General
Chemistry
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1. Introduction to Physical Sciences
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Introduction to Chemistry
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History of Chemistry
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Fundamentals of Chemistry
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Atomic Structure
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Stoichiometry
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Thermochemistry
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Gas Laws
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Quantum Mechanics and the Electronic Structure of Atoms
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Periodic Trends
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Bonding
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Solutions
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Acids and Bases
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Redox Reactions
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Organic Chemistry
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Biochemistry
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Future of Chemistry
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Careers in Chemistry
Legacy Course
The pH Scale and Calculating pH
The pH scale is a measure of the acidity or basicity of a solution, and it is based on the concentration of hydrogen ions (H+) in the solution. The pH scale ranges from 0 to 14, with a pH of 7 being neutral, a pH less than 7 being acidic, and a pH greater than 7 being basic.

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To calculate the pH of a solution, one must first determine the concentration of hydrogen ions in the solution. This can be done using the following equation:
pH = -log[H+]
where [H+] is the concentration of hydrogen ions in moles per liter (mol/L).
For example, a solution with a concentration of hydrogen ions of 1 x 10-5 mol/L has a pH of 5, because -log[1 x 10-5] = 5.
The pH of a solution is important because it determines the behavior of acids, bases, and other substances in the solution. For example, enzymes, which are proteins that catalyze chemical reactions in the body, have optimal pH ranges within which they function most efficiently. Similarly, the pH of soil can affect the growth and health of plants, and the pH of water can affect the solubility of various substances and the toxicity of pollutants. The pH of a solution can be measured using a pH meter or pH indicator strips, and it is an important parameter in many chemical and biological systems.

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