秸秆源有机物料还田对黑土团聚体稳定性及碳氮分布特征的影响

Effects of Straw-derived Organic Matter Returned on the Aggregate Stability and Distribution Characteristics of Carbon and Nitrogen in Black Soil

  • 摘要:
    目的 探究长期有机物料还田对黑土团聚体稳定性及碳氮分布的影响,为黑土区土壤结构改良和碳氮高效管理提供理论依据。
    方法 通过连续13年的田间定位试验,设置不施肥(CK0)、单施化肥(CK)、化肥配施秸秆(ST)、化肥配施生物炭(BR)、化肥配施牛粪(CM)和化肥配施堆肥(CP)6个处理,采用湿筛法对土壤团聚体进行粒径分级,测定各粒级有机碳、全氮含量及储量。研究不同有机物料添加下0 ~ 20 cm土层团聚体分布特征及碳氮赋存规律。
    结果 有机物料施用显著改善了土壤团聚体结构,相较于CK0处理,各处理土壤大粒径团聚体(> 0.25 mm)比例提高10.0% ~ 37.2%,其中CM和CP处理效果最佳(增幅32.0%、37.2%)。增施有机物料促进微团聚体向大团聚体转化,土壤团聚体平均重量直径(MWD)和几何平均直径(GMD)分别提高13.3% ~ 27.0%和12.1% ~ 29.4%。增施有机物料提高土壤有机碳含量,其中BR与CP处理增幅明显(29.5%、21.8%)。BR、CM与CP处理显著增加了大粒径团聚体的有机碳含量,仅BR处理显著增加了< 0.053 mm粒径团聚体的有机碳含量。CM与CP处理提升土壤全氮效果突出(27.2%、28.7%)。团聚体分布与碳氮含量共同调控碳氮储量及贡献率。增施有机物料后,小粒径团聚体(< 0.25 mm)碳氮储量及贡献率下降,大粒径团聚体中,CM、CP 氮储量提升明显。
    结论 研究表明长期有机物料还田通过促进微团聚体向大团聚体转化,优化了碳氮在不同粒级团聚体中的分布特征。生物炭和堆肥分别在土壤小团聚体固碳和大团聚体储氮方面具有独特优势。

     

    Abstract:
    Objective This study aimed to explore the effects of long-term organic material return on the stability of black soil aggregates and the distribution of carbon (C) and nitrogen (N), thereby to provide a theoretical basis for soil structure improvement and efficient C and N management in black soil regions.
    Method A 13-year continuous field location experiment was conducted with six treatments, namely no fertilization (CK0), chemical fertilizer alone (CK), chemical fertilizer combined with straw (ST), chemical fertilizer combined with biochar (BR), chemical fertilizer combined with cow manure (CM), and chemical fertilizer combined with compost (CP). The wet-sieving method was used to classify soil aggregates by particle size, and the contents and stocks of organic C and total N in each particle size fraction were determined.
    Result The application of organic materials significantly improved the soil aggregate structure. Compared with the CK0 treatment, the proportion of large-sized aggregates (> 0.25 mm) in all organic material treatments increased by 10.0% - 37.2%. Moreover, the CM and CP treatments showed the best effects with the increase of 32.0% and 37.2%. The addition of organic materials promoted the transformation of micro-aggregates to macro-aggregates, and the mean weight diameter (MWD) and geometric mean diameter (GMD) of soil aggregates increased by 13.3% - 27.0% and 12.1% - 29.4%. Organic material application also increased the soil organic C content, with the BR and CP treatments showing significant increasing trend with 29.5% and 21.8%. The BR, CM, and CP treatments significantly increased the organic C contents in large-sized aggregates, while only the BR treatment significantly increased the organic C content in the < 0.053 mm aggregates. The CM and CP treatments had prominent effects on increasing soil total Nn content, with the increasing trends of 27.2% and 28.7%. The distribution of aggregates and the contents of C and N jointly regulated the C-N stocks and their relative contribution rates. After the application of organic materials, the C-N stocks and contribution rates of small-sized aggregates (< 0.25 mm) decreased. In large-sized aggregates, the CM and CP treatments significantly improved the N stock.
    Conclusion The study indicates that long-term organic material return will optimize the distribution characteristics of C and N in aggregates of different particle sizes by promoting the transformation of micro-aggregates to macro-aggregates. Biochar and compost exhibit unique advantages in C sequestration in small soil aggregates and N storage in large aggregates.

     

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