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Introduction to the mathematics of general relativity

From Wikipedia, the free encyclopedia
(Redirected fromBasic introduction to the mathematics of curved spacetime)

This article is a nontechnical introduction to the subject. For the main encyclopedia article, seeMathematics of general relativity.
General relativity
Spacetime curvature schematic

Themathematics of general relativity is complicated. InNewton's theories of motion, an object's length and the rate at which time passes remain constant while the objectaccelerates, meaning that many problems inNewtonian mechanics may be solved byalgebra alone. Inrelativity, however, an object's length and the rate at which time passes both change appreciably as the object's speed approaches thespeed of light, meaning that more variables and more complicated mathematics are required to calculate the object's motion. As a result, relativity requires the use of concepts such asvectors,tensors,pseudotensors andcurvilinear coordinates.

For an introduction based on the example of particles followingcircular orbits about a large mass, nonrelativistic and relativistic treatments are given in, respectively,Newtonian motivations for general relativity andTheoretical motivation for general relativity.

Vectors and tensors

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Main articles:Euclidean vector andTensor

Vectors

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Illustration of a typical vector

Inmathematics,physics, andengineering, aEuclidean vector (sometimes called ageometric vector[1] orspatial vector,[2] or – as here – simply a vector) is a geometric object that has both amagnitude (orlength) and direction. A vector is what is needed to "carry" the pointA to the pointB; the Latin wordvector means "one who carries".[3] The magnitude of the vector is the distance between the two points and the direction refers to the direction of displacement fromA toB. Manyalgebraic operations onreal numbers such asaddition,subtraction,multiplication, andnegation have close analogues for vectors, operations which obey the familiar algebraic laws ofcommutativity,associativity, anddistributivity.

Tensors

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Stress is a second-order tensor that represents the response of a material to force applied at an angle. The two directions of the tensor represent the "normal" (at right angles to the surface) force, and "shear" (parallel to the surface) force.

A tensor extends the concept of a vector to additional directions. Ascalar, that is, a simple number without a direction, would be shown on a graph as a point, a zero-dimensional object. A vector, which has a magnitude and direction, would appear on a graph as a line, which is a one-dimensional object. A vector is a first-order tensor, since it holds one direction.A second-order tensor has two magnitudes and two directions, and would appear on a graph as two lines similar to the hands of a clock. The "order" of a tensor is the number of directions contained within, which is separate from the dimensions of the individual directions. A second-order tensor in two dimensions might be represented mathematically by a 2-by-2 matrix, and in three dimensions by a 3-by-3 matrix, but in both cases the matrix is "square" for a second-order tensor. A third-order tensor has three magnitudes and directions, and would be represented by a cube of numbers, 3-by-3-by-3 for directions in three dimensions, and so on.

Applications

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Vectors are fundamental in the physical sciences. They can be used to represent any quantity that has both a magnitude and direction, such asvelocity, the magnitude of which isspeed. For example, the velocity5 meters per second upward could be represented by the vector(0, 5) (in 2 dimensions with the positivey axis as 'up'). Another quantity represented by a vector isforce, since it has a magnitude and direction. Vectors also describe many other physical quantities, such asdisplacement,acceleration,momentum, andangular momentum. Other physical vectors, such as theelectric andmagnetic field, are represented as a system of vectors at each point of a physical space; that is, avector field.

Tensors also have extensive applications in physics:

Dimensions

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In general relativity, four-dimensional vectors, orfour-vectors, are required. These four dimensions are length, height, width and time. A "point" in this context would be an event, as it has both a location and a time. Similar to vectors, tensors in relativity require four dimensions. One example is theRiemann curvature tensor.

Coordinate transformation

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  • A vector v, is shown with two coordinate grids, ex and er. In space, there is no clear coordinate grid to use. This means that the coordinate system changes based on the location and orientation of the observer. Observer ex and er in this image are facing different directions.
    A vectorv, is shown with two coordinate grids,ex ander. In space, there is no clear coordinate grid to use. This means that the coordinate system changes based on the location and orientation of the observer. Observerex ander in this image are facing different directions.
  • Here we see that ex and er see the vector differently. The direction of the vector is the same. But to ex, the vector is moving to its left. To er, the vector is moving to its right.
    Here we see thatex ander see the vector differently. The direction of the vector is the same. But toex, the vector is moving to its left. Toer, the vector is moving to its right.

