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arXiv 1602.04469physics.geo-phphysics.ins-det
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Cosmic-Ray中子土壤水分足迹特征修正

Footprint Characteristics Revised for Field-Scale Soil Moisture Monitoring with Cosmic-Ray Neutrons

M. Köhli, M. Schrön, M. Zreda, U. Schmidt, P. Dietrich, S. Zacharias

摘要:

宇宙射线中子探测器被广泛用于监测地表附近的环境含水量。该方法平均覆盖数十公顷,在为百米尺度的农业和水文模型提供代表性数据方面无可匹敌。然而,最近的实验表明,传感器对环境异质性的反应还没有完全理解。对支持体积的了解是正确解释和验证水文地球物理数据的先决条件。在以前的研究中,几个物理简化已被引入到中子输运模型,以获得宇宙射线探测器的足迹的特性。我们利用一个完善的宇宙射线中子源和能谱,并模拟它们对各种环境条件的响应。结果表明,该方法是特别敏感的土壤水分在探头周围的前几十米,而径向权重是动态变化的环境水。根据空气的湿度、土壤湿度和植被的不同,足迹半径在130至240米之间。15至83 cm的湿度相关穿透深度随着到传感器的距离呈指数下降。然而,足迹圆保持几乎各向同性的复杂地形附近的河流,道路或山坡。我们的研究结果表明,一个动态加权平均点测量是必不可少的准确的校准和验证。新的见解将对信号解释,传感器安装,移动调查的数据插值以及选择适当的分辨率进行水文模型数据同化产生重要影响。

英文摘要:

Cosmic-ray neutron probes are widely used to monitor environmental water content near the surface. The method averages over tens of hectares and is unrivaled in serving representative data for agriculture and hydrological models at the hectometer scale. Recent experiments, however, indicate that the sensor response to environmental heterogeneity is not fully understood. Knowledge of the support volume is a prerequisite for the proper interpretation and validation of hydrogeophysical data. In a previous study, several physical simplifications have been introduced into a neutron transport model in order to derive the characteristics of the cosmic-ray probe's footprint. We utilize a refined source and energy spectrum for cosmic-ray neutrons and simulate their response to a variety of environmental conditions. Results indicate that the method is particularly sensitive to soil moisture in the first tens of meters around the probe, whereas the radial weights are changing dynamically with ambient water. The footprint radius ranges from 130 to 240 m depending on air humidity, soil moisture and vegetation. The moisture-dependent penetration depth of 15 to 83 cm decreases exponentially with distance to the sensor. However, the footprint circle remains almost isotropic in complex terrain with nearby rivers, roads or hill slopes. Our findings suggest that a dynamically weighted average of point measurements is essential for accurate calibration and validation. The new insights will have important impact on signal interpretation, sensor installation, data interpolation from mobile surveys, and the choice of appropriate resolutions for data assimilation into hydrological models.

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