A tool used in various disciplines, particularly sedimentology and soil science, analyzes particle size distribution. It helps determine the diameter (D) at which 60% of the sample’s particles are finer. This value, often expressed in millimeters or micrometers, is crucial for understanding material properties. For example, a soil sample with a D60 of 0.5mm indicates that 60% of the soil particles are smaller than 0.5mm. This information informs drainage, water retention, and erosion susceptibility assessments.
Understanding particle size distribution is fundamental for numerous applications. This analysis facilitates inferences about a material’s origin, transportation history, and overall suitability for specific purposes. Historically, this analysis relied on laborious sieving methods. Modern computational tools expedite the process and enhance accuracy, enabling researchers and engineers to efficiently characterize materials. This efficiency translates to better-informed decisions in fields like construction, agriculture, and environmental management.