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Reicosky, D.C. 2024. In. Rattan, L. (Ed.) Soil and Drought: Basic Processes. Chapter 8. pages 181-235. ISBN 978-1-00-096004-4 978-1-03-228674-7 https://doi.org/10.1201/b22954-8
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This paper from New Zealand looked at various tillage options with and without irrigation on SOC, fungal biomass and their relation to to soil aggregate sizes in a 14-year experiment. They hypothesized that long-term irrigation and intensive tillage would negatively affect soil aggregation. The experiment was started in 2003 and data taken in 2017. Two tillage treatments were intensive tillage (IT) to 20-25cm compared with no-till (direct drill - DD) and irrigation was sprinkler and none (rainfed). Soil samples (0-5 cm layer) were analyzed for pore size distribution, specific surface area and microbial biomass. Sieving was also used to separate macro- (LM) and micro-aggregates (SM), particle sized silt + clay and fine particles. Both DD and rainfed management increased total SOC content of the bulk soil. The LM and its SOC increased in DD compared to IT. A higher fungal:bacteria (F:B) ratio was generally accompanied by a greater LM fraction and mean weight aggregate diameter, highlighting the importance of fungi in the formation of LM. They concluded that detrimental effects on soil aggregation by tillage and irrigation was not conclusive and a longer study period is needed to confirm.