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梅利奇3法作为植物养分通用提取剂的实验室间验证。

Interlaboratory validation of the Mehlich 3 method as a universal extractant for plant nutrients.

作者信息

Schroder Jackie L, Zhang Hailin, Richards Jaben R, Payton Mark E

机构信息

Oklahoma State University, Department of Plant and Soil Sciences, Stillwater, OK 74078, USA.

出版信息

J AOAC Int. 2009 Jul-Aug;92(4):995-1008.

Abstract

The Mehlich 3 (M3) method is widely used to extract plant-available phosphorus from soil over a wide range of pH values. The method is also used by many laboratories to determine multiple plant-available nutrients simultaneously. However, except for P, this method has not been statistically validated within and among laboratories. The objective of this study was to determine the repeatability (within-laboratory performance) and reproducibility (among-laboratories performance) of the M3 method for several different nutrients by using a wide variety of soils. An in-house homogeneity test was conducted for 11 soils. Three replicates of each of the 11 soils were sent to 23 domestic and international laboratories for analyses primarily for K, Ca, Mg, Zn, Mn, Fe, and Cu. Samples were scooped, weighed, or both scooped and weighed for extraction. The various nutrients in the extracts were quantified by the participating laboratories by using inductively coupled plasma-atomic emission spectrometry. Ranges (in parentheses) of the repeatability relative standard deviation (RSDr) values for the scooped samples were K (3.88-6.14%), Ca (2.19-10.6%), Mg (2.27-5.73%), Zn (4.11-42.7%), Mn (3.15-8.53%), Fe (2.32-7.74%), and Cu (3.65-11.2%). For the weighed samples, the ranges (in parentheses) of the RSDr values were K (1.65-4.65%), Ca (1.43-16.9%), Mg (1.37-9.83%), Zn (2.60-33.0%), Mn (1.61-4.90%), Fe (1.56-4.47%), and Cu (2.95-17.9%). Ranges (in parentheses) of the reproducibility relative standard deviation (RSDR) values for the scooped samples were K (7.44-20.0%), Ca (7.10-33.5%), Mg (7.63-26.4%), Zn (11.6-48.7%), Mn (10.5-19.7%), Fe (12.4-22.0%), and Cu (8.86-45.3%). Ranges (in parentheses) of the RSDR values for the weighed samples were K (3.47-12.7%), Ca (7.61-34.6%), Mg (7.53-29.0%), Zn (10.6-49.2%), Mn (6.54-20.7%), Fe (11.0-21.5%), and Cu (9.73-43.0%). The Horwitz ratios (HorRat) were also used to evaluate the repeatability, HorRatr, and the reproducibility, HorRatR. Overall, the M3 method appears to be both repeatable and reproducible across the two categories for K, Mg, Zn, Mn, and Cu, and the vast majority of the HorRat values for both repeatability and reproducibility were within the acceptable range. However, a large number of soils in both the weighed and scooped categories displayed unacceptable HorRat values for the reproducibility of Ca and Fe, indicating that the M3 is not suitable for the extraction and quantitation of Ca and Fe in soils. The results of this study indicate that the M3 method for the determination of K, Mg, Zn, Mn, and Cu in soils is both accurate and precise when standardized procedures are used. The method has been proven to be suitable for use as a reference method for testing soil materials for extractable P, K, Mg, Zn, Mn, and Cu. Further study may be needed to confirm the suitability of the M3 method for Ca and Fe.

摘要

Mehlich 3(M3)方法被广泛用于在广泛的pH值范围内从土壤中提取植物有效磷。许多实验室也使用该方法同时测定多种植物有效养分。然而,除了磷之外,该方法在实验室内部和实验室之间尚未经过统计学验证。本研究的目的是通过使用多种土壤来确定M3方法对几种不同养分的重复性(实验室内部性能)和再现性(实验室之间性能)。对11种土壤进行了内部均匀性测试。将11种土壤中的每种土壤的三个重复样发送到23个国内外实验室进行分析,主要分析钾、钙、镁、锌、锰、铁和铜。样品通过铲取、称重或铲取并称重的方式进行提取。参与实验室使用电感耦合等离子体原子发射光谱法对提取物中的各种养分进行定量。铲取样品的重复性相对标准偏差(RSDr)值范围(括号内)为:钾(3.88 - 6.14%)、钙(2.19 - 10.6%)、镁(2.27 - 5.73%)、锌(4.11 - 42.7%)、锰(3.15 - 8.53%)、铁(2.32 - 7.74%)和铜(3.65 - 11.2%)。对于称重样品,RSDr值范围(括号内)为:钾(1.65 - 4.6%)、钙(1.43 - 16.9%)、镁(1.37 - 9.83%)、锌(2.60 - 33.0%)、锰(1.61 - 4.90%)、铁(1.56 - 4.47%)和铜(2.95 - 17.9%)。铲取样品的再现性相对标准偏差(RSDR)值范围(括号内)为:钾(7.44 - 20.0%)、钙(7.10 - 弦.5%)、镁(7.63 - 26.4%)、锌(11.6 - 48.7%)、锰(10.5 - 19.7%)、铁(12.4 - 22.0%)和铜(8.86 - 45.3%)。对于称重样品,RSDR值范围(括号内)为:钾(3.47 - 12.7%)、钙(7.61 - 34.6%)、镁(7.53 - 29.0%)、锌(10.6 - 49.2%)、锰(6.54 - 20.7%)、铁(11.0 - 21.5%)和铜(9.73 - 43.0%)。Horwitz比率(HorRat)也用于评估重复性(HorRatr)和再现性(HorRatR)。总体而言,M3方法在钾、镁、锌、锰和铜这两类中似乎既具有重复性又具有再现性,并且重复性和再现性的绝大多数HorRat值都在可接受范围内。然而,称重和铲取类别中的大量土壤在钙和铁的再现性方面显示出不可接受的HorRat值,这表明M3方法不适用于土壤中钙和铁的提取和定量。本研究结果表明,当使用标准化程序时,M3方法用于测定土壤中的钾、镁、锌锰和铜既准确又精确。该方法已被证明适合用作测试土壤材料中可提取磷、钾、镁、锌、锰和铜的参考方法。可能需要进一步研究以确认M3方法对钙和铁的适用性。

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