ART

In relativity, proper time along a timelike world line is defined as the time as measured by a clock following that line. It is thus independent of coordinates, and is a Lorentz scalar.[1] The proper time interval between two events on a world line is the change in proper time. This interval is the quantity of interest, since proper time itself is fixed only up to an arbitrary additive constant, namely the setting of the clock at some event along the world line.

The proper time interval between two events depends not only on the events but also the world line connecting them, and hence on the motion of the clock between the events. It is expressed as an integral over the world line (analogous to arc length in Euclidean space). An accelerated clock will measure a smaller elapsed time between two events than that measured by a non-accelerated (inertial) clock between the same two events. The twin paradox is an example of this effect.[2]
The dark blue vertical line represents an inertial observer measuring a coordinate time interval t between events E1 and E2. The red curve represents a clock measuring its proper time interval τ between the same two events.

By convention, proper time is usually represented by the Greek letter τ (tau) to distinguish it from coordinate time represented by t. Coordinate time is the time between two events as measured by an observer using that observer's own method of assigning a time to an event. In the special case of an inertial observer in special relativity, the time is measured using the observer's clock and the observer's definition of simultaneity.

The concept of proper time was introduced by Hermann Minkowski in 1908,[3] and is an important feature of Minkowski diagrams.

Mathematical formalism

The formal definition of proper time involves describing the path through spacetime that represents a clock, observer, or test particle, and the metric structure of that spacetime. Proper time is the pseudo-Riemannian arc length of world lines in four-dimensional spacetime. From the mathematical point of view, coordinate time is assumed to be predefined and an expression for proper time as a function of coordinate time is required. On the other hand, proper time is measured experimentally and coordinate time is calculated from the proper time of inertial clocks.

Proper time can only be defined for timelike paths through spacetime which allow for the construction of an accompanying set of physical rulers and clocks. The same formalism for spacelike paths leads to a measurement of proper distance rather than proper time. For lightlike paths, there exists no concept of proper time and it is undefined as the spacetime interval is zero. Instead an arbitrary and physically irrelevant affine parameter unrelated to time must be introduced.[4][5][6][7][8][9]
In special relativity

The Minkowski metric is defined by
\( \eta _{{\mu \nu }}=\left({\begin{matrix}1&0&0&0\\0&-1&0&0\\0&0&-1&0\\0&0&0&-1\end{matrix}}\right), \)

and the coordinates by
\( (x^{0},x^{1},x^{2},x^{3})=(ct,x,y,z) \)

for arbitrary Lorentz frames.

In any such frame an infinitesimal interval, here assumed timelike, between two events is expressed as
\( ds^{2}=c^{2}dt^{2}-dx^{2}-dy^{2}-dz^{2}=\eta _{{\mu \nu }}dx^{\mu }dx^{\nu } \) , (1)

and separates points on a trajectory of a particle (think clock). The same interval can be expressed in coordinates such that at each moment, the particle is at rest. Such a frame is called an instantaneous rest frame, denoted here by the coordinates \( {\displaystyle (c\tau ,x_{\tau },y_{\tau },z_{\tau })} \) for each instants. Due to the invariance of the interval (instantaneous rest frames taken at different times are related by Lorentz transformations) one may write
\( {\displaystyle ds^{2}=c^{2}d\tau ^{2}-dx_{\tau }^{2}-dy_{\tau }^{2}-dz_{\tau }^{2}=c^{2}d\tau ^{2},} \)

since in the instantaneous rest frame, the particle or the frame itself is at rest, i.e., \( {\displaystyle dx_{\tau }=dy_{\tau }=dz_{\tau }=0} \) . Since the interval is assumed timelike (ie. \( {\displaystyle ds^{2}>0}) \) , taking the square root of the above yields[10]
\( ds=cd\tau \) ,

or
\( d\tau ={\frac {ds}{c}}. \)

Given this differential expression for τ, the proper time interval is defined as

\( \Delta \tau =\int _{P}d\tau =\int {\frac {ds}{c}}. \) (2)

Here P is the worldline from some initial event to some final event with the ordering of the events fixed by the requirement that the final event occurs later according to the clock than the initial event.

