geochemistry

Layer 2 — Chemistry24 concepts in this subtree

Geochemistry — IUPAC-VII applied chemistry at the rock/mineral/fluid grain. Foundations: radiometric decay N(t) = N_0·exp(−λt), half-life t_{1/2} = ln 2 / λ (Rutherford 1900, Holmes 1913) underwrites all isotope geochronology. U-Pb…

N(t) = N₀·exp(−λt); t_{1/2} = ln 2 / λ (universal isotope clock)
K_D = C_s / C_l; 2-phase mass-bal: C_l = X_tot/(F·K_D + 1−F)
k = A·exp(−Ea/RT); ln(k₂/k₁) = (Ea/R)·(T₂−T₁)/(T₁T₂)
N(t_{1/2})/N₀ = 1/2; with λ=ln 2, t=1 ⇒ ratio = 1/2 exactly
R/R₀ = f^{α−1}: at f=1 ⇒ 1; at α=1 ⇒ 1 (no-fractionation limits)
C_l = X_tot/(F·K_D + 1−F); at F=0 ⇒ X_tot; at F=1 ⇒ X_tot/K_D
Rb-Sr isochron framework: (⁸⁷Sr/⁸⁶Sr) = (⁸⁷Sr/⁸⁶Sr)₀ + (⁸⁷Rb/⁸⁶Sr)·(e^{λt} − 1)
δ-notation framework: δ = (R_sample/R_std − 1)·1000 ‰ (parts-per-mille isotope-ratio deviation)
Goldschmidt framework: lithophile / siderophile / chalcophile / atmophile partitioning (silicate/metal/sulfide/gas affinity)
Rb-Sr slope: m = e^{λt} − 1; m|_{λt small} ≈ λt; m|_{t = t_{1/2}} = 1
δ = 1000·R_s/R_std − 1000; δ|_{R=R_std} = 0 ‰; δ|_{R=2R_std} = 1000 ‰
Goldschmidt flags: Na lithophile (1), Na siderophile (0), Fe siderophile (1), S chalcophile (1)
Isotope fractionation (Urey 1947)
Radiocarbon dating (Libby 1949)
REE patterns (McDonough-Sun 1995)
Bowen reaction series (1928)
Clay CEC (Grim 1953)
Conservative tracers (Broecker 1974)
U-Pb zircon (Tilton 1955)
Ar-Ar dating (Merrihue 1966)
Isotope fractionation (Urey detail)
Clumped isotopes (Eiler 2007)
REE Eu-Ce anomaly (Goldschmidt 1937)
Nd depleted-mantle (DePaolo 1981)
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