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相关概念视频

Emission Spectra02:39

Emission Spectra

65.2K
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.
65.2K
Rise of Liquid in a Capillary Tube01:18

Rise of Liquid in a Capillary Tube

3.1K
When very thin cylindrical tubes, called capillaries, are dipped in a liquid, the liquid rises or falls in the tube compared to the surrounding liquid. This phenomenon is called capillary action. Capillary action occurs due to the combination of two opposing forces: the cohesive forces of the liquid, which cause it to stick to itself and form a rounded shape, and the adhesive forces between the liquid and the walls of the container, which cause the liquid to be attracted to the container walls.
3.1K
Flame Photometry: Overview01:02

Flame Photometry: Overview

2.1K
Flame photometry, also known as flame emission spectrometry, is a technique used for the qualitative and quantitative analysis of elements present in a sample using a flame as the source of excitation energy. The concept of flame photometry was realized in the early 1860s by Kirchhoff and Bunsen, who discovered that specific elements emit characteristic radiation when excited in flames. The first instrument developed for this purpose was used to measure sodium (Na) in plant ash using a Bunsen...
2.1K
Flame Photometry: Lab01:16

Flame Photometry: Lab

1.3K
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...
1.3K
The Joule and Joule–Thomson Experiments01:23

The Joule and Joule–Thomson Experiments

246
Consider an adiabatic system composed of two chambers, A and B, designed such that no heat flows into or out of the system. Initially, chamber A is filled with a gas at a fixed temperature T1, pressure p1, and volume V1, while chamber B is evacuated. The gas is then gradually forced through a rigid, porous barrier to chamber B, ultimately reaching temperature T2, pressure p2, and volume V2. A piston on the right side maintains a constant pressure (p2), which is lower than p1. The significant...
246
Sulfur Assimilation01:20

Sulfur Assimilation

562
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...
562

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

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光学证据表明,岩喷泉是由先前积累的岩石气体驱动的.

Patrick Allard1, Mike Burton, Filippo Muré

  • 1INGV, Piazza Roma 2, 95123 Catania, Italy. patrick.allard@cea.fr

Nature
|January 28, 2005
PubMed
概括

岩喷泉是由气相气泡驱动的. 在埃特纳火山爆发期间对气体成分的分析表明,一个深层泡层被暴力排空,而不是在上升期间的岩脱气.

科学领域:

  • 火山学 火山学是一门学科.
  • 地质化学 地质化学
  • 地质物理学 地质物理学

背景情况:

  • 岩喷泉是低粘度喷发期间连续喷出的气体.
  • 岩喷泉的起源 (泡干扰与深泡泡的上升) 是一个争论.
  • 现场测量还没有区分这些模型.

研究的目的:

  • 通过分析驱动气体相来确定岩喷泉的起源.
  • 为了区分爆发前和爆发后的岩脱气模型.

主要方法:

  • 福里埃变换红外光谱法 (FTIR) 用于测量磁性气体的组成.
  • 在埃特纳山的强大岩喷泉期间,对火山气体物种的分析.
  • 岩辐射的吸收光谱被用来确定气体丰度.

主要成果:

  • 岩喷泉气体的二氧化碳/硫 (CO2/S) 和硫/ (S/Cl) 比其他埃特纳排放物更高.
  • 气体成分与埃特纳岩的同爆散装卸气体不一致.
  • 观察到的比率表明,大约在1.5公里深度积累的气泡层的暴力排空.

结论:

  • 这项研究提供了第一个区分岩喷泉模型的现场测量.

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  • 气体成分强烈支持深泡泡上升模型.
  • 这一发现为岩喷泉和火山气体释放的动态提供了关键的见解.