Mineralogical characterization of scalings formed in geothermal sites in the Upper Rhine Graben before and after the application of sulfate inhibitors

Scale formation processes in the surface installations of geothermal power plants may have a negative effect on
power plant performance. In addition, scales formed within the geothermal water circuit frequently accumulate
natural radionuclides. Consequently, scale formation may lead to radiation dose rates, which are of radiological
concern, and deposits, which may have to be disposed as radioactive waste. In order to minimize these problems
and to foster geothermal power plant availability, it is of major interest to understand scale formation processes
and to develop methods for their inhibition. One important pre-requisite towards this goal is a sound mineralogical
and geochemical characterization of the formed material.
Geothermal brines at sites in the Upper Rhine Graben are in general highly mineralized and become, upon
cooling in the heat exchanger, supersaturated with respect to sulfate solid-solutions, e.g. (Ba,Sr)SO4, and other
mineral phases. Some geothermal power plants very successfully tested the application of sulfate scaling inhibitors.
Here we present mineralogical analyses of scale samples from geothermal power plants in the Upper
Rhine Valley deposited in absence and presence of sulfate scaling inhibitors. ... mehrSolid samples are investigated using
wet-chemistry (after digestion), XRPD, SEM-EDX, XPS, EA-IRMS, Raman spectroscopy, and XANES (for explanation
of abbreviations, see main text).
Samples of scales deposited in the absence of a sulfate scaling inhibitor mainly consist of two phases. The
largest part is made up of a barite type (Ba,Sr,Ca)SO4 solid-solution. Traces of Ra occurring in the scaling are
assumed to be incorporated in the barite type solid solution. Further minor phases are sulfide phases, either an Xray
amorphous nano-particulate phase or galena (PbS).
Since the application of the sulfate inhibitor, sulfate minerals are no longer detectable in the scale samples.
Subsequent scalings are Pb-dominated and consist mainly of galena (PbS), elemental lead (Pb), arsenic (As) and
antimony (Sb). As and Sb are likely present as a nanocrystalline intermetallic mixed compound ((Sb, As) or
Pb3(Sb,As)2S3). The absence of barite-type minerals demonstrates the success of the application of the sulfate
inhibitor. The precipitation of elemental Pb, As, and Sb, which are more noble than iron, may enhance the
corrosion of mild steel pipes in the geothermal water circuit. Elution tests and oxidation of the scalings upon
storage at atmospheric conditions demonstrate that proper disposal of the toxic heavy metal and metalloid
containing scalings may be challenging.