Annual Variation of Local Photon Emissions’ Spectral Power within the mHz Range Overlaps with Seismic-Atmospheric Acoustic Oscillations
Michael A. Persinger
Laurentian University, Sudbury, Canada.
DOI: 10.4236/ijg.2012.31021   PDF    HTML     7,037 Downloads   9,919 Views   Citations

Abstract

Spheroidal modes of seismic and acoustic oscillations in the atmosphere occur within the 2 to 7 mHz range with peak-to-peak variations in the order of 10–12 to 10–11 m·s–2. Previous research indicated the amplitudes for 230 s and 270 s periods peak during the summer months. In the present study the amplitudes of a reliably apparent 3 mHz increment from spectral analyses of minute-to-minute measurements of background photon emissions by a photomultiplier tube housed in a dark room were sampled for a one year period. The peak increase in the power of this increment was maximal during the summer months and overlapped conspicuously with the annual variation in fundamental spheroidal modes of seismic free oscillations. Quantitative estimates indicate that relative shifts in the order of 10–11 W/m2 for photon emissions may reflect the annual variation in coupled oscillations between the earth and atmosphere.

Share and Cite:

M. Persinger, "Annual Variation of Local Photon Emissions’ Spectral Power within the mHz Range Overlaps with Seismic-Atmospheric Acoustic Oscillations," International Journal of Geosciences, Vol. 3 No. 1, 2012, pp. 192-194. doi: 10.4236/ijg.2012.31021.

Conflicts of Interest

The authors declare no conflicts of interest.

References

[1] T. Tanimoto, J. Ulm, K. Nishida and N. Kobayashi, “Earth’s Continuous Oscillations Observed on Seismically Quiet Days,” Geophysical Letters, Vol. 25, No. 10, 1998, pp. 1553- 1563. doi:10.1029/98GL01223
[2] J. Rhie and B. Romanowicz, “Excitation of Earth’s Con- tinuous Free Oscillations by Atmospheric-Ocean-Seafloor Coupling,” Nature, Vol. 431, 2004, pp. 552-555. doi:10.1038/nature02942
[3] K. Nishida, N. Kobayashi and Y. Fukao, “Resonant Osci- llations between the Solid Earth and the Atmosphere,” Science, Vol. 287, No. 5461, 2000, pp. 2244-2246. doi:10.1126/science.287.5461.2244
[4] M. A. Persinger, B. T. Dotta and G. F. Lafreniere, “Marked Increases in Background Photon Emissions in Sudbury On- tario More than One Week before the Magnitude > 8.0 Earthquakes in Japan and Chile,” in submission.
[5] B. T. Dotta, C. A. Buckner, D. Cameron, R. M. Lafrenie and M. A. Persinger, “Biophoton Emissions from Cell Cultures: Biochemical Evidence for the Plasma Membrane as the Primary Source,” General Physiology and Biophy- sics, Vol. 30, No. 4, 2011, pp. 301-309.
[6] W. H. Campbell, “Introduction to Geomagnetic Fields,” Cambridge University Press, Cambridge, 1997.
[7] A. D. Bershadky, N. Q. Balaban and B. Geiger, “Adhe- sion-Dependent Cell Mechanosensitivity,” Annual Reviews of Cell Developmental Biology, Vol. 19, 2003, pp. 677-695.
[8] M. A. Persinger, “A Simple Estimate for the Mass of the Universe: Dimensionaless Parameter A and the Construct of ‘Pressure’,” Journal of Physics, Astrophysics and Physi- cal Cosmology, Vol. 3, No. 1, 2010, pp. 1-3.
[9] B. T. Dotta, C. A. Buckner, R. M. Lafrenie and M. A. Persinger, “Photon Emissions From Human Brain and Cell Culture Exposed to Distally Rotating Magnetic Fields Shared by Separate Light-Stimulated Brains and Cells,” Brain Re- search, Vol. 1388, 2011, pp. 77-88. doi:10.1016/j.brainres.2011.03.001
[10] Y. Isojima, T. Isoshima, K. Nagai, K. Kikuchi and H. Na- kagawa, “Ultraweak Biochemiluninescence Detected from Rat Hippocampal Slices,” NeuroReports, Vol. 6, No. 4, 1995, pp. 658-660. doi:10.1097/00001756-199503000-00018
[11] F. A. Popp, “Electromagnetic Information,” Urban and Sch- wartzberg, New York, 1979, pp. 543-544.
[12] D. E.Winch, D. J. Ivers, J. P. R. Turner and R. J. Stening, “Geomagnetism and Schmidt Quasi-Normalization,” Geo- physical Journal International, Vol. 160, No. 2, 2005, pp. 487-504. doi:10.1111/j.1365-246X.2004.02472.x

Copyright © 2024 by authors and Scientific Research Publishing Inc.

Creative Commons License

This work and the related PDF file are licensed under a Creative Commons Attribution 4.0 International License.