Study of phosphorus adsorption behaviour of soils of the Qazvin plain, NW Iran

IF 1.4 Q4 SOIL SCIENCE Soil Science Annual Pub Date : 2024-02-04 DOI:10.37501/soilsa/183657
Behnoush Kamali, A. Mahdavi Mazdeh, Abbas Sotoodehnia, Stefan Wohnlich
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Abstract

Information of phosphorus adsorption characteristics in soils is of great importance for determining and applying proper management strategies in order to improve crop productivity and reduce environmental damages. A comprehensive equilibrium and kinetic adsorption study was designed to evaluate the adsorption behavior of phosphorus and the effect of soil properties on phosphorus retention in four different agricultural soils of Qazvin plain. The results showed that the Langmuir isotherm ( r 2 = 0.998, s = 0.007), and Kuo and Lotse equation ( r 2 = 0.946, s = 0.009) had the highest accuracy in equilibrium and kinetic modeling of phosphorus adsorption onto the soil surface. The results of linear regression analysis showed that the maximum adsorption capacity (q m ) was positively correlated with clay and calcium carbonate contents and negatively correlated with the percentage of organic matter (p < 0.05). Additionally, the effects of three distinct parameters including salinity (0 to 30 ppt), temperature (12 to 38°C), and pH (2.5 to 11.5) on phosphorus adsorption were found to be signi fi cant (p < 0.05; p < 0.01). According to these results, by changing the temperature from 12 to 25°C and 25 to 38°C, the maximum adsorption capacity increased in the range of 1.4–1.9 times. A rapid 82% increase in the adsorptive removal of phosphorus was observed at pH 5.36 to 7.5. However, with increasing salinity, the amount of adsorption decreased gradually and reached a plateau of about 0.189 mg g –1 over 10 ppt salinity. Furthermore, the results of thermodynamic test of the investigated soils showed that the process was endothermic and spontaneous.
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伊朗西北部加兹温平原土壤的磷吸附行为研究
土壤中磷吸附特性的信息对于确定和应用适当的管理策略以提高作物产量和减少对环境的破坏非常重要。为了评估 Qazvin 平原四种不同农业土壤中磷的吸附行为以及土壤特性对磷保留的影响,我们设计了一项全面的平衡和动力学吸附研究。结果表明,兰缪尔等温线(r 2 = 0.998,s = 0.007)和 Kuo 和 Lotse 方程(r 2 = 0.946,s = 0.009)对土壤表面磷吸附的平衡和动力学模型的准确性最高。线性回归分析结果表明,最大吸附容量(q m)与粘土和碳酸钙含量呈正相关,与有机质百分比呈负相关(p < 0.05)。此外,盐度(0 至 30 ppt)、温度(12 至 38°C)和 pH 值(2.5 至 11.5)这三个不同参数对磷吸附的影响也很显著(p < 0.05;p < 0.01)。根据这些结果,将温度从 12°C 提高到 25°C,再从 25°C 提高到 38°C,最大吸附容量增加了 1.4-1.9 倍。在 pH 值为 5.36 至 7.5 时,磷的吸附去除率迅速增加了 82%。然而,随着盐度的增加,吸附量逐渐减少,并在 10 ppt 盐度时达到约 0.189 mg g -1 的高点。此外,研究土壤的热力学测试结果表明,吸附过程是内热和自发的。
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来源期刊
Soil Science Annual
Soil Science Annual SOIL SCIENCE-
CiteScore
2.50
自引率
6.70%
发文量
0
审稿时长
29 weeks
期刊介绍: Soil Science Annual journal is a continuation of the “Roczniki Gleboznawcze” – the journal of the Polish Society of Soil Science first published in 1950. Soil Science Annual is a quarterly devoted to a broad spectrum of issues relating to the soil environment. From 2012, the journal is published in the open access system by the Sciendo (De Gruyter).
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