Gas Properties: Specific Volume, Viscosity, and Compressibility

Specific Volume (v) is the volume occupied by a unit mass of material. It is the inverse of density and does not depend on the amount of matter. For example, two pieces of iron with different sizes have different weights and volumes, but their specific gravities are equal. This is independent of the material amount. Examples of intensive properties include boiling point, brightness, color, hardness, and melting point.
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Where: V is volume, m is mass, and ρ is the density of the material.
It is expressed

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Steel Production: An Overview of Furnace Processes and Alloying Elements

Steel Production Processes

Open Hearth Furnace

One of the most popular steel production methods, the open hearth furnace, can hold 10 to 540 tons of metal. Its shallow depth allows flames to directly heat the load. Fuel sources include gas, tar, or oil. These regenerative furnaces often have side fireplaces to expel heated gases used for air and fuel heating. Open hearth furnaces typically have basic linings, but acid linings (silica and clay brick walls) also exist. Basic linings offer better control

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Nuclear Stability and Reactions: A Comprehensive Overview

Nuclear Stability and Reactions

From Two Viewpoints: Nuclear Power and Energy

A. Strong Nuclear Force

The strong nuclear force, theorized by Hideki Yukawa, is the strongest of the fundamental forces but has the shortest range. It is independent of charge and works only for particles within a distance of less than 10-16 meters. For distances between 10-16 and 10-14 meters, there is less repulsion. Nuclei with approximately equal numbers of protons (Z) and neutrons (N) are stable. As Z increases, the

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Stoichiometry and Natural Gas: LNG, LPG, and NGV

Stoichiometry

In chemistry, stoichiometry is the calculation of the quantitative relationships between reactants and products during a chemical reaction. These relationships can be deduced from the atomic theory, although historically spelled out without reference to the composition of matter, according to different laws and principles.

The first to set out the principles of stoichiometry was Jeremias Benjamin Richter (1762-1807) in 1792. He wrote:

Stoichiometry is the science that measures the quantitative

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Earth’s Seasons & Climate Zones: An In-depth Guide

Module 3: Seasons

Earth’s Axis and Movement

1. What is the Earth’s axis?
It is an imaginary straight line passing through the Earth’s center. The Earth rotates around this line. The points where this line intersects the Earth’s surface are the North and South Poles.

2. What are the movements of Earth’s axis called?

  • Precession
  • Nutation

3. What is the Equator?
It is the great circle perpendicular to the Earth’s axis that divides the Earth into two hemispheres: the Northern Hemisphere (or Boreal) and the Southern

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Chemical Reactions and Equilibrium

The Orientation of Shocks

Molecules must collide in a particular direction for a reaction to occur.

The Theory of the Transition State

Halfway between the reactants and products, an activated complex occurs. This consists of the reagents, which form a complex called an agglomerated activated complex or transition state. This complex is always higher in energy than the reactants and products, so it is very unstable and its life is very short. This theory assumes that the reactants collide with each

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