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相关概念视频

Qualitative Analysis03:46

Qualitative Analysis

29.5K
For solutions containing mixtures of different cations, the identity of each cation can be determined by qualitative analysis. This technique involves a series of selective precipitations with different chemical reagents, each reaction producing a characteristic precipitate for a specific group of cations. Metal ions within a group are further separated by varying the pH, heating the mixture to redissolve a precipitate, or adding other reagents to form complex ions.
For instance, group IV...
29.5K
¹H NMR: Interpreting Distorted and Overlapping Signals01:02

¹H NMR: Interpreting Distorted and Overlapping Signals

1.8K
Spin systems where the difference in chemical shifts of the coupled nuclei is greater than ten times J are called first-order spin systems. These nuclei are weakly coupled, and their chemical shifts and coupling constant can generally be estimated from the well-separated signals in the spectrum.
As Δν decreases and the signals move closer, the doublets appear increasingly distorted. The intensities of the inner lines increase at the cost of those of the outer lines as the signals are...
1.8K
IR Frequency Region: X–H Stretching01:24

IR Frequency Region: X–H Stretching

1.8K
In IR spectroscopy, signals produced by the X−H bonds (such as C−H, O−H, or N−H) can be observed in the frequency range of  2700–4000 cm–1. The C−H stretching vibration forms sharp bands in the region 2850–3000 cm–1. The presence of the O−H stretching vibration leads to the forming of an absorption band in the frequency range 3650–3200 cm−1. At the same time, N−H stretching can be confirmed by absorption bands in...
1.8K
IR Frequency Region: Fingerprint Region01:03

IR Frequency Region: Fingerprint Region

2.4K
IR spectra are divided into two main regions: the diagnostic region and the fingerprint region. The diagnostic region of the spectrum lies above 1500 cm−1. The absorptions resulting from single-bond vibrations of the N–H, C–H, and O–H stretch at higher wavenumbers and appear on the left side of the spectrum. The stretching absorptions of the C≡C and C≡N occur between 2100–2300 cm−1. In contrast, those arising from stretching absorptions of the...
2.4K
Magnetic Susceptibility and Permeability01:31

Magnetic Susceptibility and Permeability

2.8K
In linear magnetic materials, like paramagnets and diamagnets, magnetization is proportional to the magnetic field intensity. The constant of proportionality, a dimensionless number, is called magnetic susceptibility. The value of the susceptibility depends on the type of material.
When diamagnetic materials are placed under an external magnetic field, the moments opposite to the field are induced. Hence, the susceptibility for diamagnets has a minimal negative value of 10-5–10-6. Since...
2.8K
Inductively Coupled Plasma-Mass Spectrometry (ICP-MS): Interferences01:20

Inductively Coupled Plasma-Mass Spectrometry (ICP-MS): Interferences

1.7K
Inductively coupled plasma–mass spectrometry (ICP–MS) is a highly selective and sensitive technique for accurate elemental analysis. Though the analysis of ICP–MS mass spectra is comparatively straightforward, it is affected by spectroscopic and non-spectroscopic interferences. Spectroscopic interferences arise when the plasma contains ionic species with an m/z value the same as the analyte ion. Spectroscopic interference can be categorized as isobaric, polyatomic ions, and...
1.7K

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相关实验视频

Updated: Apr 13, 2026

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
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Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions

Published on: June 13, 2015

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上层地幔中的神秘条纹由印度东南部山脊玄武岩中的 hafnium 同位素揭示出来.

D W Graham1, J Blichert-Toft, C J Russo

  • 1College of Oceanic and Atmospheric Sciences, Oregon State University, Corvallis, Oregon 97331, USA. dgraham@coas.oregonstate.edu

Nature
|March 10, 2006
PubMed
概括

在地球上层地幔中存在着古老的组成条纹,这些条纹是由印度东南部山脊玄武岩中双模态 hafnium 同位素分布揭示的. 这些地幔条纹厚度约为40公里.

科学领域:

  • 地质化学 地质化学
  • 地质物理学 地质物理学
  • 地幔动态地幔动态

背景情况:

  • 地球的地幔在各种尺度上表现出同位素异质性.
  • 地幔对流和板块构造学影响了这种异质性.
  • 了解地幔的组成是解读地球演变的关键.

研究的目的:

  • 为了研究印度洋上层地幔的同位素组成.
  • 为了确定地幔异质性的起源和分布.
  • 分析观察到的异质性对地幔动力学的影响.

主要方法:

  • 来自印度东南部山脊 (SEIR) 的中洋山脊玄武岩 (MORB) 的分析.
  • 在玄武岩样本中测量 (Hf) 同位素分布.
  • 对同位素数据进行统计分析,以确定线条特征.

主要成果:

  • 在SEIR基岩中观察到双模态哈夫同位素分布.
  • 这种双模式表明上层地幔中存在古老的组成条纹.
  • 条纹的数量密度遵循波桑分布,平均厚度为~40公里.

结论:

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  • 观察到的条纹分布支持了高度的上层地幔模型.
  • 板块构造回收和粘性流是维持地幔异质性的关键过程.
  • 尽管地幔对流,但古老的组成结构仍然存在.