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Nuclear Transmutation03:20

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...
Tidal Forces01:06

Tidal Forces

The origin of Earth's ocean tides has been a subject of continuous investigation for over 2000 years. However, the work of Newton is considered to be the beginning of the proper understanding of the phenomenon. Ocean tides are the result of gravitational tidal forces. These same tidal forces are present in any astronomical body; they are responsible for the internal heat that creates the volcanic activity on Io, one of Jupiter's moons, and the breakup of stars that get too close to black holes.
Destabilization of Microtubules01:45

Destabilization of Microtubules

The destabilization of microtubules can occur during different stages of the microtubule lifecycle, such as nucleation or elongation. It can take place at either end of the microtubule or in the microtubule lattices as a whole. The lifespan of individual microtubules within a cell varies according to the cell type and stage of the cell cycle. During interphase, the lifespan of the microtubule is about 30 minutes, while during cell division, it is about 15 minutes. In axonal microtubules of...
Atomic Emission Spectroscopy: Instrumentation01:22

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.
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Viruses of Archaea

Archaeal viruses play a crucial role in the ecosystems of extremophilic archaea, particularly those belonging to the phyla Euryarchaeota and Crenarchaeota. By shaping host evolution and facilitating gene transfer, these viruses influence microbial communities and contribute to genetic diversity in extreme environments. The archaea they infect thrive in acidic hot springs and hydrothermal vents characterized by high temperatures and low pH. Archaeal viruses exhibit remarkable structural...
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Acid Mine Drainage

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[Evaluation of different methods for detecting resistance of staphylococcus aureus strains to methicillin].

Medycyna doswiadczalna i mikrobiologia·1994
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Simulation of tsunamis from great earthquakes on the cascadia subduction zone.

Science (New York, N.Y.)·1990
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[Mitochondrial antibodies in liver diseases].

Die Medizinische Welt·1979
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Micro-indentation hardness studies on human bones.

Acta anatomica·1979
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Haematic mummification in a buffalo--a case report.

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Video Experimental Relacionado

Updated: Jul 12, 2026

Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt
07:58

Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt

Published on: August 7, 2017

Tsunamis generados por las erupciones del volcán Monte San Agustín, Alaska.

J Kienle, Z Kowalik, T S Murty

    Science (New York, N.Y.)
    |June 12, 1987
    PubMed
    Resumen

    Una simulación numérica pronosticó las alturas potenciales de las olas de tsunami y los tiempos de viaje del colapso volcánico, utilizando un método aplicable a otros volcanes costeros. Esta investigación aborda las preocupaciones sobre los tsunamis generados por erupciones volcánicas.

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    Área de la Ciencia:

    • La geofísica es la geofísica.
    • Volcanología Volcanología.
    • Investigaciones sobre el tsunami.

    Sus antecedentes:

    • Las erupciones volcánicas costeras pueden desencadenar tsunamis devastadores, como lo demuestran eventos históricos como la erupción del Monte San Agustín en 1883.
    • Las preocupaciones sobre posibles tsunamis por el colapso del edificio volcánico existen para los volcanes cerca de aguas poco profundas, como el Monte San Agustín en Cook Inlet.
    • Los eventos volcánicos pasados han causado una pérdida significativa de vidas y propiedades debido a la generación de tsunamis.

    Objetivo del estudio:

    • Para simular el colapso del edificio volcánico del Monte San Agustín en 1883 y la ola marina resultante.
    • Para pronosticar potenciales alturas de olas de tsunami y tiempos de viaje.
    • Desarrollar un método numérico generalizable para evaluar el riesgo de tsunami de otros volcanes costeros.

    Principales métodos:

    • Simulación numérica de un evento de colapso de un edificio volcánico.
    • Modelado de la generación y propagación de ondas en aguas poco profundas.

    Principales resultados:

    • La simulación proporcionó un pronóstico de las alturas potenciales de las olas y los tiempos de viaje para el evento de 1883.
    • El método desarrollado puede aplicarse a otros volcanes costeros para evaluar el riesgo de tsunami.

    Conclusiones:

    • Si bien el Monte San Agustín no se derrumbó durante la erupción de 1986, la simulación proporciona información valiosa para la evaluación de riesgos futuros.
    • El método numérico ofrece una herramienta para pronosticar los impactos de tsunami de colapsos de flancos volcánicos.
    • Comprender y simular estos eventos es crucial para mitigar los peligros de tsunamis asociados con los volcanes costeros.