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Temperature dependence of calcite dissolution kinetics in seawater

机译:煤矿溶出动力学在海水中的温度依赖性

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摘要

Knowledge of the mechanism of calcite dissolution in seawater is a critical component of our understanding of the changing global carbon budget. Towards this goal, we provide the first measurements of the temperature dependence of seawater calcite dissolution kinetics. We measured the dissolution rates of C-13-labeled calcite in seawater at 5, 12, 21, and 37 degrees C across the full range of saturation states (0 < Omega = [Ca2+][Co-3(2-)]/K-sp' < 1). We show that the dissolution rate is non-linearly dependent on Omega and that the degree of non-linearity both increases with temperature, and changes abruptly at "critical" saturation states (Omega(crit)). The traditional exponential rate law most often utilized in the oceanographic community, R = k(1 - Omega)(n), requires different fits to k and n depending upon the degree of undersaturation. Though we calculate a similar activation energy to other studies far from equilibrium (25 +/- 2 kJ/mol), the exponential rate law could not be used to mechanistically explain our near equilibrium results. We turn to an alternative framework, derived from crystal nucleation theory, and find that our results are consistent with calcite dissolution kinetics in seawater being set by the retreat of pre-existing edges/steps from Omega = 1-0.9, defect-assisted etch pit formation from Omega = 0.9-0.75, and finally homogenous etch pit formation from Omega = 0.75-0. The Omega(crit)s for each mechanism are shifted significantly closer to equilibrium than they occur in dilute solutions, such that ocean acidification may cause marine carbonates to enter faster dissolution regimes more readily than would be expected from previous studies. We use the observed temperature dependence for each dissolution mechanism to calculate step kinetic coefficients (beta, cm/s), densities of active nucleation sites (n(s), sites/m(2)), and step edge free energies (alpha, mJ/m(2)). Homogenous dissolution is well explained within the surface nucleation framewor
机译:知识海水中石材溶解机制是我们对不断变化的全球碳预算的关键组成部分。对此目标来说,我们提供了海水胶铁溶解动力学的温度依赖性的第一次测量。我们在全系列饱和状态下测量了海水中的C-13标记方解石在海水中的溶出速率(0

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