Optimization of Flooded Soil Recovery via Plant- Arbuscular Mycorrhizal Fungi Symbiotic Interaction

Nor Hazwani Aziz, N. Zainol, N. Thangaperumal, N. Zahari
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Abstract

Flooded soil recovery was optimized using experimental design methodology by manipulating the symbiotic relationship between soil fungi, Arbuscular Mycorrhizal Fungi (AMF) and the host plant (Allium cepa L.) planted in a soil containing AMF (SA). This was achieved by measuring the amount of nutrient (nitrogen, phosphorus and potassium) uptake by AMF using HACH spectrophotometer after 14 days of planting in several condition suggested by Design-Expert® software (Ver 7.1.6). In order to determine the optimum condition for the AMF to recover the flooded soil, the experiments were designed according to a central composite design in two variables following the Response Surface Methodology (RSM). A quadratic polynomial model was generated to predict soil recovery. R2 for nitrogen, phosphorus and potassium was found at 0.89, 0.96 and 0.94 respectively of the range for the factors studied namely 24-32 ml water content and 4.0-6.0 cm depth of soil. Among two parameters, depth of soil showed significant effect on the recovery of flooded soil for phosphorus and potassium while for nitrogen both parameters showed insignificant effect. Model validation experiments showed good correspondence between experimental and predicted values at error for N, P, and K at 7.0%, 1.86% and 2.65% respectively. The optimal condition for soil recovery was at 28 ml soil water content and 5 cm soil depth. At this condition, the nutrient uptake by AMF was predicted to be at their maximum rate where the concentration of nutrients increased approximately by 2 to 3 times from the initial nutrient concentration.
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植物-丛枝菌根真菌共生互作优化淹水土壤恢复
采用试验设计方法,通过调节土壤真菌、丛枝菌根真菌(AMF)与寄主植物葱(Allium cepa L.)在含AMF (SA)土壤中的共生关系,优化水淹土壤恢复效果。这是通过在Design-Expert®软件(版本7.1.6)建议的几种条件下种植14天后,使用HACH分光光度计测量AMF对养分(氮、磷和钾)的吸收量来实现的。为了确定AMF恢复淹水土壤的最佳条件,采用响应面法(RSM)的双变量中心复合设计进行试验设计。建立了二次多项式模型来预测土壤恢复。在24 ~ 32 ml含水量和4.0 ~ 6.0 cm土壤深度范围内,氮、磷、钾的R2分别为0.89、0.96和0.94。其中,土壤深度对淹水土壤中磷、钾恢复的影响显著,而对氮恢复的影响不显著。模型验证实验结果表明,N、P、K的误差预测值与实验值吻合较好,分别为7.0%、1.86%和2.65%。土壤恢复的最佳条件为土壤含水量28 ml,土壤深度5 cm。在此条件下,当养分浓度较初始浓度增加约2 ~ 3倍时,预测AMF对养分的吸收达到最大速率。
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