尼日利亚尼日尔河三角洲东部阿夸伊博姆州一些农业土壤上四氧磷酸盐 (v) 离子的吸附研究

U.A. Umoren, S. A. Odoemelam, M. N. Ogbuagu
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引用次数: 0

摘要

磷酸盐吸附能力主要调节土壤溶液中的磷浓度和可用磷。这项工作旨在研究尼日利亚阿夸伊博姆州五种农业土壤的磷酸盐吸附特性。在 20 mL 0.01 M CaCl2 溶液中加入 20、40、60、80、100 和 120 mgL-1 的 KH2PO4,振荡 24 小时后,得到了磷酸盐吸附等温线。采用 Langmuir、Freundlich、Van Huay 和 Temkin 等温线研究了土壤样品对 PO43 的吸附特性。Freundlich 模型是磷酸盐吸附的最佳选择,其平均 R2 值为 0.9872。对 120 mgL-1 溶液的磷酸盐吸附量(µg g-1soil)、吸附位点的异质性因子(nF)和 Freundlich 常量(KF)(Lg-1)的计算结果分别为:Onna 土壤 101(84.3)、0.515 和 7.355;Onna 土壤 62.8(52.3)、0.641 和 2.464;Ogu-Itumbonuso 土壤为 60.6(50.5)、0.708 和 3.985;Ikot-Amama 1 土壤为 59.3(49.5)、0.652 和 2.505;Ikot-Nkon 土壤为 58.0(48.3)、0.704 和 3.682。磷酸盐的平衡浓度(EC-P)被用作解吸指数,以确定土壤是否可作为植物生物利用率的潜在来源,结果范围在 5.0 至 9.90 mgL-1 之间,表明磷酸盐极易流失。磷酸盐吸附参数与土壤理化性质之间的关系表明,Freundlich 吸附强度因子 nF 与有机碳和有机质(r = -0.953 和 -0.947;P<0.01)、铁和锰(r = -0.911 和 -0.812;P<0.05)呈强烈负相关。EC-P 与土壤 pH(H2O)(r = 0.959,P<0.01)、粘土(r = 0.913,P<0.05)、阳离子交换容量(CEC)(r = -0.824,P<0.05)、锰(r = -0.792,P<0.05)和铁(r = -0.826,P<0.05)密切相关。这项研究表明,土壤管理方法以使用有机肥为基础,结合土壤特性吸附 PO43-,是实现作物可持续生产和减少土壤-水环境污染的有效工具。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Sorption studies of Tetraoxophosphate (v) ions on some agricultural soils in Akwa Ibom State, eastern Niger Delta, Nigeria
The phosphate sorption capacity regulates principally the phosphorus concentration and available phosphorus in any soil solution. This work aims to study the phosphate sorption characteristics of five agricultural soils in Akwa Ibom State, Nigeria. The phosphate adsorption isotherm was obtained by shaking each soil sample with 20, 40, 60, 80, 100 and 120 mgL–1 for 24 h with 20 mL of KH2PO4 in 0.01 M CaCl2 solution. The Langmuir, Freundlich, Van Huay and Temkin isotherms were applied to study the PO43-sorption characteristics of the soil samples. The Freundlich model provided the best choice for phosphate sorption with mean R2 value of 0.9872. Results obtained for the phosphate sorbed (µg g–1soil) with 120 mgL-1 solution, heterogeneity factor of adsorption sites (nF), and the Freundlich constant (KF) (Lg–1) were 101(84.3), 0.515 and 7.355 for Onna soil; 62.8(52.3), 0.641 and 2.464 for Ikot-Amama 2; 60.6(50.5), 0.708 and 3.985 for Ogu-Itumbonuso soil; 59.3(49.5), 0.652 and 2.505 for Ikot-Amama 1 soils; 58.0(48.3), 0.704 and 3.682 for Ikot-Nkon soils, respectively. The equilibrium concentration for phosphates (EC-P) were used as desorption index to determine whether the soils could serve as potential sources for their bioavailability to plants and results ranged from 5.0 to 9.90 mgL–1, indicating high vulnerability to phosphate loss. The relationship between phosphate sorption parameters and soil physicochemical properties showed that the Freundlich adsorption intensity factor, nF, strongly correlated negatively with organic carbon and organic matter (r = -0.953 and -0.947; P<0.01), Fe and Mn (r = -0.911 and -0.812, P<0.05). The EC-P correlated strongly with soil pH(H2O) (r = 0.959, P<0.01), clay (r = 0.913, P<0.05), cation exchange capacity (CEC) (r = -0.824, P<0.05), Mn (r = -0.792, P<0.05) and Fe (r = -0.826, P<0.05). The study illustrated that soil management practices which involves the using organic fertilizers as the basis for PO43- sorption in relation to soil properties can be a useful tool for sustainable crop production and environmental soil-water contamination.
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