<p>Schipper, L. A., P. L. Mudge, et al. (2017). "A review of soil carbon change in New Zealand&rsquo;s grazed grasslands." New Zealand Journal of Agricultural Research 60(2): 93-118.</p>
<p>Abstract<br />Soil organic matter is a potential sink of atmospheric carbon (C) and critical for maintaining soil quality. We reviewed New Zealand studies of soil C changes after conversion from woody vegetation to pasture, and under long-term pasture. Soil C increased by about 13.7&#8197;t&#8197;C&#8197;ha&minus;1&nbsp;to a new steady state when forests were initially converted to pasture. In the last 3&ndash;4 decades, resampling of soil profiles demonstrated that under long-term pasture on flat land, soil C had subsequently declined for allophanic, gley and organic soils by 0.54, 0.32 and 2.9&#8197;t&#8197;C&#8197;ha&minus;1&#8197;y&minus;1, respectively, and soil C had not changed in the remainder of sampled soil orders. For the same time period, pasture soils on stable midslopes of hill country gained 0.6&#8197;t&#8197;C&#8197;ha&minus;1&#8197;y&minus;1. Whether these changes are ongoing is not known, except for the organic soils where losses will continue so long as they are drained. Phosphorus fertiliser application did not change C stocks. Irrigation decreased carbon by 7&#8197;t&#8197;C&#8197;ha&minus;1. Carbon losses during pasture renewal ranged between 0.8 and 4.1&#8197;t&#8197;C&#8197;ha&minus;1. Some evidence suggests tussock grasslands can gain C when fertilised and not overgrazed. When combined to the national scale, different data sets suggest either no change or a gain of C, but with large uncertainties. We highlight key land-use practices and soil orders that require further information of soil C stock changes and advocate for a better understanding of underpinning reasons for changes in soil C.</p>
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