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Apparent Weight and the Earth's Rotation01:28

Apparent Weight and the Earth's Rotation

Since all objects on the Earth's surface move through a circle every 24 hours, there must be a net centripetal force on each object, directed towards the center of that circle. The points of the north and south poles are the only exception to this rule.
For an object on the Earth's equator, the net centripetal force that accounts for its rotation is the Earth's pull towards its center, or the weight minus the normal force that prevents it from piercing into the Earth's surface. This force,...
The Bohr Model02:18

The Bohr Model

Following the work of Ernest Rutherford and his colleagues in the early twentieth century, the picture of atoms consisting of tiny dense nuclei surrounded by lighter and even tinier electrons continually moving about the nucleus was well established. This picture was called the planetary model since it pictured the atom as a miniature “solar system” with the electrons orbiting the nucleus like planets orbiting the sun. The simplest atom is hydrogen, consisting of a single proton as the nucleus...
Theory of Metallic Conduction01:17

Theory of Metallic Conduction

The conduction of free electrons inside a conductor is best described by quantum mechanics. However, a classical model makes predictions close to the results of quantum mechanics. It is called the theory of metallic conduction.
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Fluid Mosaic Model01:34

Fluid Mosaic Model

The fluid mosaic model was first proposed as a visual representation of research observations. The model comprises the composition and dynamics of membranes and serves as a foundation for future membrane-related studies. The model depicts the structure of the plasma membrane with a variety of components, which include phospholipids, proteins, and carbohydrates. These integral molecules are loosely bound, defining the cell’s border and providing fluidity for optimal function.LipidsThe most...
Fluid Mosaic Model01:19

Fluid Mosaic Model

Scientists identified the plasma membrane in the 1890s and its principal chemical components (lipids and proteins) by 1915. The model for plasma membrane structure, proposed in 1935 by Hugh Davson and James Danielli, was the first model to be widely accepted in the scientific community. The model was based on the plasma membrane's "railroad track" appearance in early electron micrographs. Davson and Danielli theorized that the plasma membrane's structure resembled a sandwich with the analogy of...
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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.
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Related Experiment Video

Updated: Jul 11, 2026

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

Models of the Earth's Core.

D J Stevenson

    Science (New York, N.Y.)
    |November 6, 1981
    PubMed
    Summary

    Earth

    Area of Science:

    • Geophysics and planetary science.
    • Understanding the Earth's deep interior.

    Background:

    • Current models of Earth's core are based on diverse scientific disciplines.
    • Previous research has explored core formation and composition.

    Purpose of the Study:

    • To develop comprehensive models of the Earth's core.
    • To integrate data from seismology, high-pressure experiments, and planetary evolution theories.

    Main Methods:

    • Combined inferences from seismology, high-pressure experiments, and theoretical physics.
    • Analysis of geomagnetism and fluid dynamics.
    • Application of liquid-state theory to seismic and laboratory data.

    Main Results:

    • Earth's core formed concurrently with planetary accretion.

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

    Published on: June 13, 2015

    Sediment Core Extrusion Method at Millimeter Resolution Using a Calibrated, Threaded-rod
    06:06

    Sediment Core Extrusion Method at Millimeter Resolution Using a Calibrated, Threaded-rod

    Published on: August 17, 2016

    Related Experiment Videos

    Last Updated: Jul 11, 2026

    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

    Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
    11:50

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

    Published on: June 13, 2015

    Sediment Core Extrusion Method at Millimeter Resolution Using a Calibrated, Threaded-rod
    06:06

    Sediment Core Extrusion Method at Millimeter Resolution Using a Calibrated, Threaded-rod

    Published on: August 17, 2016

  • The outer core is a fluid, likely uniform alloy of iron and lighter elements.
  • The inner core is solid iron, and its formation releases energy sustaining Earth's magnetic field.
  • Conclusions:

    • The Earth's core is not in chemical equilibrium with the mantle.
    • Thermodynamic properties of the core are constrained by experimental and seismic data.
    • Energy release from inner core solidification drives the geodynamo.