生物炭对棕壤团聚体稳定性及磷组分分布的影响

Effect of biochar on the stability of brown soil aggregates and the distribution of phosphorus fractions

  • 摘要: 土壤团聚体是调节土壤中磷储存和周转的重要因素。为评价生物炭介导土壤团聚体对土壤磷素形态、转化及分布的调控作用, 本研究基于生物炭长期田间定位实验, 选取不施肥(CK)、施生物炭(BC)、施NPK肥(NPK)、NPK肥配施生物炭(NPK+BC) 4个处理, 于2021年玉米收获后取0~20 cm土壤样品, 研究生物炭对土壤团聚体组成、稳定性和各粒级团聚体内各磷组分含量的影响, 明确土壤团聚体中磷组分的分布及不同粒级土壤团聚体对不同形态磷组分的相对贡献率。结果表明: 1) 施用生物炭显著提高了土壤团聚体中粗大团聚体(>2 mm)的比例, 降低了粉黏粒(<0.053 mm)的比例, 土壤团聚体的平均重量直径(MWD)和平均几何直径(GMD)分别提高9.6%和22.2%; 2)施用生物炭提高了粒径>0.25 mm团聚体中总无机磷(TPi)的含量, 主要表现在NaHCO3-Pi和NaOH-Pi含量的提高, 也提高了细大团聚体(0.25~2 mm)中总有机磷(TPo)含量, 主要表现在NaOH-Po和Residual-P含量的提高; 3)施用生物炭减少了粉黏粒(<0.053 mm)对不同磷组分的相对贡献率, 增加了粗大团聚体(>2 mm)对不同磷组分的相对贡献率。施用生物炭是改善土壤结构, 促进土壤磷素持留和降低土壤磷素流失风险的重要措施。

     

    Abstract: Soil aggregates play important roles in regulating the storage and turnover of phosphorus in soil. This study was conducted to evaluate the regulatory effect of biochar mediated soil aggregates on the form, transformation, and distribution of soil phosphorus. This study was based on long-term field experiments of biochar, four treatments were selected: no fertilization (CK), biochar application (BC), NPK fertilizer application (NPK), and NPK fertilizer combined with biochar application (NPK+BC). After maize harvest in 2021, 0-20cm soil samples were taken to study the effects of biochar on the composition and stability of soil aggregates, as well as the content of various phosphorus fractions in each particle size aggregate. The distribution of phosphorus fractions in soil aggregates and the relative contribution rate of different particle size soil aggregates to different forms of phosphorus were also clarified. The results showed that 1) the application of biochar significantly increased the proportion of coarse aggregates (>2 mm) by 8.7% (CK treatment) and 15.8% (NPK treatment), respectively. The proportion of silt and clay particles (<0.053 mm) was reduced by 11.5% (CK treatment) and 21.8% (NPK treatment), respectively. The application of biochar significantly increased the MWD and GMD of soil aggregates by 9.6% and 22.2%, respectively. 2) The application of biochar increased the content of TPi (total inorganic phosphorus) (mainly manifested in the increase of NaHCO3-Pi and NaOH-Pi content) in aggregates with particle size >0.25 mm, and also increased the content of TPo (total organic phosphorus) (mainly manifested in the increase of NaOH-Po and Residual-P content) in fine and large aggregates (0.25-2 mm). 3) The application of biochar reduced the relative contribution of silt and clay particles (<0.053 mm) to total phosphorus anddifferent phosphorus fractions, and increased the relative contribution of coarse aggregates (>2 mm) to total phosphorus and different phosphorus fractions, In conclusion, the application of biochar improved the stability of soil aggregates, improved the structure of soil aggregates, and promoted the distribution of phosphorus fractions in soil aggregates with larger particle sizes. The application of biochar is an important agricultural measure to improve soil structure, promote soil phosphorus retention, and reduce the risk of soil phosphorus loss.

     

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