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Feynman Path Integral Formulation

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1.10 String Theory 41<br />

of the string, provided of course one understands how to formulate the theory in a<br />

consistent and calculable way.<br />

The concept of a relativistic string (see Fig. 1.3) originated in the late sixties in<br />

the context of hadron physics, where it provided a very useful phenomenological<br />

description of certain peculiarities of strong interaction amplitudes. Later on three<br />

main motivations for studying string theories emerged: the search for a description<br />

of quark confinement in terms of gluon strings, a model of grand unification based<br />

on superstrings (Schwarz, 1982), and a description of the three-dimensional Ising<br />

model in terms of some sort of fermionic string (Polyakov, 1979).<br />

One of the first concrete field-theoretic models of a string was given in (Nambu,<br />

1969; Goto, 1971). The usual description introduces world-sheet coordinates σ and<br />

τ, defined on the two-dimensional surface swept out by the time evolution of the<br />

string. When the string is embedded in a d-dimensional space, points on the string<br />

world sheet are assigned coordinates X μ (σ,τ) with μ = 1...d. In analogy with the<br />

action for a relativistic point particle, which is proportional to the proper time, and<br />

therefore to the length of the world line, I = ∫ τ f<br />

τ i<br />

dτ, the simplest action for such a<br />

string is the total area of the world sheet, I = ∫ dA. One can re-write this quantity<br />

by introducing an induced metric g ab on the worldsheet,<br />

∂ X μ ∂ X ν<br />

g ab (σ,τ) =η μν<br />

∂σ a ∂σ b , (1.192)<br />

with σ 1 ≡ τ and σ 2 ≡ σ, and η μν the flat metric in d dimensions. Then the twodimensional<br />

volume element is dA = √ gd 2 σ with g = −det(g ab ), and one has<br />

I =<br />

∫<br />

S<br />

d 2 σ √ g . (1.193)<br />

In a gravity language what one has so far is essentially a cosmological constant term.<br />

In terms of the variables Ẋ = ∂X/∂τ and X ′ = ∂X/∂σ one has<br />

I[X] = 1 √<br />

2πα<br />

∫S<br />

′ d 2 σ (Ẋ · X ′ ) 2 − (Ẋ) 2 (X ′ ) 2 , (1.194)<br />

where a coupling constant α ′ has been introduced, having dimensions of an area,<br />

or of an inverse mass squared. The quantity T 0 = 1/2πα ′ is often referred to for<br />

obvious reasons as the string tension: a string of spatial size R and time extent T will<br />

have an energy per unit length of value T 0 . In the following it will be convenient to<br />

re-absorb such a coupling into a re-definition of the X variables.<br />

One clear distinction that appears early on in this picture is between open (describing<br />

geometrically, in their time evolution, a sheet) and closed strings (described<br />

by a tube). Another important property of the string action is its invariance under<br />

reparametrizations of the world sheet coordinates, X μ (σ,τ) → X μ [ f (σ,τ)]. These<br />

can be considered as two dimensional diffeomorphism acting within the surface;<br />

they express an invariance of the area action under σ a coordinate redefinitions.

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