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Comparison of in situ trace element concentration of soil water with concentration in aqueous extracts as a background concentration level

机译:含水提取物浓度的土壤水原位痕量元素浓度的比较作为背景浓度水平

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This study compares concentrations of trace elements measured in soil water samples with concentrations determined in batch experiments as a background concentration level. One batch experiment was conducted at a liquid/solid (LS) ratio of 5 L/kg withsamples specifically adjusted for ionic strength using Ca(NO_3)_2 as the background electrolyte. The other is an aqueous extract at a LS ratio of 2 L/kg. Both batch experiments show similar results in their ability to estimate in situ concentrations. The results illustrate that for most trace elements the concentrations, which are determined in extracts, show statistically significant relations (p-value <0.01) with those measured in in situ soil percolation water. The level of fit measured by R~2 increases in the following order Pb, Cr
机译:该研究比较了在土壤水样中测量的痕量元素的浓度,该浓度在批量实验中测定为背景浓度水平。在使用Ca(NO_3)_2作为背景电解质,以5L / kg的液/固体(LS)比以5L / kg的液体/固体(LS)比进行5L / kg的粉碎试验。另一个是LS比为2L / kg的水性提取物。两种批量实验表明它们在其原位浓度估计的能力类似的结果。结果表明,对于大多数微量元素,在提取物中确定的浓度显示出统计学上显着的关系(p值<0.01),其中与原位土壤渗碳水中测量的那些。通过R〜2测量的拟合水平在下列顺序Pb,Cr <如

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