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确定X射线吸收测量的不确定性。

Determining the Uncertainty of X-Ray Absorption Measurements.

作者信息

Wojcik Gary S

机构信息

National Institute of Standards and Technology, Gaithersburg, MD 20899-8615.

出版信息

J Res Natl Inst Stand Technol. 2004 Oct 1;109(5):479-96. doi: 10.6028/jres.109.035. Print 2004 Sep-Oct.

Abstract

X-ray absorption (or more properly, x-ray attenuation) techniques have been applied to study the moisture movement in and moisture content of materials like cement paste, mortar, and wood. An increase in the number of x-ray counts with time at a location in a specimen may indicate a decrease in moisture content. The uncertainty of measurements from an x-ray absorption system, which must be known to properly interpret the data, is often assumed to be the square root of the number of counts, as in a Poisson process. No detailed studies have heretofore been conducted to determine the uncertainty of x-ray absorption measurements or the effect of averaging data on the uncertainty. In this study, the Poisson estimate was found to adequately approximate normalized root mean square errors (a measure of uncertainty) of counts for point measurements and profile measurements of water specimens. The Poisson estimate, however, was not reliable in approximating the magnitude of the uncertainty when averaging data from paste and mortar specimens. Changes in uncertainty from differing averaging procedures were well-approximated by a Poisson process. The normalized root mean square errors decreased when the x-ray source intensity, integration time, collimator size, and number of scanning repetitions increased. Uncertainties in mean paste and mortar count profiles were kept below 2 % by averaging vertical profiles at horizontal spacings of 1 mm or larger with counts per point above 4000. Maximum normalized root mean square errors did not exceed 10 % in any of the tests conducted.

摘要

X射线吸收(或更确切地说是X射线衰减)技术已被应用于研究诸如水泥浆、砂浆和木材等材料中的水分移动和含水量。在试样某一位置处,随着时间推移X射线计数的增加可能表明含水量的降低。为了正确解释数据,必须了解X射线吸收系统测量的不确定性,通常假定其为计数数量的平方根,就像在泊松过程中一样。迄今为止,尚未进行详细研究来确定X射线吸收测量的不确定性或平均数据对不确定性的影响。在本研究中,发现泊松估计能够充分近似水试样点测量和剖面测量计数的归一化均方根误差(不确定性的一种度量)。然而,当对来自浆体和砂浆试样的数据进行平均时,泊松估计在近似不确定性大小时并不可靠。不同平均程序导致的不确定性变化可以用泊松过程很好地近似。当X射线源强度、积分时间、准直器尺寸和扫描重复次数增加时,归一化均方根误差会降低。通过以1毫米或更大的水平间距对垂直剖面进行平均,且每点计数高于4000,浆体和砂浆平均计数剖面的不确定性可保持在2%以下。在进行的任何测试中,最大归一化均方根误差均未超过10%。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4d72/4849570/0a4b7ea01c3e/j95wojf1.jpg

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