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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...
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 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...
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...
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.
Phase Diagrams02:39

Phase Diagrams

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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関連する実験動画

Updated: Jul 12, 2026

Computation of Atmospheric Concentrations of Molecular Clusters from ab initio Thermochemistry
12:11

Computation of Atmospheric Concentrations of Molecular Clusters from ab initio Thermochemistry

Published on: April 8, 2020

高度に超冷却されたシラス雲の水:確認と気候上の影響

K Sassen, K N Liou, S Kinne

    Science (New York, N.Y.)
    |January 25, 1985
    PubMed
    まとめ

    研究者は,リダールと航空機を使用して,シロストラタス雲の超冷却液体雲滴を検出しました. これらの発見は,シラス雲の液体層が大気の加熱と表面の放射性予算を大幅に変化させることを示唆しています.

    科学分野:

    • 大気科学 大気科学
    • クラウド物理学 クラウド物理
    • リモートセンシング (リモートセンサー)

    背景:

    • シロストラトゥス雲は,地球の放射的予算の重要な構成要素です.
    • 冷たいシラス雲の液体の水の存在と性質は,依然として不確実である.
    • これらの特性を理解することは,正確な気候モデリングに不可欠です.

    研究 の 目的:

    • シロストラタス雲の零下温度における液体雲滴の存在と特性を調査する.
    • これらの液体層の放射的影響を定量化するために.

    主な方法:

    • リモートセンシングのための地上ベースの偏極化レーザーレーダー (lidar) を利用しました.
    • 直接サンプルを採取するために,航空機のインシット測定に使用されます.
    • 太陽光と熱赤外線放射の予算計算を行いました.

    主要な成果:

    • シロストラタス雲の底辺で-40°C近くの超冷却液体雲滴の存在を確認した.
    • 放射性予算の計算は,大気中の熱分布の大きな変化を示した.
    • これらの液体層による表面放射量予算の潜在的な変化を観測した.

    さらに関連する動画

    Extraction and Characterization of Surfactants from Atmospheric Aerosols
    09:34

    Extraction and Characterization of Surfactants from Atmospheric Aerosols

    Published on: April 21, 2017

    関連する実験動画

    Last Updated: Jul 12, 2026

    Computation of Atmospheric Concentrations of Molecular Clusters from ab initio Thermochemistry
    12:11

    Computation of Atmospheric Concentrations of Molecular Clusters from ab initio Thermochemistry

    Published on: April 8, 2020

    Extraction and Characterization of Surfactants from Atmospheric Aerosols
    09:34

    Extraction and Characterization of Surfactants from Atmospheric Aerosols

    Published on: April 21, 2017

    結論:

    • 液体層は,凍結点よりかなり低い温度で,シラス雲の中に存在することができます.
    • これらの液体層は,大気中の放射線伝送に重大な影響を及ぼします.
    • 液体を含むシラス雲の気候への影響を完全に理解するためには,さらなる研究が必要である.