We determine the nuclear quadrupole moment Q of the most important Mossbauer nucleus Fe by comparing experimental quadrupole splittings with calculated electric field gradients (EFG) for a large number of different Fe compounds. These ab initio calculations are based on the linearized-augmented plane-wave band structure method. From the slope of the linear correlation between theoretical EFGs and experimental quadrupole splittings a new value of Q( 7Fe) = 0.16 b is deduced, twice as large as previously suggested.Our results should also stimulate nuclear physicists to revise nuclear structure shell model calculations of Q. PACS numbers: 76.80.+y, 71.25.pi, 71.25.TnMossbauer spectroscopy and other hyperfine interaction measurements such as nuclear magnetic resonance (NMR), nuclear quadrupole resonance (NQR), or perturbed angular correlation (PAC) are widely used experimental techniques that provide local information on the interaction of a nucleus with the surrounding electronic charge distribution.An interpretation of such measurements can lead to a detailed knowledge of the electronic and magnetic structure in a solid. One of the measured quantities, namely, the quadrupole splitting 50, is proportional to the product (of the principal component Vzz) of the electric field gradient (EFG) times the nuclear quadrupole moment Q. Since the EFG is directly related to the asphericity of the electron density in the vicinity of the probe nucleus, the quadrupole splittings allow the estimation of covalency or ionicity of chemical bonds in solids, provided Q is known.Although Q is a purely nuclear quantity, for some isotopes these quadrupole moments are not well known. The method presented in this Letter to determine Q(s7Fe) can also be applied to other nuclei and therefore has large implications on all the experimental techniques mentioned above. In addition, it can be used as reference for other methods determining Q, e.g. , nuclear structure shell model calculations.The Mossbauer isotope Fe is probably the most frequently used nucleus for measuring hyperfine interactions.Nevertheless, its quadrupole moment is still a matter of controversy.While for a long time Q( Fe) was believed to be in the range from 0.15 to 0.28 b, Duff, Mishra, and Das [1] found Q = 0.082 b by comparing Hartree-Fock calculations with Mossbauer measurements of FeX2 molecules (X = CI,Br) trapped in solid Ar. Subsequently, this value for Q was supported by Vajda et al. [2] using nuclear structure (shell-model) calculations of Q(5 Fe) and the known ratio of the quadrupole splittings of~4 Fe and s7Fe impurities in hcp Zn and Cd [3]. During the last decade EFG calculations for solids became available based on the full-potential-linearizedaugmented plane-wave method (LAPW). These proved to be both accurate and reliable, which has been demonstrated for various solids including ionic insulators like LisN [4], Cu20 [5], TiOz [6], several Hg (I) and (II) halides [7], (hcp) metals [8], and the high T, superconductors [9). These successful applications give us co...