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相关概念视频

Global Climate Change01:50

Global Climate Change

Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
The Sulfur Cycle01:22

The Sulfur Cycle

Sulfur, an important element in the chemical makeup of proteins, is recycled through the atmosphere and aquatic and terrestrial environments. Found in the atmosphere as sulfur dioxide (SO2), sulfur is released by decaying organisms, weathered rocks, geothermal vents, volcanos, and burning fossil fuels. It is deposited into the ecosystem, cycled through the biotic community, and either released back into the atmosphere as gas or deposited in marine sediment for long-term storage and eventual...
Sulfur Assimilation01:20

Sulfur Assimilation

Sulfur is an essential element in biological systems, contributing to synthesizing key biomolecules, including amino acids such as cysteine and methionine, and cofactors such as coenzyme A and biotin. Microorganisms primarily assimilate sulfur as sulfate (SO₄²⁻) from the environment, which must undergo a series of biochemical transformations before it can be incorporated into cellular components. As sulfate is highly oxidized, it must undergo assimilatory sulfate reduction to become...
Efflorescence in Masonry01:25

Efflorescence in Masonry

Efflorescence in masonry walls appears as a fluffy crystalline powder, often white, resulting from water-soluble salts within the masonry or mortar. When water penetrates the masonry, it dissolves these salts and brings them to the surface, where they are deposited upon evaporation of water.
While initial efflorescence is common post-construction and can be cleaned with water and a brush, in certain instances, efflorescence can reappear and gradually diminish over time as salts are leached out...
Rab Cascades01:25

Rab Cascades

Rab GTPases act in a regulated cascade during membrane fusion, helping the lipid bilayers mix. The Rab family of proteins are active when bound to GTP, and inactive when bound to GDP. Hence, they act as guanine nucleotide-dependent molecular switches. Rab-GTP recognizes and binds to long or short-range tethering proteins to capture the target vesicle. These tethers coordinate with SNAREs on the vesicle and the target membrane to assemble the trans SNARE complex that locks the mixing bilayers.
Gastroesophageal Reflux Disease01:25

Gastroesophageal Reflux Disease

Gastroesophageal reflux disease (GERD) is the backward flow of stomach contents (acid, pepsin, or bile) into the esophagus, causing mucosal inflammation known as esophagitis. It results from failure of antireflux mechanisms, mainly the lower esophageal sphincter (LES), influenced by mechanical and physiological factors.Etiology and Risk FactorsGERD develops when LES function is weakened or when intra-abdominal pressure increases. Risk factors include aging, obesity, and sliding hiatal hernia,...

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相关实验视频

Updated: Jul 2, 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

爆! 爆! 爆! 爆! 这是什么意思? 一个月的喷发在桑托里尼火山引发了火山爆发.

Victoria M Martin1, Daniel J Morgan, Dougal A Jerram

  • 1University of Durham, Department of Earth Sciences, South Road, Durham DH1 3LE, UK.

Science (New York, N.Y.)
|August 30, 2008
PubMed
概括

研究人员研究了来自希腊桑托里尼的火山材料,以确定岩入侵和喷发之间的时间. 他们发现这种关键时间延迟在3到10周之间,使用了橄晶体分析.

科学领域:

  • 地质地质地质地质地质地
  • 火山学 火山学是一门学科.
  • 地质化学 地质化学

背景情况:

  • 岩入侵和火山爆发之间的时间对于预测火山活动和减轻风险至关重要.
  • 了解这个时间表有助于评估火山爆发的触发因素和后果.

研究的目的:

  • 为了确定希腊桑托里尼尼尼卡梅尼火山中心的入侵到喷发的时间滞后.
  • 为了研究火山过程,将分析技术应用于以前爆发的材料.

主要方法:

  • 在1925-28年尼阿卡梅尼火山爆发时的橄晶体中Fe-Mg扩散的分析.
  • 使用地质化学技术重建火山材料的热历史.

主要成果:

  • 侵入到喷发的时间延迟被限制在3到10周的时间内.
  • 该研究成功地使用历史喷发材料校准了短期的火山过程.

结论:

  • 在奥利文中Fe-Mg扩散提供了一种可靠的方法来确定岩入侵到喷发的时间表.
  • 这种技术适用于其他火山中心,提高了我们研究火山过程的能力.

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Atom Probe Tomography Analysis of Exsolved Mineral Phases
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Atom Probe Tomography Analysis of Exsolved Mineral Phases

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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

Atom Probe Tomography Analysis of Exsolved Mineral Phases
08:14

Atom Probe Tomography Analysis of Exsolved Mineral Phases

Published on: October 25, 2019