Key result
Novel pipeline links Schumann resonance to heart rate variability using 730,000 Holter recordings.
Why the study?
Whether Schumann resonance dynamics are associated with human autonomic nervous system activity indexed by heart rate variability remains an open empirical question, and currently available open datasets lack large-scale, time-synchronized physiological recordings needed to address it rigorously.
Does Schumann resonance activity associate with human autonomic nervous system activity as indexed by frequency-domain heart rate variability when controlling for geomagnetic activity (Kp index)?
Does Schumann resonance activity associate with human autonomic nervous system activity as indexed by frequency-domain heart rate variability when controlling for geomagnetic activity (Kp index)?
This feasibility study establishes the analytical pipeline and study design requirements—specifically time-synchronized physiological and environmental datasets controlling for the Kp geomagnetic index—needed to rigorously test whether Schumann resonance dynamics couple with human heart rate variability.
SR-HRV association remains unproven; leaves open whether geomagnetic activity influences human autonomic function.
Schumann resonance (SR) is a global electromagnetic phenomenon generated within the Earth–ionosphere cavity, with a fundamental frequency near 7.83 Hz. Whether SR dynamics are associated with human autonomic nervous system activity as indexed by heart rate variability (HRV) remains an open empirical question. Addressing this question rigorously requires (a) large-scale, time-synchronized physiological datasets, (b) continuous SR monitoring with precise timestamps, and (c) control for geomagnetic activity (Kp index) as a major confounding variable. Currently available open datasets do not yet satisfy condition (a). Rather than forcing premature physiological conclusions, this paper presents a feasibility and methodology study that characterizes each data source, demonstrates the analysis pipeline on representative data, and identifies the design requirements for a future definitive study. Frequency-domain HRV indices were characterized using approximately 730,000 24-h Holter ECG recordings from the Allostatic State Mapping by Ambulatory ECG Repository (ALLSTAR). Broadband voltage SD (segment-wise standard deviation of AC-coupled voltage, used solely as a descriptive amplitude proxy) was characterized using the publicly available Mendeley Schumann Resonance Dataset (35 min segments, ~525,000 samples each). A partial correlation framework that controls for the NOAA Kp geomagnetic index is proposed and evaluated through simulation on representative parameter sets. Because the HRV and SR datasets were not collected at the same time or location, no direct physiological inference is drawn from their comparison. The reported association statistics are illustrative demonstrations of the pipeline applied to representative data, not empirical evidence of SR–HRV coupling. These findings define the data requirements and analytical methodology for future synchronized SR–HRV–Kp studies.
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Yuda et al. (2026) studied Autonomic nervous system activity indexed by heart rate variability (HRV) (n=730,000). Schumann resonance (SR) dynamics and partial correlation analytical pipeline controlling for NOAA Kp geomagnetic index was evaluated on Frequency-domain heart rate variability (HRV) indices and association statistics with Schumann resonance broadband voltage SD. A partial correlation pipeline integrating ~730,000 24-h Holter ECGs and 35-min SR segments (~525,000 samples) demonstrated methodology for future synchronized SR-HRV studies.
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