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Phase Transitions02:31

Phase Transitions

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Whether solid, liquid, or gas, a substance's state depends on the order and arrangement of its particles (atoms, molecules, or ions). Particles in the solid pack closely together, generally in a pattern. The particles vibrate about their fixed positions but do not move or squeeze past their neighbors. In liquids, although the particles are closely spaced, they are randomly arranged. The position of the particles are not fixed—that is, they are free to move past their neighbors to...
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Phase Transitions: Sublimation and Deposition02:33

Phase Transitions: Sublimation and Deposition

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Some solids can transition directly into the gaseous state, bypassing the liquid state, via a process known as sublimation. At room temperature and standard pressure, a piece of dry ice (solid CO2) sublimes, appearing to gradually disappear without ever forming any liquid. Snow and ice sublimate at temperatures below the melting point of water, a slow process that may be accelerated by winds and the reduced atmospheric pressures at high altitudes. When solid iodine is warmed, the solid sublimes...
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Phase Transitions: Melting and Freezing02:39

Phase Transitions: Melting and Freezing

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Heating a crystalline solid increases the average energy of its atoms, molecules, or ions, and the solid gets hotter. At some point, the added energy becomes large enough to partially overcome the forces holding the molecules or ions of the solid in their fixed positions, and the solid begins the process of transitioning to the liquid state or melting. At this point, the temperature of the solid stops rising, despite the continual input of heat, and it remains constant until all of the solid is...
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Phase Transitions: Vaporization and Condensation02:39

Phase Transitions: Vaporization and Condensation

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The physical form of a substance changes on changing its temperature. For example, raising the temperature of a liquid causes the liquid to vaporize (convert into vapor). The process is called vaporization—a surface phenomenon. Vaporization occurs when the thermal motion of the molecules overcome the intermolecular forces, and the molecules (at the surface) escape into the gaseous state. When a liquid vaporizes in a closed container, gas molecules cannot escape. As these gas phase molecules...
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Properties of Transition Metals02:58

Properties of Transition Metals

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Transition metals are defined as those elements that have partially filled d orbitals. As shown in Figure 1, the d-block elements in groups 3–12 are transition elements. The f-block elements, also called inner transition metals (the lanthanides and actinides), also meet this criterion because the d orbital is partially occupied before the f orbitals.
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Phase Diagrams02:39

Phase Diagrams

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A phase diagram combines plots of pressure versus temperature for the liquid-gas, solid-liquid, and solid-gas phase-transition equilibria of a substance. These diagrams indicate the physical states that exist under specific conditions of pressure and temperature and also provide the pressure dependence of the phase-transition temperatures (melting points, sublimation points, boiling points). Regions or areas labeled solid, liquid, and gas represent single phases, while lines or curves represent...
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在高压相位过渡之前,石中的电荷转移.

Marcin Stachowicz1, Agnieszka A Huć2,3, Tomasz Poręba4,5

  • 1Faculty of Geology, University of Warsaw, Żwirki i Wigury 93, 02-089 Warszawa, Poland.

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概括

碳酸盐岩石如石在高压下发生显著变化,影响全球碳循环. 这项研究揭示了压力诱导的电子再分配在结构变化之前,碳在压缩下独特地膨胀.

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科学领域:

  • 地质化学 地质化学
  • 矿物物理 矿物物理
  • 计算化学计算化学

背景情况:

  • 了解地幔压力下的碳酸盐岩的行为对于全球碳循环建模至关重要.
  • 石 (CaCO3) 从石-I转变为石-II大约1.6GPa,但其电子和化学反应变化尚不清楚.

研究的目的:

  • 为了研究高压下石的电子和结构变化.
  • 了解对矿物学和地球内部深处的碳循环的影响.

主要方法:

  • 高压X射线衍射实验利用EBS-ESRF同步机上的ID27光线.
  • 电荷密度分析以确定原子电荷,盆地体积和形状.

主要成果:

  • 在石相过渡之前观察到Ca,C和O原子之间的不连续的电荷再分配.
  • 在碳中确定了负原子可压缩性,由于电子吸收而在压力下膨胀.
  • 证明了实验电荷密度方法能够解决压力诱导的电子密度重排的能力.

结论:

  • 石灰岩相转换之前有显著的电子重新排列,而不仅仅是结构变化.
  • 碳在压力下的独特行为为地球深层矿物学提供了新的见解.
  • 实验性电荷密度分析提供了前所未有的细节在极端条件下矿物行为的.