24 research outputs found

    The stable isotopic signature of biologically produced molecular hydrogen (H<sub>2</sub>)

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    Biologically produced molecular hydrogen (H<sub>2</sub>) is characterised by a very strong depletion in deuterium. Although the biological source to the atmosphere is small compared to photochemical or combustion sources, it makes an important contribution to the global isotope budget of H<sub>2</sub>. Large uncertainties exist in the quantification of the individual production and degradation processes that contribute to the atmospheric budget, and isotope measurements are a tool to distinguish the contributions from the different sources. Measurements of &delta; D from the various H<sub>2</sub> sources are scarce and for biologically produced H<sub>2</sub> only very few measurements exist. <br><br> Here the first systematic study of the isotopic composition of biologically produced H<sub>2</sub> is presented. In a first set of experiments, we investigated &delta; D of H<sub>2</sub> produced in a biogas plant, covering different treatments of biogas production. In a second set of experiments, we investigated pure cultures of several H<sub>2</sub> producing microorganisms such as bacteria or green algae. A Keeling plot analysis provides a robust overall source signature of &delta; D = &minus;712&permil; (±13&permil;) for the samples from the biogas reactor (at 38 °C, &delta; D<sub>H2O</sub>= +73.4&permil;), with a fractionation constant &varepsilon;<sub>H2-H2O</sub> of −689&permil; (±20&permil;) between H<sub>2</sub> and the water. The five experiments using pure culture samples from different microorganisms give a mean source signature of &delta; D = &minus;728&permil; (±28&permil;), and a fractionation constant &varepsilon;<sub>H2-H2O</sub> of −711&permil; (±34&permil;) between H<sub>2</sub> and the water. The results confirm the massive deuterium depletion of biologically produced H<sub>2</sub> as was predicted by the calculation of the thermodynamic fractionation factors for hydrogen exchange between H<sub>2</sub> and water vapour. Systematic errors in the isotope scale are difficult to assess in the absence of international standards for &delta; D of H<sub>2</sub>. <br><br> As expected for a thermodynamic equilibrium, the fractionation factor is temperature dependent, but largely independent of the substrates used and the H<sub>2</sub> production conditions. The equilibrium fractionation coefficient is positively correlated with temperature and we measured a rate of change of 2.3&permil; / °C between 45 °C and 60 °C, which is in general agreement with the theoretical prediction of 1.4&permil; / °C. Our best experimental estimate for &varepsilon;<sub>H2-H2O</sub> at a temperature of 20 °C is −731&permil; (±20&permil;) for biologically produced H<sub>2</sub>. This value is close to the predicted value of −722&permil;, and we suggest using these values in future global H<sub>2</sub> isotope budget calculations and models with adjusting to regional temperatures for calculating &delta; D values

    The Oscillating Universe: an Alternative to Inflation

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    The aim of this paper is to show, that the 'oscillating universe' is a viable alternative to inflation. We remind that this model provides a natural solution to the flatness or entropy and to the horizon problem of standard cosmology. We study the evolution of density perturbations and determine the power spectrum in a closed universe. The results lead to constraints of how a previous cycle might have looked like. We argue that most of the radiation entropy of the present universe may have originated from gravitational entropy produced in a previous cycle. We show that measurements of the power spectrum on very large scales could in principle decide whether our universe is closed, flat or open.Comment: revised version for publication in Classical and Quantum Gravity, 23 pages, uuencoded compressed tarred Latex file with 7 eps figures included, fig.8 upon reques

    A many-analysts approach to the relation between religiosity and well-being

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    The relation between religiosity and well-being is one of the most researched topics in the psychology of religion, yet the directionality and robustness of the effect remains debated. Here, we adopted a many-analysts approach to assess the robustness of this relation based on a new cross-cultural dataset (N=10,535 participants from 24 countries). We recruited 120 analysis teams to investigate (1) whether religious people self-report higher well-being, and (2) whether the relation between religiosity and self-reported well-being depends on perceived cultural norms of religion (i.e., whether it is considered normal and desirable to be religious in a given country). In a two-stage procedure, the teams first created an analysis plan and then executed their planned analysis on the data. For the first research question, all but 3 teams reported positive effect sizes with credible/confidence intervals excluding zero (median reported β=0.120). For the second research question, this was the case for 65% of the teams (median reported β=0.039). While most teams applied (multilevel) linear regression models, there was considerable variability in the choice of items used to construct the independent variables, the dependent variable, and the included covariates

    Evidence of anaerobic syntrophic acetate oxidation in biogas batch reactors by analysis of <sup>13</sup>C carbon isotopes

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    Between 2008 and 2010 various batch experiments were carried out to study the stable carbon isotopic composition of biogas (CH4 and CO2) produced from (i) pure sludge and (ii) sludge including maize. From the evolution of the natural isotopic signature, a temporal change of methanogenic pathways could be detected for the treatment with maize showing that a dominance in acetotrophic methanogenesis was replaced by a mixture of hydrogenotrophic and acetotrophic methanogenesis. For pure sludge, hydrogenotrophic methanogenesis was the dominant or probably exclusive pathway. Experiments with isotopically labelled acetate (99% (CH3COONa)-C-13 and 99% (CH3COONa)-C-13) indicated a significant contribution of syntrophic acetate oxidation (SAO) for all the investigated treatments. In the case of pure sludge, experiments from 2008 showed that acetate was almost entirely oxidised to CO2, i.e. acetotrophic methanogenesis was negligible. However, in 2010, the sludge showed a clear dominance in acetotrophic methanogenesis with a minor contribution by SAO indicating a significant change in the metabolic character. Our results indicate that SAO during anaerobic degradation of maize might be a significant process that needs to be considered in biogas research

    Stable carbon isotopes of methane for real- time process monitoring in anaerobic digesters

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    Efficient operation and stability of biogas plants requires continuous monitoring of the digester content. Traditional laboratory analysis of digester sludge is often complex and time-consuming and shows a delayed response to disruptions within the fermentation process. As a new approach, we applied an online measurement technique (laser absorption spectroscopy) for real-time monitoring of stable carbon isotopes of methane (13C CH 4) in a pilot-scale biogas digester (3500 L) regularly fed with maize silage. Generally, isotopic composition of methane gives information about specific substrate degradation, that is, methanogenic pathways that reflect the actual digester state. First results of a 2-wk monitoring experiment show that stable carbon isotopes of methane respond promptly and highly dynamic to changes in the process state of the digester. In combination with other monitoring parameters (methane production rate, concentration of volatile fatty acids, and pH) the fluctuations in 13C CH 4 can be interpreted as a change in methanogenic pathways due to a high organic loading rate. In this context, 13C CH 4 might be used as a new parameter tool for monitoring and characterization of the process state of the digester
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