The hotter part of the fluid becomes less dense and rises to the top.
Where as the colder part of the fluid will be more dense and will sink to the bottom.
the fluid rises
the fluid rises
The hotter part of the fluid becomes less dense and rises to the top. Where as the colder part of the fluid will be more dense and will sink to the bottom.
When the density of a fluid gets hotter, it usually decreases. This is because as the fluid gets hotter, its molecules gain energy and move farther apart, causing the fluid to expand. This expansion leads to a decrease in density.
As a fluid gets hotter, its density generally decreases. This is because heat causes the fluid molecules to move faster and spread out, leading to decreased packing and therefore lower density. This relationship is known as thermal expansion.
The density of a fluid goes down (becomes less dense) when heat is applied.
When the density of a fluid increases due to heating, the molecules within the fluid move faster and spread further apart, causing the fluid to expand. This expansion leads to a decrease in density, as the same mass now occupies a larger volume.
When the mantle gets hotter, it becomes more fluid and less viscous, causing it to flow more easily. This increased flow can lead to the movement of tectonic plates and the creation of volcanic activity as magma rises to the surface. Additionally, higher temperatures in the mantle can affect the density of the material and impact convection currents within the Earth's interior.
If the low density water was put over another fluid of lower density it would sink but if it was put over a high density fluid like Mercury it would floats.
When pressure in a fluid changes, the volume and density of the fluid may also change. If the pressure increases, the volume decreases and the density increases, leading to compression of the fluid. Conversely, if the pressure decreases, the volume increases and the density decreases, causing expansion of the fluid.
sulphuric acid
deep