Prediction of soil surface salinity in arid region of central Iran using auxiliary variables and genetic programming. Issue 1 (2nd January 2016)

• Record Type: Journal Article
• Authors: Taghizadeh-Mehrjardi, Ruhollah; Ayoubi, Shamsollah; Namazi, Zeinab; Malone, B. P.; Zolfaghari, Ali A.; Sadrabadi, F. Roustaei
• Is Part Of: Arid land research and management. Volume 30:Issue 1(2016)
• Page Start: 49
• Page End: 64
• Publication Date: 2016-01-02
• Subjects: Auxiliary data -- digital soil mapping -- EM38 -- Iran; Arid soils -- Periodicals; Arid regions agriculture -- Periodicals; Desert reclamation -- Periodicals; 631.47154
• DOI: 10.1080/15324982.2015.1046092
• Languages: English
• ISSNs: 1532-4982

Abstract

ABSTRACT: Spatial information on soil salinity is increasingly needed for decision making and management practices in arid environments. In this article, we attempted to investigate soil salinity variation via a digital soil mapping approach and genetic programming in an arid region, Chah-Afzal, located in central Iran. A grid sampling strategy with 2-km distance was used. In total, 180 soil surface samples were collected and then analyzed. A symbolic regression was then adopted to correlate electrical conductivity (ECe ) with a suite of auxiliary data including predicted maps of apparent electrical conductivity (vertical: ECav and horizontal: ECah ), Landsat spectral data and terrain attributes derived from a digital elevation model. The accuracy of the genetic programming model was evaluated using root mean square error (RMSE), mean error (ME), and coefficient of determination ( R 2 ) based on an independent validation data set (20% of database or thirty soil samples). In general, results showed that ECah had the strongest influence on the prediction of soil salinity followed by salinity index wetness index, Landsat Band 3, multi-resolution valley bottom flatness index, elevation, and normalized difference vegetation index. Furthermore, results indicated that the genetic programming model predicted ECe over the study area accurately ( R 2 = 0.87, ME = −1.04 and RMSE = 16.36 dSm −1 ). Overall, it is suggested that similar applications of this technique could be used for mapping soil salinity in other arid regions of Iran.