We have used specific heat and neutron diffraction measurements on single crystals of URuFeSi for Fe concentrations 0.7 to establish that chemical substitution of Ru with Fe acts as “chemical pressure” as previously proposed by Kanchanavatee et al. [Phys. Rev. B {\bf 84}, 245122 (2011)] based on bulk measurements on polycrystalline samples. Notably, neutron diffraction reveals a sharp increase of the uranium magnetic moment at , reminiscent of the behavior at the “hidden order” (HO) to large moment antiferromagnetic (LMAFM) phase transition observed at a pressure 0.5-0.7~GPa in URuSi. Using the unit cell volume determined from our measurements and an isothermal compressibility $\kappa_{T} = 5.2 \times 10^{-3}^{-1}22P{ch}{2-x}_x_2x$. The resulting temperature -chemical pressure phase diagram for URuFeSi is in agreement with the established temperature -external pressure phase diagram of URuSi.

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