Soil organic matter pools response to perennial grain cropping and nitrogen fertilizer

被引:23
|
作者
Kim, Keunbae [1 ]
Daly, Erin J. [1 ]
Gorzelak, Monika [2 ]
Hernandez-Ramirez, Guillermo [1 ]
机构
[1] Univ Alberta, Dept Renewable Resource, 454 Earth Sci Bldg, Edmonton, AB T6G 2E3, Canada
[2] Agr & Agri Food Canada, Lethbridge Res & Dev Ctr, Lethbridge, AB, Canada
来源
SOIL & TILLAGE RESEARCH | 2022年 / 220卷
基金
加拿大自然科学与工程研究理事会;
关键词
Particulate organic matter; Mineral-associated organic matter; Perennial grain cropping; Soil carbon sequestration; N fertilizer; Soil organic matter; CARBON INPUTS; ROOT BIOMASS; DYNAMICS; PARTICULATE; ROTATIONS; INCREASES; TILLAGE;
D O I
10.1016/j.still.2022.105376
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Carbon sequestration in agricultural soils can play a pivotal role in the mitigation of accelerating climate change. Our research evaluated a continuum of agricultural cropping systems, including innovative perennial grain cropping, to assess which systems promote increases in and stabilization of soil organic matter (SOM). In comparison with conventional annual cropping systems, perennial grain cropping may be conducive to increased C accrual resulting from no-tillage management, longer growing seasons, and extensive root growth associated with these novel systems. Furthermore, the effects of N fertilizer addition on SOM dynamics under contrasting cropping systems were examined. We conducted physical SOM fractionation into particulate (POM) and mineral-associated organic matter (MAOM) in samples taken over two years from two experimental sites in Central Alberta, Canada. Five contrasting cropping systems (perennial-forage, perennial-grain, fall-grain, spring-grain and fallow) both with and without N fertilizer were tested. Our findings demonstrate that perennial-grain cropping was consistently superior in sequestering SOM-C compared to annual-grain crops at the surface soil layer (0-15 cm depth, Ps< 0.05). Over the duration of this experiment, perennial-grain cropping considerably boosted C accumulation in the recalcitrant SOM pools as represented by increasing MAOM, particularly at the Edmonton site, which is characterized by a clay-rich, Black Chernozemic soil (MAOM: 41.5 and 45.3 g C kg-1 in annual and perennial crops, respectively, P < 0.05). However, recurrent N fertilizer additions diminished C sequestration by perennial-grain cropping in both POM and MAOM fractions (Ps< 0.05). Correlation analysis indicated that accrual and allocation of C within the soil profile was more closely related to aboveground crop biomass productivity as opposed to root growth, particularly for generating more intermediate-labile POM. Our results shed light on how to achieve greater soil C sequestration as a function of cropping system options, N fertilizer addition and underlying soil texture.
引用
收藏
页数:12
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