PARAMETERIZING TEMPORAL CHANGES IN AGGREGATION IN A SLUDGE-AMENDED SOIL

Statistical comparison of the changes in aggregate size distributions (ASD) with time among treatments in a given soil or among soils is dif ficult. The objective of this study was to compare the use of fractal dimension (D), geometric mean diameter (GMD), and alpha (alpha) parame ters as indices to characterize the temporal changes in ASD of a soil subsequent to the incorporation of an oily waste sludge. Soil samples for dry and wet aggregate size distribution (DASD and WASD, respective ly) measurements were collected from a loamy sand during a 4-yr period following sludge Incorporation. Sludge incorporation produced a conti nuous oil content, i.e., 0, 1.0, 1.5, 3.0, and 7.0%, variable in the s oil (by mass). The wind erodible fraction (WEF; <0.84 mm) in the sludg e treated plots decreased from 80 to 38% but increased with time to 78 % 4 yr later. The reduction in WEF was reflected as gains in larger si ze fractions which decreased with time. The 4.76- to 8-mm water stable aggregates in the sludge treated plots increased from 10 to 80% but d ecreased with time to 40% 4 yr later. An opposite trend was observed f or smaller size aggregates. After sludge incorporation, the D for DASD and WASD decreased with increasing oil content and increased with tim e. An opposite trend was observed for GMD and a. Initial oil content a nd time of sampling accounted for 91% of the variability in DASD chara cterized by GMD, 89% by D, and 60% by a. Initial oil content and time accounted for 78% of the variability in WASD characterized by D and 67 % by GMD. Our results indicate that the temporal changes in DASD can b e characterized equally well by GMD and D and the changes in WASD by D .