Can an Iron Ball Find Equilibrium in Deep Desert Sand?

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Discussion Overview

The discussion explores whether an iron ball can find an equilibrium level when placed in deep desert sand, considering factors like density, perturbations, and the nature of sand as a material. The scope includes theoretical reasoning and conceptual clarification regarding the behavior of the ball in a non-ideal medium.

Discussion Character

  • Exploratory
  • Technical explanation
  • Debate/contested

Main Points Raised

  • Some participants propose that the iron ball will sink until its density equals that of the surrounding material, assuming the sand behaves like a fluid.
  • Others argue that the sand is not an ideal fluid and question the implications of this on the ball's sinking behavior.
  • One participant suggests that if the sand's density increases with depth, the ball will stop sinking when it reaches a depth where the sand's density matches its own.
  • Another participant emphasizes that the nature of sand, including factors like air and water between grains, complicates the fluid analogy.
  • Some participants discuss the concept of liquefaction and how it might affect the behavior of the sand under the ball.
  • There is a contention about whether sand can be accurately described as a fluid, with some asserting it can be treated as such for the purposes of this discussion.
  • One participant highlights the differences between forces acting in fluids versus those in granular materials, suggesting that a fluid model may not suffice for long-term studies.

Areas of Agreement / Disagreement

Participants express differing views on the nature of sand and its behavior under the weight of the iron ball, leading to multiple competing perspectives without a clear consensus on the model to apply.

Contextual Notes

Limitations include assumptions about the density of sand, the treatment of sand as a fluid, and the effects of external perturbations on the system. The discussion does not resolve these complexities.

mersecske
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Let assume a desert with very deep sand
and an iron ball on the ground level.
Due to small perturbations (wind, small earthquakes, etc.)
the iron ball will sinking down.
Is there an equilibrium level,
or the iron ball will sink down to "negative infinity level"?
 
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The ball will (in an ideal system) sink to the point where it's density is equal to the density of the rock around it.
The density of the Earth's liquid outer Core is around 10-12 g/cc
Iron has a density of around 7.8 g/cc so will sink to this level
 
I don't know if you mean the sand is "deep" enough that you consider it infinite, since I can't imagine you are referring to the centre of the Earth when you say "negative infinity".The ball should fall until its density is equal to the density of the sand around it, as long as you treat the sand as a fluid. I don't know if an earthquake will move a grain of sand once it becomes so deep that there is 1 metric tonne of sand directly above it.
 
But it is not an ideal fluid.
 
No one said anything about an ideal fluid. For the purposes of this problem, sand can be considered as a fluid. Now, if you were to drop something in water, which is only very slightly compressible and so has the same density "all the way down", if you drop an object into water, one of three things can happen. If the density of the object is less than the density of water, it will float on top of the water. If the density of the object is greater than the density of water, it will sink to the bottom. If the density of the object is exactly the same as the density of water, it will float at a height determined by other things (the force with which it hit the water when it was dropped for example).

Now, if you are assuming that your "sand" always has the same density, then the object will sink all the way to the bottom of the sand (to the center of the Earth if the sand goes that far). If you are assuming that the "sand" increases in density as you go deeper, then the object will sink until the density of the "sand" around it is equal to its density as NobodySpecial said.
 
But it is not fluid.
And I think that density can change in homogeneous gravitational field.
 
maybe "granular fluid" but its only notation
 
We aren't saying sand is a fluid, we are describing it as one. The particles of sand react in a similar way to the molecules in a fluid.

You are just nit-picking over semantics.
 
Last edited:
  • #10
jarednjames said:
We aren't saying sand is a fluid, we are describing it as one. The particles of sand react in a similar way to the molecules in a fluid.

I don't think so. Between sand grain there is air and also water can enter into the material.
And also in fluids between molecules there are volume forces, but in sand there are only surface forces I think. Maybe fluid model is a good assumption, but in this situation when we want to study long time scale, i think its not enough.
 

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