Jove
Visualize
联系我们
JoVE
x logofacebook logolinkedin logoyoutube logo
关于 JoVE
概览领导团队博客JoVE 帮助中心
作者
出版流程编辑委员会范围与政策同行评审常见问题投稿
图书馆员
用户评价订阅访问资源图书馆顾问委员会常见问题
研究
JoVE JournalMethods CollectionsJoVE Encyclopedia of Experiments存档
教育
JoVE CoreJoVE BusinessJoVE Science EducationJoVE Lab Manual教师资源中心教师网站
使用条款与条件
隐私政策
政策

相关概念视频

Precipitation of Ions03:11

Precipitation of Ions

Predicting Precipitation
The equation that describes the equilibrium between solid calcium carbonate and its solvated ions is:
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...
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...
Area Problem01:26

Area Problem

Determining the area of a region with straight edges is straightforward, as geometric formulas for rectangles, triangles, and polygons can be applied directly. However, traditional geometric methods are insufficient when a region has a curved boundary, such as the area under a function.fromThe area problem involves finding a systematic way to measure such regions. One approach to solving this problem is through approximation. Instead of attempting to compute the area exactly at the outset, the...

您也可能阅读

相关文章

通过共同作者、期刊和引用图与本文相关的文章。

排序
Same author

Spectra, intermittency, and extremes of weather, macroweather and climate.

Scientific reports·2018
Same author

The joint space-time statistics of macroweather precipitation, space-time statistical factorization and macroweather models.

Chaos (Woodbury, N.Y.)·2015
Same author

Fractal aircraft trajectories and nonclassical turbulent exponents.

Physical review. E, Statistical, nonlinear, and soft matter physics·2004
Same author

Large particle number limit in rain.

Physical review. E, Statistical, nonlinear, and soft matter physics·2003
Same author

Direct evidence of multifractal atmospheric cascades from planetary scales down to 1 km.

Physical review letters·2001
Same author

Functional box-counting and multiple elliptical dimensions in rain.

Science (New York, N.Y.)·1987

相关实验视频

Updated: Jun 18, 2026

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

雨和云区域的区域-周边关系.

S Lovejoy

    Science (New York, N.Y.)
    |April 9, 1982
    PubMed
    概括

    云和雨区周边表现出碎形几何学,缺乏特有的水平尺度. 这一基于卫星和雷达数据的发现与碎形理论一致,并表明天气模式中的规模不变性属性.

    科学领域:

    • 气象学 天气学
    • 地质物理学 地质物理学
    • 碎形几何学 碎形几何学

    背景情况:

    • 曼德尔布罗特的碎形理论为分析不规则形状提供了一个框架.
    • 了解云和雨区的几何结构对于气象建模至关重要.

    研究的目的:

    • 调查卫星和雷达确定的云和雨区的几何形状.
    • 应用面积-周长关系来分析碎形维度.

    主要方法:

    • 利用卫星和雷达数据对云和雨区进行测量,范围为1至1.2 x 10^6 km^2.
    • 应用了面积-周边关系,P ~ A ^ ^ D/2),其中P是周边,A是面积,D是分数维度.

    主要成果:

    • 面积-周边长数据符合一个公式,其中周边长大约是面积的平方根,提高到D的权力.
    • 分形维度 (D) 确定了云和雨周边.

    结论:

    • 云和雨水周边被证实是碎形.
    • 这些碎形周长线没有表现出1至1000公里的特征水平长度尺度.

    更多相关视频

    Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information
    10:28

    Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information

    Published on: June 13, 2020

    In Situ Soil Moisture Sensors in Undisturbed Soils
    08:20

    In Situ Soil Moisture Sensors in Undisturbed Soils

    Published on: November 18, 2022

    相关实验视频

    Last Updated: Jun 18, 2026

    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

    Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information
    10:28

    Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information

    Published on: June 13, 2020

    In Situ Soil Moisture Sensors in Undisturbed Soils
    08:20

    In Situ Soil Moisture Sensors in Undisturbed Soils

    Published on: November 18, 2022