CHANGES IN SOIL AGGREGATION ASSOCIATED WITH TALLGRASS PRAIRIE RESTORATION

To investigate the dynamics of soil aggregation associated with the restoration of cultivated soil to tallgrass prairie, changes in soil aggregation and aboveground production were compared in a corn field, restored prairie plantings of various ages (second, fifth, eighth, and eleventh growing season), and an uncultivated prairie remnant. The restored prairie was also compared with a long-term (fourteenth growing season) ungrazed pasture dominated by Eurasian grasses. All plots were located on similar soils. The regression model, Y = 95.8 - 56.2/X (R² = 0.93), best described the relatively rapid recovery of water-stable soil aggregates >0.2 mm diameter with time (in years) since cultivation. Similar models were also found to describe changes in the percentages of aggregates > 1 and > 2 mm diameter. Aggregates > 0.2 and > 2 mm diameter were more closely associated with prairie graminoids than with other vegetation categories. However, time without disturbance may be a more important factor in soil aggregate formation than vegetation type, but it was difficult to separate the effects of these two factors in this study. The percentage of aggregates > 0.2 mm diameter was found to be significantly higher (P = 0.0553) in the oldest restored prairie than in ungrazed pasture although the former had been cultivated more recently. This suggests that C₄ prairie graminoids may confer some advantage over introduced C₃ Eurasian grasses for the development of water-stable aggregates in soils of the Prairie Peninsula.