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Sector Structure of Interplanetary Magnetic Field Influence upon the Results of the Measurements of Gravitational Constant
Abstract
The results of continues measurements of gravitational constant using installations of O.V. Karagios - V.P. Izmailov (1991) are compared with the data about sector structure of interplanetary magnetic field. It was obtained that the value measured is more systematically in the days of negative polarity. The same effect have been revealed also for Test-F of G. Piccardi. It is well known for some biologic indexes. The comparison and the analysis of different data show strongly that the agent influencing upon the installation is amplitude - spectral variations of electromagnetic background fields for the frequencies < 10 kHz. These fields modulate elastic parameters of the torsion pendulum's thread via the effect of magnetoelastisity.
... The difference is within the range of 10 −4 which was considered by Vladimirskii [2] to be the boundary for accuracy to infer G with torsion balances. Vladimirskii [2] and later Vladimirsky and Bruns [3] reported a source of variability that could account for the spread in G of ~400 ppm noted by Quinn et al. [1]. ...
... This source involved heliophysical perturbations as inferred by inferences of geomagnetic activity. Subtle variations in G which are systematically and quantitatively related to alterations in geomagnetic activity could be secondary to direct influences upon instrumentation [2] [3]. However if there is a third variable that is shared by both variation in G and geomagnetic activity, it may have both theoretical and practical significance. ...
... According to Figure 3 from [1] the means of the coefficients for G from 11 different sources range from 6.6725 to 6.6756 or ~3.1 × 10 −3 of an average for G. This value is within error measurement variability of 5.2 × 10 −3 reported [3] between days when the interplanetary magnetic field shifted from a positive to a negative sign and geomagnetic A p values ranged between −8 and +8 nT. In those previous measurements [2] between 29 August and 23 December 1991, the mean value for the coefficient of G was 6.6728 for the 77 measurements during which A p values were <15 nT and 6.6675 during the 48 measurements during which the A p values were >30 nT. ...
We compared the small quantitative changes (range) in G over repeated
measures (days) with recently improved methods of determinations and those
recorded over 20 years ago. The range in the Newtonian constant of gravitation
G is usually in the order of 400 ppm as reflected in experimentally-determined
values. The moderate strength negative correlation between daily fluctuations
in G, in the range of 3 × 10-3 of the average value, and an index of
global geomagnetic activity reported by Vladimirsky and Bruns in 1998 was also
found for the daily fluctuations in the angular deflection θ (in arcseconds) and geomagnetic activity within 24 hr for the
Quinn et al. 2013 data. A temporal
coupling between increases of geomagnetic activity in the order of 10-9 T with decreases in G in the order of 10-14 m3·kg-1·s-2 could suggest a recondite shared source of variance. The energy equivalence for
this change in G and geomagnetic activity within 1 L of water is ~3 × 10-14 J.
... A quantized unit for the gravitational field should be relatable to electromagnetism in a reasonable and quantitative manner. Previously Persinger and St-Pierre [9], by relating the superb measurements of variation in G by Vladimirsky and Bruns [10] and Quinn et al [11] to concurrent subtle changes in global geomagnetic activity and associated variations in the interplanetary magnetic field, reported a consistent inverse correlation between the two such that increases in empirical measurements of variations in G were associated with discrete decreases in concurrent electromagnetic intensities. Here I develop the argument by quantification that this inverse relationship between photon flux density and magnetic field strength generalizes across different Δts of measurement and creates the condition for the graviton to be verified as the integrating factor or at least one of the major integrating factors. ...
Measurements have shown an inverse association between natural electromagnetic intensities and irradiance from background photons. In general for every ~10-12 W·m-2 increase in photon radiant flux densitythere was a1 nT decrease in intensity of the ambient static (geo-)magnetic field. Dimensional equivalence of the two quantities required the latter to be multiplied by ~10-3 A·s-1. Assuming ~1079 particles universally, each with a unit charge, the rest mass of that particle would be ~10-65 kg or the median solution for the graviton. On the bases of the calculations and conceptual inferences, entanglement phenomena across the space-time that defines the universe could be mediated by a gravitational field whose quantized component, the mass of a graviton, when expressed as the square of the hypothetical entanglement velocity, is light. This velocity (1023 m·s-1) is derivable from independent approaches that require the consideration of the universe as a single set. If this inference derived form empirical measurements is valid, then there is additional evidence that “excess correlation†and entanglement of photons anywhere in the universe is mediated by quantized components of a gravitational field that is contained within the total spatial and temporal boundaries.
