Xin Yang, Jun Zhu, Tao Ren, Jian Zhao, Yating Fang, Rihuan Cong, Zhifeng Lu, Xiaokun Li, Jianwei Lu
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引用次数: 0
Abstract
Aims
Crop rotation is a vital practice in sustainable agricultural management. This study aimed to investigate soil labile organic carbon, carbon-degrading microorganisms, and soil organic carbon (SOC) mineralization in oilseed rape-rice (OR), wheat-rice (WR), oilseed rape-maize (OM), and wheat–maize (WM) rotations without (CK) and with the application of chemical fertilizers (NPK).
Methods
A 7-year field experiment involving different crop rotations was conducted in Shayang County, China. Fluorescence excitation—emission matrix (EEM) was used in analyzing dissolved organic carbon (DOC) structure, metagenomics was employed to investigate the specific glycoside hydrolase (GH) and auxiliary activity (AA) families. The mineralization of SOC was investigated through an incubation experiment.
Results
The paddy-upland (OR, WR) rotations showed higher soil labile organic carbon content and simpler DOC structure than their corresponding continuous upland (OM, WM) rotations. Oilseed rape contained (OR, OM) rotations showed higher soil labile carbon content than the corresponding wheat contained (WR, WM) rotations. The abundance of soil GH family genes was higher in paddy-upland rotations than those in continuous upland rotations. Furthermore, both the abundance of soil GH family genes and β-glucosidase activity were higher in OM rotation than in WM rotation after fertilization. The SOC mineralization was higher in oilseed rape contained rotations than in wheat contained rotations and higher in paddy-upland rotations than in continuous rotations without fertilization. Fertilization increased SOC mineralization, but reduced the difference among crop rotation patterns.
Conclusion
Oilseed rape contained rotations had higher SOC mineralization than wheat contained rotations, rotations affected SOC mineralization mainly by regulating DOC content, abundance of GH gene families and β-glucosidase activity.
期刊介绍:
Plant and Soil publishes original papers and review articles exploring the interface of plant biology and soil sciences, and that enhance our mechanistic understanding of plant-soil interactions. We focus on the interface of plant biology and soil sciences, and seek those manuscripts with a strong mechanistic component which develop and test hypotheses aimed at understanding underlying mechanisms of plant-soil interactions. Manuscripts can include both fundamental and applied aspects of mineral nutrition, plant water relations, symbiotic and pathogenic plant-microbe interactions, root anatomy and morphology, soil biology, ecology, agrochemistry and agrophysics, as long as they are hypothesis-driven and enhance our mechanistic understanding. Articles including a major molecular or modelling component also fall within the scope of the journal. All contributions appear in the English language, with consistent spelling, using either American or British English.