| Literature DB >> 35552552 |
Masahiro Kohno1, Toshiaki Kamachi2, Koji Fukui1.
Abstract
Elucidation of the static states and dynamic behavior of oxygen and nitrogen dissolved in water is one of the most important issues in the life sciences. In the present study, experimental trials and theoretical calculations were performed based on the hypothesis that the dissolution of gas molecules in water is related to excitation by the Earth's magnetic field. Using quantum theories such as those used to describe electro magnetic resonance and nuclear magnetic resonance, this study investigated the states of oxygen, nitrogen and hydrogen dissolved in water. The results indicate that the Earth's magnetic field is involved in the bonding and dissociation of molecules at the gas-liquid interface. These calculations assessed the effect of a field strength of 1.0 x 10-4 T and reproduced the influences of temperature changes on dissolved gas concentrations. Molecular interactions caused by electromagnetic properties and the external geomagnetic field were found to affect intermolar bonding associated with water cluster structures. It is concluded that the binding between molecules typically attributed to Coulomb coupling by magnetic charge and van der Waals forces results from excitation in the Earth's magnetic field.Entities:
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Year: 2022 PMID: 35552552 PMCID: PMC9097990 DOI: 10.1371/journal.pone.0267391
Source DB: PubMed Journal: PLoS One ISSN: 1932-6203 Impact factor: 3.752
Fig 1EPR spectra of pure gaseous oxygen and of air acquired under ambient conditions.
The former and latter generated strong and weak peaks, respectively, for oxygen. EPR conditions: Resonance frequency 9.4566 GHz, resonance magnetic field 750 ± 500 mT, magnetic field modulation 100 kHz, modulation width 0.2 mT, amplification rate 100×, time constant 0.3 s, observation time 4 min.
Dissolved gas concentrations at specific temperatures (n = 2).
| Temperature (°C) | Cluster number of nH2O | O2(mol/l) | H2(mol/l) | N2 (mol/l) |
|---|---|---|---|---|
| 5 | 19.0 | 0.00159 | 0.00093 | |
| 10 | 19.8 | 0.00153 | 0.00088 | 0.00064 |
| 15 | 22.0 | 0.00137 | 0.00085 | |
| 20 | 24.8 | 0.00122 | 0.00081 | 0.00052 |
| 25 | 27.6 | 0.00110 | 0.00078 | 0.00048 |
| 30 | 31.0 | 0.00098 | 0.00074 | 0.00043 |
| 35 | 34.9 | 0.00087 | 0.00072 | |
| 40 | 39.8 | 0.00076 | 0.00069 | 0.00037 |
| 50 | 42.2 | 0.00072 | 0.00063 | 0.00033 |
*) Nitrogen concentrations were obtained from the Basic Handbook of Chemistry, Chemical Society of Japan [37]
**) The number of water clusters was calculated from the relative concentration ratio of oxygen dissolved and bulk water. It is a value calculated assuming that the molecular bond between water and oxygen maintains a steady state at the ratio 1836.4:1 due to the Coulomb force due to electric charge.
Fig 2Arrhenius plots for dissolved gases in pure water.
Legend: ◆: O2, ■: H2, ▲: N2.
Excitation energies provided by the Earth’s magnetic field at specific temperatures.
| Temp. (°C) | nH2O(x10-7) JT-1 | O2 (x10-7) JT-1 | H2 (x10-7) JT-1 | N2 (x10-7) JT-1 |
|---|---|---|---|---|
| 5 | 17.57 | 6.57 | 52.36 | |
| 10 | 16.89 | 6.31 | 49.54 | 26.43 |
| 15 | 15.18 | 5.67 | 47.86 | |
| 20 | 13.47 | 5.03 | 45.60 | 21.48 |
| 25 | 12.12 | 4.53 | 43.91 | 19.82 |
| 30 | 10.78 | 4.03 | 41.66 | 17.76 |
| 35 | 9.58 | 3.58 | 40.54 | |
| 40 | 8.39 | 3.14 | 38.85 | 15.28 |
| 50 | 7.93 | 2.96 | 35.47 | 13.63 |
Gibbs energy (ΔG) and magnetic moments for dissolved gases.
| Molecule | ΔG (kJ mol-1) | Magnetic moments (S and I) (JT-1) |
|---|---|---|
| O2 | +16.1 | -0.94 |
| N2 | +12.7 | -0.94 |
| H2 | +6.36 | -0.60 |
| nH2O | -55.4 | +1.00 |
Fig 3Relationship between the magnetic moments of gas molecules and gibs energy.