『Abstract
　The crystallographic diversity of pyrrhotite (Fe1-xS), one of the most common iron sulfide minerals, offers insights into how mineral-fluid interactions are controlled by crystal structures. We have conducted oxidative dissolution experiments on monoclinic 4C-pyrrhotite and ‘hexagonal’ NC-pyrrhotite in aqueous H2O2/H2SO4 and FeCl3/HCl media at pH between 1.8 and 2.9 using polished surfaces of single crystals. Quantification and detailed characterization of the reaction interfaces has been accomplished by confocal 3D topometry and transmission electron microscopy (TEM) in conjunction with focused ion beam (FIB) preparation. Crystallographically coherent intergrowths of 4C- and NC-pyrrhotite in a single sample allowed unambiguous identification of strong intrinsic reactivity differences between the two closely related phases. On {110} faces in the H2O2 medium at 35℃ and pH below 2.70, NC-pyrrhotite (N〜4.85) reacts about 50-80% faster than 4C-pyrrhotite. Above pH 2.70, the behavior inverts and 4C-pyrrhotite dissolves faster, while overall reaction rates drop drastically by up to two orders of magnitude. Because the two pyrrhotite phases show only marginally different Fe/S ratios but substantial differences in structural complexity with regards to vacancy ordering, we attribute the reactivity differences to structurally controlled processes at the mineral-water interface. The transition at pH 2.70 is close to the reported isoelectric point of pyrrhotite. We attribute the pH dependent changes in reaction rates and behaviors to protonation/deprotonation of surface sulfhydryl groups and related changes in speciation and bonding mode of reactive oxygen species at the mineral interface. At pH＜2.70, we find elemental sulfur as a frequent reaction product in H2O2 and FeCl3 media, indicating incomplete sulfur oxidation. Above pH 2.70, elemental sulfur was not found in H2O2 experiments (no data for FeCl3). Our results show that the effects of crystal anisotropy are strong and directional preference of dissolution changes at the pH 2.70 transition point as well, leading to complex sub-μm-scale textural development at the reaction interfaces throughout the pH range studied. High resolution TEM imaging of cross sections through reacted mineral surfaces show crystalline pyrrhotite up to the reaction interface and the absence of significant non-equilibrium layers or S-enriched (poly)sulfides.』

1. Introduction
　1.1. General introduction
　1.2. Mineralogy of pyrrhotite
　1.3. Reactions at pyrrhotite surfaces
　1.4. Outline of approach
2. Samples and experimental procedure
　2.1. Sample description
　2.2. Sample preparation
　2.3. Experimental setup and conditions
　2.4. Analytical methods
3. Results
　3.1. General observations and identification of alteration phases
　　3.1.1. Experiments with FeCl3 solution - surface mineralogy
　　3.1.2. Experiments with FeCl3 solution - pyrrhotite reactivity and experimental reproducibility
　　3.1.3. Experiments with H2O2 solution - surface mineralogy
　3.2. Phase-specific quantification of dissolution rates from H2O2 experiments
　　3.2.1. Reactivity of NC-pyrrhotite versus 4C-pyrrhotite
　　3.2.2. Effect of additional solutes
　3.3. Orientation dependence of pyrrhotite dissolution
　　3.3.1. Reaction at pH 2.05
　　3.3.2. Reaction at pH 2.88-2.92
　　3.3.3. Control of superstructure on dissolution anisotropy
　　3.3.4. Anomalous dissolution behavior in microenvironments
　3.4. Interface morphology
　3.5. High resolution TEM interface observations
4. Discussion
　4.1. pH dependence of dissolution rates and anisotropy
　　4.1.1. Dissolution rates and the isoelectric point
　　4.1.2. Dissolution anisotropy and chemical state of pyrrhotite surfaces
　　4.1.3. Oxidant species
　　4.1.4. Non-oxidative dissolution and the role of Fe³⁺
　4.2. Reactivity differences between 4C- and NC-pyrrhotite
　4.3. Existence of sulfidic non-equilibrium layers
5. Conclusions
Acknowledgements
References