In [
17] the claim was made that, upon using an isotropic helium–carbon potential in model (
1), one could observe a (metastable) superfluid phase at coverage below
θ0, typically by introducing a few vacancies, or by reducing the
4He coverage to approximately 0.058 Å
−2. Our study yielded no evidence of any low-coverage superfluid liquid phase. Specifically, our simulations at coverage
θ ≤
θ0 unambiguously show crystalline order, consistently with the coexistence of a crystal (of coverage
θ0) and vapor, which is in agreement with the findings of [
18]. The claim of a liquidlike phase of [
17] is based on the observation of a sudden drop of the peak of the static structure factor, on lowering the coverage from
θ0 to approximately 0.9
θ0, and from the visual inspection of the configuration generated in the course of a Monte Carlo simulation, suggesting loss of local crystalline order at the lower coverage. On the other hand, if an anisotropic pair potential is utilized the static structure factor does not drop as significantly, and local crystalline order is retained. The results of our simulations show that, while, on the one hand, the anisotropic potential can plausibly be more effective at ‘pinning’ helium atoms in place than the isotropic one, the main physical behavior is actually unchanged in the case of an isotropic potential. Figure
3 shows a comparison of the static structure factor computed at
T = 1 K (the main results and observations do not change at lower temperatures, down to the lowest considered here, namely
T = 0.25 K) for the case of coverage
θ0 (circles) and
θ = 0.0577 Å
−2 (diamonds). The peak of
S(
q) is lower at the lower coverage (though the difference is nowhere near as large as that reported in [
17]), but this is insufficient to conclude that no crystalline order is present at the lower coverage. For example, the calculation of [
17] at coverage
θ0 yields a ∼50% higher peak of
S(
q) if an anisotropic He–C pair potential is used, but in both cases the crystalline character of the monolayer is not in question. Furthermore, although indeed the main peak is depressed by approximately a third (left part of figure
3), nevertheless it remains relatively sharp, suggesting that crystalline order is largely retained, as confirmed by snapshots of instantaneous many-particle world line configurations (right part of figure
3).