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相关概念视频

Precipitation Processes01:12

Precipitation Processes

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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...
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Precipitation and Co-precipitation01:17

Precipitation and Co-precipitation

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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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Precipitation Gravimetry01:03

Precipitation Gravimetry

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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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The Water Cycle01:00

The Water Cycle

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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.
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Types of Coprecipitation01:10

Types of Coprecipitation

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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...
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What is Climate?01:16

What is Climate?

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Climate refers to the prevailing weather conditions in a specific area over an extended period. As the saying goes, “Climate is what you expect. Weather is what you get.” Climate is influenced by geographic factors, such as latitude, terrain, and proximity to bodies of water.
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相关实验视频

Updated: Mar 15, 2026

A Protocol for Conducting Rainfall Simulation to Study Soil Runoff
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热带气旋降雨延伸到内陆地区.

E Deng1, Qian Xiang2, De-Hui Ouyang1

  • 1State Key Laboratory of Climate Resilience for Coastal Cities, Department of Civil and Environmental Engineering, The Hong Kong Polytechnic University, Hong Kong, China.

Nature communications
|March 14, 2026
PubMed
概括
此摘要是机器生成的。

热带气旋降雨正在全球范围内进一步延伸到内陆. 这一由海洋变暖带来的趋势增加了内陆沿海社区的洪水风险.

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Continuous Instream Monitoring of Nutrients and Sediment in Agricultural Watersheds
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Last Updated: Mar 15, 2026

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Continuous Instream Monitoring of Nutrients and Sediment in Agricultural Watersheds
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科学领域:

  • 气候学 气候学 气候学
  • 气象学 天气学
  • 海洋学 海洋学 海洋学

背景情况:

  • 热带气旋 (TC) 在海洋上的降雨强度得到了充分记录.
  • 沿海地区面临着TC引起的降雨造成的洪水风险日益增加.
  • 距离海岸线100公里以外的内陆地区往往没有为TC洪水做好准备.

研究的目的:

  • 评估陆地热带气旋降雨的全球变化,特别是大雨事件.
  • 为了确定TC降雨是否在全球范围内扩展到内陆,并量化这一趋势.

主要方法:

  • 1980年至2023年全球TC降雨数据的分析.
  • 统计评估大雨 (≥30毫米每3小时) 的陆地范围.
  • 利用观测和模型模拟来调查导致因素.

主要成果:

  • 全球TC降雨量在1980年至2023年期间扩展到内陆.
  • 北半球的大陆海岸显示,每十年3.8±1.8公里的重型TC降雨量增加.
  • 近岸海面温度 (SST) 的升温与这种向陆地延伸有关.

结论:

  • 热带气旋大雨正在全球范围内越来越多地延伸到内陆.
  • 海面温度升温和沿海城市化可能是这种现象的驱动因素.
  • 在TC降雨中的陆地转移给内陆沿海人口带来了不断升级的洪水风险.