长期施肥对灌漠土有机碳含量及碳储量的影响
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S158

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张掖市市级科技计划项目(ZY2022KY04)和中央引导地方科技发展资金项目(24ZYQA053)资助。


Effects of Long-term Fertilization on Organic Carbon Content and Carbon Storage in Irrigated Desert Soil
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Effects of long-term fertilization on organic carbon and carbon storage in irrigated desert soil

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    摘要:

    为阐明长期施肥对灌漠土剖面有机碳时空演变规律,依托始建于1982年的甘肃张掖灌漠土长期定位试验,系统分析了2003年(累计22年)与2022年(累计41年)3种典型种植制度(小麦–小麦–玉米轮作、小麦∥玉米间作、玉米连作)下,8种施肥处理(CK:不施肥;N:单施氮肥;NP:氮磷肥;NPK:氮磷钾肥; M:单施有机肥;MN:有机肥+氮肥;MNP:有机肥+氮磷肥;MNPK:有机肥+氮磷钾肥)对0~200 cm剖面土壤有机碳含量及储量的调控作用。结果表明:①施肥模式显著影响土壤有机碳储量,其含量顺序为MNP、MNPK > M、MN > N、CK > NP、NPK。其中,CK与N处理土壤有机碳含量持续下降,而M处理土壤有机碳提升显著,MNPK配施增幅最高。②土壤有机碳垂直分布呈显著分层特征,耕层(0~20 cm)土壤有机碳含量与储量最高(2003年分别为9.67~16.15 g/kg和28.7~45.5 t/hm2;2022年分别为10.47~15.70 g/kg和29.5~44.3 t/hm2),随土层加深呈递减趋势。③种植制度调控碳利用效率,小麦–玉米轮作体系下,有机肥碳固存率达38.6%,单位粮食产量有机碳消耗量为132.2 kg/t;而小麦∥玉米间作、玉米连作下碳固存率降至24.7%,碳消耗量增至156.6 kg/t,表明作物配置影响碳投入–封存平衡。综上,有机无机配施可协同提升耕层碳库容量,是干旱区灌漠土碳汇功能优化与粮食产能协同提升的核心策略;此外,建议在灌漠土区实行小麦–玉米轮作制度提升土壤碳汇功能。研究结果为区域农业碳中和路径提供了关键科学依据。

    Abstract:

    To elucidate the spatiotemporal evolution of soil organic carbon (SOC) in irrigation desert soil under long-term fertilization, this study utilized a long-term field experiment established in 1982 in Zhangye, Gansu Province. The regulatory effects of eight fertilization treatments (CK: no fertilization; N: nitrogen; NP: nitrogen + phosphorus; NPK: nitrogen + phosphorus + potassium; M: manure; MN: manure + nitrogen; MNP: manure + nitrogen + phosphorus; MNPK: manure + nitrogen + phosphorus + potassium) on SOC content and storage across the 0-200 cm soil profiles under three cropping systems (wheat-wheat-maize rotation, wheat/maize intercropping, and maize monoculture) were systematically analyzed during two sampling periods (2003: after 22 years; 2022: after 41 years). The results showed that: 1) Fertilization regimes significantly influenced SOC accumulation efficiency, with SOC content ranked as MNP, MNPK>M, MN>N, CK>NP, NPK. SOC in CK and N declined continuously, while M markedly enhanced SOC, with MNPK showing the greatest increase. 2) SOC exhibited distinct vertical stratification, with topsoil (0-20 cm) showing the highest SOC content and storage (2003: 9.67-16.15 g/kg, 28.7-45.5 t/hm2; 2022: 10.47-15.70 g/kg, 29.5-44.3 t/hm2), decreasing exponentially with depth. 3)Cropping systems modulated carbon use efficiency. Organic manure application achieved a carbon sequestration rate of 38.6% with 132.2 kg organic carbon consumed per ton of grain yield under wheat rotation, whereas the carbon sequestration rate decreased to 24.7% and the carbon consumption increased to 156.6 kg/t under maize intercropping/monoculture, highlighting the role of crop configuration in balancing carbon input and sequestration. In conclusion, organic-inorganic combined fertilization synergistically enhances topsoil carbon capacity and subsoil carbon stability, serving as a core strategy for optimizing carbon sequestration and grain productivity in arid irrigation-silted soils. In addition, it is recommended to implement a wheat maize rotation system in irrigated desert soil areas to enhance soil carbon sequestration function. These findings provide critical scientific insights for designing regional agricultural carbon neutrality pathways.

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张建文,杜健,孙建好,吴海燕,孙宁科,索东让,赵小宁,许依,夏龙龙,马煜卿,张盛.长期施肥对灌漠土有机碳含量及碳储量的影响[J].土壤,2025,57(5):1004-1012. ZHANG Jianwen, DU Jian, SUN Jianhao, WU Haiyan, SUN Ningke, SUO Dongrang, ZHAO Xiaoning, XU Yi, XIA Longlong, MA Yuqing, ZHANG Sheng. Effects of Long-term Fertilization on Organic Carbon Content and Carbon Storage in Irrigated Desert Soil[J]. Soils,2025,57(5):1004-1012

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  • 收稿日期:2025-03-09
  • 最后修改日期:2025-07-12
  • 录用日期:2025-07-14
  • 在线发布日期: 2025-11-24
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