Materials Science: Properties, History, and Nanotechnology

Introduction to Materials Science

Everything in the universe exists in a material form. Matter, as it occurs in nature, has specific properties. Matter is constituted by particles. The Big Bang created atoms, initially Hydrogen and Helium. The nucleus of stars produces heavier atoms like Iron. Supernova explosions create the rest of the heavy atoms. Materials can be used as pure substances or mixtures.

Types of Materials

  • Raw Materials: Obtained directly from nature, such as wood, granite, and sand.
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Soil Formation, Composition, and Conservation

Soils: Formation and Composition

Soils: are formed from the superficial layer of the crust. This process is called pedogenesis.

Stages of Soil Formation:

  1. Formation of Horizon C: Mainly due to temperature changes, the rocks undergo physical weathering, disintegrating into pieces. Chemical weathering alters some minerals in the rocks.
  2. Appearance of Horizon A: Living organisms are established on horizon C. First, lichens and mosses, then bacteria, fungi, and finally more evolved living organisms. Living
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Rock Deformation, Magmatism, and Seismic Activity

Deformation of Rocks

  • Compressive stresses: Convergent forces that usually occur in subduction zones and collision areas.
  • Tensional stresses: Divergent forces that act on the rocks of rifts.
  • Shear stresses: Transform forces that occur at transform boundaries.

How Do Rocks Respond to Stress?

Rocks respond in an elastic way (they accumulate elastic energy). If the stress continues near the surface, the rocks break and release the elastic energy (they are rigid), causing earthquakes and fault joints.

Factors

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Renewable Energy Sources: Geothermal and Tidal Power

Geothermal and Tidal Energy Sources

The heat for geothermal power comes from ongoing radioactive decay and primordial heat left over from the formation of the Earth. The energy can be tapped anywhere on the Earth’s surface, but it is best in volcanically active areas.

Radioactive Decay

The decomposition of species gives rise to uranium-235 and thorium-232. This process continually replenishes geothermal energy.

Primordial Heat

As the name implies, primordial heat has existed since the creation of the

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Ecosystems and Biomes: A Comprehensive Look at Earth’s Habitats

Ecosystems: Interconnectedness of Life

From Geosphere to Biosphere

Ecology is the science that studies the characteristics of living beings and the environment in which they live. Key concepts include:

  • Biotope: The physical environment where living organisms of an ecosystem develop their life.
  • Biocenosis: The community of living beings in a particular ecosystem.
  • Habitat: The specific location where an organism lives.

Terrestrial and Aquatic Environments

  • Terrestrial Environment: The surface of continents.
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Internal Geological Processes: Volcanoes and Earthquakes

Internal Geological Processes

Internal geological processes are caused by the heat inside the Earth. These include volcanic activity, earthquakes, and the formation of ridges. The heat inside the Earth not only causes volcanic activity but also the movements of lithospheric plates that produce earthquakes and cause the great ranges.

Volcanoes

Definition

Volcanoes are often steep, conical mountains. However, not all volcanoes are high mountains or perfect cones. They are often under the sea, and their

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