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Spatial variability and correlation of soil properties in the Annabaplain (North-East Algeria)

机译:Annabaplain土壤性质的空间变异性和相关性(东北阿尔及利亚)

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摘要

The present study was conducted to study the spatial variability of soil acidity (pH), electrical conductivity (EC), texture and calcium carbonate (CaCO_3). The total of 23 soil samples were collected from different plots at 0-0.3 m in depth and were analyzed in the laboratory. The statistical analysis showed high spatial variability across the experimental field based on EC, CaC0_3, clay, sand and silt indicated by values of the coefficient of variation (CV) of 46.537, 38.156, 32.289, 49.037 and 34.742%, respectively. However, very low variability was observed for soil pH; with CV value of 2.759%. Correlation matrix indicated that soil pH was significantly correlated with CaC0_3 (r=0.74) and electrical conductivity (r=-0.448). Clay was positively andsignificantly correlated with silt (r= 0.635) and negatively and significantly correlated with sand (r=0.907). Silt was negatively and significantly correlated with sand (r= - 0.907).
机译:进行本研究以研究土壤酸度(pH),电导率(EC),质地和碳酸钙(Caco_3)的空间变异性。 在深度0-0.3米的不同图中收集23种土壤样品,并在实验室分析。 统计分析在基于EC,CACO_3,粘土,砂和淤泥的基于EC,CACO_3,粘土,砂和淤泥的实验场的高空间变异,分别为46.537,38.156,32.289,49.037和34.742%的变异系数(CV)。 然而,对土壤pH值观察到非常低的可变性; CV值为2.759%。 相关矩阵表明土壤pH与CaCO_3(r = 0.74)和电导率显着相关(R = -0.448)。 粘土与淤泥(r = 0.635)呈正显着,与砂(R = 0.907)负面且显着相关。 淤泥与砂呈负面且显着相关(r = - 0.907)。

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