Soil organic matter quality and aggregate stability under eight potato cropping sequences in a fine sandy loam of Prince Edward Island

Soil degradation and soil organic matter (SOM) reduction have long been sus pected to occur under intensive potato (Solanum tuberosum L.) production in Prince Edward Island. Thus, this study was conducted to evaluate the effec t of eight potato cropping sequences involving barley (Hordeum vulgare L.), ryegrass (Lolium multiflorum L.), red clover (Trifolium pratense L.) and b arley under-seeded with red clover on aggregate stability and SOM propertie s of a Charlottetown fine sandy loam (Orthic Humo-Ferric Podzol). Total C a nd N, light-fraction (density < 1.7 g cm(-3)) C (LF-C) and light-fraction N (LF-N), microbial biomass C (MBC), carbohydrate content, alkaline phosphat ase activity (APA) and aggregate stability were determined in the 0- to 15- cm soil layer in the 6th and 10th years of the trial. Average C and N conte nts were 20 to 27% greater in sequences that included 3 or 4 yr of potatoes and a high frequency of red clover than in a 9-yr potato sequence; and wer e attributed to the less frequent tillage and higher organic matter inputs associated with the forage component. The response for MBC, LF-C, LF-N and APA was greater than those for total C and N suggesting that the former par ameters may better reveal SOM changes caused by variations in potato manage ment than the latter. Light-fraction N was particularly sensitive to the in clusion of perennial legumes in the cropping sequence. Wet-aggregate stabil ity was 33% higher after 6 yr in the sequence with 50% frequency of red clo ver than in the continuous potato system, but no effect was noted after 10 yr. The results of this study indicate that sequences which are limited to 30 to 40% of potatoes and have a high frequency of perennial forage such as red clover, lead to greater SOM content and quality of a Charlottetown fin e sandy loam compared to continuous potatoes. Trends in aggregate stability generally followed those of SOM fractions but the effects were relatively smaller and varied with time.