• ISSN 1008-505X
  • CN 11-3996/S
王雅润, 赵娟, 杨振兴, 周怀平, 解文艳, 刘志平. 不同施肥模式下褐土的有机碳组分及碳固存效应变化[J]. 植物营养与肥料学报. DOI: 10.11674/zwyf.2023456
引用本文: 王雅润, 赵娟, 杨振兴, 周怀平, 解文艳, 刘志平. 不同施肥模式下褐土的有机碳组分及碳固存效应变化[J]. 植物营养与肥料学报. DOI: 10.11674/zwyf.2023456
WANG Ya-Run, ZHAO Juan, YANG Zhen-xing, ZHOU Huai-ping, XIE Wen-Yan, LIU Zhi-Ping. Organic carbon composition and carbon sequestration effect of cinnamon soil as affected by fertilization modes[J]. Journal of Plant Nutrition and Fertilizers. DOI: 10.11674/zwyf.2023456
Citation: WANG Ya-Run, ZHAO Juan, YANG Zhen-xing, ZHOU Huai-ping, XIE Wen-Yan, LIU Zhi-Ping. Organic carbon composition and carbon sequestration effect of cinnamon soil as affected by fertilization modes[J]. Journal of Plant Nutrition and Fertilizers. DOI: 10.11674/zwyf.2023456

不同施肥模式下褐土的有机碳组分及碳固存效应变化

Organic carbon composition and carbon sequestration effect of cinnamon soil as affected by fertilization modes

  • 摘要:
    目的 基于长期定位试验研究长期有机无机配施对褐土有机碳含量及其组分构成的演变特征,可更加深入了解有机肥对土壤碳固存能力的影响机制,为提高褐土维护生态环境稳定的功能以及生产力提供养分管理依据。
    方法 有机无机配施试验于1992年在山西寿阳旱地农业生态系统国家野外科学观测研究站进行,种植制度为一年一季玉米。试验采用氮、磷、有机肥三因素四水平正交设计,共18个处理。本研究选择其中9个处理:N0P0M0、N1P1M0、N2P2M0、N3P3M0、N4P4M0、N2P1M1、N3P2M3、N4P2M2、N0P0M6,N0、N1、N2、N3、N4 的施N量分别为0、60、180、240、300 kg/hm2,P0、P1、P2、P3的施P量分别为0、37.5、75、135 kg/hm2,M0、M1、M2、M3、M6的有机肥用量分别为0、67.5、22.5 t/hm2 45、135 t/hm2。以5年为1个周期,在1996、2001、2006、2011、2016年、2020年玉米收获后,采集 0—20 cm 土层土壤样品,测定总有机质含量,以及有机碳各组分含量,分析碳投入与土壤有机碳及各碳组分含量之间的关系,探讨固碳速率和固碳效率在不同碳投入下的响应。
    结果 连续试验 29 年后,与不施肥处理N0P0M0相比,化肥有机肥配合处理N3P2M3、N4P2M2、N0P0M6的土壤有机碳含量分别提高了25.7%、72.4%、30.3%和220%,各项碳组分含量均显著增加。与初始值相比,化肥处理N1P1M0、N3P3M0、N4P4M0的土壤颗粒有机碳含量分别降低了0.41 g/kg、0.89 g/kg和0.41 g/kg,易氧化有机碳含量大幅降低了40.3%、26.4%和9.6%。各处理土壤碳库管理指数总体表现为先大幅降低再逐渐上升,其中N0P0M6处理碳库管理指数最高,较N0P0M0处理提高了6.6倍。长期施肥定位试验中,化肥配施有机肥处理N2P1M1、N3P2M3、N4P2M2的土壤总有机碳固碳速率分布在0.22~0.58 t/(ha∙yr),远高于化肥处理N1P1M0、N2P2M0、N3P3M0、N4P4M0,土壤有机碳各组分的固持速率变化趋势与总有机碳基本一致。现阶段土壤各组分有机碳储量和增加量同累积碳投入间呈显著正线性相关关系(P<0.01),且仍未出现饱和现象。
    结论 长期有机无机肥配合施用显著增加了褐土有机碳及其组分含量,提高了土壤固碳速率和固碳潜力,且施用高量有机肥最有利于农田土壤碳固持、维持土壤肥力。因此,长期有机培肥是有效提高褐土土壤质量,增强土壤碳“汇”功能的农田施肥措施。

     

    Abstract:
    Objectives We studied the evolution of organic carbon content and composition of cinnamon soil based on a long-term positioning experiment, to deeper understand the machanism of organic fertilizer on the carbon sequestration of soil, and to provide nutrient management basis for improving the function and productivity of cinnamon soil in maintaining ecological environment stability.
    Methods The long-term fertilization experiment started since 1992, and located in the National Field Scientific Observation and Research Station of the Dry Land Agricultural Ecosystem in Shouyang, Shanxi Province, with planting system of one crop a year. An orthogonal design of three factors and four levels was used for the experiment, and nine of the 18 treatments were chosen for this research, including one blank control (N0P0M0), four chemical fertilizer treatments (N1P1M0, N2P2M0, N3P3M0, and N4P4M0), and four chemical and manure combination treatments (N2P1M1, N3P2M3, N4P2M2, and N0P0M6). The four N rate were 60, 120, 180, 240, and 300 kg/hm2; the four P rate were 37.5, 75, 112.5, and 150 kg/hm2; and the organic fertilizer rate for M1, M2, M3, and M6 were 22.5, 67.5, 45, and 135 t/hm2. Soils (-20 cm) were sampled in frequency of 5-years, i.e. at harvest of maize in 1996, 2001, 2006, 2011, 2016, and 2020, for the determination of total organic matter and organic carbon component contents. The relationship between carbon input and the content of soil organic carbon and each carbon component, and the response of carbon sequestration rate and efficiency of treatment soils were assessed.
    Results After 29 years of continuous experiments, N3P2M3, N4P2M2 and N0P0M6 treatment increased soil organic carbon content by 25.7%, 72.4%, 30.3% and 220%, respectively, and significantly increased the contents of various carbon components, compared with N0P0M0; N1P1M0, N3P3M0 and N4P4M0 treatments decreased soil particulate organic carbon content by 0.41, 0.89, and 0.41 g/kg, respectively, and drastically decreased the readily oxidizable carbon content by 40.3%, 26.4% and 9.6%, respectively, compared with the initial test value. During the 29 years period, the soil carbon pool management indices of all the treatments decreased sharply at first and then gradually increased, N0P0M6 treatment was tested the highest carbon pool management index, which was 6.6 times higher than that of N0P0M0. The total soil organic carbon sequestration rates in N2P1M1, N3P2M3, and N4P2M2 treatments were 0.22~0.58 t/(hm2∙yr), which was much higher than those of N1P1M0, N2P2M0, N3P3M0, and N4P4M0 treatments. The increment of all the organic carbon components had a positive and linear relationship with the cumulative carbon input, and did not reach platform within the tested organic carbon input levels yet.
    Conclusions Long-term combined application of organic and inorganic fertilizers significantly increased the total and each component of organic carbon contents, and increased the carbon sequestration rate and potential of the cinnamon soil. The application of high amounts of organic fertilizers is the most conducive to soil carbon sequestration and fertility maintenance. Therefore, long-term and high rate of organic fertilizer input is an effective fertilization measurement to improve the fertility and function of carbon sink of cinnamon soil.

     

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