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Hess's Law03:40

Hess's Law

44.0K
There are two ways to determine the amount of heat involved in a chemical change: measure it experimentally, or calculate it from other experimentally determined enthalpy changes. Some reactions are difficult, if not impossible, to investigate and make accurate measurements for experimentally. And even when a reaction is not hard to perform or measure, it is convenient to be able to determine the heat involved in a reaction without having to perform an experiment.
44.0K
Enthalpy of Solution02:39

Enthalpy of Solution

21.1K
There are two criteria that favor, but do not guarantee, the spontaneous formation of a solution:
21.1K
Aqueous Solutions and Heats of Hydration02:42

Aqueous Solutions and Heats of Hydration

14.3K
Water and other polar molecules are attracted to ions. The electrostatic attraction between an ion and a molecule with a dipole is called an ion-dipole attraction. These attractions play an important role in the dissolution of ionic compounds in water.
When ionic compounds dissolve in water, the ions in the solid separate and disperse uniformly throughout the solution because water molecules surround and solvate the ions, reducing the strong electrostatic forces between them. This process...
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Solubility Equilibria: Overview01:09

Solubility Equilibria: Overview

1.8K
When a substance such as sodium chloride is added to water, it dissolves, forming an aqueous solution. The extent of dissolution is called solubility. The process of dissolution can exist in equilibrium, just like other chemical processes. Solubility equilibria are also called precipitation equilibria because the process of solubility can be reversible. The reverse of the solubility process is called precipitation.
Solubility is important in biological and environmental processes. A notable...
1.8K
Solubility Equilibria: Ionic Product of Water01:16

Solubility Equilibria: Ionic Product of Water

2.2K
Pure water is a weak electrolyte; only a small amount ionizes into hydrogen and hydroxide ions. At any given temperature, the concentration of undissociated water is almost constant, so the ionic product of water is the product of the hydrogen and hydroxide ion concentrations, denoted as Kw. The square root of Kw gives the individual ion concentrations.
The ionic product of water varies with temperature, and its value is 1.0 x 10−14 at standard experimental conditions. Per Le...
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Gas Solubility01:31

Gas Solubility

132
Gas solubility in liquids forms liquid-gas solutions, such as soft drinks, where carbon dioxide is dissolved in water, and the ocean, where the solubility of oxygen and carbon dioxide supports marine life. The ability of oceans to dissolve gases impacts weather conditions in the troposphere.However, gas-liquid interactions vary. For instance, hydrogen chloride gas is highly soluble in water, while oxygen's solubility is much lower. Because these solutions are non-ideal, Raoult’s law,...
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相关实验视频

Updated: Apr 29, 2026

Simulation of the Planetary Interior Differentiation Processes in the Laboratory
06:04

Simulation of the Planetary Interior Differentiation Processes in the Laboratory

Published on: November 16, 2013

11.3K

在奥利文中的溶解度以及海洋岛屿玄武岩中高3He/4He的含量.

Stephen W Parman1, Mark D Kurz, Stanley R Hart

  • 1Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Building 54, Cambridge, Massachusetts 02139, USA. stephen.parman@durham.ac.uk

Nature
|October 21, 2005
PubMed
概括

海洋岛屿玄武岩中的高-3/-4比率暗示了一个未含气的地幔. 新的实验表明,在地幔化过程中比和更兼容,在耗尽的残留物中保持这些比率.

科学领域:

  • 地质化学 地质化学
  • 同位素地球化学 同位素地球化学
  • 石化学 石化学是一门学科.

背景情况:

  • 海洋岛基岩 (OIB) 中高的3He/4He比率是未有气体的地幔储库的关键证据.
  • 地幔融模型依赖于的化学行为,但分区估计冲突.

研究的目的:

  • 为了实验性地确定在olivine中的可溶性.
  • 为了澄清地幔融化过程中的分离行为.

主要方法:

  • 在大气压下实验测量天然和合成橄中的可溶性.
  • 与气氛平衡,然后进行粉碎和融化分析.

主要成果:

  • 确定了的奥利文融分区系数,范围从0.0025 ± 0.0005到0.0060 ± 0.0007.
  • 在地幔融化过程中,似乎比和更兼容.

结论:

  • 实验数据表明在化过程中的兼容性,可能在耗尽的残留物中保持高的3He/4He比率.
  • 这解决了OIB和中海基岩度之间的差异,支持高3He/4HeOIB的耗尽来源.

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