Treated wastewater reuse for recharge in agricultural fields: Retention dynamics and geochemical modeling of macronutrients in soils

IF 5.9 1区 农林科学 Q1 AGRONOMY Agricultural Water Management Pub Date : 2024-12-18 DOI:10.1016/j.agwat.2024.109250
Ajit Kumar, Basant Yadav
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Abstract

Reusing treated wastewater (TWW) with high concentrations of macronutrients (nitrogen, phosphorus, and potassium) in Agricultural-Based Managed Aquifer Recharge (AgMAR) presents various challenges to soils, crops, water resources, microbes, public health, and economics. This study investigates the behavior of macronutrients in agricultural soil during TWW recharge through AgMAR, focusing on the effects of mineral formation during the recharge process. Batch experiments, kinetic studies, and pH edge experiments were conducted to understand the retention behaviors of ammonium (NH4+), phosphate (PO43), and Potassium ion (K+) in soils. Visual MINTEQ was employed to evaluate the saturation indices of nutrient dissolution, equilibrium, and precipitation conditions, using macronutrient concentrations from TWW and soil mineral data as inputs. The Freundlich isotherm model provided the best fit for the experimental results for ammonium and potassium, with correlation coefficients of 0.98 and 0.99, respectively. For phosphorus, the Temkin model showed the best fit, with a correlation coefficient of 0.96. Retention behaviors varied with pH: ammonium and potassium exhibited higher retention under basic conditions, while phosphate demonstrated greater retention in acidic conditions. The pseudo-second-order kinetic model best described the retention kinetics observed in the experiments. The saturation index (SI) results revealed that manganese hydrogen phosphate (MnHPO4) fully precipitates and calcium phosphate Ca3(PO4)2 precipitates at pH levels above 8, while other nutrients remained in dissolution. This study highlights that nutrient retention from TWW effluent enhances nutrient availability for plants. However, the precipitation of certain forms, such as MnHPO₄ and Ca₃(PO₄)₂, may clog soil pores, restricting recharge pathways. These findings support the reuse of TWW as a sustainable method for supplementing agricultural nutrients and ensuring safe groundwater recharge, while also offering a safe disposal solution for wastewater treatment plants
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在以农业为基础的含水层管理回灌(AgMAR)中重复使用经处理的高浓度宏量营养元素(氮、磷和钾)废水(TWW)对土壤、作物、水资源、微生物、公共卫生和经济学提出了各种挑战。本研究调查了 TWW 通过 AgMAR 回灌过程中农业土壤中宏量营养元素的行为,重点是回灌过程中矿物形成的影响。为了解土壤中铵 (NH4+)、磷酸盐 (PO4-3) 和钾离子 (K+) 的保留行为,进行了批量实验、动力学研究和 pH 边缘实验。采用可视化 MINTEQ 评估养分溶解、平衡和沉淀条件的饱和指数,并将 TWW 和土壤矿物数据中的宏量养分浓度作为输入。Freundlich 等温线模型对铵和钾的实验结果拟合最佳,相关系数分别为 0.98 和 0.99。对于磷,Temkin 模型的拟合效果最好,相关系数为 0.96。保留行为随 pH 值的变化而变化:铵和钾在碱性条件下的保留率较高,而磷酸盐在酸性条件下的保留率较高。伪二阶动力学模型最好地描述了实验中观察到的保留动力学。饱和指数(SI)结果显示,当 pH 值超过 8 时,磷酸氢锰(MnHPO4)完全沉淀,磷酸钙 Ca3(PO4)2 沉淀,而其他营养物质仍处于溶解状态。这项研究表明,从 TWW 污水中截留养分可提高植物对养分的利用率。然而,某些形式的沉淀,如 MnHPO₄ 和 Ca₃(PO₄)₂,可能会堵塞土壤孔隙,限制补给途径。这些研究结果支持将原水回用作为补充农业养分和确保地下水安全回灌的可持续方法,同时也为污水处理厂提供了安全的处置方案。
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来源期刊
Agricultural Water Management
Agricultural Water Management 农林科学-农艺学
CiteScore
12.10
自引率
14.90%
发文量
648
审稿时长
4.9 months
期刊介绍: Agricultural Water Management publishes papers of international significance relating to the science, economics, and policy of agricultural water management. In all cases, manuscripts must address implications and provide insight regarding agricultural water management.
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