用生长律方程反褶积法校正慢响应传感器数据的响应时间

IF 1.8 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Knut Ola Dølven, Juha Vierinen, Roberto Grilli, Jack Triest, Bénédicte Ferré
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引用次数: 0

摘要

精确的高分辨率测量对于提高我们对环境过程的理解至关重要。一些依赖于膜分离萃取技术的化学传感器由于依赖于分离被测介质(即测量室)和感兴趣介质(即溶剂)的膜上的平衡分配,响应时间较慢。我们提出了一种利用统计逆理论对慢速传感器响应信号进行反卷积的新技术;应用带生长律的加权线性最小二乘估计量作为测量模型。利用模型稀疏性对解决方案进行正则化,假设测量量在特定的时间步长发生变化,这可以根据特定领域的知识或l曲线分析来选择。该方法的优点是:(1)建模误差传播,提供响应时间校正信号的显式不确定性估计;(2)能够对溶液的自一致性进行评价;(3)只需要仪器精度、响应时间和数据作为输入参数。通过模拟、实验室和现场测量证明了该技术的功能。在野外试验中,信号反褶积后,慢响应甲烷传感器的决定系数(R2)较替代的快速响应甲烷传感器显著提高,从0.18提高到0.91。这表明所提出的方法可以为由于依赖扩散过程的有效性而遭受缓慢响应时间的传感器和方法开辟相当广泛的应用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Response time correction of slow-response sensor data by deconvolution of the growth-law equation
Accurate high-resolution measurements are essential to improve our understanding of environmental processes. Several chemical sensors relying on membrane separation extraction techniques have slow response times due to a dependence on equilibrium partitioning across the membrane separating the measured medium (i.e., a measuring chamber) and the medium of interest (i.e., a solvent). We present a new technique for deconvolving slow-sensor-response signals using statistical inverse theory; applying a weighted linear least-squares estimator with the growth law as a measurement model. The solution is regularized using model sparsity, assuming changes in the measured quantity occur with a certain time step, which can be selected based on domain-specific knowledge or L-curve analysis. The advantage of this method is that it (1) models error propagation, providing an explicit uncertainty estimate of the response-time-corrected signal; (2) enables evaluation of the solution self consistency; and (3) only requires instrument accuracy, response time, and data as input parameters. Functionality of the technique is demonstrated using simulated, laboratory, and field measurements. In the field experiment, the coefficient of determination (R2) of a slow-response methane sensor in comparison with an alternative fast-response sensor significantly improved from 0.18 to 0.91 after signal deconvolution. This shows how the proposed method can open up a considerably wider set of applications for sensors and methods suffering from slow response times due to a reliance on the efficacy of diffusion processes.
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来源期刊
Geoscientific Instrumentation Methods and Data Systems
Geoscientific Instrumentation Methods and Data Systems GEOSCIENCES, MULTIDISCIPLINARYMETEOROLOGY-METEOROLOGY & ATMOSPHERIC SCIENCES
CiteScore
3.70
自引率
0.00%
发文量
23
审稿时长
37 weeks
期刊介绍: Geoscientific Instrumentation, Methods and Data Systems (GI) is an open-access interdisciplinary electronic journal for swift publication of original articles and short communications in the area of geoscientific instruments. It covers three main areas: (i) atmospheric and geospace sciences, (ii) earth science, and (iii) ocean science. A unique feature of the journal is the emphasis on synergy between science and technology that facilitates advances in GI. These advances include but are not limited to the following: concepts, design, and description of instrumentation and data systems; retrieval techniques of scientific products from measurements; calibration and data quality assessment; uncertainty in measurements; newly developed and planned research platforms and community instrumentation capabilities; major national and international field campaigns and observational research programs; new observational strategies to address societal needs in areas such as monitoring climate change and preventing natural disasters; networking of instruments for enhancing high temporal and spatial resolution of observations. GI has an innovative two-stage publication process involving the scientific discussion forum Geoscientific Instrumentation, Methods and Data Systems Discussions (GID), which has been designed to do the following: foster scientific discussion; maximize the effectiveness and transparency of scientific quality assurance; enable rapid publication; make scientific publications freely accessible.
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