有机水溶肥料通过激发土著微生物活化周转土壤磷能力促进棉花生长和磷吸收

Organic water-soluble fertilizers promote cotton growth and phosphorus uptake by stimulating indigenous microbiota-mediated soil phosphorus activation

  • 摘要: 为揭示6类常见有机水溶肥料激发土著微生物介导的土壤磷活化利用、促进作物磷吸收和生长的共性机理与浓度效应, 以轻度盐渍土-棉花盆栽为试验体系, 设置有机水溶肥料类型(即以海藻精粉剂、海藻精水剂、聚谷氨酸、甲壳素、鱼蛋白和糖蜜类为代表的6类有机水溶肥料)与有机碳施用量梯度(0、厂家推荐用量、40、80、160和240 mg·pot−1)两个因素, 分析了同一类型有机水溶肥料在不同有机碳施用量条件下和不同类型有机水溶肥料在相同有机碳施用量条件下对棉花幼苗生长(株高、叶面积动态、生物量和吸磷量)、土壤微生物活性(土壤微生物生物量磷含量和土壤碱性磷酸酶活性)以及土壤有效磷含量的影响, 并比较了6类有机水溶肥料的碳激发效应(即单位质量有机碳施用量引起的微生物生物量磷含量、碱性磷酸酶活性、生物有效性磷以及植株吸磷量的变化值)。结果表明: 6种有机水溶肥料激发土壤磷活化利用、增强棉花幼苗磷吸收和改善棉花幼苗生长的效应与有机碳施用量水平相关, 其定量关系可以用线性加平台模型拟合。不同类型有机水溶肥料对棉花幼苗生长的激发效应存在有机碳施用量的临界阈值, 尽管不同类型有机水溶肥料的有机碳施用量阈值存在一定差别, 但绝大部分处于30~60 mg·pot−1范围内。相同有机碳施用量条件下, 不同类型有机水溶肥料对棉花幼苗的促生效应无显著差异, 但有机碳施用量对土壤微生物生物量磷含量、碱性磷酸酶活性及土壤有效磷的激发效应存在显著差异, 表明土施有机水溶肥料对植物生长的促进效应并非通过直接刺激产生, 而是通过激发土壤微生物介导的土壤磷活化利用间接实现。土壤微生物对不同类型有机水溶肥料碳源的利用能力不同, 糖蜜类有机水溶肥料对微生物生物量磷的激发效应高于其他5类。同时, 本文还对现行有机水溶肥料的定义进行了探讨, 提出有机水溶肥料的“肥料”作用是通过水溶性有机碳激发土著微生物活化周转土壤磷的活性与功能实现的。

     

    Abstract: To elucidate the common mechanisms and concentration effects of six typical organic water-soluble fertilizers (OWSFs) on soil phosphorus (P) activation mediated by indigenous microorganisms, crop P uptake, and growth enhancement, a pot experiment with cotton in slightly saline soil was conducted. The study investigated two factors: 1) OWSF types (including six representatives: alginic acid powder, alginic acid aqueous solution, polyglutamic acid-based, chitin-based, fish protein-based, and molasses-based fertilizers) and 2) organic carbon (C) application rates (0, manufacturer-recommended dose, 40, 80, 160, and 240 mg·pot−1). The effects of C rates within each OWSF type and across different OWSF types under the same C rate were evaluated for cotton seedling growth (plant height, leaf area dynamics, biomass, and P uptake), soil microbial activity (microbial biomass P and phosphatase activity), and soil available P content. The C priming effect (i.e., changes in microbial biomass P, phosphatase activity, bioavailable P, and plant P uptake per unit C input) of the six OWSFs was quantified. The key findings showed that 1) all six OWSFs enhanced soil P activation, cotton P uptake, and seedling growth in a C dose-dependent manner, with dose-response relationships well fitted by linear-plateau models. Threshold C rates (30~60 mg·pot−1) for growth stimulation varied among OWSF types. 2) At equivalent C rates, OWSF types showed no significant differences in promoting cotton growth but exhibited distinct priming effects on microbial biomass P, phosphatase activity, and P availability (P < 0.05). This indicates that OWSFs enhance plant growth indirectly by stimulating microbially mediated soil P activation rather than through direct effects. 3) The efficiency of the priming effect of six OWSF-C sources varied significantly, with molasses-based OWSF demonstrating the highest priming effect on microbial biomass P among the six types. We further discuss the current definition of OWSFs, proposing that their "fertilizer" function is primarily achieved through water-soluble organic C priming microbial activity to activate soil P turnover.

     

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