The coefficient of uniformity (cu) is a numerical measure that describes the gradation of a soil sample, specifically indicating the range of particle sizes within that sample. A higher cu value signifies a greater range of particle sizes, which often suggests that the soil is more well-graded and may have better engineering properties, while a lower cu indicates a more uniformly sized particle distribution. This measure plays a critical role in soil classification and understanding the physical behavior of soils in engineering applications.