... Although gravitational energies were not apparent, it may not be spurious that the solution between 13-14 nT includes the range of interplanetary magnetic field strength that is associated with the variation in Newton's Gravitational constant as measured by two different researchers over a period of 30 years [14][15][16]. This magnetic flux density is also approximately half of the magnetic field strength (B) for the entire universe based upon the total energy estimate of ~2.2·10 69 J and when applied through a volume of 8.4·10 78 m 3 by the relationship: ...
The strength of the magnetic field for different ratios of matter densities relative to the permittivity of a vacuum solves for values approaching the velocity of light. When the strength of the field associated with densities similar to liquid water, ice, or stars (such as the Sun) is considered with respect to the magnetic permeability and average mass density of the universe, the emergent velocity is ~10 23 m•s -1 . This value has been derived from several approaches as the latency for excess correlation or “entanglement” and is consistent with a process that might explain the integrity of large-scale spatial structure over distances that are within fractions of the universe’s present diameter. The estimated latency to traverse this diameter with this velocity relative to the total duration of the universe (the final epoch) when considered as an Aharanov-Bohm type phase shift, results in an energy quantum that is convergent with Planck’s constant. One interpretation is that the duration of a single electron’s orbit is the phase shift between duration (latency) to traverse the universe and its total duration (final epoch). If this approach is valid then non-local effects and related excess correlations (Schrodinger’s “entanglement”) between photon emissions and specific dynamics of densities similar to liquid water may be a property of these conditions immersed within an average universal mass density of about one proton per cubic meter. It may also accommodate the challenges of understanding the apparent homogeneity across large scale space.
... Persinger and St-Pierre [74] quantitatively examined the results from the recent work by Quinn and his colleagues [75] and Vladimirsky et al. [76,77] from about twenty years ago. Both groups of researchers had found fluctuations in G that were in the range of 3·10 -3 of the average value for G. ...
... The average slope indicates that for every 1 nT increase in geomagnetic fluctuations there is a ~10 -12 W·m -2 decrease in photon emissions. Changes within the 1 to 20 nT range for the solar wind as it interacts with the magnetopause have been correlated negatively in two separate measurements [13] with the variations in G [14], which are in the order of 10 -3 of the actual constant. All of these empirical measures suggest that very small energies associated with geomagnetic activity, the background fluctuations in G, and global seismic energy radiation or some process that determines the numbers of discrete seismic events per day may share a source of variance with which more distal sources could interact. ...
... Typical daily fluctuations in G are within the range of ~3 × 10 −3 of the average value. Recently Persinger and St-Pierre [10] confirmed the relationship measured by Vladimirsky and Bruns [11] over 25 years ago that approximately 5 nT increases in ambient geomagnetic activity were associated with decreases in ΔG such that an increment of 10 −9 T and 10 −14 m 3 ·kg −1 ·s −2 might share the same source of variance. The energy equivalence for the ΔG and this magnitude of magnetic field intensity within 1 L of space converged to be ~3 × 10 −14 J [10]. ...
States of excess correlation have previously been achieved at macroscopic levels by simultaneously exposing two non-local spaces to weak electromagnetic field patterns, generated by toro-ids, presented in a sequence such that the angular velocity of the field is modulated by changes in frequency over time. Here we systematically investigated effects upon the local space at the center of a single toroid generating the excess correlation sequence. The results indicated that a 1-5 nT diminishment in field intensity on the Y-or east-west axis was characteristic of the excess correlation sequence which was not indicated for control conditions. Statistically significant shifts in field intensity approximately 40 to 60 s before the onset of the first field associated with the excess correlation sequence indicated a temporally non-linear effect which converged upon the ratio of g and the rotational velocity of the Earth for the local space where Coriolis-like forces were inferred. Intensity shifts associated with the excess correlation sequence but not controls were quantitatively convergent upon parameters of the hydrogen line (1.42 GHz). Implications for these findings were discussed in relation to Mach's principle and, in particular, to the electron as a physical unit which was found to relate classical and quantum systems.
This paper is a short review of publications on the influence that solar activity and geomagnetic disturbances (cosmic weather)
have on physical-chemical systems. The effects of cosmic weather may some-times be detected by the presence of an uncontrolled
factor in these experiments. Direct reactions to cosmic weather are reliably identified in quantitative observations over
various test systems, mainly water solutions. The effects of cosmic weather are also found from the data obtained by monitoring
some simple physical systems, including semiconductors. All these effects are either cosmic physical rhythms or they are easily
registered sporadic heliogeophysical events (e.g., magnetic storms). There are convincing data that demonstrate the influence
that cosmic weather has on the accident rate in various engineering and physical systems. Researchers are at odds on the physical
nature of the main physical agent, but the contribution of electromagnetic fields to these processes is considered important.
Keywordscosmic weather–physical-chemical systems–technosphere–accident rate
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