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ERROR ANALYSIS AND QUALITY IMPROVEMENT OF THE COSHOCTON WEIGHING LYSIMETERS

机译:棉磅称重仪的误差分析和质量改进

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Weighing lysimeter-computed evapotranspiration (ET) is sometimes used to assess ET computer-model predictions and to compare water use under different management or climatic conditions. For any use of lysimeter-computed ET, the uncertainty associated with this value should be known and reported. The uncertainty associated with individual lysimeter-mass measurements has been previously presented, but ET-measurement uncertainty is a function of water-budget measurements (percolate volume, water-storage change, etc.), measurement-component uncertainty (uncertainty in mass and percolation measurements), and systematic error (e.g., load-cell and potentiometer slope bias). The Coshocton lysimeters were not sufficiently accurate to compute hourly ET to the desired depth resolution, thus a quality-improvement plan was initiated that utilized Pareto analysis. The objectives of this article are to: (1) derive expressions for ET uncertainty; (2) determine the effect of the quality-improvement procedures applied to the Coshocton lysimeters on ET-measurement uncertainty; (3) perform an error analysis on the measurement components of the improved Coshocton weighing lysimeters. The quality improvements reduced the ET uncertainty from 0.36 mm/d to 0.032 mm/d under the condition of no rainfall (ET and percolation only). The ET-measurement uncertainty of the improved Coshocton lysimeters was sensitive to various measurement components especially the number of rainfall events and the uncertainty associated with mass and percolation measurements. This indicates that the improved measurement systems of the Coshocton weighing lysimeters are sufficiently accurate to compute hourly ET, and that lysimeter-mass and percolation measurements should be monitored regularly (quality-control procedures should be followed).
机译:称量溶渗计计算的蒸散量(ET)有时用于评估ET计算机模型的预测,并比较不同管理或气候条件下的用水量。对于用溶渗仪计算的ET的任何使用,应该知道并报告与此值相关的不确定性。先前已经介绍了与单个溶渗仪质量测量相关的不确定性,但是ET测量不确定性是水预算测量(渗滤液体积,储水量变化等),测量成分不确定性(质量和渗滤不确定性)的函数测量值)和系统误差(例如,称重传感器和电位计的斜率偏差)。 Coshocton溶渗仪的精度不足以计算每小时的ET到所需的深度分辨率,因此启动了利用Pareto分析的质量改进计划。本文的目的是:(1)得出ET不确定性的表达式; (2)确定应用于Coshocton溶渗仪的质量改进程序对ET测量不确定性的影响; (3)对改进的Coshocton称重测渗仪的测量组件进行误差分析。在没有降雨的情况下(仅限ET和渗滤),质量改进将ET的不确定度从0.36 mm / d降低到0.032 mm / d。改进的Coshocton渗漏仪的ET测量不确定度对各种测量成分敏感,特别是降雨事件的数量以及与质量和渗滤测量相关的不确定度。这表明改进的Coshocton称重测渗仪的测量系统足够准确,可以计算每小时的ET,并且应定期监测测渗仪的质量和渗滤测量值(应遵循质量控制程序)。

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