In physics, as well as mathematics, a vector is often identified with atuple, or list of numbers, which depend on a coordinate system orreference frame. If the coordinates are transformed, such as by rotation or stretching the coordinate system, the components of the vector also transform. The vector itself does not change, but the reference frame does. This means that the components of the vector have to change to compensate.

The vector is calledcovariant orcontravariant depending on how the transformation of the vector's components is related to the transformation of coordinates.

  • Contravariant vectors have units of distance (such as a displacement) or distance times some other unit (such as velocity or acceleration) and transform in the opposite way as the coordinate system. For example, in changing units from meters to millimeters the coordinate units get smaller, but the numbers in a vector become larger: 1 m becomes 1000 mm.
  • Covariant vectors, on the other hand, have units of one-over-distance (as in agradient) and transform in the same way as the coordinate system. For example, in changing from meters to millimeters, the coordinate units become smaller and the number measuring a gradient will also become smaller: 1 Kelvin per m becomes 0.001 Kelvin per mm.

InEinstein notation, contravariant vectors and components of tensors are shown with superscripts, e.g.xi, and covariant vectors and components of tensors with subscripts, e.g.xi. Indices are "raised" or "lowered" by multiplication by an appropriate matrix, often the identity matrix.

Coordinate transformation is important because relativity states that there is not one reference point (or perspective) in the universe that is more favored than another. On earth, we use dimensions like north, east, and elevation, which are used throughout the entire planet. There is no such system for space. Without a clear reference grid, it becomes more accurate to describe the four dimensions as towards/away, left/right, up/down and past/future. As an example event, assume that Earth is a motionless object, and consider the signing of theDeclaration of Independence. To a modern observer onMount Rainier looking east, the event is ahead, to the right, below, and in the past. However, to an observer in medieval England looking north, the event is behind, to the left, neither up nor down, and in the future. The event itself has not changed: the location of the observer has.

Oblique axes

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Anoblique coordinate system is one in which the axes are not necessarilyorthogonal to each other; that is, they meet at angles other thanright angles. When using coordinate transformations as described above, the new coordinate system will often appear to have oblique axes compared to the old system.

Nontensors

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See also:Pseudotensor

A nontensor is a tensor-like quantity that behaves like a tensor in the raising and lowering of indices, but that does not transform like a tensor under a coordinate transformation. For example,Christoffel symbols cannot be tensors themselves if the coordinates do not change in a linear way.

In general relativity, one cannot describe the energy and momentum of the gravitational field by an energy–momentum tensor. Instead, one introduces objects that behave as tensors only with respect to restricted coordinate transformations. Strictly speaking, such objects are not tensors at all. A famous example of such a pseudotensor is theLandau–Lifshitz pseudotensor.

Curvilinear coordinates and curved spacetime

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High-precision test of general relativity by theCassini space probe (artist's impression): radio signals sent between the Earth and the probe (green wave) aredelayed by the warping ofspace and time (blue lines) due to theSun's mass. That is, the Sun's mass causes the regular grid coordinate system (in blue) to distort and have curvature. The radio wave then follows this curvature and moves toward the Sun.

Curvilinear coordinates are coordinates in which the angles between axes can change from point to point. This means that rather than having a grid of straight lines, the grid instead has curvature.

A good example of this is the surface of the Earth. While maps frequently portray north, south, east and west as a simple square grid, that is not in fact the case. Instead, the longitude lines running north and south are curved and meet at the north pole. This is because the Earth is not flat, but instead round.

In general relativity, energy and mass have curvature effects on the four dimensions of the universe (= spacetime). This curvature gives rise to the gravitational force. A common analogy is placing a heavy object on a stretched out rubber sheet, causing the sheet to bend downward. This curves the coordinate system around the object, much like an object in the universe curves the coordinate system it sits in. The mathematics here are conceptually more complex than on Earth, as it results infour dimensions of curved coordinates instead of three as used to describe a curved 2D surface.

Parallel transport

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Main article:Parallel transport
Example: Parallel displacement along a circle of a three-dimensional ball embedded in two dimensions. The circle of radiusr is embedded in a two-dimensional space characterized by the coordinatesz1 andz2. The circle itself is characterized by coordinatesy1 andy2 in the two-dimensional space. The circle itself is one-dimensional and can be characterized by its arc lengthx. The coordinatey is related to the coordinatex through the relationy1 =r cosx/r andy2 =r sinx/r. This givesy1/x = −sinx/r andy2/x = cosx/r In this case the metric is a scalar and is given byg = cos2x/r + sin2x/r = 1. The interval is thends2 =g dx2 =dx2. The interval is just equal to the arc length as expected.

