E. Emilia, L. Destiarti, Adhitiyawarman Adhitiyawarman
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摘要

泥炭水在不同的地方具有不同的特征。所提到的特征包括有机物、pH值、电导率和浊度的水平。基于这些差异,有必要研究采用单独的校准方法确定分析参数以及基质差异对锰含量的影响,并使用紫外可见分光光度计进行标准添加。锰的测定采用过硫酸盐法,即在酸性热气氛中,用过硫酸盐氧化水中的锰,生成紫红色的二氧化锰。单独标定法测定分析参数的精密度为7.75% ~ 63.96%,准确度为0.80% ~ 5.24%,线性度为r = 0.997,检出限为0.170 ppm,定量限为0.567 ppm。同时,加法法的精密度为2.19% ~ 20.35%,在I、II、III点的精密度和线性度分别为10.65% ~ 25.47%;20.9% ~ 26.8%;2.76% ~ 27.24%, 0.995;0.999;0.995. 此外,各点的线性度及校准曲线均满足SNI 6989.5: 2009的最小值(R≥0.995)。另外,根据对单独校准和标准添加的水平的结果比较,其值不同,但t检验的结果在t计数中结果一致
本文章由计算机程序翻译,如有差异,请以英文原文为准。
PENENTUAN KADAR MANGAN (Mn) PADA AIR GAMBUT SECARA SPEKTROFOTOMETRI UV-Vis DENGAN PERBANDINGAN METODE KURVA KALIBRASI DAN ADISI STANDAR (DETERMINATION OF MANGANESE IN PEAT WATER USING UV-Vis SPECTROPHOTOMETER: COMPARATION OF CALIBRATION OF CURVE AND STANDARD ADDITION METHOD)
Peat water has different characteristics from one location to another. The characteristics referred to include levels of organic matter, pH, conductivity, and turbidity. Based on these differences, it is necessary to research to determine the analytic parameters and the effect of matrix differences on manganese levels using a separate calibration method and standard addition using a Uv-vis spectrophotometer. The determination of manganese was carried out by the persulfate method, that is the oxidation of Mn in water by persulfate in an acidic and hot atmosphere to form MnO4 which is purple-red. The obtained results from the determination of the analytical parameters of the separate calibration method are precision of 7.75% to 63.96%, an accuracy of 0.80% to 5.24%, the linearity of r = 0.997, a detection limit of 0.170 ppm, and a limit of quantification of 0.567 ppm. Meanwhile, the addition method produces a precision of 2.19% to 20.35%, accuracy and linearity at points I, II, III are 10.65% to 25.47% respectively; 20.9% to 26.8%; 2.76% to 27.24% and 0.995; 0.999; 0.995. Linearity in addition as well as in calibration curves at all points have met the minimum value of SNI 6989.5: 2009 (R ≥ 0.995). In addition, based on the results of the comparison of the levels of the separate calibration and standard additions, the values are different, but the results of the t-test result in t-count
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