Monte Carlo simulation strategies for computing the wetting properties of fluids at geometrically rough surfaces J. Chem. Phys. 135, 184702 (2011) Semi-bottom-up coarse graining of water based on microscopic simulations J. Chem. Phys. 135, 184101 (2011) Hydrophobic interactions in presence of osmolytes urea and trimethylamine-N-oxide J. Chem. Phys. 135, 174501 (2011) Potential of mean force between identical charged nanoparticles immersed in a size-asymmetric monovalent electrolyte J. Chem. Phys. 135, 164705 (2011) Additional information on J. Chem. Phys. The nuclear isotropic shielding constants ͑ 17 O͒ and ͑ 13 C͒ of the carbonyl bond of acetone in water at supercritical ͑P = 340.2 atm and T = 673 K͒ and normal water conditions have been studied theoretically using Monte Carlo simulation and quantum mechanics calculations based on the B3LYP/ 6-311+ + G͑2d ,2p͒ method. Statistically uncorrelated configurations have been obtained from Monte Carlo simulations with unpolarized and in-solution polarized solute. The results show that solvent effects on the shielding constants have a significant contribution of the electrostatic interactions and that quantitative estimates for solvent shifts of shielding constants can be obtained modeling the water molecules by point charges ͑electrostatic embedding͒. In supercritical water, there is a decrease in the magnitude of ͑ 13 C͒ but a sizable increase in the magnitude of ͑ 17 O͒ when compared with the results obtained in normal water. It is found that the influence of the solute polarization is mild in the supercritical regime but it is particularly important for ͑ 17 O͒ in normal water and its shielding effect reflects the increase in the average number of hydrogen bonds between acetone and water. Changing the solvent environment from normal to supercritical water condition, the B3LYP/ 6-311+ + G͑2d ,2p͒ calculations on the statistically uncorrelated configurations sampled from the Monte Carlo simulation give a 13 C chemical shift of 11.7Ϯ 0.6 ppm for polarized acetone in good agreement with the experimentally inferred result of 9 -11 ppm.