利用放线菌提高北苏门答腊纳曼特兰安地斯不同土壤湿度条件下的磷酸盐利用率

M. R. Alfikri, T. Sabrina, A. Sahar
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引用次数: 0

摘要

安地斯土壤中的高磷酸盐潴留导致磷的可用性很低,植物无法吸收。放线菌能够溶解结合磷酸盐。本研究旨在确定安地斯-纳曼特兰土壤中的放线菌,评估它们提高磷酸盐可用性的能力,并了解它们是如何在这种土壤中提高磷酸盐可用性的。研究设计采用了 2 个因子的因子随机区组设计;因子 1 是放线菌分离,包括 A₀ = 无接种剂,A₁ = 接种剂 A₁₃₂(蔬菜作物;32×10⁸CFU毫升-¹),A₂ = A₄₆₈(森林植物;41×10⁸CFU毫升-¹),A₃ = A₄₅₈ (森林植物;58×10⁸CFU毫升-¹),A₄ = A₄₇₁ (咖啡植物;35×10⁸CFU毫升-¹),A₅ = A₄₅₉(森林植物;63×10⁸CFU毫升-¹),A₆ = A₃₂₁ (木槿植物;37×10⁸CFU毫升-¹),以及 A₇ = A₃₅₆ (蔬菜植物;33 × 10⁸ CFU mL-¹),因子 2 是土壤含水量,包括 K₁ = 50%、K₂ = 75% 和 K₃ = 100%。结果表明,施用放线菌后,安地斯土壤中的钾含量从 42.46 ppm 增加到 159.20-266.60 ppm。放线菌处理中的放线菌数量为 27.33-31.58 × 10⁸ CFU mL-¹),土壤 pH 值为 4.41。含水量为 100%最能提高土壤 pH 值和放线菌数量,但对土壤中的可利用钾影响不大。放线菌的分子鉴定结果表明,A₃>A₅>A₂>A₄>A₁ 最具溶解 P 的潜力。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Utilization of Actinomycetes to increase phosphate availability at different soil moisture conditions in Andisols Namanteran, North Sumatera
The high phosphate retention in Andisols causes the availability of P to be low, can not be absorbed by plants. Actinomycetes are capable of solubilizing bound phosphates. This research aimed to identify Actinomycetes in Andisols Namanteran, assess their ability to increase phosphate availability, and understand how they work to increase phosphate availability in this soil. The research design used a factorial randomized block design with 2 factors; factor 1 was Actinomycetes isolate, consisting of A₀ = No Inoculant, A₁ = Inoculant A₁₃₂ (vegetable crops; 32 × 10⁸ CFU mL⁻¹), A₂ = A₄₆₈ (forest plants; 41 × 10⁸ CFU mL⁻¹), A₃ = A₄₅₈ (forest plant; 58 × 10⁸ CFUmL⁻¹), A₄ = A₄₇₁ (coffee plant; 35 × 10⁸ CFU mL⁻¹), A₅ = A₄₅₉ (forest plant; 63 × 10⁸ CFU mL⁻¹), A₆ = A₃₂₁ (hibiscus plant; 37 × 10⁸ CFU mL⁻¹), and A₇ = A₃₅₆ (vegetable plant; 33 × 10⁸ CFU mL⁻¹), and factor 2 was soil water content, consisting of K₁ = 50%, K₂ = 75% and K₃ = 100% of field capacity. The results showed that the availability of P in Andisols increased due to the application of Actinomycetes from 42.46 ppm to 159.20−266.60 ppm. The population of Actinomycetes in Actinomycetes treatment ranged from 27.33−31.58 × 10⁸ CFU mL⁻¹), with a soil pH of 4.41. Water content of 100% was the best in increasing soil pH and Actinomycetes population, but not having significant effects on the available P of the soil. The results of molecular identification of Actinomycetes that have the best potential in dissolving P include A₃>A₅>A₂>A₄>A₁.
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