The interval in a high-dimensional space

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In aEuclidean space, the separation between two points is measured by the distance between the two points. The distance is purely spatial, and is always positive. In spacetime, the separation between two events is measured by theinvariant interval between the two events, which takes into account not only the spatial separation between the events, but also their separation in time. The interval,s2, between two events is defined as:

s2=Δr2c2Δt2{\displaystyle s^{2}=\Delta r^{2}-c^{2}\Delta t^{2}\,}     (spacetime interval),

wherec is the speed of light, andΔr andΔt denote differences of the space and time coordinates, respectively, between the events. The choice of signs fors2 above follows thespace-like convention (−+++). A notation likeΔr2 meansr)2. The reasons2 and nots is called the interval is thats2 can be positive, zero or negative.

Spacetime intervals may be classified into three distinct types, based on whether the temporal separation (c2Δt2) or the spatial separation (Δr2) of the two events is greater: time-like, light-like or space-like.

Certain types ofworld lines are calledgeodesics of the spacetime – straight lines in the case of flat Minkowski spacetime and their closest equivalent in the curved spacetime of general relativity. In the case of purely time-like paths, geodesics are (locally) the paths of greatest separation (spacetime interval) as measured along the path between two events, whereas in Euclidean space and Riemannian manifolds, geodesics are paths of shortest distance between two points.[4][5] The concept of geodesics becomes central ingeneral relativity, since geodesic motion may be thought of as "pure motion" (inertial motion) in spacetime, that is, free from any external influences.

The covariant derivative

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Main article:Covariant derivative

The covariant derivative is a generalization of the directional derivative from vector calculus. As with the directional derivative, the covariant derivative is a rule, which takes as its inputs: (1) a vector,u, (along which the derivative is taken) defined at a pointP, and (2) a vector field,v, defined in a neighborhood ofP. The output is a vector, also at the pointP. The primary difference from the usual directional derivative is that the covariant derivative must, in a certain precise sense, be independent of the manner in which it is expressed in a coordinate system.

Parallel transport

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Given the covariant derivative, one can define theparallel transport of a vectorv at a pointP along a curveγ starting atP. For each pointx ofγ, the parallel transport ofv atx will be a function ofx, and can be written asv(x), wherev(0) =v. The functionv is determined by the requirement that the covariant derivative ofv(x) alongγ is 0. This is similar to the fact that a constant function is one whose derivative is constantly 0.

Christoffel symbols

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Main article:Christoffel symbols

The equation for the covariant derivative can be written in terms of Christoffel symbols. The Christoffel symbols find frequent use in Einstein's theory ofgeneral relativity, wherespacetime is represented by a curved 4-dimensionalLorentz manifold with aLevi-Civita connection. TheEinstein field equations – which determine the geometry of spacetime in the presence of matter – contain theRicci tensor. Since the Ricci tensor is derived from the Riemann curvature tensor, which can be written in terms of Christoffel symbols, a calculation of the Christoffel symbols is essential. Once the geometry is determined, the paths of particles and light beams are calculated bysolving the geodesic equations in which the Christoffel symbols explicitly appear.

Geodesics

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Main article:Geodesics in general relativity

Ingeneral relativity, ageodesic generalizes the notion of a "straight line" to curvedspacetime. Importantly, theworld line of a particle free from all external, non-gravitational force, is a particular type of geodesic. In other words, a freely moving or falling particle always moves along a geodesic.

In general relativity, gravity can be regarded as not a force but a consequence of a curved spacetime geometry where the source of curvature is thestress–energy tensor (representing matter, for instance). Thus, for example, the path of a planet orbiting around a star is the projection of a geodesic of the curved 4-dimensional spacetime geometry around the star onto 3-dimensional space.

A curve is a geodesic if thetangent vector of the curve at any point is equal to theparallel transport of thetangent vector of the base point.

Curvature tensor

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Main article:Riemann curvature tensor

TheRiemann curvature tensorRρσμν tells us, mathematically, how much curvature there is in any given region of space. In flat space this tensor is zero.

Contracting the tensor produces 2 more mathematical objects:

  1. TheRicci tensor:Rσν, comes from the need in Einstein's theory for a curvature tensor with only 2 indices. It is obtained by averaging certain portions of the Riemann curvature tensor.
  2. Thescalar curvature:R, the simplest measure of curvature, assigns a single scalar value to each point in a space. It is obtained by averaging the Ricci tensor.

