RESUMEN
Hydrogen sulfide (H2S), an environmentally harmful pollutant, is a byproduct of geothermal energy production. To reduce the H2S emissions, H2S-charged water is injected into the basaltic subsurface, where it mineralizes to iron sulfides. Here, we couple geophysical induced polarization (IP) measurements in H2S injection wells and geochemical reactive transport models (RTM) to monitor the H2S storage efforts in the subsurface of Nesjavellir, one of Iceland's most productive geothermal fields. An increase in the IP response after 40 days of injection indicates iron-sulfide formation near the injection well. Likewise, the RTM shows that iron sulfides readily form at circumneutral to alkaline pH conditions, and the iron supply from basalt dissolution limits its formation. Agreement in the trends of the magnitude and distribution of iron-sulfide formation between IP and RTM suggests that coupling the methods can improve the monitoring of H2S mineralization by providing insight into the parameters influencing iron-sulfide formation. In particular, accurate fluid flow parameters in RTMs are critical to validate the predictions of the spatial distribution of subsurface iron-sulfide formation over time obtained through IP observations. This work establishes a foundation for expanding H2S sequestration monitoring efforts and a framework for coupling geophysical and geochemical site evaluations in environmental studies.
Asunto(s)
Sulfuro de Hidrógeno , Sulfuro de Hidrógeno/química , Monitoreo del Ambiente/métodos , Islandia , Hierro/químicaRESUMEN
Groundwater contamination is a threat to drinking water resources and ecosystems. Remediation by injection of chemical reagents into the aquifer may be preferred to excavation to reduce cost and environmental footprint. Yet, successful remediation requires complete contact between contamination and reagents. Subsurface heterogeneities are often responsible for diffusion into low-permeable zones, which may inhibit this contact. Monitoring the spatial distribution of injected reagents over time is crucial to achieve complete interaction. Source zone contamination at megasites is particularly challenging to remediate and monitor due to the massive scale and mixture of contaminants. Source zone remediation at Kærgård Plantation megasite (Denmark) is monitored here, with a new methodology, using high-resolution cross-borehole electrical resistivity tomography (XB-ERT) imaging calibrated by chemical analyses on groundwater samples. At this site, high levels of toxic non-aqueous phase liquids (NAPL) are targeted by in-situ chemical oxidation using activated persulfate. It may take numerous injection points with extensive injection campaigns to distribute reagents, which requires an understanding of how reagent may transport within the aquifer. A geophysical (XB-ERT) monitoring network of unprecedented size was installed to identify untreated zones and help manage the remediation strategy. The combination of spatially continuous geophysical information with discrete but precise chemical information, allowed detailed monitoring of sulfate distribution, produced during persulfate activation. Untreated zones identified in the first remediation campaign were resolved in the second campaign. The monitoring allowed adjusting the number of injection screens and the injection strategy from one campaign to the next, which resulted in better persulfate distribution and contaminant degradation in the second campaign. Furthermore, geophysical transects repeated over the timespan of a remediation campaign allowed high-resolution time-lapse imaging of reagent transport, which could in the future improve the predictability of transport models, compared to only using on a-priori assumptions of the hydraulic conductivity field.
RESUMEN
BACKGROUND: Intraleaflet hematomas are associated with advanced stages of aortic valve calcification and suspected to be involved in disease progression. However, the mechanism by which the entry of blood cells into the valves affects the biology of aortic valvular interstitial cells (VICs) remains to be elucidated. OBJECTIVES: This study sought to evaluate the putative link between intraleaflet hematoma and aortic valve calcification and to assess its pathophysiological implications. METHODS: The spatial relationship between calcium deposits and intraleaflet hematomas was analyzed by whole-mount staining of calcified and noncalcified human aortic valves, obtained in the context of heart transplantation and from patients who underwent surgical valve replacement. Endothelial microfissuring was evaluated by en face immunofluorescence and scanning electron microscopic analyses of the fibrosa surface. Red blood cell (RBC) preparations were used in vitro to assess, by immunofluorescence microscopy and Alizarin red staining, the potential impact of intraleaflet hematomas on phenotypic changes in VICs. RESULTS: Intraleaflet hematomas, revealed by iron deposits and RBCs into the fibrosa, secondary to endothelial microfissuring, were consistently found in noncalcified valves. The contact of primary VICs derived from these valves with RBCs resulted in a global inflammatory and osteoblastic phenotype, reflected by the up-regulation of interleukin-6, interleukin-1ß, bone sialoprotein, osteoprotegerin, receptor activator of nuclear factor kappa B, bone morphogenic protein 2, and muscle segment homeobox 2, the production of osteocalcin, and the formation of calcium deposits. CONCLUSIONS: The acquisition of an osteoblastic phenotype in VICs that come into contact with the senescent RBCs of intraleaflet hematomas may play a critical role in the initiation of calcium deposition into the fibrosa of human aortic valves.