首页> 外文期刊>Journal of food, agriculture & environment >Determination of regression equations to predict soil extract salinity from aqueous soil samples (1:2 and 1:5) for calcareous and non-calcareous loamy soils
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Determination of regression equations to predict soil extract salinity from aqueous soil samples (1:2 and 1:5) for calcareous and non-calcareous loamy soils

机译:钙质和非钙质植物土壤中预测水土水溶液(1:2和1:5)中土壤提取物(1:2和1:5)的回归方程的测定

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摘要

The aim of the study was to reveal regression equations to predict soil extract salinities (ECe) for calcareous and non-calcareous soils. For this purpose, 12 calcareous and 12 non-calcareous soil samples were artificially salinizedby 1.0,5.0 and lOdSm~(-1) saline waters which were prepared witl NaCl. In order not to disturb the homogeneity of application of each sample, the saline waters were added to unapplied soils by the ratio of l.T(w/ w), and then oven dried at 105°C until reaching constant weight to prepare the saline soils to analyze. Hence, 3 salinity levels (1.0, 5.0 and 1( dSm~(-1)), 24 soil samples (12 calcareous and 12 non-calcareous) and 3 methods (EC_e, EC_(1:2) and EC_(1.5) ), total of 216 analyzes were performed. Saturatiot percentage of soils were recorded in order to recalculate aqueous soil samples back to soihwater ratio at saturation level. Thus, 8 regression equations were developed for specified conditions such as i) four equations for direct conversion from EC_(12)or EC toEC_e, where there was no data on soihwater ratio at saturation point, for calcareous and non-calcareous conditions andii) another four equations were calculated by soil: water ratio ai saturation point from EC_(12)or EC_(15) to EC_e, on where there weredata on soihwater ratio at saturation point, for calcareous and non-calcareous conditions.
机译:该研究的目的是揭示回归方程以预测钙质和非钙质土壤的土壤提取物(ECE)。为此目的,12种钙质和12个非钙质土壤样品是人工落入的1.0,5.0和Lodsm〜(-1)盐水水溶液,其制备了Witl NaCl。为了不打扰每个样品的施加均匀性,通过LT(w / w)的比例将盐水水加入未缺少的土壤中,然后在105℃下干燥烘箱直至达到恒定的重量以使盐渍土壤制备分析。因此,3个盐度水平(1.0,5.0和1(DSM〜(-1)),24个土壤样品(12种钙质和12个非钙质)和3种方法(EC_E,EC_(1:2)和EC_(1.5)) ,总共进行了216分析。记录了土壤的饱和百分比,以将水性土壤样品重新计算回到饱和水平的SIHWater比率。因此,对于从EC_直接转换的四个方程式开发了8个回归方程(12)或EC ToEc_e,如果饱和点没有SIHWater比数据,对于钙质和非钙质条件,对于钙质和非钙质条件,通过土壤计算另外四个方程:来自EC_(12)或EC_的水比AI饱和点(15 )到EC_E,在饱和点的SIHWATER比率下,用于钙质和非钙质条件。

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