Question about the sun and the earth long long ago.

In summary: The sun will expand as it enters the red giant phase and will oddly then begin to lose mass - upto 25% of the outer envelope is ejected.As an example of the range of densities, Betelgeuse (the red star at Orion's shoulder) is about 14times the mass of the sun but 650 times the radius, so it has about 275Million times the volume but only 1/20 millionth the density.Red Giant Branch and Asymptotic Giant Branch stars are really just small dense fusion cores surrounded by a very BIG atmosphere. The two parts of the star don't mix and the outer layers eventually get blown away. Smaller stars - smaller than the Sun - are more like the
  • #1
LostInSpaceTime
23
0
I might already know the answer to this but i just need to make sure. Does a suns mass reflect its volume? I ask because...


The formation of a star simply put is: a planet gathers mass there-by gathering gravity there-by igniting and becoming a star…it becomes a star with x amount of mass to start then burns and burns and burns until it looses enough stuff to burn causing an implosion then an explosion(super nova). Correct??

So if this is true where was Earth when our sun was reeeeeeeeealy big? Is it not true that the sun looses x amount of mass a year and by rewinding the whole sequence you should be able to see how big the sun was say about 4.6 billion years ago? If around that time say a planet was trying to evolve wouldn’t the sun have pulled this planet in leaving it, well, not there? Seeing how the sun loses a lot of mass now, 4.6 billion years ago would put the sun at…BIG (at least I assume big enough to reach our orbit) we’ll say maybe too big for the Earth to be just kinda hanging around unharmed. Now let’s move 1.6 billion years ahead. Somehow this planet survived orbiting closely or even within the sun, 1.6 million years should shrink the sun a bit. About this time this planet starts to have life appear, the sun would still be really close, close enough to be super heating the Earth and kill those pesky possible life forms. I don’t know the #’s but I’m sure some of you do.
How much mass the sun is loosing at present/year (x)
then
(x)4.6billion=y
then
Y + present day mass of sun = mass of sun 4.6billion years ago. (We’ll call this z)
Now how much volume would the sun fill with (z) amount of mass? Or would the same amount of volume hold greater amounts of mass? Leaving the sun heavier but none the more bigger
 
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  • #2
Main sequence stars don't loose much mass, there is a tiny (by comparison to their size) amount thrown out as the solar wind.
The sun will expand as it enters the red giant phase and will oddly then begin to lose mass - upto 25% of the outer envelope is ejected.
Depending on how much mass is lost the Earth's orbit may increase so that it escapes being swallowed by the larger sun, but either way it is going to get severly roasted.

ps. Our sun is not large enough to supernova, it will expand to a large low density red giant and then a small core will be left as a white dwarf.

As an example of the range of densities, Betelgeuse (the red star at Orion's shoulder) is about 14times the mass of the sun but 650 times the radius, so it has about 275Million times the volume but only 1/20 millionth the density.
 
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  • #3
Excellent; thanks!
 
  • #4
mgb_phys said:
The sun will expand as it enters the red giant phase and will oddly then begin to lose mass - upto 25% of the outer envelope is ejected.

As an example of the range of densities, Betelgeuse (the red star at Orion's shoulder) is about 14times the mass of the sun but 650 times the radius, so it has about 275Million times the volume but only 1/20 millionth the density.

Red Giant Branch and Asymptotic Giant Branch stars are really just small dense fusion cores surrounded by a very BIG atmosphere. The two parts of the star don't mix and the outer layers eventually get blown away. Smaller stars - smaller than the Sun - are more like the cores of bigger stars. For example, a 0.1 Solar mass red-dwarf star is just 0.125 times the size of the Sun, meaning its average density is 51.2 times the Sun's and its surface gravity is 6.4 times stronger.
 

1. What was the relationship between the sun and the earth long long ago?

Long long ago, the sun and the earth had a similar relationship as they do now. The sun was the central source of heat and light for the earth, providing energy for life to exist. However, the earth's orbit around the sun may have been slightly different and the sun may have been slightly dimmer.

2. How did the sun and the earth affect each other's climates in the distant past?

The sun and the earth have always had a complex and dynamic relationship, with the sun's energy and the earth's atmosphere working together to regulate the climate. In the distant past, variations in the sun's energy output and the earth's orbit may have led to periods of warming and cooling on the planet.

3. Did the sun and the earth have any major impacts on each other's evolution?

The sun and the earth have definitely had an impact on each other's evolution. The sun's energy has allowed for the development of life on earth, while the earth's magnetic field has protected the planet from harmful solar radiation. Changes in the sun's energy output and the earth's climate have also influenced the evolution of species on the planet.

4. How has our understanding of the sun and the earth's relationship changed over time?

Our understanding of the sun and the earth's relationship has greatly evolved over time. In ancient times, the sun was often seen as a deity and the earth was thought to be the center of the universe. As our scientific knowledge has grown, we have come to understand the sun and the earth's relationship in a more detailed and accurate way through observations, experiments, and advanced technology.

5. What can studying the sun and the earth's past tell us about their future?

Studying the sun and the earth's past can provide valuable insights into their future. By understanding how they have changed and interacted in the past, we can make predictions about how they may continue to change in the future. This knowledge is crucial for understanding and preparing for potential climate and environmental changes on our planet.

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