• ISSN 1008-505X
  • CN 11-3996/S

长期施肥对红壤性水稻土磷组分及phoCphoD功能微生物群落特征的影响

Effects of long-term fertilization on phosphorus fractions and the characteristics of phoC- and phoD-harboring microbial communities in red paddy soil

  • 摘要:
    目的 磷是影响农作物生产力的重要限制因素之一。分析长期不同施肥对土壤磷素形态转化及功能微生物群落的影响,可为磷肥高效管理与农业可持续发展提供理论依据。
    方法 基于江西省南昌市双季稻连作长期定位施肥试验,选取不施肥(CK)、氮磷肥(NP)、氮钾肥(NK)、磷钾肥(PK)和氮磷钾平衡施肥(NPK)5个处理。采用改进的Hedley磷分级法测定土壤中不同磷组分含量,利用荧光微孔板酶检测法测定土壤磷酸酶(PHOS)活性,并通过高通量测序技术分析编码酸性磷酸酶(phoC)和碱性磷酸酶(phoD)的功能微生物群落。结合Mantel检验和偏最小二乘路径模型分析施肥处理、微生物群落与磷组分间的关系。
    结果 长期施磷(NP、PK、NPK)显著提高了早稻和晚稻季土壤全磷(TP)、Olsen-P、H2O-Pi、NaHCO3-Pi、NaHCO3-Po、NaOH-Pi、NaOH-Po和HCl-Pi含量。土壤中活性磷组分(LP)、中等活性磷组分(MLP)和稳定性磷组分(NLP)占比分别介于7.41%~18.70%、35.31%~49.81%和33.00%~51.80%之间,长期施用磷肥显著增加了早稻和晚稻土壤LP和MLP组分占比,降低了NLP组分占比。土壤PHOS活性以NPK处理最高,其次为NK和NP处理,但三者间差异不显著。同时,NPK处理显著提高了土壤phoCphoD功能微生物的α多样性(Chao指数和Shannon指数)。其中,phoD功能微生物α多样性与土壤LP组分含量和占比,以及NaOH-Pi和Olsen-P含量均呈显著正相关。此外,施肥显著影响了早稻和晚稻季土壤中携带phoD基因和phoC基因微生物的群落组成结构。长期施用氮肥降低了phoC功能微生物优势种群的相对丰度,其中寡养单胞菌属(Stenotrophomonas)相对丰度在施氮处理中显著降低;而施用磷肥增加了phoD功能基因优势种群的相对丰度,其中罗尔斯通氏菌属(Ralstonia)和假拉布里斯菌属(Pseudolabrys)的相对丰度显著增加。偏最小二乘路径模型分析显示,施肥主要通过影响phoD功能微生物群落组成,进而促进土壤磷转化。
    结论 长期施用磷肥有效促进双季稻连作体系红壤性水稻土中不同磷组分的积累,而氮磷钾平衡施肥显著提高土壤PHOS活性以及phoCphoD功能微生物多样性,促进土壤磷循环。相较于phoC功能微生物,phoD功能微生物在红壤性水稻土磷转化过程中可能发挥更为关键作用。

     

    Abstract:
    Objectives Phosphorus is one of the major limiting factors affecting crop productivity. This study aimed to investigate the effects of long-term different fertilization on soil phosphorus transformation and functional microbial communities, providing a theoretical basis for efficient phosphorus management and sustainable agricultural development.
    Methods This study was based on a long-term fertilization experiment under a double-cropping rice system in Nanchang, Jiangxi Province, China. Five treatments were selected: no fertilization (CK), nitrogen and phosphorus fertilization (NP), nitrogen and potassium fertilization (NK), phosphorus and potassium fertilization (PK), and balanced nitrogen, phosphorus, and potassium fertilization (NPK). Soil phosphorus fractions were determined using the modified Hedley phosphorus fractionation method. Soil phosphatase (PHOS) activity was measured using a fluorometric microplate enzyme assay. High-throughput sequencing was employed to analyze the functional microbial communities encoding acid phosphatase (phoC) and alkaline phosphatase (phoD). Mantel test and Partial least squares path modeling were used to analyze the relationships among fertilization treatments, microbial communities, and phosphorus fractions.
    Results Long-term phosphorus application (NP, PK, NPK) significantly increased the contents of soil total phosphorus (TP), Olsen-P, H2O-Pi, NaHCO3-Pi, NaHCO3-Po, NaOH-Pi, NaOH-Po, and HCl-Pi during both early and late rice seasons. The proportions of labile phosphorus (LP), moderately labile phosphorus (MLP), and non-labile phosphorus (NLP) in the soil ranged from 7.41% to 18.70%, 35.31% to 49.81%, and 33.00% to 51.80%, respectively. Long-term phosphorus fertilization significantly increased the proportions of LP and MLP while decreasing the proportion of NLP in soils collected during both early and late rice seasons. Soil phosphatase (PHOS) activity was highest under the NPK treatment, followed by the NK and NP treatments, although no significant differences were observed among them. Moreover, the NPK treatment significantly increased the α-diversity (Chao and Shannon indices) of both phoC- and phoD-harboring functional microbial communities. The α-diversity of phoD harboring microorganisms was significantly positively correlated with the content and proportion of LP, as well as with NaOH-Pi and Olsen-P contents. Furthermore, fertilization significantly influenced the community composition of microorganisms harboring the phoD and phoC genes in soils during the early and late rice seasons. Long-term nitrogen application reduced the relative abundance of dominant phoC-harboring microbial taxa, with a significant decrease in the relative abundance of Stenotrophomonas under nitrogen fertilization. In contrast, phosphorus application increased the relative abundance of dominant phoD-harboring microbial taxa, with significant increases in the relative abundance of Ralstonia and Pseudolabrys. Partial least squares path modeling revealed that fertilization mainly promoted the transformation of soil phosphorus fractions by influencing the community composition of phoD-harboring microorganisms.
    Conclusions Long-term phosphorus fertilization effectively increased the accumulation of different phosphorus fractions in the soil, while balanced NPK fertilization effectively enhances soil phosphatase (PHOS) activity and the diversity of phoC- and phoD-harboring functional microorganisms, thereby promoting soil phosphorus cycling. Compared with phoC-harboring microorganisms, phoD-harboring microorganisms may play a more important role in the process of soil phosphorus transformation in this system.

     

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