2010
DOI: 10.3906/bot-0903-21
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Using vegetation units as salinity predictors in the Lower Cheliff Algeria

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Cited by 3 publications
(2 citation statements)
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“…In this context, the aim of this study was the development of classes PTFs in order to predict soil aggregate stability in the salted lower Cheliff plain, one of the most vulnerable areas to the structural disintegration using easily measurable soil properties such as particle size distribution, EC, pH, OM, CaCO 3 , pH, and cation exchange capacity. Results showed that the lower Cheliff is one of the most salted plain in northwestern Algeria, as reported by [34][35][36] this variable is the most important parameters affecting soil disintegration in this area. Except CaCO 3 and pH, the soil aggregation was significantly related to sand, silt, EC and highly significantly related to OM, CEC and clay, meaning that these variables were highly suitable for developing aggregate stability PTFs.…”
Section: Fig 4 Theoretical Map Of Mwd In the Lower Cheliff Plain Obta...supporting
confidence: 71%
“…In this context, the aim of this study was the development of classes PTFs in order to predict soil aggregate stability in the salted lower Cheliff plain, one of the most vulnerable areas to the structural disintegration using easily measurable soil properties such as particle size distribution, EC, pH, OM, CaCO 3 , pH, and cation exchange capacity. Results showed that the lower Cheliff is one of the most salted plain in northwestern Algeria, as reported by [34][35][36] this variable is the most important parameters affecting soil disintegration in this area. Except CaCO 3 and pH, the soil aggregation was significantly related to sand, silt, EC and highly significantly related to OM, CEC and clay, meaning that these variables were highly suitable for developing aggregate stability PTFs.…”
Section: Fig 4 Theoretical Map Of Mwd In the Lower Cheliff Plain Obta...supporting
confidence: 71%
“…The Normalised Difference Vegetation Index derived from the radiometric data of remote sensing, are largely used in the monitoring plans of the dynamics of the vegetation and the cartography of the changes which have occurred in the various ecosystems (Rondeaux, et al, 1996) ; (Bannari, 1999 ;Chirici et al, 2001). Remote sensing techniques have been mainly applied to overcome the shortcomings of classical inventory methods, and they resulted in a large variety of inventory data and derivative products (Ababou et al, 2010;McRoberts & Tomppo, 2007). Since the launching of the first Landsat dealing with a Multispectral Scanner System (MSS) dated to 1972, remote sensing and different modeling methods have been used in forest inventory studies: regression analysis (Ardö, 1992;West, 1995 ;Lu, 2005;Salvador & Pons, 1998;); k-nearest neighbor method (Franco-Lopez et al, 2001;McRoberts & Tomppo, 2007 ;Tomppo et al, 2008;Gasparri et al, 2010;Dandan Xu, Xilun Guo 2014;Khader et al, 1014) ; neural networks (Foody et al, 2003); and fuzzy logic (Triepke et al, 2008).…”
Section: Introductionmentioning
confidence: 99%