2023
DOI: 10.1029/2022jb026253
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Coefficients of Reaction‐Diffusion Processes Derived From Patterns in Rocks

Abstract: Self-organization develops autonomously in reaction-diffusion systems and is observed in many rock textures in geology (

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Cited by 6 publications
(9 citation statements)
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“…This finding supports that a common formation mechanism for Liesegang rings is stemming from a driving force for the solute transport (like Mnor Fe-bearing acidic fluid) which is either an extremely slow flux induced by an (electro-)chemical potential difference or a slow mechanically forced fluid flow caused by a stress gradient, for example, compaction from overburden stress or tectonic forces (Liu et al, 2023a), or a combination thereof. Liesegang rings consequently can form independent of the primary high permeability interbed layers or secondary crack interfaces that control dendrites.…”
Section: Discussionsupporting
confidence: 72%
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“…This finding supports that a common formation mechanism for Liesegang rings is stemming from a driving force for the solute transport (like Mnor Fe-bearing acidic fluid) which is either an extremely slow flux induced by an (electro-)chemical potential difference or a slow mechanically forced fluid flow caused by a stress gradient, for example, compaction from overburden stress or tectonic forces (Liu et al, 2023a), or a combination thereof. Liesegang rings consequently can form independent of the primary high permeability interbed layers or secondary crack interfaces that control dendrites.…”
Section: Discussionsupporting
confidence: 72%
“…Scaled parameters for both simulations are truea¯=100 $\bar{a}=100$, a 0 = 0, m 0 = −1.5, D b = 1.0, κ = 1.0, ɛ = 1.0, γ = 0.15, σ = 0.2, and η c = 0, except b 0 = 1.0 and D a = 2 for the local bands A while b 0 = 0.75 and D a = 3 for the local bands (b) For parameter definitions refer to Liu et al. (2023a).…”
Section: Discussionmentioning
confidence: 99%
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