Using (1) and again the invariance of the interval, one may write[11]

\( {\begin{aligned}\Delta \tau &=\int _{P}{\frac {1}{c}}{\sqrt {\eta _{{\mu \nu }}dx^{\mu }dx^{\nu }}}\\&=\int _{P}{\sqrt {dt^{2}-{dx^{2} \over c^{2}}-{dy^{2} \over c^{2}}-{dz^{2} \over c^{2}}}}\\&=\int {\sqrt {1-{\frac {1}{c^{2}}}\left[\left({\frac {dx}{dt}}\right)^{2}+\left({\frac {dy}{dt}}\right)^{2}+\left({\frac {dz}{dt}}\right)^{2}\right]}}dt\\&=\int {\sqrt {1-{\frac {v(t)^{2}}{c^{2}}}}}dt=\int {\frac {dt}{\gamma (t)}},\end{aligned}} \) (3)

where v(t) is the coordinate speed at coordinate time t, and x(t), y(t), and z(t) are space coordinates. The first expression is manifestly Lorentz invariant. They are all Lorentz invariant, since proper time and proper time intervals are coordinate-independent by definition.

If t, x, y, z, are parameterised by a parameter λ, this can be written as
\( \Delta \tau =\int {\sqrt {\left({\frac {dt}{d\lambda }}\right)^{2}-{\frac {1}{c^{2}}}\left[\left({\frac {dx}{d\lambda }}\right)^{2}+\left({\frac {dy}{d\lambda }}\right)^{2}+\left({\frac {dz}{d\lambda }}\right)^{2}\right]}}\,d\lambda . \)

If the motion of the particle is constant, the expression simplifies to
\( \Delta \tau ={\sqrt {\left(\Delta t\right)^{2}-{\frac {\left(\Delta x\right)^{2}}{c^{2}}}-{\frac {\left(\Delta y\right)^{2}}{c^{2}}}-{\frac {\left(\Delta z\right)^{2}}{c^{2}}}}}, \)

where Δ means the change in coordinates between the initial and final events. The definition in special relativity generalizes straightforwardly to general relativity as follows below.
In general relativity

Proper time is defined in general relativity as follows: Given a pseudo-Riemannian manifold with a local coordinates xμ and equipped with a metric tensor gμν, the proper time interval Δτ between two events along a timelike path P is given by the line integral[12]

\( \Delta \tau =\int _{P}\,d\tau =\int _{P}{\frac {1}{c}}{\sqrt {g_{{\mu \nu }}\;dx^{\mu }\;dx^{\nu }}}. \) (4)

This expression is, as it should be, invariant under coordinate changes. It reduces (in appropriate coordinates) to the expression of special relativity in flat spacetime.

In the same way that coordinates can be chosen such that x1, x2, x3 = const in special relativity, this can be done in general relativity too. Then, in these coordinates,[13]

\( \Delta \tau =\int _{P}d\tau =\int _{P}{\frac {1}{c}}{\sqrt {g_{{00}}}}dx^{0}. \)

This expression generalizes definition (2) and can be taken as the definition. Then using invariance of the interval, equation (4) follows from it in the same way (3) follows from (2), except that here arbitrary coordinate changes are allowed.
Examples in special relativity
Example 1: The twin "paradox"

For a twin paradox scenario, let there be an observer A who moves between the A-coordinates (0,0,0,0) and (10 years, 0, 0, 0) inertially. This means that A stays at x = y = z = 0 {\displaystyle x=y=z=0} x=y=z=0 for 10 years of A-coordinate time. The proper time interval for A between the two events is then
\( {\displaystyle \Delta \tau ={\sqrt {(10{\text{ years}})^{2}}}=10{\text{ years}}.} \)

So being "at rest" in a special relativity coordinate system means that proper time and coordinate time are the same.

Let there now be another observer B who travels in the x direction from (0,0,0,0) for 5 years of A-coordinate time at 0.866c to (5 years, 4.33 light-years, 0, 0). Once there, B accelerates, and travels in the other spatial direction for another 5 years of A-coordinate time to (10 years, 0, 0, 0). For each leg of the trip, the proper time interval can be calculated using A-coordinates, and is given by
\( \Delta \tau ={\sqrt {(5\;{\mathrm {years}})^{2}-(4.33\;{\mathrm {years}})^{2}}}={\sqrt {6.25\;{\mathrm {years}}^{2}}}={\sqrt {6.25\;}}{\mathrm {years}}=2.5\;{\mathrm {years}}.

So the total proper time for observer B to go from (0,0,0,0) to (5 years, 4.33 light-years, 0, 0) and then to (10 years, 0, 0, 0) is 5 years. Thus it is shown that the proper time equation incorporates the time dilation effect. In fact, for an object in a SR spacetime traveling with a velocity of v for a time \( \Delta T \) , the proper time interval experienced is
\( \Delta \tau ={\sqrt {\Delta T^{2}-(v_{x}\Delta T/c)^{2}-(v_{y}\Delta T/c)^{2}-(v_{z}\Delta T/c)^{2}}}=\Delta T{\sqrt {1-v^{2}/c^{2}}}, \)

which is the SR time dilation formula.
Example 2: The rotating disk

An observer rotating around another inertial observer is in an accelerated frame of reference. For such an observer, the incremental ( d τ {\displaystyle d\tau } d\tau ) form of the proper time equation is needed, along with a parameterized description of the path being taken, as shown below.

