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MEASUREMENT UNCERTAINTY ARISING FROM SAMPLING - IMPLICATIONS FOR THE OBJECTIVES OF GEOANALYSIS

机译:采样引起的测量不确定度-对地理分析目标的含义

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Four new methods for the estimation of the measurement uncertainty due to field sampling have been evaluated, by an application to soil sampling on contaminated land, The methods range in cast and complexity from one designed for a single sampler using one sampling protocol, to another designed for groups of different sampling organisations applying different sampling protocols, The size of the uncertainty arising from sampling is often large, ranging up to 55%, and this is much larger than the uncertainty generated by the analytical determinations in the laboratory (e.g., 5%), Although further applications of these methods to different geochemical sampling media are needed to confirm the generality of this finding, two implications seem important to the objectives of geoanalysis, Firstly, rather than simply measuring concentration values, geoanalysts need also to estimate the uncertainties on these measurements, Users of the concentration measurements can then propagate these uncertainty values through geochemical models, to give an estimate of the uncertainty in the interpretation. An example of this is given for the classification of contaminated land, Secondly, geoanalysts need to begin the estimation of uncertainty at the stage of field sampling, which is the first stage of the measurement, This will require the geoanalyst to be involved in the design of sampling as well as analytical protocols, The objective of geoanalysis should therefore be: 'to determine the composition of the earth and its parts, with realistic estimates of measurement uncertainty arising from both sampling and analysis'. Given this information it will then be possible for geoanalysts to decide objectively whether the quality of the measurements are fit-for-purpose. This will enable measurements with relatively high uncertainty (e.g., field sensors, laser ablation) to be shown to be fit For some purposes, and considered as equally valid-when compared with traditional laboratory-based techniques with lower uncertainty. [References: 24]
机译:通过将其应用于污染土地上的土壤采样,已经评估了四种新方法来估计由于野外采样而导致的测量不确定性。这些方法的类型和复杂性,从针对一种采样器的一种设计(使用一种采样方案)到另一种设计对于采用不同采样方案的不同采样组织的组,采样产生的不确定性的大小通常很大,高达55%,这远大于实验室中分析测定所产生的不确定性(例如5%)。 ),尽管需要将这些方法进一步应用到不同的地球化学采样介质中以证实这一发现的普遍性,但对于地质分析的目标而言,有两个含义似乎很重要:首先,除了简单地测量浓度值外,地球分析人员还需要估算不确定性这些测量值,浓度测量值的用户可以传播这些不确定性通过地球化学模型获得nty个值,以估算解释中的不确定性。举例说明了受污染土地的分类,其次,地质分析人员需要在现场采样阶段(测量的第一步)开始不确定性的估算,这将要求地质分析人员参与设计。因此,地球分析的目标应该是:“确定地球及其部分的组成,并从采样和分析中得出对测量不确定度的现实估计”。有了这些信息,地球分析人员就可以客观地确定测量质量是否适合目的。与具有较低不确定性的传统基于实验室的技术相比,这将使得具有较高不确定性的测量(例如,场传感器,激光烧蚀)被证明适合某些目的,并且被认为具有同等有效性。 [参考:24]

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