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関連する概念動画

Precipitation Processes01:12

Precipitation Processes

The experimental conditions in a gravimetric analysis should be optimized to maximize the particle size and purity of the obtained precipitate. Ideally, the concentration of the precipitating reagent should be low with effective stirring to maintain low relative supersaturation for the growth of large crystals. In homogeneous precipitation, the precipitant is slowly generated by a chemical reaction in the solution to avoid local reagent excesses. For example, urea decomposes gradually to...
States of Water01:23

States of Water

Water exists in any one of the three classical states: solid (ice), liquid (water), and gas (steam or water vapor). The state of water depends on i) the intermolecular forces that draw molecules together and ii) the kinetic energy that leads to movements that pull them apart.
Water freezes when the intermolecular forces are greater than the kinetic energy. Unlike most other substances, water is less dense in its solid state than in its liquid state. This is because each water molecule can form...
Precipitation and Co-precipitation01:17

Precipitation and Co-precipitation

Precipitation and coprecipitation methods can be used to separate a mixture of ions in a solution. In qualitative inorganic analysis, ions that form sparingly soluble precipitates with the same reagent are separated based on the differences in solubility products. For example, consider the separation of Cu(II) and Fe(II) ions by precipitation as insoluble sulfides. First, copper(II) sulfide is precipitated by the addition of acidic H2S, where the dissociation of H2S is suppressed. Adding H2S...
Precipitation of Ions03:11

Precipitation of Ions

Predicting Precipitation
The equation that describes the equilibrium between solid calcium carbonate and its solvated ions is:
Types of Coprecipitation01:10

Types of Coprecipitation

Coprecipitation is the contamination of a precipitate by otherwise soluble species and occurs via different processes. In colloidal precipitates, coprecipitation occurs via surface adsorption. For instance, barium sulfate has a primary layer of adsorbed barium ions and a secondary layer of nitrate counterions. This results in contamination of the precipitate by barium nitrate.
Sometimes, ions in a crystal lattice can undergo isomorphous replacement by inclusions of similar charge and size. For...
Precipitation Gravimetry01:03

Precipitation Gravimetry

Precipitation gravimetry is based on converting an analyte into a sparingly soluble precipitate, which is separated by filtration and weighed. An ideal precipitate should be pure, insoluble, of known composition, and easily filtered from the reaction mixture.
In determining nickel by gravimetric analysis, a precipitant of ethanolic dimethylglyoxime is added to a hot nickel salt solution. This is quickly followed by the dropwise addition of dilute ammonia solution until precipitation occurs. A...

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Simulating Impacts of Ice Storms on Forest Ecosystems
06:27

Simulating Impacts of Ice Storms on Forest Ecosystems

Published on: June 30, 2020

火星 水の氷の雲と降雨

J A Whiteway1, L Komguem, C Dickinson

  • 1Department of Earth and Space Science and Engineering, York University, Toronto, Ontario, Canada. whiteway@yorku.ca

Science (New York, N.Y.)
|July 4, 2009
PubMed
まとめ

火星 火星 火星 火星

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Simulating Impacts of Ice Storms on Forest Ecosystems
06:27

Simulating Impacts of Ice Storms on Forest Ecosystems

Published on: June 30, 2020

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Laboratory Drop Towers for the Experimental Simulation of Dust-aggregate Collisions in the Early Solar System

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08:16

Ice Generation and the Heat and Mass Transfer Phenomena of Introducing Water to a Cold Bath of Brine

Published on: March 13, 2017

科学分野:

  • 惑星科学 惑星科学
  • 大気科学 大気科学
  • クラウド物理学 クラウド物理

背景:

  • フェニックスミッションは,火星の水氷雲を観測した.
  • 雲は地球のシラス雲に似ている.
  • 秋の流れは,氷結晶の降水を示しています.

研究 の 目的:

  • 火星の大気中の水氷雲を調査する.
  • 雲の形成と降水過程を理解する.
  • 惑星境界層の役割について説明します.

主な方法:

  • フェニックスミッションのライト検出・レンジング (LIDAR) 装置を利用した.
  • 大気中の塵の測定を分析した.
  • 観測された雲の構造と落下線.

主要な成果:

  • 惑星境界層 (PBL) の上部と地面近くで検出された水氷雲.
  • PBLは,昼間のコンベクションによって4kmまでよく混合されました.
  • 夏の終わりに,気温が下がるにつれ,毎晩雲が形成される.

結論:

  • 火星の水氷雲は,上向きに混合した水蒸気から毎晩形成されます.
  • 交流と乱流は,雲の形成に重要な役割を果たします.
  • 降水サイクルには,氷の結晶が形成され,表面に落下します.