文献类型： 外文期刊

作者： Kravchenko, A. N. ¹ ; Zheng, H. ³ ; Kuzyakov, Y. ⁴ ; Robertson, G. P. ¹ ; Guber, A. K. ¹ ;

作者机构： 1.Michigan State Univ, Dept Plant Soil & Microbial Sci, E Lansing, MI 48824 USA

2.Michigan State Univ, DOE Great Lakes Bioenergy Res Ctr, E Lansing, MI 48824 USA

3.Jilin Acad Agr Sci, Res Inst Agr Resources & Environm, Changchun 130033, Peoples R China

4.Univ Gottingen, Dept Agr Soil Sci, Gottingen, Germany

5.Inst Physicochem & Biol Problems Soil Sci, Pushchino 142290, Russia

6.RUDN Univ, Moscow, Russia

7.Michigan State Univ, WK Kellogg Biol Stn, Hickory Corners, MI 49060 USA

关键词： X-ray computed micro-tomography; (CO2)-C-13 pulse labeling; Prairie; Switchgrass; Big bluestem; Wild bergamot; Pore-size distribution; Soil pore architecture; Soil pore structure

期刊名称：SOIL BIOLOGY & BIOCHEMISTRY （ 影响因子：7.609； 五年影响因子：8.312 ）

ISSN： 0038-0717

年卷期： 2021 年 159 卷

页码：

收录情况： SCI

摘要： Diverse plant communities are known to increase soil carbon (C) levels compared to monocultures, but an incomplete understanding of the underlying mechanisms of this phenomenon limits the development of strategies for optimizing soil C sequestration. We hypothesized that the identity of neighboring plants influences the amounts of C that a plant inputs into the soil, the resultant formation of soil pore architecture, and the fate of the plant's C inputs. To test this hypothesis, we combined (CO2)-C-13 plant pulse labeling with X-ray computed micro-tomography (mu CT) in assessing plant-assimilated C from three species common to North American prairie: switchgrass, big bluestem, and wild bergamot. The plants were grown in a greenhouse in monoculture and in all-pair combinations. The C-13 labeling was conducted so as to ensure that only one member of each pair has received C-13. The results demonstrated that greater belowground C exchange among neighboring plants enhanced inputs of plant-assimilated C into soil, suggesting that the involvement of plant community members in belowground C transfer, rather than community's diversity per se, drives rapid soil C accrual. Moreover, the magnitudes of C losses as well as properties of soil pore architecture also depend not only on the identity of the C source plant itself but also on the identities of its neighbors. These findings propose belowground interspecific C transfer as a previously overlooked mechanism for enriching and stabilizing soil C and suggest genomic and management potentials for selecting species that participate in intensive interspecific assimilate exchange in order to promote rapid and stable soil C gains.