ABSTRACTS
Tuesday - Session I Thermodynamics
Pyrohydrolysis of metal chlorides feasibility study
Dr.-Ing. Oliver Gnotke, Kronos International, Inc & Mr. Jim Berthold, OLI (speaker)
Production titanium dioxide creates significant amounts of an aqueous metal chloride solution as a by-product. Instead of neutralizing the metal chloride solution and landfilling the solid residue, pyrohydrolysis is a viable way to convert metal chlorides from TiO2 production into the valuable products hydrochloric acid and metal oxides with iron oxide as main component. The metal chloride solutions are complex highly concentrated aequeous solutions of di- and trivalent iron chlorides, other metal chlorides and hydrochloric acid. Kronos followed a theoretical approach for a feasibility study to assess the pyrohydrolysis process. As a first step it was essential to evaluate the applicability of OLI Stream Analyser for metal chloride solutions. For the simulation of a pyrohydrolysis process especially the prediction of solubility limits of salts and vapour pressures of HCl are important . Available literature data was taken for the system FeCl2-HCl-Water and compared with OLI results. The deviation of OLI results and literature data were quite small. This qualified OLI as a valuable tool for the feasibility study.
The impact of surface complexation on metal solubility
Mr. Marc Laliberté, Veolia Water Solution & Technologies
Surface complexation plays a significant and under appreciated role in limiting the solubility of many metals. The presentation will use cadmium as an example. We will cover basic properties of the Cd+2 ion in water, and show that hydroxide precipitation is inconsistent with environmental regulations and experimental results. We will then show how the experimental data is explained by surface complexation, how to incorporate surface complexation in OLI software and calibrate the model, and how once surface complexation is taken into account environmental regulations can be met. The presentation concludes with a review of ions where surface complexation plays a significant role, the limits of surface complexation modelling as implemented by OLI, and the implications of taking into account surface complexation for water treatment.
New development in boric acid studies
Professor Peter Tramaine, University of Guelph
Advances in electrolyte thermodynamics
Mr. Andre Anderko, PhD, OLI
Engineering a rare earth filtration system
Kevin Blinn, Rutgers
Tuesday - Session II - Applications
Product development updates
Mr. Chris Depetris, OLI
Autoclave simulation
Mr. Tracey Jackson, PhD Baker Hughes
Bringing OLI MSE into PHREEQC for reservoir simulations – application to subsurface challenges
Tim Tambach, Shell Global Solutions Int’l B.V.
Projects involving injection of reactive fluids and gases in subsurface reservoirs are becoming more common in the oil and gas industry, for example subsurface storage of CO2 and water flooding for improved oil recovery (IOR). Such operations demand forecasting of the geochemical changes to the reservoir minerals and formation water, which can be computed using reactive transport modelling (RTM). This simulation technique couples gas and fluid flow with geochemical reactions. In Shell we use our in-house reservoir simulator MoReS, coupled to the open source geochemical software PHREEQC [1], for RTM computations.
A reliable geochemical database is of crucial importance for accurate predictions of the geochemical impact. PHREEQC is distributed with several different databases, which frequently produce significantly different results [2]. At the same time, OLI MSE [3] has a solid foundation and is currently the standard tool in Shell for computing chemical reactions and phase partitioning of solids, fluids, and gases in wells and downstream applications (production chemistry). For the reasons given above we implemented the OLI MSE model into MoReS-PHREEQC, enabling accurate and consistent integrated RTM simulations. We validated our work by computing saturation indices (SIs) and species molalities using both OLI and MoReS-PHREEQC in a wide pressure, temperature, and salinity range.
We used RTM to compute the long-term fate of CO2 injection in a carbonate aquifer, based on a measured formation water composition. The results demonstrate that CO2 dissolves and dissociates in the formation water, leading to a lower pH and dissolution of calcite and dolomite. This leads to oversaturation and precipitation of anhydrite. The overall balance of mineral reactions in terms of porosity is very small, which is comparable to observations in other work [4]. We also used RTM to understand the potential and risk of barite scaling as a result of seawater injection for IOR. The measured and simulated production water geochemistry as a function of time shows good agreement. We used the results to identify which production wells are likely to encounter scaling and require protective measures in the near future.