The Riemann curvature tensor can be expressed in terms of the covariant derivative.

The Einstein tensorG is a rank-2tensor defined overpseudo-Riemannian manifolds. In index-free notation it is defined as

G=R12gR,{\displaystyle \mathbf {G} =\mathbf {R} -{\tfrac {1}{2}}\mathbf {g} R,}

whereR is theRicci tensor,g is themetric tensor andR is thescalar curvature. It is used in theEinstein field equations.

Stress–energy tensor

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Main article:Stress–energy tensor
Contravariant components of the stress–energy tensor

Thestress–energy tensor (sometimesstress–energy–momentum tensor orenergy–momentum tensor) is atensor quantity inphysics that describes thedensity andflux ofenergy andmomentum inspacetime, generalizing thestress tensor of Newtonian physics. It is an attribute ofmatter,radiation, and non-gravitationalforce fields. The stress–energy tensor is the source of thegravitational field in theEinstein field equations ofgeneral relativity, just as mass density is the source of such a field inNewtonian gravity. Because this tensor has 2 indices (see next section) the Riemann curvature tensor has to be contracted into the Ricci tensor, also with 2 indices.

Einstein equation

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Main article:Einstein field equations

TheEinstein field equations (EFE) orEinstein's equations are a set of 10equations inAlbert Einstein'sgeneral theory of relativity which describe thefundamental interaction ofgravitation as a result ofspacetime beingcurved bymatter andenergy.[6] First published by Einstein in 1915[7] as atensor equation, the EFE equate local spacetimecurvature (expressed by theEinstein tensor) with the local energy andmomentum within that spacetime (expressed by thestress–energy tensor).[8]

The Einstein field equations can be written as

Gμν=8πGc4Tμν,{\displaystyle G_{\mu \nu }={8\pi G \over c^{4}}T_{\mu \nu },}

whereGμν is theEinstein tensor andTμν is thestress–energy tensor.

This implies that the curvature of space (represented by the Einstein tensor) is directly connected to the presence of matter and energy (represented by the stress–energy tensor).

Schwarzschild solution and black holes

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Main article:Schwarzschild metric

InEinstein's theory ofgeneral relativity, theSchwarzschild metric (alsoSchwarzschild vacuum orSchwarzschild solution), is a solution to theEinstein field equations which describes thegravitational field outside a spherical mass, on the assumption that theelectric charge of the mass, theangular momentum of the mass, and the universalcosmological constant are all zero. The solution is a useful approximation for describing slowly rotating astronomical objects such as manystars andplanets, including Earth and the Sun. The solution is named afterKarl Schwarzschild, who first published the solution in 1916, just before his death.

According toBirkhoff's theorem, the Schwarzschild metric is the most generalspherically symmetric,vacuum solution of theEinstein field equations. ASchwarzschild black hole orstatic black hole is ablack hole that has nocharge orangular momentum. A Schwarzschild black hole is described by the Schwarzschild metric, and cannot be distinguished from any other Schwarzschild black hole except by its mass.

See also

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Notes

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  1. ^Ivanov 2001
  2. ^Heinbockel 2001
  3. ^From Latinvectus,perfect participle ofvehere, "to carry". For historical development of the wordvector, see"vectorn.".Oxford English Dictionary (Online ed.). Oxford University Press. (Subscription orparticipating institution membership required.) andJeff Miller."Earliest Known Uses of Some of the Words of Mathematics". Retrieved2007-05-25.
  4. ^This characterization is not universal: both the arcs between two points of agreat circle on a sphere are geodesics.
  5. ^Berry, Michael V. (1989).Principles of Cosmology and Gravitation.CRC Press. p. 58.ISBN 0-85274-037-9.
  6. ^Einstein, Albert (1916)."The Foundation of the General Theory of Relativity".Annalen der Physik.354 (7): 769.Bibcode:1916AnP...354..769E.doi:10.1002/andp.19163540702. Archived fromthe original(PDF) on 2006-08-29.
  7. ^Einstein, Albert (November 25, 1915)."Die Feldgleichungen der Gravitation".Sitzungsberichte der Preussischen Akademie der Wissenschaften zu Berlin:844–847. Retrieved2006-09-12.
  8. ^Misner, Charles W.;Thorne, Kip S.;Wheeler, John Archibald (1973).Gravitation. San Francisco:W. H. Freeman.ISBN 978-0-7167-0344-0. Chapter 34, p 916

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