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Measuring small propagation frequency shifts and fluctuations by phase to avoid cross-correlation errors

机译:按相位测量微小的传播频率偏移和波动,以避免互相关误差

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This paper investigates the practicality of measuring microhertz to millihertz frequency differences by phase differences using an off-the-shelf SDR receiver. The phase difference method is two orders of magnitude faster if the phase can be measured to 3.60. The method has been used to confirm the discovery of a 16.2 (±1) μHz red-shift of the frequency over a 190 km ground wave path. The estimate by extrapolation from previous ionospheric HF measurements is 15-20 μHz on a transmitter absolute frequency error of ~1 mHz. The mechanism now assumed is that the frequency red-shift is proportional to the curvature angle of the path, and also proportional to the square root of frequency. The new Propagation-Phase/Frequency-Shift (PPFS) theory is now being analysed using a new Coupling-Graph technique. It is based on the `Filamentary Model of Electromagnetism' originally announced in 2011. It further supports the concept of EM detection and generation of gravity-potential-waves. The phase-difference method is found to be impervious self- and cross-correlation random `spurs' and `spectrum-collapse' that can bedevil phase noise measurements.
机译:本文研究了使用现成的SDR接收器通过相位差测量微赫至毫赫频率差的实用性。如果可以将相位测量为3.6,则相位差方法的速度要快两个数量级 0 。该方法已用于确认在190 km地波路径上发现频率的16.2(±1)μHz红移。在〜1 mHz的发射机绝对频率误差下,根据先前的电离层HF测量推断得出的估计值为15-20μHz。现在假定的机制是频率红移与路径的曲率角成比例,并且也与频率的平方根成正比。现在正在使用一种新的耦合图技术来分析新的传播相/频移(PPFS)理论。它基于2011年最初发布的“电磁丝模型”。它进一步支持EM检测和重力势波生成的概念。发现相位差方法是不可渗透的自相关和互相关的随机“杂散”和“频谱崩溃”,可能会干扰相位噪声的测量。

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