用于精细尺度生态水文测量的激光水位传感器的研制

J. Benjamin, D. Kaplan
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引用次数: 3

摘要

蒸散发(ET)是全球水循环的一个关键组成部分,但由于缺乏准确和负担得起的传感器技术,很难对其进行估计。在地下水位接近地表的地区,测量特定地点ET的一种低成本方法是利用由ET驱动的地表水和地下水的日波动。这种方法需要高度敏感的测量来准确量化地下水位变化。这项工作的目标是开发和测试一种基于激光的水位传感器(LB-WLS),以改进通过水位日变化对ET的估计。在实验室和远程环境下,将LB-WLS与传统的总压力传感器(TPT)进行了比较。LB-WLS具有较低的残余噪声,平均均方根误差(RSE)为0.05±0.04 cm,而TPT传感器的均方根误差为0.19±0.16 cm。虽然传感器的开发仍在进行中,但这种性能水平代表了地表水和地下水精细监测的重大改进。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Development of a laser-based water level sensor for fine-scale ecohydrological measurements
Evapotranspiration (ET) is a critical component of the global water cycle, but one that is difficult to estimate due in part to a lack of accurate and affordable sensor technology. One low-cost approach to measuring site-specific ET in areas where the water table is close to the surface is to take advantage of the diurnal fluctuations in surface water and groundwater driven by ET. This method requires highly sensitive measurement to accurately quantify water table variation. The goal of this work is to develop and test a laser-based water level sensor (LB-WLS) to improve the estimate of ET via diurnal variations in water level. The LB-WLS was compared against traditional total pressure transducers (TPT) in both laboratory and remote settings. The LB-WLS was found to have lower residual noise, with an average Root Square Error (RSE) of 0.05±0.04 cm, compared to 0.19±0.16 cm for the TPT sensor. While sensor development is ongoing, this level of performance represents a major improvement in fine-scale monitoring of surface water and groundwater.
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