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Radio Ground Wave Monitoring of Lake Salinity

机译:湖泊盐度的无线电地波监测

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The propagation loss over the Earth's surface of vertically polarised high frequency (3-30 MHz) radio ground wave signals is dependent on the radio frequency, path length and, in particular, on the electrical conductivity and relative permittivity of the surface medium. The electrical conductivity of water is directly related to its concentration of dissolved salts, or salinity. This paper reports an extended series of trial measurements of the salinity of Lake Alexandrina, at the mouth of the Murray River in South Australia, over an interval of almost 2 years, using the frequency-dependent ground wave loss technique. Each measurement provided a single "average" value of salinity over the propagation path. Excellent agreement was obtained with conventional laboratory measurements on water samples taken from an adjacent point of the lake at almost the same time. The success of the measurement program suggests a system for operational use which, in conjunction with a water temperature sensor and a communications link, would provide a convenient means of automatically monitoring the solinity of lakes and rivers from a remote laboratory.
机译:垂直极化的高频(3-30 MHz)无线电地波信号在地球表面上的传播损耗取决于无线电频率,路径长度,尤其取决于表面介质的电导率和相对介电常数。水的电导率与其溶解盐的浓度或盐度直接相关。本文使用频率相关的地波损耗技术,对南澳大利亚州墨累河河口亚历山大湖的盐度进行了一系列扩展的试验测量,历时近两年。每次测量都在传播路径上提供了一个单一的盐度“平均”值。用常规实验室测量几乎在同一时间从湖的相邻点采集的水样获得了极好的一致性。测量程序的成功表明,该系统可与水温传感器和通信链路结合使用,为操作使用提供了一种方便的方法,可从远程实验室自动监测湖泊和河流的溶解度。

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