Soil aggregates stability and storage of soil organic carbon respond to cropping systems on Black Soils of Northeast China

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作者
Meng Zhou
Chunzhu Liu
Jie Wang
Qingfeng Meng
Ye Yuan
Xianfa Ma
Xiaobing Liu
Yingxue Zhu
Guangwei Ding
Jizhou Zhang
Xiannan Zeng
Weiling Du
机构
[1] Northeast Agricultural University,School of Resources and Environment
[2] Chinese Academy of Sciences,Northeast Institute of Geography and Agroecology
[3] Harbin Academy of Agricultural Sciences,Department of Biological Center
[4] Heilongjiang Branch of China Tobacco Corporation,Mudanjiang Tobacco Science Rsearch Institute
[5] Northern State University,Chemistry Department
[6] Heilongjiang Academy of Sciences,Institute of Natural Resources and Ecology
[7] Heilongjiang Academy of Agricultural Sciences,Institute of Crop Cultivation and Tillage
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摘要
Monoculture and improper management may reduce soil fertility and deteriorate soil structure in Black soils (Mollisols) of Northeast China. The experiment was carried out from 2015 to 2016 in Black Soils comprising five cropping systems: continuous corn (CC), soybean-corn rotation (SC), corn-soybean rotation (CS), fallow-corn (FC), and fallow-soybean (FS). Our results showed that CS and FS treatments significantly increased mean weight diameter (MWD) and fractal dimension (D) in mechanical stability aggregates (MSAs), and increased MWD and geometric mean diameter (GMD) in water-stable aggregates (WSAs) compared with CC treatment. These two treatments were also significantly increased water-stable aggregates stability rate (WSAR), but decreased percentage of aggregates destruction (PAD) than CC treatment. Meanwhile, CS and FS treatments exhibited a higher carbon accumulation than CC treatment in bulk soils. Soil organic carbon (SOC) concentration in WSA0.106-0.25,WSA2-5 mm and WSA0.5-1 mm had a dominant effect on aggregate stability. Simutaneously, SOC in WSA>5 mm affected SOC concentration in bulk soils. As a whole, the CS and FS treatments can increase the percentage of macro-aggregates, enhance aggregate stability, as well as increase SOC concentration in bulk soils and all soil aggregate sizes.
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