TY - JOUR
T1 - Boron isotope geochemistry during diagenesis. Part I. Experimental determination of fractionation during illitization of smectite
AU - Williams, Lynda
AU - Hervig, Richard
AU - Holloway, John R.
AU - Hutcheon, Ian
N1 - Funding Information:
The authors (LBW and RLH) acknowledge financial support for this research by the U.S. Dept. of Energy (DE-FG05-97ER14404) and partial support by the Imperial Oil Charitable Foundation (IH). Technical support was provided by Al Higgs (electronics), David Wright (lab), Stan Klonowski (isotope lab), and Joan Bahamonde (computer) at ASU. The expertise of Mike Wieser and Maurice Shevalier, who provided analytical assistance at UC, is gratefully acknowledged. We thank also Fred Longstaffe and Bill Leeman who provided conventional and TIMS isotope analyses for calibration of the SIMS methods. The insights of reviewers Libby Sterne and David Awwiller are also greatly appreciated.
PY - 2001
Y1 - 2001
N2 - Experiments were performed to measure the isotopic fractionation of boron between illite/smectite (I/S) clay minerals and water as a function of temperature (300° and 350°C) and degree of illitization. Corresponding changes in the oxygen isotopes were monitored as an indication of the approach to equilibrium. The kinetics of the B-isotope exchange follows the mineralogical restructuring of smectite as it recrystallizes to illite. An initial decline in δ11BI/S occurs when the I/S is randomly ordered (RO). The δ11BI/S values reach a plateau during R1 ordering of the I/S, representing a metastable condition. The greatest change in δ11BI/S is observed during long-range (R3) ordering of the I/S when neoformation occurs. Values of δ11BI/S measured on the equilibrium reaction products were used to construct a B-isotope fraction curve. There is a linear correlation among data from these experiments and 1100°C basaltic melt-fluid fractionation experiments (Hervig and Moore, 2000) that can be extrapolated to include adsorption experiments at 25°C (Palmer et al., 1987). Unlike other stable isotopic systems (e.g., oxygen) there is no mineral-specific fractionation of B-isotopes, but rather a coordination dependence of the fractionation. Under diagenetic conditions B is predominantly in trigonal coordination in fluids but substitutes in tetrahedral sites of silicates. The preference of 10B for tetrahedral bonds is the major fractionating factor of B in silicates.
AB - Experiments were performed to measure the isotopic fractionation of boron between illite/smectite (I/S) clay minerals and water as a function of temperature (300° and 350°C) and degree of illitization. Corresponding changes in the oxygen isotopes were monitored as an indication of the approach to equilibrium. The kinetics of the B-isotope exchange follows the mineralogical restructuring of smectite as it recrystallizes to illite. An initial decline in δ11BI/S occurs when the I/S is randomly ordered (RO). The δ11BI/S values reach a plateau during R1 ordering of the I/S, representing a metastable condition. The greatest change in δ11BI/S is observed during long-range (R3) ordering of the I/S when neoformation occurs. Values of δ11BI/S measured on the equilibrium reaction products were used to construct a B-isotope fraction curve. There is a linear correlation among data from these experiments and 1100°C basaltic melt-fluid fractionation experiments (Hervig and Moore, 2000) that can be extrapolated to include adsorption experiments at 25°C (Palmer et al., 1987). Unlike other stable isotopic systems (e.g., oxygen) there is no mineral-specific fractionation of B-isotopes, but rather a coordination dependence of the fractionation. Under diagenetic conditions B is predominantly in trigonal coordination in fluids but substitutes in tetrahedral sites of silicates. The preference of 10B for tetrahedral bonds is the major fractionating factor of B in silicates.
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U2 - 10.1016/S0016-7037(01)00557-9
DO - 10.1016/S0016-7037(01)00557-9
M3 - Article
AN - SCOPUS:0034976634
SN - 0016-7037
VL - 65
SP - 1769
EP - 1782
JO - Geochimica et Cosmochimica Acta
JF - Geochimica et Cosmochimica Acta
IS - 11
ER -