SR12185Three long-term trials end with a quasi-equilibrium between soil C, N, and pH: an implication for C sequestration
We measured the long term changes in soil carbon and pH on three trials in the Riverina. The accumulation of soil C required a matching accumulation of N and was accompanied by a decrease in soil pH. The release of N to crop plants will require a rundown in soil C whereas a build up in soil C will lead to a requirement for liming.