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The global hydrogen demand is steadily increasing, and one way of accelerating the green hydrogen supply is to stimulate the green hydrogen economy. Utilization of waste heat from hydrogen production can increase the profitability of produced green hydrogen. Therefore, the aim of this study is to propose a system for integration of waste heat on the district heating (DH) network in Luleå, Sweden. Furthermore, an economic evaluation of the proposed system was conducted. In this study, the system was developed and investigated for two cases i.e. for a PEM and alkaline electrolyzer with an installed capacity of 100 MW. A large-scale heat pump and a heat exchanger were further added to the system to integrate the waste heat on the DH-network, while simultaneously providing cooling to the electrolyzer stack. The system was modelled for static conditions in the software MATLAB, with retrieved hourly DH data from Luleå Energi. The results showed that 203 060 MWhth can be extracted from the PEM electrolyzer with a waste heat temperature of 79 oC, while 171 770 MWhth can be integrated on the DH network annually. For the alkaline electrolyzer, 310 630 MWhth can be extracted at a waste heat temperature of 80 oC, while 226 220 MWhth can be integrated on the DH annually. The overall system efficiency is 94.7 % and 88.4 % for PEM and alkaline connected systems, respectively. Furthermore, the Levelized Cost of Heat (LCOH) is 0.218 SEK/kWhth and 0.23 SEK/kWhth for a PEM and alkaline connected system, respectively. For future scenarios with fourth generation of DH-networks, it is predicted that the LCOH can reach 0.018 SEK/kWth for a PEM electrolyzer system, and 0.017 SEK/kWth for an alkaline electrolyzer system. One conclusion that can be drawn from this study is that the utilized heat from the proposed system is price competitive in comparison with other thermal energy sources.

L to D isomerization of amino acids in a commercially prepared alkali-treated food-grade soy isolate was investigated. A soy flour product was also investigated as a control which had not been alkali treated. Methionine and valine collected from two soy flour and two soy isolate samples were coupled with L-leucine-N-carboxyanhydride. If both D- and L-forms were present this would produce diastereomeric dipeptide derivatives. The derivatives were separated by ion-exchange chromatography using a TSM Amino Acid Analyzer. Comparison of the sample methionine and valine dipeptide peaks to standard dipeptide peaks revealed the presence of L-valine, L-methionine and D-methionine in both soy flour and soy isolate samples. Methionine was substantially isomerized in both products. D-valine was not observed in either soy flour or soy isolate samples. Thus, isomerization of methionine appeared to occur at a faster rate than valine. Acid hydrolysis, toasting of soy meal, and alkaline treatment are all conditions which may be responsible for the isomerization of methionine. / Master of Science

We may summarize the purposes of this investigation as follows: A report on this investigation was made to Dr. John H. Yoe of the University of Virginia in order to see what reactions he considered to be of analytical significance and should be further investigated. He considers only three to be of any practical importance. They are as follows: 1. 7A-Oleic Acid. Solubility of the alkaline earth salts of some higher fatty acids. 2. 69A- 2-Acetamino 6-Aminobenzo Thiazole. A colorimetric reagent for iridium. 3. 71A 2-Hydroxy 3-Nitro 5-Sulfobenzoic Acid. A colorimetric reagent for ferric iron. A further investigation of compound 71A, as a colorimetric reagent for ferric iron, reveals that the sensitivity of this reaction is not great enough for it to be of any practical importance, since we have reagents (2) for this ion that are several times more sensitive. Prospective reagent No. 69A for iridium is being further investigated by Mr. J. R. Noell (1). A report on 7A will be taken up in Part II of this thesis. 1. It has been shown that there is very little difference in the solubility of the same alkaline earth salt of stearic, oleic, linoleic, and linolenic acids in the solvents, water, benzene, absolute ethyl alcohol and ether. 2. It has been shown that there is very little difference in the solubility of the different alkaline earth salt of stearic, oleic, linoleic, and linolenic acids in the solvents, water, benzene, absolute ethyl alcohol and ether, and benzene. 3. The solubility of the alkaline earth salt of these acids increases slightly with unsaturation, but does not increase as the degree of unsaturation increases. / M.S.

