In collaboration with Landcare Research and GNS Science we have been analysing re-sampled soil profiles from grazed pasture around New Zealand. We demonstrated large losses of total C and N from Allophanic and Gley Soils on flat land. Other soil orders had no detectable change in soil C or N. Conversely, pastures on hill country were gaining carbon.
Supported by MSI through a subcontract with Landcare Research and the Ministry of Primary Industries.
Schipper, L.A.; Parfitt, R.L.; Ross, C.; Baisden, W.T; Claydon J.J.; Fraser S. (2010) Gains and losses in C and N stocks of New Zealand pasture soils depend on land use. Agriculture Ecosystems and Environment. 139: 611–617.
Schipper, L.A.; Parfitt, R.L.; Fraser, S.; Littler R.A.; Baisden, T.W.; Ross, C. (2014) Soil order and grazing management effects on changes in soil C and N in New Zealand pastures. Agriculture Ecosystems and Environment. 184: 67-75.
We are trying to determine why this carbon has changed with a number of hypothesis being tested – including the role of cow urine in solubilising soil organic matter:
Lambie, S.M.; Schipper, L.A.; Balks, M.R.; Baisden, W.T. (2012) Solubilisation of soil carbon following treatment with cow urine under laboratory conditions. Soil Research. 50: 50–57.
Gains on hill country may be due to recovery of topsoil following wide-spread erosion when land was cleared from native forests some ~100 years ago:
Parfitt, R.L.; Baisden, W.T.; Ross, C.; Rosser, B.J.; Schipper, L.A.; Barry B. (2013) Influence of erosion and deposition on carbon and nitrogen accumulation in resampled steepland soils under pasture in New Zealand. Geoderma. 192:154-159.