Metric tensor at the earth surface

In summary, the Schwarzschild metric is a vacuum solution that is valid for the exterior of the Earth, resulting in a vanishing Ricci tensor and scalar. However, inside the Earth, the Ricci tensor is non-zero due to the presence of matter. The Weyl curvature tensor describes the curvature in vacuum regions and is non-zero, providing a better understanding of the curvature caused by the mass of the Earth.
  • #1
tm007
3
0
I want to find the ricci tensor and ricci scalar for the space-time curvature at the Earth surface. Ignoring the moon and the sun. I have used the scwharzschilds metric, but then the ricci tensor and the scalar where equal to zero.
 
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  • #2
The Schwarzschild metric is a vacuum solution so of course the Ricci tensor and Ricci scalar will vanish. The Schwarzschild metric is valid for the exterior of the Earth, ignoring the Earth's rotation and the presence of the other celestial bodies.
 
  • #3
The Kretschmann scalar is non-zero M2/r6
 
  • #4
Another thing you could look at is the Weyl curvature tensor. This specifically describes the type of curvature in vacuum regions in GR. Unfortunately, it is really hard to compute by hand, even for a metric as simple as the Scwharzschild.
 
  • #5
The mass of the Earth should curve the space surounding the Earth. Why is then the ricci tensor equal to zero.
 
  • #6
Outside the Earth, there is a vacuum, so Ricci is zero. Inside the Earth, Ricci is non-zero. A somewhat crude model takes the Earth as a constant density, non-rotating sphere. Then, Schwarzschild's interior solution can be used. When [itex]G=c=1[/itex],

[tex]
ds^{2}=\left( \frac{3}{2}\sqrt{1-\frac{2M}{R}}-\frac{1}{2}\sqrt{1-\frac{2Mr^{2}}{R^{3}}}\right) ^{2}dt^{2}-\left( 1-\frac{2Mr^{2}}{R^{3}}\right) ^{-1}dr^{2}-r^{2}\left( d\theta ^{2}+\sin ^{2}\theta d\phi ^{2}\right),
[/tex]

where [itex]R[/itex] is the [itex]r[/itex] coordinate at the surface of the Earth.

This metric is treated in many relativity texts, e.g., texts by Schutz, by Hobson, Efstathiou, Lasenby, and by Misner, Thorne, Wheeler.
 
  • #7
tm007 said:
The mass of the Earth should curve the space surounding the Earth.

It does, but the curvature produced in the vacuum region around the Earth is Weyl curvature, not Ricci curvature.
 
  • #8
tm007 said:
The mass of the Earth should curve the space surounding the Earth. Why is then the ricci tensor equal to zero.
Spacetime is curved, that's why several curvature invariants and Weyl curvature are non-zero, whereas Ricci-curvature is zero
 
  • #9
tm007 said:
The mass of the Earth should curve the space surounding the Earth. Why is then the ricci tensor equal to zero.

Keep in mind that different curvature tensors measure different kinds of curvature; the Weyl curvature is the trace free part of the Riemann curvature and will not vanish in general for vacuum solutions whereas the Ricci tensor always vanishes for vacuum solutions. However you can always rely on the Riemann curvature tensor because this can vanish identically if and only if the manifold is locally isometric to euclidean space (which is of course flat).

Both the Ricci and Weyl curvatures can be made sense of physically in GR by looking at geodesic congruences and seeing which of the three kinematical quantities (expansion, shear, and twist) are dominated by which curvature quantity. See here for a start: http://en.wikipedia.org/wiki/Weyl_tensor
 

1. What is the metric tensor at the earth surface?

The metric tensor at the earth surface is a mathematical quantity that describes the local geometry of the earth's surface. It is used in the study of general relativity and is essential for understanding the curvature of spacetime near the earth's surface.

2. How is the metric tensor at the earth surface calculated?

The metric tensor at the earth surface is calculated using a combination of mathematical equations and physical measurements. The equations take into account factors such as the earth's mass and rotation, as well as the distribution of matter on its surface. Physical measurements, such as the gravitational field and curvature of spacetime, are also used to calculate the metric tensor.

3. Why is the metric tensor important at the earth surface?

The metric tensor at the earth surface is important because it helps us understand the structure of spacetime around the earth. It is also crucial for predicting the behavior of objects near the earth's surface, such as satellites and spacecraft. Additionally, the metric tensor is used in the development of accurate GPS systems and other geodetic applications.

4. How does the metric tensor at the earth surface differ from other locations in the universe?

The metric tensor at the earth surface may differ from other locations in the universe due to variations in factors such as mass distribution, rotation, and gravitational forces. This means that the geometry of spacetime near the earth's surface may differ from that at other locations, leading to different values for the metric tensor.

5. Can the metric tensor at the earth surface change over time?

Yes, the metric tensor at the earth surface can change over time due to factors such as tectonic plate movements, changes in the earth's mass distribution, and fluctuations in its rotation. These changes can lead to variations in the curvature of spacetime near the earth's surface, resulting in a different metric tensor value.

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