MODERN-THEORIES-ON-THE-ORIGIN-OF-THE-UNIVERSE-PHYSICAL-SCIENCE-12
The universe began approximately 14 billion years ago from an infinitely tiny and dense point known as the singularity.
Initially, there was no matter; only pure energy existed.
A violent explosion led to the universe's inflation and expansion.
Four Fundamental MODERN THEORIES ON THE ORIGIN OF THE UNIVERSE AND THE ORIGIN OF THE SOLAR SYSTEM
Prepared by: Cherry P. Marañan
BIG BANG THEORY
Forces Formed
Gravity: The force that causes attraction between bodies.
Electromagnetic Force: Binds atoms into molecules.
Strong Nuclear Force: Binds protons and neutrons together in the atomic nucleus.
Weak Nuclear Force: Responsible for radioactive decay by breaking down an atom’s nucleus.
INFLATIONARY UNIVERSE
Proposed by physicist Alan Guth, this model builds upon the Big Bang theory.
The universe experienced a rapid expanse known as cosmic inflation about 10^-36 seconds after the Big Bang.
This model addresses issues of the standard model, such as the horizon and flatness problems, leading to the development of the inflationary model.
MULTIVERSE
The concept was developed and popularized by physicists Hugh Everett III and Bryce DeWitt in the 1960s and 1970s.
It suggests that our universe is just one among many "bubbles" that expanded as part of a larger multiverse.
THE ORIGIN OF THE SOLAR SYSTEM
Formed from dust-sized particles originating from the Big Bang.
The solar system and Earth are approximately 4.54 billion years old, based on meteorite analysis which indicates simultaneous formation with the rest of the solar system.
FORMATION HYPOTHESES
ENCOUNTER HYPOTHESIS
One of the earliest theories for the formation of planets.
This hypothesis explains why planets revolve in the same direction.
NEBULAR HYPOTHESIS
Suggests that the solar system evolved from a large cloud of gas that contracts due to self-gravity.
PROTOPLANET HYPOTHESIS
Proposes that the solar system began with a fragment from an interstellar cloud composed primarily of hydrogen and helium, along with trace elements.