What ’ s Geophysics

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What’s Geophysics Understanding the Earth’s composition and dynamics, and their relationships with the surface geological phenomena, using the means of Physics. Analogy: How do you figure out what is going on inside an apple, egg, golf ball, human body, without slicing it open? (Suggestions: you can weigh it, spin it, heat it, probe it with electromagnetism, etc. You can also look at what is naturally emitted from it.)

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What ’ s Geophysics. Understanding the Earth ’ s composition and dynamics, and their relationships with the surface geological phenomena, using the means of Physics. - PowerPoint PPT Presentation

Transcript of What ’ s Geophysics

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What’s Geophysics

• Understanding the Earth’s composition and dynamics, and their relationships with the surface geological phenomena, using the means of Physics.

• Analogy: How do you figure out what is going on inside an apple, egg, golf ball, human body, without slicing it open? (Suggestions: you can weigh it, spin it, heat it, probe it with electromagnetism, etc. You can also look at what is naturally emitted from it.)

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Tapping the Earth

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Gravity Recovery and Climate Experiment (GRACE)

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General Goals

• A modest foundation of factual knowledge about the Earth, and a feeling for the size of things.

• A basic understanding of the underlying physical principles for the observed Earth’s phenomena.

• An awareness of geophysical methodologies and how they are combined to solve problems.

• An appreciation of the level of current knowledge in geophysics, and the many exciting problems that still remain to be tackled.

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Why Geophysics?

• Human Nature.

• Related to our daily life.

• Necessary tools for economic applications.

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Earth as a Planet

• Mass M = 6 x 1027 g.• Radius R = 6371 km.• Mean density = M/(4/3

R3) = 5.5 g/cm3

• Moment of inertia I of the Earth: – I = r2 dm

– I/(MR2) = 0.331.

– for a uniform sphere I/(MR2) = 0.4.

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Interior of the Earth

• Crust: variable thickness with an average value of 35 km in the continents and 7-8 km in the oceanic regions. Volume ~1019 m3 Mass 2.8 x 1022 kg.

• Mantle: between the Moho discontinuity (crust-mantle) and the core-mantle boundary (R = 3480 km). Volume 9 x 1020 m3 Mass 4 x 1024 kg.

• Core: from the center of the Earth to the core-mantle boundary. Volume 1.77 x 1020 m3 Mass 1.94 x 1024 kg.

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