<abstract> <b><sc>Abstract.</sc></b> Moisture is an important external factor that impacts the stability and viability of grains. Movement of moisture through grain has been investigated, but not specifically as a function of water activity, and previous work did not use recently developed moisture sorption instrumentation. Moisture sorption isotherms can provide the information needed to determine moisture penetration rates into grain over different water activity ranges and can be generated automatically using recently developed instrumentation. The purpose of this study was to investigate moisture movement into grain using moisture sorption isotherms. Two methods for generating isotherms were used: static and dynamic. The information provided by each method was unique and, when combined, provided information about changes in moisture penetration into grain that occur as the water activity changes. Static isotherm data were used to calculate permeance values for the grain at different water activities, while dynamic isotherm data were used to determine a critical water activity (RHc) at which the permeance of the grain underwent significant changes, causing an inflection in the dynamic isotherm. Comparing the permeance values generated from static isotherm data and the RHc from dynamic isotherm data confirmed that permeance changes significantly when the water activity is above the RHc. Generating dynamic dewpoint isotherm (DDI) curves and finding the RHc for coated materials using automatic isotherm generators has potential to provide a simple approach to finding the water activity level at which the moisture barrier resistance of the coating is reduced.