调查大地遥感卫星数据用于地面电导率连续监测:对翁多西部中频传播的影响

R.A. Adenodi, A. Ikusika
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摘要

地面导电率(GEC)有许多应用,因此值得继续研究。除了无线电发射机和接收机的配置外,它还是中频(MF)波段无线电波电场强度的主要决定因素。通常的测量方法是研究人员和测量仪器都与地面直接接触,并以预先确定的固定间隔进行测量,以确保良好的空间覆盖和均匀的空间分布。 当研究区域较大时,直接方法就会变得繁琐,因为必须知道许可覆盖区域内的 GEC,这样才能预测电场强度。在规划阶段,这可确保许可区域的所有部分都能收到有用的信号,从而在任何时间和季节都能抑制干扰。这项研究的动机是利用大地遥感卫星估算 GEC 的可能性。这项研究利用大地遥感卫星图像首先估算归一化差异盐度指数,然后借助地图代数生成另一个栅格 2,其像素值就是 GEC。研究覆盖翁多西部地方政府区(OWLGA)967 公里的陆地面积。在分析过程中,GEC 被分为五个等级。结果显示,极低、低、中、高和极高 GEC 的范围分别为 0.124 至 0.437、0.438 至 0.937、0.938 至 1.635、1.636 至 2.524 和 2.525 至 3.600 mS/m,其平均值分别为 0.346 ± 0.109、0.754 ± 0.103、1.071 ± 0.089、1.351 ± 2 0.067 和 1.564 ± 0.106 mS/m,分别分散在 176.45、202.24、214.14、374.17 和 228.56 km 范围内。本研究记录的 GEC 值、其各自的覆盖范围和空间分布足够强大,足以在建立中波的情况下维持有用电场强度在翁多西部地方政府整个陆地上的传播。该研究建议对该地区 GEC 随时间的变化进行研究。
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Investigating Landsat data for continuous monitoring of ground electrical conductivity: implication for propagation at medium frequency in Ondo West
Ground electrical conductivity (GEC) has many applications, which makes it worthy of continuous research. Apart from the configurations  of the radio transmitter and receiver, it is a major determinant of the electric field intensity of radio waves in the Medium Frequency (MF)  band. It is usually measured in such a way that both the researcher and the measuring instrument are in direct contact with the ground,  and measurements are made at some predetermined constant intervals to ensure good spatial coverage and even spatial distribution.  The direct method becomes cumbersome when the field of study is large because the GEC over the licensed coverage area must be  known such that electric field intensity can be predicted. At the planning stage, this ensures all parts of the licensed region are reached by  useful signals that can suppress interference at all times and seasons. The study is motivated by the possibility of using Landsat to  estimate GEC. This study utilizes Landsat images to first estimate the normalized difference salinity index and then, with the aid of map  algebra, generate another raster 2 whose pixels' values are the GEC. The study covers a landmass of 967 km in the Ondo West Local  Government Area (OWLGA). During analysis, the GEC was divided into five classes. The results reveal that the ranges of very low, low,  moderate, high, and very high GEC are 0.124 to 0.437, 0.438 to 0.937, 0.938 to 1.635, 1.636 to 2.524, and 2.525 to 3.600 mS/m, which have  mean values of 0.346 ± 0.109, 0.754 ± 0.103, 1.071 ± 0.089, 1.351 ± 2 0.067, and 1.564 ± 0.106 mS/m, and are dispersed over 176.45, 202.24,  214.14, 374.17, and 228.56 km , respectively. The values of GEC, their respective coverage, and spatial distribution recorded in this study  are strong enough to sustain the propagation of useful electric field intensity over the entire landmass of Ondo West Local Government if  a medium wave is established. The study recommends that the change in GEC with time in this field be studied. 
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