Geodesic
Critical phenomena in deep inelastic scattering
Informatics and Automation, Problems of modern theoretical and mathematical physics: Gauge theories and superstrings, Tome 272 (2011), pp. 162-169.

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Saturation in deep inelastic scattering (DIS) and deeply virtual Compton scattering is associated with a phase transition between the partonic gas, typical of moderate $x$ and $Q^2$, and a partonic fluid (liquid), appearing at increasing $Q^2$ and decreasing Bjorken $x$. In the statistical interpretation of DIS, the large-$x$, $(1-x)^n$ factor in the structure functions is associated with a statistical distribution (perfect gas), while the low-$x$, Regge behaved factor $x^{b(Q^2)}$ introduces deviation from the perfect gas and ultimately leads to a gas-liquid phase transition. 
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L. Jenkovszky; S. Troshin; N. Tyurin. Critical phenomena in deep inelastic scattering. Informatics and Automation, Problems of modern theoretical and mathematical physics: Gauge theories and superstrings, Tome 272 (2011), pp. 162-169. http://geodesic.mathdoc.fr/item/TRSPY_2011_272_a12/

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