Let there be an observer C on a disk rotating in the xy plane at a coordinate angular rate of ω {\displaystyle \omega } \omega and who is at a distance of r from the center of the disk with the center of the disk at x=y=z=0. The path of observer C is given by \( (T,\;\,r\cos(\omega T),\;\,r\sin(\omega T),\;\,0) \), where T is the current coordinate time. When r and \( \omega \) are constant, \( dx=-r\omega \sin(\omega T)\;dT \) and \( dy=r\omega \cos(\omega T)\;dT \) . The incremental proper time formula then becomes
\( d\tau ={\sqrt {dT^{2}-(r\omega /c)^{2}\sin ^{2}(\omega T)\;dT^{2}-(r\omega /c)^{2}\cos ^{2}(\omega T)\;dT^{2}}}=dT{\sqrt {1-\left({\frac {r\omega }{c}}\right)^{2}}}. \)

So for an observer rotating at a constant distance of r from a given point in spacetime at a constant angular rate of ω between coordinate times \( T_{1} \) and \( T_{2} \) , the proper time experienced will be
\( {\displaystyle \int _{T_{1}}^{T_{2}}d\tau =(T_{2}-T_{1}){\sqrt {1-\left({\frac {r\omega }{c}}\right)^{2}}}=\Delta T{\sqrt {1-v^{2}/c^{2}}},} \)

as v=rω for a rotating observer. This result is the same as for the linear motion example, and shows the general application of the integral form of the proper time formula.
Examples in general relativity

The difference between SR and general relativity (GR) is that in GR one can use any metric which is a solution of the Einstein field equations, not just the Minkowski metric. Because inertial motion in curved spacetimes lacks the simple expression it has in SR, the line integral form of the proper time equation must always be used.
Example 3: The rotating disk (again)

An appropriate coordinate conversion done against the Minkowski metric creates coordinates where an object on a rotating disk stays in the same spatial coordinate position. The new coordinates are
\( r=\sqrt{x^2 + y^2} \)

and
\( \theta =\arctan \left({\frac {y}{x}}\right)-\omega t. \)

The t and z coordinates remain unchanged. In this new coordinate system, the incremental proper time equation is
\( d\tau ={\sqrt {\left[1-\left({\frac {r\omega }{c}}\right)^{2}\right]dt^{2}-{\frac {dr^{2}}{c^{2}}}-{\frac {r^{2}\,d\theta ^{2}}{c^{2}}}-{\frac {dz^{2}}{c^{2}}}-2{\frac {r^{2}\omega \,dt\,d\theta }{c^{2}}}}}. \)

With r, θ, and z being constant over time, this simplifies to
\( d\tau =dt{\sqrt {1-\left({\frac {r\omega }{c}}\right)^{2}}}, \)

which is the same as in Example 2.

Now let there be an object off of the rotating disk and at inertial rest with respect to the center of the disk and at a distance of R from it. This object has a coordinate motion described by dθ = −ω dt, which describes the inertially at-rest object of counter-rotating in the view of the rotating observer. Now the proper time equation becomes
\( d\tau ={\sqrt {\left[1-\left({\frac {R\omega }{c}}\right)^{2}\right]dt^{2}-\left({\frac {R\omega }{c}}\right)^{2}\,dt^{2}+2\left({\frac {R\omega }{c}}\right)^{2}\,dt^{2}}}=dt. \)

So for the inertial at-rest observer, coordinate time and proper time are once again found to pass at the same rate, as expected and required for the internal self-consistency of relativity theory.[14]
Example 4: The Schwarzschild solution – time on the Earth

The Schwarzschild solution has an incremental proper time equation of
\( d\tau ={\sqrt {\left(1-{\frac {2m}{r}}\right)dt^{2}-{\frac {1}{c^{2}}}\left(1-{\frac {2m}{r}}\right)^{{-1}}dr^{2}-{\frac {r^{2}}{c^{2}}}d\phi ^{2}-{\frac {r^{2}}{c^{2}}}\sin ^{2}(\phi )\,d\theta ^{2}}}, \)

where

t is time as calibrated with a clock distant from and at inertial rest with respect to the Earth,
r is a radial coordinate (which is effectively the distance from the Earth's center),
ɸ is a co-latitudinal coordinate, the angular separation from the north pole in radians.
θ is a longitudinal coordinate, analogous to the longitude on the Earth's surface but independent of the Earth's rotation. This is also given in radians.
1=m is the geometrized mass of the Earth, m = GM/c2,
M is the mass of the Earth,
G is the gravitational constant.

