Toward an Intuitive Interpretation of Gauge Fields: Cross-Sectional Differences and Spherical Analysis

This paper proposes an intuitive reinterpretation of the gauge field equation Mathematically, FμνF_{\mu\nu}Fμν is defined as the antisymmetric derivative of a potential field, but its connection to real structures is not always clear. Here, we describe the gauge field as the difference between gradients observed when slicing a potential in orthogonal directions. If both views coincide (Fμν=0), the system is symmetric and structureless; if they differ, asymmetry appears, and a field emerges. To illustrate, an onion cut concentrically preserves symmetry and releases no liquid, whereas orthogonal cuts introduce asymmetry and cause fluid to spread. This “onion analogy” clarifies gauge fields as structural distortions. Moreover, spherical analysis—considering concentric shells—is argued to be more realistic than planar cross-sections for many systems, such as Earth’s gravitational field, electron closed surfaces, and biological enclosures. By treating gauge fields as asymmetry detectors and employing spherical analysis, this work provides a more intuitive bridge between mathematical formalisms and observable reality, making gauge curvature easier to understand across physics and applied sciences.

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Publication Details

Journal
Zenodo (CERN European Organization for Nuclear Research)
Published
2025-09-18
DOI
https://doi.org/10.5281/zenodo.17150513
Primary Topic
Geochemistry and Geologic Mapping
Type
article
Field-Weighted Citation Impact
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article

Toward an Intuitive Interpretation of Gauge Fields: Cross-Sectional Differences and Spherical Analysis

Zenodo (CERN European Organization for Nuclear Research)
Geochemistry and Geologic Mapping
article

Toward an Intuitive Interpretation of Gauge Fields: Cross-Sectional Differences and Spherical Analysis

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Abstract

This paper proposes an intuitive reinterpretation of the gauge field equation Mathematically, FμνF_{\mu\nu}Fμν is defined as the antisymmetric derivative of a potential field, but its connection to real structures is not always clear. Here, we describe the gauge field as the difference between gradients observed when slicing a potential in orthogonal directions. If both views coincide (Fμν=0), the system is symmetric and structureless; if they differ, asymmetry appears, and a field emerges. To illustrate, an onion cut concentrically preserves symmetry and releases no liquid, whereas orthogonal cuts introduce asymmetry and cause fluid to spread. This “onion analogy” clarifies gauge fields as structural distortions. Moreover, spherical analysis—considering concentric shells—is argued to be more realistic than planar cross-sections for many systems, such as Earth’s gravitational field, electron closed surfaces, and biological enclosures. By treating gauge fields as asymmetry detectors and employing spherical analysis, this work provides a more intuitive bridge between mathematical formalisms and observable reality, making gauge curvature easier to understand across physics and applied sciences.

Zenodo (CERN European Organization for Nuclear Research)
Kappa Omicron Nu Honor Society (US)
Openalex Percentile: Top 35%
Geochemistry and Geologic Mapping
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Toward an Intuitive Interpretation of Gauge Fields: Cross-Sectional Differences and Spherical Analysis · Zenodo (CERN European Organization for Nuclear Research) (2025) | TGRS Research Map | TGRS