Abstract

Two topics in soft collinear effective theory (SCET) for gravitational interactions are explored. First, the collinear Wilson lines---necessary building blocks for maintaining multiple copies of diffeomorphism invariance in gravity SCET---are extended to all orders in the SCET expansion parameter $\ensuremath{\lambda}$, where it has only been known to $O(\ensuremath{\lambda})$ in the literature. Second, implications of reparametrization invariance (RPI) for the structure of gravity SCET Lagrangians are studied. The utility of RPI is illustrated by an explicit example in which $O({\ensuremath{\lambda}}^{2})$ hard interactions of a collinear graviton are completely predicted by RPI from its $O(\ensuremath{\lambda})$ hard interactions. It is also pointed out that the multiple diffeomorphism invariances and RPI together require certain relations among $O(\ensuremath{\lambda})$ terms, thereby reducing the number of $O(\ensuremath{\lambda})$ terms that need to be fixed by matching onto the full theory in the first place.

Highlights

  • In this note, we extend the discussions of soft collinear effective theory (SCET) for gravity presented in [1]

  • This is a necessary ingredient in gravity SCET as the hard interaction, Lhard, in the effective Lagrangian must be invariant under collinear diff gauge groups

  • We discussed reparametrization invariance (RPI) and illustrated how RPI can significantly constrain the structure of the effective Lagrangian by working out an example in which Oðλ2Þ interactions in Lhard are completely fixed by RPI from given OðλÞ interactions

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Summary

INTRODUCTION

We extend the discussions of soft collinear effective theory (SCET) for gravity presented in [1]. As in QCD SCET, the nth collinear sector is most conveniently described in terms of the nth light cone coordinates, which is defined such that the components of a collinear momentum q in this sector should scale in λ as ðqþn ; q−n ; qin Þ 1⁄4 ðq−n ; qþn ; −qin Þ ∼ ðλ0; λ2; λÞ; ð2Þ with in 1⁄4 1n, 2n referring to the two spatial directions orthogonal to the jet axis of the nth collinear sector. We will illustrate the utility of RPI in gravity SCET by deriving all Oðλ2Þ operators from OðλÞ operators in Lhard for the scattering of two scalars into two scalars plus a collinear graviton at tree level

COLLINEAR DIFF WILSON LINES TO ALL ORDERS
REPARAMETRIZATION INVARIANCE
SUMMARY AND DISCUSSIONS
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