Lightning on Mars (msf:48270): A USP Field Theory Explanation of Dust-Devil Micro-Discharges

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1. Verfasser: Sepehri, Sadegh
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Sprache:Englisch
Veröffentlicht: Zenodo 2025
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author Sepehri, Sadegh
author_facet Sepehri, Sadegh
contents <p>Recent rover observations at Jezero Crater have confirmed electrical micro-discharges inside Martian dust devils. In standard atmospheric physics, these sparks are explained by triboelectric charging of dust grains combined with the low breakdown threshold of CO₂ near the Paschen minimum.</p> <p> </p> <p>In USP Field Theory, lightning is interpreted as a rapid collapse of a strong “Delta f” (Δf) gradient within a mixed medium. Atmospheric structure is described through a scalar mismatch field:</p> <p> </p> <p>Δf = a_T (T − T₀) + a_ρ (ρ − ρ₀) + a_s S² + a_d n_d</p> <p> </p> <p>where T is temperature, ρ is density, S is shear, and n_d is dust number density. Pressure responds to Δf via:</p> <p> </p> <p>p = p₀ + α_f Δf</p> <p> </p> <p>Dust grains in a vortex experience strong Δf gradients, producing a polarization:</p> <p> </p> <p>P = χ · (∇Δf) · n_d</p> <p> </p> <p>Charge density and electric field follow:</p> <p> </p> <p>ρ_e = −∇·P</p> <p>∇·(εE) = ρ_e</p> <p> </p> <p>Breakdown occurs when:</p> <p> </p> <p>|E| ≥ E_brk</p> <p> </p> <p>For Mars (p ≈ 6 mbar, CO₂), breakdown typically occurs at several hundred V/cm across centimeter-scale gaps. Using the USP relation:</p> <p> </p> <p>E ≈ (χ · n_d · ∇Δf) / ε</p> <p> </p> <p>only modest Δf gradients are needed to reach ignition in dust-rich columns.</p> <p> </p> <p>This document presents the USP framework for Martian lightning, compares it to standard triboelectric models, provides quantitative scaling estimates, and explains why micro-sparks should naturally occur in dust devils on Mars.</p>
format Recurso digital
id zenodo_https___doi_org_10_5281_zenodo_17889358
institution Zenodo
language eng
publishDate 2025
publisher Zenodo
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spellingShingle Lightning on Mars (msf:48270): A USP Field Theory Explanation of Dust-Devil Micro-Discharges
Sepehri, Sadegh
Mars atmosphere
lightning
dust devils
atmospheric electricity
Δf field
USP Field Theory
CO2 Paschen breakdown
triboelectric charging
msf:48270
planetary science
<p>Recent rover observations at Jezero Crater have confirmed electrical micro-discharges inside Martian dust devils. In standard atmospheric physics, these sparks are explained by triboelectric charging of dust grains combined with the low breakdown threshold of CO₂ near the Paschen minimum.</p> <p> </p> <p>In USP Field Theory, lightning is interpreted as a rapid collapse of a strong “Delta f” (Δf) gradient within a mixed medium. Atmospheric structure is described through a scalar mismatch field:</p> <p> </p> <p>Δf = a_T (T − T₀) + a_ρ (ρ − ρ₀) + a_s S² + a_d n_d</p> <p> </p> <p>where T is temperature, ρ is density, S is shear, and n_d is dust number density. Pressure responds to Δf via:</p> <p> </p> <p>p = p₀ + α_f Δf</p> <p> </p> <p>Dust grains in a vortex experience strong Δf gradients, producing a polarization:</p> <p> </p> <p>P = χ · (∇Δf) · n_d</p> <p> </p> <p>Charge density and electric field follow:</p> <p> </p> <p>ρ_e = −∇·P</p> <p>∇·(εE) = ρ_e</p> <p> </p> <p>Breakdown occurs when:</p> <p> </p> <p>|E| ≥ E_brk</p> <p> </p> <p>For Mars (p ≈ 6 mbar, CO₂), breakdown typically occurs at several hundred V/cm across centimeter-scale gaps. Using the USP relation:</p> <p> </p> <p>E ≈ (χ · n_d · ∇Δf) / ε</p> <p> </p> <p>only modest Δf gradients are needed to reach ignition in dust-rich columns.</p> <p> </p> <p>This document presents the USP framework for Martian lightning, compares it to standard triboelectric models, provides quantitative scaling estimates, and explains why micro-sparks should naturally occur in dust devils on Mars.</p>
title Lightning on Mars (msf:48270): A USP Field Theory Explanation of Dust-Devil Micro-Discharges
topic Mars atmosphere
lightning
dust devils
atmospheric electricity
Δf field
USP Field Theory
CO2 Paschen breakdown
triboelectric charging
msf:48270
planetary science
url https://doi.org/10.5281/zenodo.17889358