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10.46243/jst.20xx.v9.i1.pp01-05 · How the Sun’s Core Changes the Direction of the Sun’s Magnetic Axes and Maintains the Sun’s Equilibrium, similarly to the Function of the Earth’s Core

APA (7th edition)

Yeshayahu Greitzer (2025). How the Sun’s Core Changes the Direction of the Sun’s Magnetic Axes and Maintains the Sun’s Equilibrium, similarly to the Function of the Earth’s Core. *Journal of Science & Technology*, *10*(09), 01–05. https://doi.org/10.46243/jst.20xx.v9.i1.pp01-05

⬇ text Italics are shown as *asterisks* in plain text — the journal or book title and the volume.

BibTeX

@article{yeshayahugreitzer2025suns,
  author    = {Yeshayahu Greitzer},
  title     = {{How the Sun’s Core Changes the Direction of the Sun’s Magnetic Axes and Maintains the Sun’s Equilibrium, similarly to the Function of the Earth’s Core}},
  journal   = {Journal of Science \& Technology},
  year      = {2025},
  month     = {sep},
  volume    = {10},
  number    = {09},
  pages     = {01--05},
  publisher = {Longman Publishers},
  issn      = {2456-5660},
  doi       = {10.46243/jst.20xx.v9.i1.pp01-05},
  url       = {https://doi.org/10.46243/jst.20xx.v9.i1.pp01-05},
  language  = {en},
  abstract  = {The Sun’s magnetic field shifts every eleven years, from north to south and vice versa. In my view, this occurs due to the movement of the Sun’s core from north to south and vice versa, in order to maintain the Sun’s equilibrium as it revolves around its axis from west to east. In principle, something similar occurs on Earth, as it revolves around its axis from west to east and its core moves alternately north or south, which allows the Earth to maintain its equilibrium, with its magnetic field shifting from north to south and vice versa. The essential difference between the Earth and the Sun in this regard is that the Sun is composed of gaseous material, while the Earth is composed of solid plastic and fluid material. The Sun’s gaseous mass moves and changes rapidly, so the Sun’s core is required to move rapidly in turn and change direction every eleven years in order to maintain the Sun’s equilibrium. Just as the changes that occur on the Earth, such as the movement of the continents or the creation of mountains, are relatively slow, in accordance so too the movement of the Earth’s core is slow and it shifts direction at intervals of from thousands to millions of years, with the time periods between changes being inconsistent.}
}

⬇ .bib

RIS (EndNote, Zotero, Mendeley)

TY  - JOUR
TI  - How the Sun’s Core Changes the Direction of the Sun’s Magnetic Axes and Maintains the Sun’s Equilibrium, similarly to the Function of the Earth’s Core
AU  - Yeshayahu Greitzer
JO  - Journal of Science & Technology
PY  - 2025
DA  - 2025/09/08/
VL  - 10
IS  - 09
SP  - 01
EP  - 05
PB  - Longman Publishers
SN  - 2456-5660
LA  - en
AB  - The Sun’s magnetic field shifts every eleven years, from north to south and vice versa. In my view, this occurs due to the movement of the Sun’s core from north to south and vice versa, in order to maintain the Sun’s equilibrium as it revolves around its axis from west to east. In principle, something similar occurs on Earth, as it revolves around its axis from west to east and its core moves alternately north or south, which allows the Earth to maintain its equilibrium, with its magnetic field shifting from north to south and vice versa. The essential difference between the Earth and the Sun in this regard is that the Sun is composed of gaseous material, while the Earth is composed of solid plastic and fluid material. The Sun’s gaseous mass moves and changes rapidly, so the Sun’s core is required to move rapidly in turn and change direction every eleven years in order to maintain the Sun’s equilibrium. Just as the changes that occur on the Earth, such as the movement of the continents or the creation of mountains, are relatively slow, in accordance so too the movement of the Earth’s core is slow and it shifts direction at intervals of from thousands to millions of years, with the time periods between changes being inconsistent.
DO  - 10.46243/jst.20xx.v9.i1.pp01-05
UR  - https://doi.org/10.46243/jst.20xx.v9.i1.pp01-05
ER  -

⬇ .ris

CSL-JSON

{
    "type": "article-journal",
    "id": "10.46243/jst.20xx.v9.i1.pp01-05",
    "DOI": "10.46243/jst.20xx.v9.i1.pp01-05",
    "URL": "https://doi.org/10.46243/jst.20xx.v9.i1.pp01-05",
    "title": "How the Sun’s Core Changes the Direction of the Sun’s Magnetic Axes and Maintains the Sun’s Equilibrium, similarly to the Function of the Earth’s Core",
    "source": "Smart Scholars DOI Registry",
    "container-title": "Journal of Science & Technology",
    "author": [
        {
            "family": "Yeshayahu Greitzer"
        }
    ],
    "issued": {
        "date-parts": [
            [
                2025,
                9,
                8
            ]
        ]
    },
    "volume": "10",
    "issue": "09",
    "page": "01-05",
    "publisher": "Longman Publishers",
    "language": "en",
    "abstract": "The Sun’s magnetic field shifts every eleven years, from north to south and vice versa. In my view, this occurs due to the movement of the Sun’s core from north to south and vice versa, in order to maintain the Sun’s equilibrium as it revolves around its axis from west to east. In principle, something similar occurs on Earth, as it revolves around its axis from west to east and its core moves alternately north or south, which allows the Earth to maintain its equilibrium, with its magnetic field shifting from north to south and vice versa. The essential difference between the Earth and the Sun in this regard is that the Sun is composed of gaseous material, while the Earth is composed of solid plastic and fluid material. The Sun’s gaseous mass moves and changes rapidly, so the Sun’s core is required to move rapidly in turn and change direction every eleven years in order to maintain the Sun’s equilibrium. Just as the changes that occur on the Earth, such as the movement of the continents or the creation of mountains, are relatively slow, in accordance so too the movement of the Earth’s core is slow and it shifts direction at intervals of from thousands to millions of years, with the time periods between changes being inconsistent.",
    "ISSN": "2456-5660"
}

⬇ .json What citeproc and reference managers read; the DOI system hands it out for Accept: application/vnd.citationstyles.csl+json, and so does this registry's resolver.

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