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Modeling of Permanent Wilting from Particle Size Fractions of Coastal Plain Sands Soils in Southeastern Nigeria

机译:尼日利亚东南沿海平原沙土粒度分数的永久枯萎模拟

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Permanent wilting points in soils have been found to correlate significantly with particle size fractions. This study was conducted to establish functional relationship between soil particle size fractions and permanent wilting point of soils of coastal plain sands in southeastern Nigeria. A total of 102 surface samples were collected from three different dominantly Ultisols toposequences (i.e., 34 samples from each). Permanent wilting point experiment was carried out in pots with the 102 samples in the greenhouse while the particle size analysis was carried out in the laboratory. There was significant correlation among the textural separates, permanent wilting point correlated significantly with clay (??=0.21, ??≤0.05). The general linear model showed significant differences between permanent wilting point of soils found in the upper and lower slope positions. Regression equation established that 54% of the total variation in permanent wilting point could be accounted for by the clay and coarse sand content of the soils. Prediction of permanent wilting point of Ultisols formed on coastal plain sands soils of humid tropical southeastern Nigeria will effectively depend on reliability of determination of clay and coarse sand contents of the soils.
机译:已经发现土壤中的永久萎points点与粒径分数显着相关。进行这项研究是为了建立尼日利亚东南沿海平原砂土的土壤粒径分数与永久性枯萎点之间的函数关系。从三个不同的显性Ultisols至序列中总共收集了102个表面样品(即每个样品34个样品)。在温室中用102个样品在盆中进行永久性枯萎实验,而在实验室中进行粒度分析。质地分离之间存在显着相关性,永久萎wil点与黏土显着相关(Δε= 0.21,Δε≤0.05)。总体线性模型显示出在上,下坡位置的土壤永久枯萎点之间存在显着差异。回归方程确定,永久性枯萎点总变化的54%可以由土壤中的粘土和粗砂含量引起。尼日利亚东南部潮湿热带沿海沿海沙土上形成的Ultisols永久枯萎点的预测将有效地取决于确定土壤黏土和粗砂含量的可靠性。

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