Clays are considered as potential host rocks and backfill material for deep geological repositories for radioactive waste. Therefore, profound understanding of radionuclide retention processes at clay mineral surfaces is essential for a long-term safety assessment. This understanding has already been generated in the past for simple chemical systems, in which experiments are easy to conduct and interpretation is straightforward. However, there is still a lack of molecular process understanding when considering complex natural systems (low radionuclide concentrations, high ionic strength, high pH values, multi-mineral solid phases, complex solution composition). This thesis aims to close some of these knowledge gaps, focusing on U(VI) and Np(VI) sorption on clays at (hyper)alkaline conditions. pH values between 10 and 13 can prevail in the near-field of a radioactive waste repository as a result of the degradation of concrete, which is part of the geo-engineered barrier. Existing studies on radionuclide sorption on clays do not exceed pH 10. Therefore, within this work, a comprehensive investigation in the pH range 8-13 was conducted. This included the quantification of radionuclide retention in batch sorption experiments as well as spectroscopic investigations to generate understanding about the underlying retention mechanisms on a molecular level. Beside the pH, additional focus was on the influence of dissolved carbonate and calcium on radionuclide sorption at (hyper)alkaline conditions. Next to two small chapters dealing with the stability and surface charge of Ca-bentonite at (hyper)alkaline conditions (chapter 4.1) and the influence of ISA on U(VI) sorption at high pH values (chapter 4.3), the thesis can be subdivided in two major parts. The first part (chapter 4.2) is a detailed investigation of U(VI) sorption on Ca-bentonite at (hyper)alkaline conditions in mixed electrolyte solutions. Batch sorption experiments were conducted, varying a number of experimental parameters (sorption time, S/L ratio, U(VI) concentration, pH value, carbonate concentration) and assessing their effect on U(VI) sorption. In order to be able to explain the observed sorption behavior, next to U(VI) solubility tests, spectroscopic techniques were applied. The aqueous speciation of U(VI) was investigated with TRLFS, while its surface speciation was probed with ATR FT-IR, site-selective TRLFS, EXAFS and CTR/RAXR. Since the results of this chapter indicated a great importance of the presence of calcium (see below), the second major part of the thesis (chapter 4.4) was dedicated to a careful evaluation of the influence of calcium on An(VI) sorption on clay minerals at (hyper)alkaline conditions. This encompasses the sorption of Ca(II) on Ca-bentonite and its effect on the bentonite surface charge. Furthermore, U(VI) batch sorption experiments with Na-montmorillonite, synthetic kaolinite and muscovite were conducted in 0.1 M NaCl as well as in 0.1 M NaCl + 0.02 M CaCl2 at pH 8-13, in order to quantify the influence of calcium on U(VI) sorption on supposedly Ca-free mineral phases. Site-selective TRLFS was applied with the aim to observe U(VI) sorption species involving calcium. Finally, complementary sorption experiments Np(VI) on muscovite were performed in order to check whether its sorption behavior is analogous to U(VI) under the given conditions. Batch sorption experiments demonstrate that U(VI) retention on Ca-bentonite can be very effective at pH > 10, even in the presence of carbonate and despite the prevalence of anionic aqueous species. Above a certain pH, depending on the concentration of carbonate in solution, carbonate does not play a role in the aqueous U(VI) speciation anymore due to the predominance of hydrolysis. TRLFS measurements revealed a clear correlation between sorption behavior and aqueous U(VI) speciation, showing that retention reaches a maximum at pH 10-12, where UO2(OH)3− is the predominant aqueous species. This raised the question whether the strong retention can be achieved by adsorption of an anionic species to the negatively charged mineral surface or rather by precipitation of uranates. By in situ ATR FT-IR and CTR/RAXR experiments the formation of U(VI) precipitates on the mineral surface was observed at U(VI) concentrations of 2×10-5 M and 5×10-5 M, respectively. However, solubility tests at sub-micromolar U(VI) concentrations, which were also applied in the batch sorption experiments, showed that the observed complete U(VI) removal at pH 10-12 cannot be attributed to precipitation of (earth) alkali-uranates from the solution. In order to unambiguously distinguish between surface precipitation and surface complexation, direct spectroscopic investigations of the U(VI) complexes on the Ca-bentonite surface were performed with site-selective TRLFS and EXAFS. The occurrence of luminescence line-narrowing and the frequency of the total symmetric stretch vibration obtained from the site-selective TRLFS emission spectra, indicate the presence of two U(VI) surface complexes. Also EXAFS spectroscopy confirmed the presence of two independent U(VI) sorption species on Ca-bentonite at pH 8-13. With increasing pH, the nature of the retained U(VI) complexes shifts from bidentate inner-sphere surface complexes with an overall equatorial coordination of five adsorbed on aluminol or silanol edge sites to surface complexes with a 4-fold equatorial coordination, resembling the aqueous species UO2(OH)42−. For the first time, a 4-fold coordination in the equatorial plane of U(VI) was univocally proven with the help of a multiple-scattering feature originating from the strong symmetry of the complexes, and without the need for error-prone shell fitting. The lack of scattering paths from the substrate and the comparatively high value for the total symmetric stretch vibration indicate that the high-pH-component is an outer-sphere complex. Concerning the character of the second sorption species at very high pH it was hypothesized that the anionic uranyl hydroxide complexes are mediated to the surface by calcium cations. It was found that calcium sorbs strongly on Ca-bentonite between pH 8 and 13. Also zeta potential measurements showed a partial compensation of the strongly negative surface charge of Ca-bentonite due to adsorption of calcium. U(VI) sorption on kaolinite and muscovite was strongly reduced in the absence of calcium at pH > 10. An increased retention upon addition of calcium proved the sorption enhancing effect of calcium at pH 10-12. Site-selective TRLFS allowed the spectroscopic observation and identification of calcium-induced U(VI) sorption complexes on muscovite. The obtained spectra correspond to the outer-sphere species found on Ca-bentonite. Combining the findings from batch sorption, zeta potential, TRLFS and EXAFS suggests that calcium adsorbs to the mineral surface in the first place, displaying locally positively charged sites which enable an electrostatically driven attachment of anionic uranyl hydroxides. The same effect could also be demonstrated for Np(VI) sorption on muscovite, which was also strongly enhanced in the presence of calcium at pH 9-12. ISA leads to a mobilization of U(VI) at (hyper)alkaline conditions only when present in very high excess of U(VI). A reduction of sorption on Ca-bentonite and the formation of aqueous U(VI)-ISA complexes, detected with TRLFS, occurred at an U:ISA ratio of 1:100,000. Such conditions are not likely to be found in deep geological repository environments. Based on these findings it can be concluded that under certain alkaline repository conditions, where precipitation does not occur (due to very low concentrations or kinetic restraints), U(VI) and Np(VI) are still effectively retained in argillaceous minerals and rocks by adsorption despite the anionic character of prevailing aqueous species. Repulsive forces between the actinide species and the mineral surfaces are overcome by mediating Ca2+. This finding is of great relevance, as also the migration of very small amounts of uranium or neptunium out of waste repositories could lead to a hazardous accumulation in the long term. The achieved knowledge gain concerning radionuclide retention at environmental conditions helps to take the next step towards realistic long-term safety assessment of nuclear waste repositories.