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Adequacy of laser diffraction for soil particle size analysis

机译:激光衍射在土壤粒径分析中的适用性

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摘要

Sedimentation has been a standard methodology for particle size analysis since the early 1900s. In recent years laser diffraction is beginning to replace sedimentation as the prefered technique in some industries, such as marine sediment analysis. However, for the particle size analysis of soils, which have a diverse range of both particle size and shape, laser diffraction still requires evaluation of its reliability. In this study, the sedimentation based sieve plummet balance method and the laser diffraction method were used to measure the particle size distribution of 22 soil samples representing four contrasting Australian Soil Orders. Initially, a precise wet riffling methodology was developed capable of obtaining representative samples within the recommended obscuration range for laser diffraction. It was found that repeatable results were obtained even if measurements were made at the extreme ends of the manufacturer’s recommended obscuration range. Results from statistical analysis suggested that the use of sample pretreatment to remove soil organic carbon (and possible traces of calcium-carbonate content) made minor differences to the laser diffraction particle size distributions compared to no pretreatment. These differences were found to be marginally statistically significant in the Podosol topsoil and Vertosol subsoil. There are well known reasons why sedimentation methods may be considered to ‘overestimate’ plate-like clay particles, while laser diffraction will ‘underestimate’ the proportion of clay particles. In this study we used Lin’s concordance correlation coefficient to determine the equivalence of laser diffraction and sieve plummet balance results. The results suggested that the laser diffraction equivalent thresholds corresponding to the sieve plummet balance cumulative particle sizes of < 2 μm, < 20 μm, and < 200 μm, were < 9 μm, < 26 μm, < 275 μm respectively. The many advantages of laser diffraction for soil particle size analysis, and the empirical results of this study, suggest that deployment of laser diffraction as a standard test procedure can provide reliable results, provided consistent sample preparation is used.
机译:自1900年代初以来,沉淀一直是进行粒度分析的标准方法。近年来,激光衍射已开始取代沉淀法,在某些行业中,例如海洋沉积物分析,已成为首选技术。然而,对于具有不同范围的粒径和形状的土壤的粒径分析,激光衍射仍需要对其可靠性进行评估。在这项研究中,采用基于沉降的筛子垂降平衡法和激光衍射法来测量代表四个相反澳大利亚土壤阶的22个土壤样品的粒径分布。最初,开发了一种精确的湿法刻划方法,该方法能够在推荐的遮蔽范围内获得代表性样品,用于激光衍射。发现即使在制造商建议的遮蔽范围的极端进行测量,也可以获得可重复的结果。统计分析的结果表明,与不进行预处理相比,使用样品预处理除去土壤有机碳(以及可能的痕量碳酸钙含量)对激光衍射粒度分布的影响很小。发现这些差异在Podosol表层土壤和Vertosol下层土壤中具有统计学上的显着性。众所周知,为什么可以采用沉降法“高估”板状粘土颗粒,而激光衍射会“低估”粘土颗粒的比例。在这项研究中,我们使用Lin的一致性相关系数来确定激光衍射和筛子直线下降平衡结果的等效性。结果表明,与<2μm,<20μm和<200μm的筛子对中平衡累积粒度相对应的激光衍射等效阈值分别为<9μm,<26μm和<275μm。激光衍射在土壤粒径分析中的许多优势以及本研究的经验结果表明,如果使用一致的样品制备方法,则将激光衍射作为标准测试程序进行部署可以提供可靠的结果。

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