de ceniza y tasas de crecimiento a lo largo del tiempo.
- Intensidad de erupción correlacionada con las características de la nube de ceniza observada.
Principales resultados:
- Se identificaron y estudiaron ocho erupciones principales.
- Se observaron variaciones significativas en la intensidad de la erupción y el crecimiento de la nube de ceniza.
- La erupción del 17 de abril fue la más intensa, formando una nube de ceniza de 96.000 km2 en 4 horas.
- La erupción menos intensa formó una nube de 16.000 kilómetros cuadrados.
Conclusiones:
- Las imágenes satelitales de infrarrojos proporcionan datos valiosos para monitorear la evolución de la nube de ceniza volcánica.
- La intensidad de la erupción se correlaciona directamente con el tamaño y el rápido crecimiento de las nubes de ceniza.
- El estudio destaca la naturaleza dinámica de las erupciones volcánicas y sus peligros asociados.
Videos de Conceptos Relacionados
Emission Spectra
When solids, liquids, or condensed gases are heated sufficiently, they radiate some of the excess energy as light. Photons produced in this manner have a range of energies, and thereby produce a continuous spectrum in which an unbroken series of wavelengths is present.
Precipitation Gravimetry
Precipitation gravimetry is based on converting an analyte into a sparingly soluble precipitate, which is separated by filtration and weighed. An ideal precipitate should be pure, insoluble, of known composition, and easily filtered from the reaction mixture.
In determining nickel by gravimetric analysis, a precipitant of ethanolic dimethylglyoxime is added to a hot nickel salt solution. This is quickly followed by the dropwise addition of dilute ammonia solution until precipitation occurs. A...
In determining nickel by gravimetric analysis, a precipitant of ethanolic dimethylglyoxime is added to a hot nickel salt solution. This is quickly followed by the dropwise addition of dilute ammonia solution until precipitation occurs. A...
Energy of a Satellite in a Circular Orbit
Thousands of artificial satellites orbit the Earth every day at various distances from the Earth. Satellites that orbit the Earth below an altitude of 1,600 km are considered to be orbiting in low-Earth orbit (LEO). Research satellites and Earth observation satellites are usually placed in LEO, and mostly orbit the Earth in elliptical orbits. Navigation satellites are placed in medium-Earth orbit (MEO), ranging from 2,000 km to 36,000 km from the surface of the Earth. Meanwhile, communication...
Flame Photometry: Lab
In a flame photometer, when a solution like potassium chloride is aspirated into the flame, the solvent evaporates, leaving behind dehydrated salt. This salt dissociates into free gaseous atoms in their ground state. Some of these atoms absorb energy from the flame, leading to their excitation. The excited atoms return to the ground state, emitting photons at characteristic wavelengths. Because only electronic transitions are involved, the resulting emission lines are very narrow. The intensity...
Atomic Emission Spectroscopy: Interference
In atomic emission spectroscopy (AES), high-temperature atomizers excite a broad range of elements and molecules that generate complex emissions from sources such as oxides, hydroxides, and flame combustion products in the flame or plasma. Several strategies can be employed to minimize spectral interferences caused by overlapping emission lines or bands. These include increasing instrument resolution, choosing alternative emission lines, optimally placing the detector in low-background regions,...
Atomic Emission Spectroscopy: Instrumentation
The instrumentation of atomic emission spectrometry (AES) involves various components, including atomization devices that convert samples into gas-phase atoms and ions. There are two main types of atomization devices: continuous and discrete atomizers. Continuous atomizers, like plasmas and flames, introduce samples in a constant stream, while discrete atomizers inject individual samples using syringes or autosamplers. The most common discrete atomizer is the electrothermal atomizer.

