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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...
The Water Cycle01:00

The Water Cycle

The Earth’s hydrosphere includes all of the areas where the storage and movement of water occurs. Since water is the basis of all living processes, the cycling of water is extremely important to ecosystem dynamics.
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...
What is Weather?01:07

What is Weather?

Overview
Precipitation Titration: Overview01:26

Precipitation Titration: Overview

Precipitation titration involves the reaction of a titrant and an analyte to generate an insoluble precipitate. While precipitation titration uses various precipitating agents, silver nitrate is the most common precipitating reagent; titrations involving Ag+ are called argentometric titrations. Usually, the endpoint in a precipitation titration can be detected by visual indicators.
A precipitation titration curve demonstrates the change in concentration of the titrant or analyte upon adding the...
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...

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関連する実験動画

Updated: Jul 12, 2026

Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface
13:27

Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface

Published on: June 8, 2015

コンベクティブな嵐雲の水分含有量

T G Kyle, W R Sand

    Science (New York, N.Y.)
    |June 22, 1973
    PubMed
    まとめ

    研究者は,貫通する航空機を使用して,コンベクティブストームで凝縮された水を測定しました. 彼らは,嵐の雲の中で,高い水分含有量の重要な領域を発見しました.

    科学分野:

    • 大気科学 大気科学
    • 気象学 気象学 気象学
    • クラウド物理学 クラウド物理

    背景:

    • コンベクティブ・ストームは複雑な気象現象である.
    • 内部構造,特に水分含有量を理解することは,正確な予測に不可欠です.
    • 以前の研究では,嵐の内部にある微物理学的性質に関するデータが限られていた.

    研究 の 目的:

    • コンベクティブな嵐雲の中の凝縮された水の含有量を定量化するために.
    • 水分量が多い地域の空間的範囲と特徴を特定する.
    • クラウドモデルの改善のためにインシットデータを提供します.

    主な方法:

    • 大気測定をするために装備された研究用航空機を利用した.
    • 浸透したアクティブコンベクティブストームシステム.
    • 特殊な計器具を用いて凝縮水分を測定した.

    主要な成果:

    • 雲の内部で高濃縮水分を有する明確な領域を特定した.
    • これらの地域は,1〜2キロメートルの範囲でした.
    • 測定された凝縮水の含有量は,これらの地域で立方メートルあたり約20グラムに達しました.

    さらに関連する動画

    Capturing Flow-weighted Water and Suspended Particulates from Agricultural Canals During Drainage Events
    06:26

    Capturing Flow-weighted Water and Suspended Particulates from Agricultural Canals During Drainage Events

    Published on: November 7, 2017

    A Protocol for Conducting Rainfall Simulation to Study Soil Runoff
    10:35

    A Protocol for Conducting Rainfall Simulation to Study Soil Runoff

    Published on: April 3, 2014

    関連する実験動画

    Last Updated: Jul 12, 2026

    Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface
    13:27

    Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface

    Published on: June 8, 2015

    Capturing Flow-weighted Water and Suspended Particulates from Agricultural Canals During Drainage Events
    06:26

    Capturing Flow-weighted Water and Suspended Particulates from Agricultural Canals During Drainage Events

    Published on: November 7, 2017

    A Protocol for Conducting Rainfall Simulation to Study Soil Runoff
    10:35

    A Protocol for Conducting Rainfall Simulation to Study Soil Runoff

    Published on: April 3, 2014

    結論:

    • 凝縮された水の含有量は,コンベクティブな嵐の中で均一に分布していません.
    • 水密度が高い特定の局所的な地域は,特徴的な特徴です.
    • これらの発見は,嵐のダイナミクスと降水過程を理解するための意味を持つ.