Eric W. Slessarev, Jennifer Pett-Ridge, Kyungjin Min, Asmeret Asefaw Berhe, Srabani Das, Randall D. Jackson, Julie D. Jastrow, Megan Kan, Sandeep Kumar, Todd Longbottom, Karis J. McFarlane, Erik Oerter, Brian K. Richards, G. Philip Robertson, Gregg R. Sanford, Erin E. Nuccio
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引用次数: 0
Abstract
Agriculture depletes soil organic carbon (SOC), partly due to the exclusion of deep-rooted perennials. Reintroducing deep-rooted perennials to cultivated land may help to mitigate SOC loss. We quantified the effect of deep roots on SOC by comparing 8 to 30 year-old stands of switchgrass (Panicum virgatum L.) with paired annual row crop fields at 12 sites across the central and eastern USA. We hypothesized that switchgrass would store more root C and SOC than neighboring shallow-rooted annual crops, and that these effects would extend deeper than 30 cm. We also evaluated whether switchgrass stimulates decomposition of SOC at depth using radiocarbon (14C). Finally, we explored whether the effect of switchgrass on SOC is moderated by soil chemical and physical properties. While the effect of switchgrass on SOC in the surface 100 cm was positive at most sites, the average effect was not statistically significant (difference in SOC = 0.6 kg C m−2 [95% CI −0.8 to +1.9 kg C m−2]). By contrast, we found that root C was consistently more abundant under switchgrass, yielding an estimated additional 0.6 kg C m−2 in the surface 100 cm of soil [95% CI +0.5 to +0.7 kg C m−2]. 14C measurements suggested that root C inputs were adding to existing SOC without stimulating decomposition. The effect of switchgrass on belowground C was not strongly related to any of the soil properties that we evaluated. Our observations show that root C can contribute substantially to belowground C stocks when deep-rooted perennials replace shallow-rooted crops.
农业消耗土壤有机碳(SOC),部分原因是由于排除了根深蒂固的多年生植物。在耕地上重新引入深根多年生植物可能有助于减轻土壤有机碳的损失。通过比较美国中部和东部12个地点8 ~ 30年树龄柳枝稷林分与成对的一年生行作田,我们量化了深根对土壤有机碳的影响。我们假设柳枝稷比邻近的浅根一年生作物储存更多的根碳和有机碳,并且这些效应会延伸到30厘米以上。我们还利用放射性碳(14C)评估了柳枝稷是否能促进深层有机碳的分解。最后,探讨柳枝稷对土壤有机碳的影响是否受到土壤理化性质的调节。虽然柳枝稷对地表100 cm土壤有机碳的影响在大多数地点都是积极的,但平均影响没有统计学意义(SOC差异= 0.6 kg C m−2 [95% CI为−0.8至+1.9 kg C m−2])。相比之下,我们发现柳枝稷下的根C一直更丰富,在100厘米的土壤表面估计额外产生0.6 kg cm - 2 [95% CI +0.5至+0.7 kg cm - 2]。14C测量表明,根C输入增加了现有的有机碳而不刺激分解。柳枝稷对地下碳的影响与我们评估的任何土壤性质都没有很强的相关性。我们的观察结果表明,当深根多年生植物取代浅根作物时,根系C对地下C储量的贡献很大。
期刊介绍:
Earth’s Future: A transdisciplinary open access journal, Earth’s Future focuses on the state of the Earth and the prediction of the planet’s future. By publishing peer-reviewed articles as well as editorials, essays, reviews, and commentaries, this journal will be the preeminent scholarly resource on the Anthropocene. It will also help assess the risks and opportunities associated with environmental changes and challenges.