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関連する概念動画

Atomic Nuclei: Nuclear Relaxation Processes01:23

Atomic Nuclei: Nuclear Relaxation Processes

In the absence of an external magnetic field, nuclear spin states are degenerate and randomly oriented. When a magnetic field is applied, the spins begin to precess and orient themselves along (lower energy) or against (higher energy) the direction of the field. At equilibrium, a slight excess population of spins exists in the lower energy state. Because the direction of the magnetic field is fixed as the z-axis,  the precessing magnetic moments are randomly oriented around the z-axis. This...
Random Variables01:09

Random Variables

A random variable is a single numerical value that indicates the outcome of a procedure. The concept of random variables is fundamental to the probability theory and was introduced by a Russian mathematician, Pafnuty Chebyshev, in the mid-nineteenth century.
Uppercase letters such as X or Y denote a random variable. Lowercase letters like x or y denote the value of a random variable. If X is a random variable, then X is written in words, and x is given as a number.
For example, let X = the...
Randomized Experiments01:13

Randomized Experiments

The randomization process involves assigning study participants randomly to experimental or control groups based on their probability of being equally assigned. Randomization is meant to eliminate selection bias and balance known and unknown confounding factors so that the control group is similar to the treatment group as much as possible. A computer program and a random number generator can be used to assign participants to groups in a way that minimizes bias.
Simple randomization
Simple...
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...
Magnetic Damping01:17

Magnetic Damping

Eddy currents can produce significant drag on motion, called magnetic damping. For instance, when a metallic pendulum bob swings between the poles of a strong magnet, significant drag acts on the bob as it enters and leaves the field, quickly damping the motion.
If, however, the bob is a slotted metal plate, the magnet produces a much smaller effect. When a slotted metal plate enters the field, an emf is induced by the change in flux; however, it is less effective because the slots limit the...
Mechanistic Models: Compartment Models in Algorithms for Numerical Problem Solving01:29

Mechanistic Models: Compartment Models in Algorithms for Numerical Problem Solving

Mechanistic models play a crucial role in algorithms for numerical problem-solving, particularly in nonlinear mixed effects modeling (NMEM). These models aim to minimize specific objective functions by evaluating various parameter estimates, leading to the development of systematic algorithms. In some cases, linearization techniques approximate the model using linear equations.
In individual population analyses, different algorithms are employed, such as Cauchy's method, which uses a...

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関連する実験動画

Updated: Jul 9, 2026

A Random-displacement Measurement by Combining a Magnetic Scale and Two Fiber Bragg Gratings
08:23

A Random-displacement Measurement by Combining a Magnetic Scale and Two Fiber Bragg Gratings

Published on: September 30, 2019

地磁気逆転の新しいストキャスティックモデル

I K Crain1, P L Crain

  • 1Department of Geology, School of General Studies, Australian National University, Canberra, ACT.

Nature
|October 3, 1970
PubMed
まとめ

地磁気反転のための新しい非静止型モデルは,平均極性間隔の長さが160万年であることを示唆しています. この研究により,地球についての理解が深まる.

科学分野:

  • 地質物理学 地質物理学とは地質物理学です.
  • 地球科学 地球科学 地球科学
  • パレオマグネティズム (古磁気学) とは

背景:

  • 地磁気反転は,地球の歴史における重要な出来事です.
  • 以前のモデルはしばしば静止性を仮定し,その予測力を制限していた.

研究 の 目的:

  • 地磁気逆転のための新しい非静止モデルを提案する.
  • 極性間隔の平均期間を予測するために.

主な方法:

  • 非静止数学的モデルの開発.
  • シミュレートされた地磁気逆転データの分析.

主要な成果:

  • このモデルは,すべての極性間隔の平均長さが160万年であると予測しています.
  • この発見は,地磁場変化のダイナミクスに関する新しい洞察を提供します.

結論:

  • 非静止型モデルは,地磁気反転を研究するためのより現実的な枠組みを提供します.
  • 予測された平均間隔の長さは,古磁気学の研究と地球のダイナモ理論に意味を持っています.

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Last Updated: Jul 9, 2026

A Random-displacement Measurement by Combining a Magnetic Scale and Two Fiber Bragg Gratings
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A Random-displacement Measurement by Combining a Magnetic Scale and Two Fiber Bragg Gratings

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A Mouse Model of Lumbar Spine Instability

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Cell Patterning Using Magnetic-Archimedes Strategy

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