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Cold Weather Concreting01:27

Cold Weather Concreting

358
When freshly poured concrete is exposed to freezing temperatures before it has set, the water within the concrete can freeze. This expansion disrupts the setting process, delays chemical reactions necessary for hardening, and increases the volume of pores within the hardened concrete, which weakens its overall structure. If the concrete manages to reach an appreciable strength before it freezes, the damage can be somewhat mitigated.
To counteract the negative impacts of cold weather, ensuring...
358
Sample Handling01:02

Sample Handling

1.6K
Transportation of samples from the collection point to the laboratory, as well as storage and preservation techniques, are crucial for maintaining sample integrity and ensuring accurate and reliable test results.
Samples should be transported carefully from collection points to the laboratory. They should be properly sealed and clearly labeled to prevent cross-contamination. To preserve the sample integrity, optimal temperature conditions during transport are essential. This could involve using...
1.6K
Cryo-electron Microscopy01:28

Cryo-electron Microscopy

4.1K
Conventional electron microscopy (EM) involves dehydration, fixation, and staining of biological samples, which distorts the native state of biological molecules and results in several artifacts. Also, the high-energy electron beam damages the sample and makes it difficult to obtain high-resolution images. These issues can be addressed using cryo-EM, which uses frozen samples and gentler electron beams. The technique was developed by Jacques Dubochet, Joachim Frank, and Richard Henderson, for...
4.1K
Masonry in Cold and Hot Weather Conditions01:21

Masonry in Cold and Hot Weather Conditions

329
In cold weather, masonry construction requires specific precautions to ensure mortar does not freeze before curing, as this can significantly weaken its strength and watertightness. Mortar temperature should be maintained between 60°F and 80°F to support proper hydration and curing. Below 40°F, mortar water must be heated, but should not exceed 120°F as high temperatures can reduce mortar's compressive and bond strength.
Other key practices include keeping masonry units...
329
Decreased Body Temperature01:29

Decreased Body Temperature

1000
A decreased body temperature can occur in patients with hypothermia and frostbite. Heat loss with extended cold exposure overpowers the body's ability to create heat, resulting in hypothermia. Core temperature readings help classify hypothermia. Mild hypothermia is temperatures between 32 °C (89.6 °F) and 35°C (95 °F) and is caused by impaired thermoregulation. Moderate hypothermia is temperatures between 28 C (82.4 °F) and 32 °C (89.6 °F) caused by...
1000
Mass Concreting01:22

Mass Concreting

320
Mass concreting refers to the process of placing large volumes of concrete, such as in gravity dams. The heat generated during the cement hydration process and differential cooling rates within the concrete mass can lead to a temperature gradient, which can result in thermal cracks in the concrete mass.
To reduce the risk of such cracking, the concrete mix may incorporate low-heat cement and pozzolans to reduce the temperature rise. Pre-cooled angular aggregates and water-reducing admixtures...
320

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Video Experimental Relacionado

Updated: Jan 15, 2026

Innovative Strategies for Organ Preservation in Heart Transplantation: Uniform Cooling Preservation and Ex-situ Normothermic Perfusion
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Innovative Strategies for Organ Preservation in Heart Transplantation: Uniform Cooling Preservation and Ex-situ Normothermic Perfusion

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Almacenamiento en frío

Kai Kupferschmidt1

  • 1Svalbard.

Science (New York, N.Y.)
|October 16, 2025
PubMed
Resumen
Este resumen es generado por máquina.

Los suelos congelados del Ártico pueden contener virus antiguos, ofreciendo información sobre pandemias pasadas y posibles amenazas futuras. Esta investigación explora la historia viral oculta conservada en el permafrost.

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Área de la Ciencia:

  • Virología ambiental
  • La paleogenómica
  • Microbiología del Ártico

Sus antecedentes:

  • El permafrost, o suelo permanentemente congelado, cubre vastas áreas del Ártico.
  • Estos entornos congelados actúan como cápsulas de tiempo naturales, conservando potencialmente material biológico antiguo.
  • Comprender la vida microbiana dentro del permafrost es crucial para evaluar los riesgos ecológicos y de salud.

Objetivo del estudio:

  • Investigar la presencia y diversidad de virus en muestras de permafrost del Ártico.
  • Para explorar el potencial del permafrost como un depósito de material genético viral antiguo.
  • Evaluar las implicaciones del deshielo del permafrost para la liberación viral y la salud pública.

Principales métodos:

  • Recopilación de muestras de núcleos de permafrost de un archipiélago ártico.
  • Secuenciación metagenómica para identificar secuencias virales dentro del suelo.
  • Análisis bioinformático para reconstruir genomas virales y evaluar la diversidad.

Principales resultados:

  • Detección de diversas secuencias virales, incluidos tipos virales conocidos y potencialmente nuevos.
  • Evidencia de material genético viral conservado durante largos períodos en suelo congelado.
  • Identificación de firmas virales que pueden indicar interacciones pasadas entre el virus y el huésped.

Conclusiones:

  • El permafrost ártico alberga una importante reserva de información genética viral antigua.
  • El deshielo del permafrost debido al cambio climático plantea un riesgo potencial de reaparición del virus antiguo.
  • Se necesita más investigación para caracterizar completamente estos virus y su impacto potencial.