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  • 1
    Publication Date: 2022-06-07
    Description: Abstract
    Description: This data was collected to write an extensive review on organic compounds in geothermal fluids as part of the REFLECT (Redefining geothermal fluid properties at extreme conditions to optimize future geothermal energy extraction). The data is mainly focussed on geothermal sites were organic compound data was reported in the literature. It includes data from the literature (Feldbusch, 2016; Vetter, 2012; Brehme et al., 2019; Westphal et al., 2019; Sanjuan et al., 2016) as well as own data that was analysed at the GFZ German Research Centre for Geosciences in section 3.2 (Organic Geochemistry). It comprises 130 samples from 19 different sites including DOC, organic acid anion as well as main inorganic anion concentrations, well depths, and reservoir temperatures of various geothermal sites in Europe. Due to confidentiality agreements Site names are all given in ID’s which are fully explained in the publication “Organic compounds in geothermal fluids – a review” when available. Sample ID’s are also given if the samples, both from the literature or own samples were measured at GFZ German Research Centre for Geosciences. This project has received funding from the European Union’s Horizon 2020 research and innovation programme under grant agreement nº 850626 (REFLECT).
    Keywords: Geothermal fluids ; Brine ; Dissolved organic matter ; Dissolved organic carbon ; Inhibitor ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOCHEMISTRY ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOCHEMISTRY 〉 GEOCHEMICAL PROPERTIES 〉 CHEMICAL CONCENTRATIONS ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOTHERMAL DYNAMICS 〉 GEOTHERMAL ENERGY
    Type: Dataset , Dataset
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  • 2
    Publication Date: 2023-04-27
    Description: Abstract
    Description: This dataset comprises 47 fluid samples from 11 geothermal sites (Germany, Austria, Iceland, Turkey, Netherlands, Belgium, French West Indies). The samples were collected within the REFLECT project (Redefining geothermal properties at extreme conditions to optimize future geothermal energy extraction). The focus with these analyses were on the organic compound composition of the fluids, since they are rarely included in the analyses of fluids taken from geothermal power plants. Understanding the organic compound composition of geothermal fluids might help to better understand chemical reactions within the fluids and might help to mitigate problems that arise with the operation of a geothermal power plant such as mineral precipitation (scaling) and corrosion of the casing and pipes.
    Description: Methods
    Description: The samples were taken by the onsite project partners and sent to GFZ for the analyses. Generally, the fluid samples were taken at the surface instalments and remained untreated after sampling (otherwise given as remark in the datasheet). Sampling bottles were rinsed and flushed with the fluids prior to filling them up. Sampling volumes ranged from 250-500 ml per sample.
    Keywords: Geothermal fluids ; Brine ; Dissolved organic matter ; Dissolved organic carbon ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOCHEMISTRY ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOCHEMISTRY 〉 GEOCHEMICAL PROPERTIES 〉 CHEMICAL CONCENTRATIONS ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOTHERMAL DYNAMICS 〉 GEOTHERMAL ENERGY
    Type: Dataset , Dataset
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  • 3
    Publication Date: 2024-04-02
    Description: Abstract
    Description: This dataset is the result of an experimental series that was carried out in September/October 2022 at GFZ German Research Centre for Geosciences, Potsdam, Germany to observe biosorption of lead under extreme conditions. Synthetic solutions, simulating the geothermal fluids from the Heemskerk geothermal power plant were were prepared in 30 ml glass vials (Rotalibo screw neck ND24 EPA). To prepare the stock solutions, sodium chloride (NaCl, 99.8 %, Cellpure, Merck, DE) was added at 265 g/L and Pb(II), in form of lead nitrate (Pb(NO3 )2 , Merck, DE), at 1 g/L to ultrapure water. To assess the impact of acetic acid on lead biosorption, two treatments were done: one without acetic acid and one where acetic acid (100 %, Merck, DE) was added at 60 mg/L. Finally, dead biomass of the fungus Penicillium citrinum was added in the samples at a concentration of 4 g/L (Wahab et al., 2017). The samples were incubated in an autoclave at a pressure of 8 bars on a rotative shaker. The temperature was set at 25 °C, 60 °C or 98 °C with three contact times (1, 2 and 3 h). All treatments were performed in triplicates. For each treatment, two controls without biomass were done. Control samples without the addition of NaCl were done in duplicate, at 25 °C and for 2 h. After incubation, samples were filtered through a 0.22 µm nitrocellulose filter (Sartorius Stedim Biotech, FR) to separate the biomass from the liquid. The biomass on the filters was dried for 24 h at 45 °C before being scraped from the filter and kept in a Falcon tube at room temperature.
    Keywords: geothermal ; biosorption ; lead biosorption ; Penicillium cintrinum ; batch experiments ; brine
    Type: Dataset , Dataset
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  • 4
    Publication Date: 2020-04-30
    Description: With ongoing climate change, permafrost soils and their function as carbon sinks are becoming more important as they might become carbon sources with rising global air temperatures. Landscapes are also changing, forming distinct features such as retrogressive thaw slumps, which not only release large amounts of organic carbon but also nitrogen, heavy metals, trace elements, major ions, sediment and fresh water into the environment depending on the regional settings. This thesis examines the release of dissolved and particulate matter due to the permafrost thaw in the Batagaika mega thaw slump in central Yakutia (Russia) (67�34'41.83" N, 134�45'46.91" E) and how it affects the subsequent streams the Batagaika and Yana River. In total 11 samples were taken: 5 slump, 4 Batagaika River and 2 Yana River samples, representing the flow path from the slump to the Yana River. The samples were analyzed for electrical conductivity, hydrogen carbonate content, DOC, nitrogen, major ion concentrations, heavy and trace metals, stable oxygen, hydrogen and carbon isotopes and were dated using radiocarbon measurements. When available, particulate matter in suspension was analyzed for total carbon, total organic carbon, total nitrogen and stable carbon isotopes, and were radiocarbon dated. The results show a significant release of dissolved organic and inorganic matter in the thaw slump affecting the water chemistry of the Batagaika River but showing no observable impact on the Yana River. Particulate matter does not seem to have had a strong impact on the subsequent rivers as sediment contents in suspension in the slump are 〉50% and 〈2% in the Batagaika and Yana River. Also TOC values are clearly lower in the slump compared to the Batagaika River. Trying to relate radiocarbon ages, stable isotopes and TOC values with specific stratigraphical units and ice wedges of the slumps headwall showed a connection to the upper sand unit of the NNE headwall and might lead to the conclusion of stronger erosion of a few units or sections of the headwall. However, the low sample resolution in this thesis both spatially and temporally must be considered in the interpretation of the results.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Thesis , notRev
    Format: application/pdf
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