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Prediction leaching of potassium using the convective-dispersive and the convective log-normal transfer function models

Jalali, M. and Rowell, D. L. (2008) Prediction leaching of potassium using the convective-dispersive and the convective log-normal transfer function models. Environmental Geology, 55 (4). pp. 863-874. ISSN 0943-0105

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To link to this article DOI: 10.1007/s00254-007-1038-6

Abstract/Summary

There is increasing concern about soil enrichment with K+ and subsequent potential losses following long-term application of poor quality water to agricultural land. Different models are increasingly being used for predicting or analyzing water flow and chemical transport in soils and groundwater. The convective-dispersive equation (CDE) and the convective log-normal transfer function (CLT) models were fitted to the potassium (K+) leaching data. The CDE and CLT models produced equivalent goodness of fit. Simulated breakthrough curves for a range of CaCl2 concentration based on parameters of 15 mmol l(-1) CaCl2 were characterised by an early peak position associated with higher K+ concentration as the CaCl2 concentration used in leaching experiments decreased. In another method, the parameters estimated from 15 mmol l(-1) CaCl2 solution were used for all other CaCl2 concentrations, and the best value of retardation factor (R) was optimised for each data set. A better prediction was found. With decreasing CaCl2 concentration the value of R is required to be more than that measured (except for 10 mmol l(-1) CaCl2), if the estimated parameters of 15 mmol l(-1) CaCl2 are used. The two models suffer from the fact that they need to be calibrated against a data set, and some of their parameters are not measurable and cannot be determined independently.

Item Type:Article
Divisions:Faculty of Science > School of Archaeology, Geography and Environmental Science
ID Code:3669
Uncontrolled Keywords:convective-dispersive equation convective log-normal transfer function leaching potassium retardation SOLUTE TRANSPORT POROUS-MEDIA WESTERN IRAN SANDY SOIL GROUNDWATER WATER
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