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相关概念视频

Charging Conductors By Induction01:15

Charging Conductors By Induction

The Earth is a good conductor of electricity, and it is so big that it can be considered an infinite source or sink of charges. It can easily exchange charges with any matter.
Generally, conductors like metals do not allow any excess charge to be present on them. Any excess charge added to metals easily flows away, for example, when a metal is placed on the Earth. This process is called earthing.
However, conductors can be charged by a process called induction. For example, consider charging a...
Magnetic Field Lines01:19

Magnetic Field Lines

The representation of magnetic fields by magnetic field lines is very useful in visualizing the strength and direction of the magnetic field. Each of the magnetic field lines forms a closed loop. The field lines emerge from the north pole (N), loop around to the south pole (S), and continue through the bar magnet back to the north pole.
Magnetic field lines follow several hard-and-fast rules:
Magnetostatic Boundary Conditions01:28

Magnetostatic Boundary Conditions

An electric field suffers a discontinuity at a surface charge. Similarly, a magnetic field is discontinuous at a surface current. The perpendicular component of a magnetic field is continuous across the interface of two magnetic mediums. In contrast, its parallel component, perpendicular to the current, is discontinuous by the amount equal to the product of the vacuum permeability and the surface current. Like the scalar potential in electrostatics, the vector potential is also continuous...
Types of Building Separation Joints01:23

Types of Building Separation Joints

Building separation joints divide large or complex building structures into smaller, discrete units that can move independently. These joints are categorized into three types: volume-change joints, settlement joints, and seismic separation joints.
Volume-change joints address the effects of expansion and contraction due to temperature and moisture variations. They are strategically placed at discontinuities in a building's mass where cracking is most likely and are spaced about 150 to 200 feet...
Influence of Earth's Curvature and Atmospheric Refraction on Leveling01:26

Influence of Earth's Curvature and Atmospheric Refraction on Leveling

During leveling, the Earth's curvature and atmospheric refraction introduce deviations in the line of sight from a true horizontal reference. When the line of sight is leveled, it remains perpendicular to the plumb line only at a single point. Beyond this, it deviates due to the Earth’s curvature, represented by the correction C. For a sight distance D, the deviation can be derived using the relationship:This relationship shows that the deviation increases quadratically with distance. Over a...
Microbes and Other Elemental Cycles01:24

Microbes and Other Elemental Cycles

Microbial activity plays a pivotal role in the biogeochemical cycling of iron and manganese, especially at the redox gradients characteristic of stratified aquatic environments. These cycles are driven by microbial transformations between oxidized and reduced forms of the metals, allowing organisms to exploit them for metabolic energy and structural purposes.Iron Cycling Across Redox GradientsIn neutral, oxygen-rich surface waters, iron is predominantly found in its oxidized, insoluble ferric...

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Simulation of the Planetary Interior Differentiation Processes in the Laboratory
06:04

Simulation of the Planetary Interior Differentiation Processes in the Laboratory

Published on: November 15, 2013

铁在地球地幔中的分割:朝着深层下层地幔不连续性的方向.

James Badro1, Guillaume Fiquet, François Guyot

  • 1Laboratoire de Mine Université ralogie-Cristallographie de Paris, Université Paris VI, Université Paris 7, CNRS, IPGP, 4 place Jussieu, F-75252 Paris Cedex 05, France.

Science (New York, N.Y.)
|April 5, 2003
PubMed
概括

地球下层地幔中的铁经历了大约2000公里深处的高旋转到低旋转过渡. 这导致铁在ferropericlase中缩,可能在深层地幔中形成不同的层.

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Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
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Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt
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Simulation of the Planetary Interior Differentiation Processes in the Laboratory
06:04

Simulation of the Planetary Interior Differentiation Processes in the Laboratory

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Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
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Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt

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科学领域:

  • 地质物理学 地质物理学
  • 矿物物理 矿物物理
  • 地球科学 地球科学 地球科学

背景情况:

  • 地球的下层地幔主要由铁烯酸和酸盐矿组成.
  • 了解铁在高压下的行为对于建模地球深层过程至关重要.

研究的目的:

  • 为了研究与下层地幔相关的高压下铁烯酸中铁的旋转状态.
  • 确定旋转过渡发生的压力及其对铁分区的影响.

主要方法:

  • 在高压实验中对铁烯酶 ((Mg0.83Fe0.17) O) 进行了实验.
  • 铁的自旋状态在60-70千兆帕斯卡尔的压力范围内被测量.

主要成果:

  • 在ferropericlase中观察到铁的高旋转到低旋转过渡在60和70GPa之间.
  • 这种压力范围对应于地球下层地幔中约2000公里的深度.
  • 在ferropericlase和酸矿石之间,铁的分割系数可能会显著增加.

结论:

  • 旋转过渡表明下层地幔的潜在分层成不同的富含铁和缺乏铁的层.
  • 这种分层可能会对地球深层的热量和质量传输产生重大影响.
  • 这些发现完善了下层地幔组成和动态的模型.