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相关概念视频

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...
4.0K
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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Responses to Drought and Flooding02:41

Responses to Drought and Flooding

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Water plays a significant role in the life cycle of plants. However, insufficient or excess of water can be detrimental and pose a serious threat to plants.
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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...
14.2K
Global Climate Change01:50

Global Climate Change

28.7K
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.
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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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相关实验视频

Updated: Jan 17, 2026

Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information
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降雨量维持了多年的拉尼尼亚现象.

Feng Tian1,2, Rong-Hua Zhang3,4, Chuanyu Liu5,6

  • 1Key Laboratory of Ocean Observation and Forecasting & Laboratory of Ocean Circulation and Waves, Institute of Oceanology, Chinese Academy of Sciences, Qingdao, China. tianfeng@qdio.ac.cn.

Nature communications
|January 14, 2026
PubMed
概括

多年拉尼娜现象正在增加. 这项研究揭示了降雨减少和混合层盐度 (MLS) 异常如何产生反循环,加强长期的拉尼娜现象并影响热带太平洋.

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Continuous Instream Monitoring of Nutrients and Sediment in Agricultural Watersheds
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Continuous Instream Monitoring of Nutrients and Sediment in Agricultural Watersheds

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Last Updated: Jan 17, 2026

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科学领域:

  • 气候科学 气候科学
  • 海洋学 海洋学 海洋学
  • 大气科学 大气科学

背景情况:

  • 多年拉尼娜现象变得越来越频繁,改变了热带太平洋的降雨模式.
  • 这些降雨变化影响区域混合层盐度 (MLS),但反机制尚未完全理解.
  • 了解这些相互作用对于预测气候变化至关重要.

研究的目的:

  • 通过混合层盐度 (MLS) 效应,研究累积降雨异常如何调节多年拉尼娜事件.
  • 确定维持长期拉尼尼亚现象的关键机制.
  • 评估对ENSO预测和水文循环的影响.

主要方法:

  • 分析历史观测和气候模型实验.
  • 量化降雨减少对拉尼尼亚幅度的影响.
  • 研究海洋动态过程和循环反应.

主要成果:

  • 西中赤道太平洋地区的积极MLS异常增强了长期的拉尼娜现象.
  • 降雨量减少使拉尼尼亚的幅度在第一年增加了14%,第二年增加了32%.
  • 快速和缓慢的海洋反应的组合创造了一个积极的降雨盐度反循环.

结论:

  • 雨水度反被认为是维持多年拉尼娜现象的关键机制.
  • 这些发现增强了我们对ENSO动态的理解.
  • 这项研究对改善气候预测和了解水文循环变化有重大影响.