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Minerals01:26

Minerals

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Minerals are essential nutrients that the human body needs in small amounts to work properly. They play a vital role in many bodily functions, such as building strong bones and transmitting nerve impulses. Some minerals are needed for hormone production or to maintain a normal heartbeat. Major minerals include calcium, phosphorus, potassium, sulfur, sodium, chlorine, and magnesium, while trace minerals include iron, manganese, copper, iodine, zinc, cobalt, fluoride, and selenium.
 
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Porosity in Cement Paste01:18

Porosity in Cement Paste

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The porosity of concrete is a measure of the void spaces within its structure. These spaces impact its strength and durability significantly. When water and cement interact, a chemical reaction called hydration creates a semi-solid paste. This paste includes combined water, making up approximately 23% of the cement's dry mass, and gel water, which fills minuscule voids known as gel pores, accounting for about 28% of the cement gel volume.
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Magnetic Susceptibility and Permeability01:31

Magnetic Susceptibility and Permeability

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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.
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...
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Conditions on Early Earth02:06

Conditions on Early Earth

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Around 4 billion years ago, oceans began to condense on earth while volcanic eruptions released nitrogen, carbon dioxide, methane, ammonia, and hydrogen into the primordial atmosphere. However, organisms with the characteristics of life were not initially present on earth. Scientists have used experimentation to determine how organisms evolved that could grow, reproduce, and maintain an internal environment.
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Phase Transitions: Sublimation and Deposition02:33

Phase Transitions: Sublimation and Deposition

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Some solids can transition directly into the gaseous state, bypassing the liquid state, via a process known as sublimation. At room temperature and standard pressure, a piece of dry ice (solid CO2) sublimes, appearing to gradually disappear without ever forming any liquid. Snow and ice sublimate at temperatures below the melting point of water, a slow process that may be accelerated by winds and the reduced atmospheric pressures at high altitudes. When solid iodine is warmed, the solid sublimes...
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Crystal Field Theory - Octahedral Complexes02:58

Crystal Field Theory - Octahedral Complexes

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Crystal Field Theory
To explain the observed behavior of transition metal complexes (such as colors), a model involving electrostatic interactions between the electrons from the ligands and the electrons in the unhybridized d orbitals of the central metal atom has been developed. This electrostatic model is crystal field theory (CFT). It helps to understand, interpret, and predict the colors, magnetic behavior, and some structures of coordination compounds of transition metals.
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Related Experiment Video

Updated: Feb 19, 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

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Perovskite in Earth's deep interior.

Kei Hirose1,2, Ryosuke Sinmyo3,2, John Hernlund3

  • 1Earth-Life Science Institute, Tokyo Institute of Technology, Meguro, Tokyo 152-8550, Japan. kei@elsi.jp.

Science (New York, N.Y.)
|November 11, 2017
PubMed
Summary

Silicate perovskites are key minerals in Earth's deep interior and influence planetary evolution. Understanding their properties is crucial for comprehending mantle dynamics and the development of rocky planets.

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Related Experiment Videos

Last Updated: Feb 19, 2026

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

  • Geophysics
  • Mineral Physics
  • Planetary Science

Background:

  • Silicate perovskites are abundant in Earth's lower mantle (>660 km depth).
  • Magnesium-rich perovskite transitions to post-perovskite at the core-mantle boundary.
  • Calcium-rich perovskite, though minor, records chemical differentiation.

Purpose of the Study:

  • To elucidate the significance of mantle perovskites in Earth's structure and evolution.
  • To highlight the role of perovskites in understanding terrestrial planet development.

Main Methods:

  • Analysis of mineral physics properties.
  • Geochemical interpretation of trace elements in perovskites.

Main Results:

  • Perovskite properties dictate lower mantle rock transport.
  • These minerals are vital for understanding Earth's dynamic evolution.
  • Perovskites are crucial components of rocky planets beyond Mars.

Conclusions:

  • Mantle perovskites are fundamental to Earth's internal dynamics.
  • Their study provides insights into the evolution of terrestrial planets across the universe.