Lesson 01: Introduction to the Atmosphere

Lesson 40/66 | Study Time: 30 Min
Course: Chemistry X
Lesson 01: Introduction to the Atmosphere

 



Learning Outcomes:



i. Define and describe the atmosphere, the gaseous envelope that surrounds Earth.



ii. Explain the significance of the atmosphere in supporting life on Earth.



iii. Identify the major components of Earth's atmosphere and their relative proportions.



iv. Understand the concept of atmospheric pressure and its variation with altitude.



 



Introduction:



The atmosphere, the invisible yet vital layer that envelops our planet, is a dynamic and complex system that plays a fundamental role in sustaining life on Earth. In this introductory lesson, we embark on a journey to unravel the mysteries of the atmosphere, delving into its composition, significance, and impact on our existence.



i. Defining the Atmosphere:



The atmosphere is a vast expanse of gases that extends from the Earth's surface to an altitude of approximately 500 kilometers. It is a mixture of various gases, primarily consisting of nitrogen (78%), oxygen (21%), and argon (0.9%). Trace amounts of other gases, including carbon dioxide, neon, helium, methane, and hydrogen, also contribute to the atmosphere's composition.



ii. Significance of the Atmosphere:



The atmosphere is not merely a blanket of air; it is a life-supporting system that sustains the delicate balance of Earth's ecosystems. It protects us from the harmful radiation of the sun, regulates temperature, provides essential gases for respiration, and enables the formation of clouds and precipitation. Without the atmosphere, life on Earth as we know it would not exist.



iii. Major Components of the Atmosphere:



Nitrogen, the most abundant component of the atmosphere, serves as a diluent, preventing oxygen levels from becoming too high, which could be toxic. Oxygen, the essential gas for respiration, is the second most abundant component. Argon, an inert gas, plays a crucial role in atmospheric stability and temperature regulation.



iv. Atmospheric Pressure:



Atmospheric pressure, the force exerted by the weight of the atmosphere on the Earth's surface, decreases with increasing altitude. This is because the weight of the overlying atmosphere decreases as we move away from the Earth's surface. Atmospheric pressure is essential for various biological processes, including respiration and cell function.



The atmosphere, a delicate and intricate system, is a cornerstone of life on Earth. Its composition, significance, and impact on our environment are essential aspects of environmental chemistry. Understanding the atmosphere empowers us to appreciate its importance and take responsibility for protecting this precious resource.



 



 

Ahmed Hassan

Ahmed Hassan

Product Designer

Class Sessions

1- Lesson 01: Introduction to Chemical Equilibrium 2- Lesson 02: Forward and Reverse Reactions 3- Lesson 03: Law of Mass Action 4- Lesson 04: Equilibrium Constant Expression 5- Lesson 05: Necessary Conditions for Equilibrium 6- Lesson 01: The Essentials of Respiratory Physiology 7- Lesson 02: Bronsted-Lowry Theory 8- Lesson 03: Lewis Acids and Bases 9- Lesson 04: Self-Ionization of Water 10- Lesson 05: Classifying Solutions 11- Lesson 06: Neutralization Reactions 12- Lesson 01: Introduction to Organic Chemistry 13- Lesson 02: General Characteristics of Organic Compounds 14- Lesson 03: Diversity and Magnitude of Organic Compounds 15- Lesson 04: Sources of Organic Compounds 16- Lesson 05: Uses of Organic Compounds 17- Lesson 06: Functional Groups in Molecules 18- Lesson 07: Saturated and Unsaturated Hydrocarbons 19- Lesson 08: Naming Alkanes up to Decane 20- Lesson 09: Converting Alkanes into Alkyl Radicals 21- Lesson 10: Differentiating Alkanes and Alkyl Radicals 22- Lesson 11: Introduction to Functional Groups 23- Lesson 12: Differentiating Organic Compounds Based on Functional Groups 24- Lesson 13: Classifying Organic Compounds 25- Lesson 01: Importance of Systematic Naming 26- Lesson 02: Characterizing Hydrocarbons 27- Lesson 03: Electron Cross and Dot Structures of Alkanes 28- Lesson 04: Preparation of Alkanes 29- Lesson 05: Structural Formulas of Alkanes, Alkenes, and Alkynes 30- Lesson 06: Preparation of Alkenes and Alkynes 31- Lesson 07: Halogenation of Hydrocarbons 32- Lesson 08: Reaction with KMnO4 33- Lesson 01: Types of Saccharides 34- Lesson 02: Protein Molecule Bonding 35- Lesson 03: Sources and Uses of Biomolecules 36- Lesson 04: Differentiating Fats and Oils 37- Lesson 05: Importance of Nucleic Acids 38- Lesson 06: Vitamins and Their Significance 39- Lesson 01: Introduction to the Atmosphere 40- Lesson 02: Composition of the Atmosphere 41- Lesson 03: Stratosphere and Troposphere Differences 42- Lesson 04: Components of Stratosphere and Troposphere 43- Lesson 05: Major Air Pollutants 44- Lesson 06: Sources and Effects of Air Pollutants 45- Lesson 07: Ozone Formation 46- Lesson 08: Acid Rain and Its Effects 47- Lesson 09: Ozone Depletion and Its Effects 48- Lesson 10: Global Warming 49- Lesson 01: Occurrence and Importance of Water 50- Lesson 02: Dependence on Water and Water Quality 51- Lesson 03: Composition and Properties of Water 52- Lesson 04: Types of Water Hardness 53- Lesson 05: Eliminating Water Hardness 54- Lesson 06: Water Pollutants 55- Lesson 07: Effects of Water Pollutants 56- Lesson 08: Waterborne Diseases 57- Lesson 01: Metallurgical Operations 58- Lesson 02: Raw Materials for Solvay Process 59- Lesson 03: Reactions of Solvay Process 60- Lesson 04: Flow Sheet Diagram of Solvay Process 61- Lesson 05: Composition of Urea 62- Lesson 06: Manufacture of Urea 63- Lesson 07: Uses of Urea 64- Lesson 08: Definition and Formation of Petroleum and Natural Gas 65- Lesson 09: Composition of Petroleum 66- Lesson 10: Fractional Distillation of Petroleum