To demonstrate the use of the proper time relationship, several sub-examples involving the Earth will be used here.

For the Earth, M = 5.9742 × 1024 kg, meaning that m = 4.4354 × 10−3 m. When standing on the north pole, we can assume \( dr=d\theta =d\phi =0 \) (meaning that we are neither moving up or down or along the surface of the Earth). In this case, the Schwarzschild solution proper time equation becomes \( d\tau =dt\,{\sqrt {1-2m/r}} \) . Then using the polar radius of the Earth as the radial coordinate (or r=6,356,752 meters), we find that
\( d\tau ={\sqrt {\left(1-1.3908\times 10^{{-9}}\right)\;dt^{2}}}=\left(1-6.9540\times 10^{{-10}}\right)\,dt. \)

At the equator, the radius of the Earth is r = 6,378,137 meters. In addition, the rotation of the Earth needs to be taken into account. This imparts on an observer an angular velocity of \( \ d\theta /dt \) of 2π divided by the sidereal period of the Earth's rotation, 86162.4 seconds. So \( d\theta =7.2923\times 10^{{-5}}\,dt \) . The proper time equation then produces
\( d\tau ={\sqrt {\left(1-1.3908\times 10^{{-9}}\right)dt^{2}-2.4069\times 10^{{-12}}\,dt^{2}}}=\left(1-6.9660\times 10^{{-10}}\right)\,dt. \)

From a non-relativistic point of view this should have been the same as the previous result. This example demonstrates how the proper time equation is used, even though the Earth rotates and hence is not spherically symmetric as assumed by the Schwarzschild solution. To describe the effects of rotation more accurately the Kerr metric may be used.
See also

Lorentz transformation
Minkowski space
Proper length
Proper acceleration
Proper mass
Proper velocity
Clock hypothesis
Peres metric

Footnotes

Zwiebach 2004, p. 25
Hawley, John F.; Holcomb, J Katherine A. (2005). Foundations of Modern Cosmology (illustrated ed.). Oxford University Press. p. 204. ISBN 978-0-19-853096-1. Extract of page 204
Minkowski 1908, pp. 53–111
Lovelock & Rund 1989, pp. 256
Weinberg 1972, pp. 76
Poisson 2004, pp. 7
Landau & Lifshitz 1975, p. 245
Some authors include lightlike intervals in the definition of proper time, and also include the spacelike proper distances as imaginary proper times e.g Lawden 2012, pp. 17, 116
Kopeikin, Efroimsky & Kaplan 2011, p. 275
Zwiebach 2004, p. 25
Foster & Nightingale 1978, p. 56
Foster & Nightingale 1978, p. 57
Landau & Lifshitz 1975, p. 251

Cook 2004, pp. 214–219

References

Cook, R. J. (2004). "Physical time and physical space in general relativity". Am. J. Phys. 72 (2): 214–219. Bibcode:2004AmJPh..72..214C. doi:10.1119/1.1607338. ISSN 0002-9505.
Foster, J.; Nightingale, J.D. (1978). A short course in general relativity. Essex: Longman Scientific and Technical. ISBN 0-582-44194-3.
Kleppner, D.; Kolenkow, R.J. (1978). An introduction to mechanics. McGraw–Hill. ISBN 0-07-035048-5.
Kopeikin, Sergei; Efroimsky, Michael; Kaplan, George (2011). Relativistic Celestial Mechanics of the Solar System. John Wiley & Sons. ISBN 978-3-527-40856-6.
Landau, L. D.; Lifshitz, E. M. (1975). The classical theory of fields. Course of theoretical physics. 2 (4th ed.). Oxford: Butterworth–Heinemann. ISBN 0-7506-2768-9.
Lawden, Derek F. (2012). An Introduction to Tensor Calculus: Relativity and Cosmology. Courier Corporation. ISBN 978-0-486-13214-3.
Lovelock, David; Rund, Hanno (1989), Tensors, Differential Forms, and Variational Principles, New York: Dover Publications, ISBN 0-486-65840-6
Minkowski, Hermann (1908), "Die Grundgleichungen für die elektromagnetischen Vorgänge in bewegten Körpern", Nachrichten von der Königlichen Gesellschaft der Wissenschaften und der Georg-August-Universität zu Göttingen, Göttingen, archived from the original on 2012-07-08
Poisson, Eric (2004), A Relativist's Toolkit: The Mathematics of Black-Hole Mechanics, Cambridge University Press, ISBN 978-0521537803
Weinberg, Steven (1972), Gravitation and Cosmology: Principles and Applications of the General Theory of Relativity, New York: John Wiley & Sons, ISBN 978-0-471-92567-5
Zwiebach, Barton (2004). A First Course in String Theory (first ed.). Cambridge University Press. ISBN 0-521-83143-1.

