Freundlich, Langmuir and Temkin isotherm studies of silicon sorption on soils derived from three parent materials in Edo State, Nigeria

E. Orhue, A. Emomu
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Abstract

The study was conducted to assess Freundlich, Langmuir, and Temkin isotherm studies of silicon sorption of soils derived from three parent materials in Edo State, Nigeria. A completely randomized design was used to collect fifteen soil samples from five depths in three replications at three locations namely, NIFOR, Uhomora, and Ososo which are developed on Coastal Plain Sand, Imo Shale, and Basement complex rock parent materials respectively. Some soil physical and chemical properties were determined according to standard procedure, in the Faculty of Agriculture laboratory, University of Benin. Samples were equilibrated in 50 ml distilled water containing various amounts of Si as Calcium-Magnesium silicate (CaMgSiO2) to give 50, 100, 200, 400, and 800 mg Si L-1 for 30 min., allowed to stand overnight, equilibrated again for 30 minutes, filtered and Si read colorimetrically. Data obtained were fitted to Freundlich, Langmuir, and Temkin adsorption models. Results showed that the Temkin model expressed Si sorption capacity better considering the R2 values of 0.733, 0.296, and 0.288 for coastal plain sand, Imo shale, and Basement complex rock soils, respectively. The soils formed on Basement complex rock adsorbed more Si than soils formed on Coastal plain sand and Imo shale parent materials, considering the mean Temkin BT (retention capacity of adsorbed Si) values. The Temkin model could be relied upon as a suitable model to determine Si sorption in soils of the study area. 
Freundlich, Langmuir和Temkin对尼日利亚埃多州三种母质土壤中硅吸附的等温研究
该研究的目的是评估Freundlich、Langmuir和Temkin对尼日利亚埃多州三种母质土壤硅吸附的等温研究。采用完全随机设计,在NIFOR、Uhomora和Ososo 3个地点,从5个深度3个重复采集15个土壤样品,分别发育在海岸平原砂、Imo页岩和基底复杂岩石母质上。根据标准程序在贝宁大学农学院实验室测定了一些土壤的物理和化学性质。样品在含有不同Si量的硅酸钙镁(CaMgSiO2)的50 ml蒸馏水中平衡,分别得到50、100、200、400和800 mg Si L-1 30分钟,静置过夜,再次平衡30分钟,过滤并比色读取Si。所得数据拟合Freundlich, Langmuir和Temkin吸附模型。结果表明,沿海平原砂、Imo页岩和基底复杂岩石土壤的R2分别为0.733、0.296和0.288,Temkin模型能更好地表达硅的吸附能力。考虑到吸附硅的平均Temkin BT值,基底复合岩上形成的土壤比沿海平原砂和伊莫页岩母质上形成的土壤对硅的吸附更多。Temkin模型可作为测定研究区土壤硅吸附的合适模型。
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