L1B Flashcards
(9 cards)
1
Q
Hubble’s Law
A
Objects in space are moving apart
2
Q
Big Bang Theory Evidence
A
- Hubble’s Law
Measures this doppler effect to describe how objects in space move apart from one another
If objects are moving apart, they must have started together at a single point
- The universe is permeated by background radiation
This background radiation is believed to be the fading afterglow of the Big Bang
3
Q
Nucleosynthesis
A
creation of nuclei from pre-existing nucleons
4
Q
Big Bang Nucleosynthesis
A
- will create forms of hydrogen and helium (and some lithium)
- Few minutes later – cooled below 109 K*, no more nuclear reactions possible, until stars
5
Q
Stellar Nucleosynthesis
A
- Stars are fueled by fusion of H to He. As stars age, other elements burns to fuel the star
- Combining helium with other elements creates many more
6
Q
Nebulae
A
are stellar nurseries
7
Q
Galactic Nucleosynthesis
A
- Cosmic rays collide with heavier atoms
- Atoms break apart into fragments via spallation
8
Q
Origin of the solar system
A
- Hot origin – comet collision:
- Proposed a “hot origin” of the planets from a collision between a comet and the sun
- Earth initially very hot, but as it cooled, molten rock hardened - Nebular hypothesis:
- Condensation of a hot gaseous nebula in progressive stages
- As centre of nebula (sun) rotated and contracted, gas ejected form rings
- Rings condensed to form molten balls, which cool and harden into planets (oldest planets farthest from the sun) - Cold origin – planetesimal hypothesis:
- Gravity of star that passed close to the sun lead to the extraction of a succession of solar gases
- Orbiting material cooled and condensed into particles that accreted into small bodies (planetesimals) - Modern nebular:
- Planets as byproducts of star formation
- Local instability in nebula causes gravitational collapse into central sphere
- Laws of physics shape a central sphere (proto-star) surrounded by disk
- Planets formed by accretion, starting with micron sized grains into larger bodies
9
Q
Chemical versus Physical Layering (differentiation)
A
Chemical: - refers to the composition -Core: metallic iron, high density -Mantle: rocky, intermediate density -Crust: rocky, low density – Oceanic: thin but denser – Continental: thick but lighter
Physical:
- refers to the material properties
- Inner core: solid
- Outer core: molten
- Mesosphere (mantle except the upper mantle): solid
- Asthenosphere (upper mantle): weak and plastic
- Lithosphere (uppermost mantle plus crust): strong and rigid