• 中文核心期刊
  • CSCD来源期刊
  • 中国科技核心期刊
  • CA、CABI、ZR收录期刊

生物炭耦合木霉菌对滨海沙土持水固肥的改良机制

Biochar/Trichoderma Application for Aeolian Amelioration and Fertility Stabilization of Sandy Soil

  • 摘要:
    目的 探究生物炭与哈茨木霉对东山岛滨海风沙土的协同改良效应,明确其对土壤持水性、养分转化及植物吸收的影响机制,为沙土绿色改良提供高效途径。
    方法 以上海青为供试植物开展盆栽试验,设置4个处理:不施改良剂对照(CK)、添加1%生物炭(T1)、添加0.25%哈茨木霉菌剂(T2)、1%生物炭+0.25%木霉菌剂(T3)。测定土壤理化性质,土壤N-乙酰-β-D-氨基葡萄糖苷酶(NAG)、β-葡萄糖苷酶(β-GC)、亮氨酸氨基肽酶(LAP)活性,上海青生物量、全氮、全磷含量及氮磷积累量,分析木霉菌定殖动态及指标间相关性。
    结果 T3处理田间持水量最高(208.17 g·kg−1),有效水含量为CK的1.4倍,萎蔫系数与CK无显著差异。21 d培养期内,T3处理木霉菌定殖量达1.02×106 CFU·g−1,显著高于T2处理(5.55×105 CFU·g−1)。T3处理有机质、全氮、碱解氮、速效钾含量较CK分别提升104.41%、96.77%、87.55%、159.07%,硝态氮含量较CK显著降低21.59%。T3处理NAG活性较CK提升62.15%,而β-GC和LAP活性则以T1处理提升幅度最大(分别为50.48%和148.32%)。T3处理上海青鲜重和干重较CK分别提高57.77%和58.43%,氮、磷积累量分别提高92.94%和94.89%。偏最小二乘结构方程模型表明,土壤理化性质通过促进植物氮磷积累(路径系数0.559)和激活土壤酶活性(路径系数0.563)间接驱动生物量提升,其中“土壤理化性质→植物氮磷积累→生物量”是关键增产路径(间接效应0.455)。
    结论 生物炭耦合哈茨木霉菌可显著促进木霉菌根际定殖,协同提升沙土持水与养分库容,激活几丁质周转关键酶(NAG)活性,实现作物增产,是改良滨海沙土贫瘠水肥性状的有效措施。

     

    Abstract:
    Objective Effects of applying biochar and Trichoderma harzianum on mitigating aeolian, improving water retention, and maintaining fertility of sandy soil on the coast of Dongshan Island were studied.
    Method A pot experiment growing Brassica chinensis L. on soil collected from the beaches on Dongshan Island was conducted under 4 conditions including control without amendment (CK) and treatments with addition of 1% biochar (T1), 0.25% T. harzianum agent (T2) or T1+T2 (T3). Physiochemical properties and N-acetyl-β-D-glucosaminidase (NAG), β-glucosidase (β-GC), and leucine aminopeptidase (LAP) activities in the soil as well as plant biomass, total nitrogen, total phosphorus, nitrogen, phosphorus of the vegetables grown in the pots were measured. Trichoderma colonization and correlations among various indicators were analyzed.
    Result Among all tested conditions, T3 rendered the greatest water-holding capacity of the soil at 208.17g·kg−1, with available water content 1.4 times that of CK without significant changes on wilting coefficient. After 21d of cultivation, Trichoderma population in T3 grew to 1.02×106 CFU·g−1, which was significantly higher than in T2 of 5.55×105 CFU·g−1. Compared with CK, T3 also significantly raised the soil organic matter, total nitrogen, alkali-hydrolysable nitrogen, and available potassium by 104.41%, 96.77%, 87.55%, and 159.07%, respectively, while significantly reduced the nitrate nitrogen by 21.59%. The NAG activity in T3-treated soil was enhanced by 62.15% relative to CK, whereas the highest β-GC and LAP activities in T1-treated counterparts increased by 50.48% and 148.32%, respectively. Under T3, the fresh and dry weights of Shanghai green increased by 57.77% and 58.43%, respectively, and nitrogen and phosphorus accumulation by 92.94% and 94.89%, respectively, over those of CK. A partial least squares structural equation modeling revealed that the soil physicochemical properties indirectly drove the biomass increase by promoting plant N and P accumulation at a path coefficient of 0.559 and activating soil enzyme activities at a path coefficient of 0.563. The “soil physicochemical properties → plant N and P accumulation → biomass” was the key yield-enhancing route with an indirect effect of 0.455.
    Conclusion The application of biochar in combination with T. harzianum not only significantly promoted the Trichoderma colonization in rhizosphere but also enhanced the water-holding capacity, preserved the nutrient pool, and activated the chitin turnover-related NAG in sandy soil resulting in an elevated vegetable yield.

     

/

返回文章
返回