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author | Jaron Kent-Dobias <jaron@kent-dobias.com> | 2021-10-25 09:47:59 +0200 |
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committer | Jaron Kent-Dobias <jaron@kent-dobias.com> | 2021-10-25 09:47:59 +0200 |
commit | 9b87a6609ee320e22e11cd7b165fa22eac35fd50 (patch) | |
tree | ff9180f4871118fbaffc96fd07672061d245f350 /ising_scaling.tex | |
parent | 32a3ee96ae4ae5a54b82365491a40edfc2212494 (diff) | |
download | paper-9b87a6609ee320e22e11cd7b165fa22eac35fd50.tar.gz paper-9b87a6609ee320e22e11cd7b165fa22eac35fd50.tar.bz2 paper-9b87a6609ee320e22e11cd7b165fa22eac35fd50.zip |
Writing
Diffstat (limited to 'ising_scaling.tex')
-rw-r--r-- | ising_scaling.tex | 9 |
1 files changed, 5 insertions, 4 deletions
diff --git a/ising_scaling.tex b/ising_scaling.tex index 04cc0eb..cc16cb9 100644 --- a/ising_scaling.tex +++ b/ising_scaling.tex @@ -282,7 +282,7 @@ functions with different asymptotic expansions in different limits, we adopt another coordinate system, in terms of which a scaling function can be defined that has polynomial expansions in \emph{all} limits. -In all dimensions, the Schofield coordinates $R$ and $\theta$ will be implicitly defined by +The Schofield coordinates $R$ and $\theta$ are implicitly defined by \begin{align} \label{eq:schofield} u_t(R, \theta) = R(1-\theta^2) && @@ -701,13 +701,14 @@ accuracy of the fit results can be checked against the known values here. dat = 'data/phi_comparison.dat' set xlabel '$n$' - set ylabel '$|\Delta\mathcal F_0^{(m)}(0)|$' + set xrange [1.5:7.5] + set ylabel '$|\Delta\mathcal F_0^{(m)}(0)|$' set format y '$10^{%T}$' - set style data linespoints set logscale y + + set style data linespoints set key title '\raisebox{0.5em}{$m$}' bottom left - set xrange [1.5:9.5] plot \ dat using 1:2 title '0', \ |