vte

Time
Key concepts

Past
history deep time Present Future Futures studies Far future in religion Timeline of the far future Eternity Eternity of the world


Wooden hourglass 3.jpg
Measurement
and standards
Chronometry

UTC UT TAI Unit of time Planck time New Earth Time Second Minute Hour Day Week Month Season Year Decade Century Millennium Tropical year Sidereal year Samvatsara

Measurement systems

6-hour clock (Italian) 6-hour clock (Thai) 12-hour clock 24-hour clock Daylight saving time Decimal Hexadecimal Metric Sidereal Solar Time zone

Calendars

Gregorian Julian Hebrew Islamic Lunar Solar Hijri Mayan Intercalation Leap second Leap year

Clocks

Horology History of timekeeping devices Main types
astrarium atomic
quantum hourglass marine sundial sundial markup schema watch
mechanical stopwatch water-based Cuckoo clock Digital clock Grandfather clock

ChronologyHistory

Astronomical chronology Big History Calendar era Chronicle Deep time Periodization Regnal year Timeline

ReligionMythology

Dreamtime Kaal Kalachakra Prophecy Time and fate deities Wheel of time Immortality

Philosophy of time

A series and B series B-theory of time Causality Duration Endurantism Eternal return Eternalism Event Multiple time dimensions Perdurantism Presentism Static interpretation of time Temporal finitism Temporal parts "The Unreality of Time"

Human experience
and use of time

Accounting period Chronemics Fiscal year Generation time Mental chronometry Music Procrastination Punctuality Temporal database Term Time discipline Time management Time perception
Specious present Time-tracking software Time-use research Time-based currency Time value of money Time clock Timesheet Yesterday – Today – Tomorrow

Time in
Geology

Geological time
age chron eon epoch era period Geochronology Geological history of Earth

Physics

Absolute space and time Arrow of time Chronon Coordinate time Imaginary time Planck epoch Planck time Proper time Rate Spacetime Theory of relativity Time dilation
gravitational Time domain Time translation symmetry Time reversal symmetry

Other subject areas

Chronological dating Chronobiology Circadian rhythms Dating methodologies in archaeology Time geography

Related topics

Carpe diem Clock position Space System time Tempus fugit Time capsule Time complexity Time signature Time travel

Category Category Commons page Commons

vte

Time measurement and standards

Chronometry Orders of magnitude Metrology

International standards

Coordinated Universal Time
offset UT ΔT DUT1 International Earth Rotation and Reference Systems Service ISO 31-1 ISO 8601 International Atomic Time 12-hour clock 24-hour clock Barycentric Coordinate Time Barycentric Dynamical Time Civil time Daylight saving time Geocentric Coordinate Time International Date Line Leap second Solar time Terrestrial Time Time zone 180th meridian


WPtimetracer.png
Obsolete standards

Ephemeris time Greenwich Mean Time Prime meridian

Time in physics

Absolute space and time Spacetime Chronon Continuous signal Coordinate time Cosmological decade Discrete time and continuous time Planck time Proper time Theory of relativity Time dilation Gravitational time dilation Time domain Time translation symmetry T-symmetry

Horology

Clock Astrarium Atomic clock Complication History of timekeeping devices Hourglass Marine chronometer Marine sandglass Radio clock Watch
stopwatch Water clock Sundial Dialing scales Equation of time History of sundials Sundial markup schema

Calendar

Astronomical Dominical letter Epact Equinox Gregorian Hebrew Hindu Holocene Intercalation Islamic Julian Leap year Lunar Lunisolar Solar Solstice Tropical year Weekday determination Weekday names

Archaeology and geology

Chronological dating Geologic time scale International Commission on Stratigraphy

Astronomical chronology

Galactic year Nuclear timescale Precession Sidereal time

Other units of time

Flick Shake Jiffy Second Minute Moment Hour Day Week Fortnight Month Year Olympiad Lustrum Decade Century Saeculum Millennium

Related topics

Chronology Duration
music Mental chronometry Decimal time Metric time System time Time metrology Time value of money Timekeeper

Physics Encyclopedia

World

Index

Hellenica World - Scientific Library

Retrieved from "http://en.wikipedia.org/"
All text is available under the terms of the GNU Free Documentation License