An Ensemble Modeling Approach for Estimating Diffusive Tortuosity for Saturated Soils From Porosity. Issue 2 (February 2017)

• Record Type: Journal Article
• Authors: Chakraborty, Poulamee; Das, Bhabani Sankar; Singh, Rajendra
• Is Part Of: Soil science. Volume 182:Issue 2(2017)
• Publication Date: 2017-02
• Subjects: Diffusion coefficient -- ensemble approach -- percolation theory -- porosity -- tortuosity; Soil science -- Periodicals; 631.405
• DOI: 10.1097/SS.0000000000000195
• Languages: English
• ISSNs: 0038-075X

Abstract

Abstract : ABSTRACT: Apparent diffusion constants in soil are generally estimated by dividing molecular diffusion coefficient for a solute with soil tortuosity (τ) values. Several models have been proposed to estimate τ from soil porosity (φ) alone, but most of these models fail when the variability in observed τ-φ pairs increases. Pedotransfer functions can be used to predict τ from easy-to-measure soil properties such soil texture, organic carbon contents, and φ, but such an approach requires more measurements to be performed than just measuring φ. Here, we show that τ may be estimated from φ alone using the ensemble averaging approach. We examined seven different analytical expressions for τ-φ and seven different ensemble-modeling approaches to estimate τ for 100 pairs of τ-φ collected from a wide geographical area. Modeling results showed that the Bayesian model averaging method was the best ensemble-modeling approach for estimating τ from φ. Of 119 different combinations of τ (φ) models, three models derived considering (1) packing of square-shaped particles, (2) fractal geometry with particles of different sizes, and (3) percolation theory were identified as the best individual models for ensemble modeling. The coefficient of determination (0.67), root-mean-squared error (0.23), and the Akaike information criterion (94.37) values for this ensemble model were better than those when a single model was used for prediction. Inclusion of these three models that are based on both fractal and regular geometrical shapes for particles of different sizes may be a reason for improved performance of the ensemble approach. These results suggest that τ may be estimated from φ using the ensemble approach without the need for additional soil data, as is done in a pedotransfer function approach. Abstract : Supplemental digital content is available in the text.