There is a considerable lack of essential information about Entisols derived from shale in the arid desert environment. This study was thus carried out to characterize and map the spatial variability of primary properties of Entisols in Dakhla Oasis, Western Desert, Egypt. Soil properties of twenty-seven profiles represented by Entisols were carefully examined. Geostatistical analysis was performed to map soil variability based on the ordinary kriging interpolation method. Results show that most of the studied soils (92.1%) were fine and medium in texture. The values of electrical conductivity of soil paste extract (ECe) ranged between 0.45 and 36.40 dS m −1 (mean = 10.35 dS m −1 ). Most of the studied soil samples (82.9%) were extremely low in organic matter (OM) (≤ 3.4 g kg −1 ). The cation exchange capacity (CEC) ranged between 9.37 and 50.84 cmol(+) kg −1 with an average of 29.09 cmol(+) kg −1 . The coefficient of variation was high to very high for sand, ECe, and OM; moderate for silt, clay, saturation percentage, and CEC; and low for the soil pH. Significantly positive and negative correlations were observed among the Entisol properties (at P < 0.01 and/or P < 0.05), and most of these relationships are likely associated with the parent material. Precise maps created efficiently with geostatistics were crucial for a proper understanding of the current spatial variability in the study area. This study provides valuable information and new knowledge about the properties and the spatial variability of this type of Entisols.Keywords Arid environment . Dakhla Oasis . Entisols . Geostatistical analysis . Ordinary kriging . Soil properties Highlights • We investigated the characteristics of Entisols derived from shale in arid desert environment.• This study provides important information about properties of this type of soils, which has a severe lack of information. • Geostatistical analyses provide powerful analytical tools to capture the horizontal variability of soil properties. • The coefficient of variation (CV) is a useful indicator for spatial and vertical variations of soil properties. • The parent material plays an effective role in the diversity of soil properties in the arid regions.
The original version of this paper was published with error. Figure 3 were corrected into Figs. 3 and 4, but the old titles were used for these two figures and the updated captions which author sent in the last modification of the images were not used. Given in this article are the correct captions.
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