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   <subfield code="a">The effect of temperature on the rate, affinity, and 15N fractionation of NO3 − during biological denitrification in soils</subfield>
   <subfield code="h">[Elektronische Daten]</subfield>
   <subfield code="c">[Federico Maggi, William Riley]</subfield>
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   <subfield code="a">Nine independent experiments of NO3 − denitrification were analysed using the Arrhenius law and the Eyring's transition-state theory to highlight how temperature affects reaction rate constants, affinities, and kinetic isotopic effects. For temperatures between 20 and 35°C, the Arrhenius law and the transition-state theory described equally well observed temperature increases in 14NO3 − and 15NO3 −denitrification rates (R&gt;0.99 and residuals NRMSE&lt;3.39%, p&lt;0.01). These increases were partly caused by an increase in frequency factor and a slight decrease in activation energy (enthalpy and entropy). Parametric analysis also showed that the affinity of 14NO3 − and 15NO3 − toward a microbial enzyme increased exponentially with temperature and a strong correlation with the rate constants was found (R=0.93, p&lt;0.01). Experimental time- and temperature-averaged fractionation factor α P/S showed only a slight increase with increasing temperature (i.e. lower isotopic effects); however, a comprehensive sensitivity analysis in the concentration-temperature domain using average thermodynamic quantities estimated here showed a more complex response; α P/S was relatively constant for initial bulk concentrations [NO3 −]0≤0.01molkg−1, while substantial nonlinearities developed for [NO3 −]0≥0.01molkg−1 and appeared to be strongly correlated with microbial biomass, whose concentration and activity varied primarily as a function of temperature and available substrate. Values of α P/S ranging between 0.9 and 0.98 for the tested temperatures suggested that interpretations of environmental isotopic signatures should include a sensitivity analysis to the temperature as this affects directly the rate constants and affinities in biochemical reactions and may hide process- and source-related isotopic effects.</subfield>
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   <subfield code="a">Springer International Publishing Switzerland, 2015</subfield>
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  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Denitrification</subfield>
   <subfield code="2">nationallicence</subfield>
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  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">14N and 15N</subfield>
   <subfield code="2">nationallicence</subfield>
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  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Kinetic isotopic effects</subfield>
   <subfield code="2">nationallicence</subfield>
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  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Affinity</subfield>
   <subfield code="2">nationallicence</subfield>
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  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Temperature</subfield>
   <subfield code="2">nationallicence</subfield>
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  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Arrhenius</subfield>
   <subfield code="2">nationallicence</subfield>
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  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Transition-state theory</subfield>
   <subfield code="2">nationallicence</subfield>
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  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">α : Fractionation factor (-)</subfield>
   <subfield code="2">nationallicence</subfield>
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  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">δ : Isotopic composition (-)</subfield>
   <subfield code="2">nationallicence</subfield>
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  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">x, y : Stoichiometric coefficients (-)</subfield>
   <subfield code="2">nationallicence</subfield>
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  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">G : Gibbs free energy (Jmol−1)</subfield>
   <subfield code="2">nationallicence</subfield>
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  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">h : Planck constant (Js)</subfield>
   <subfield code="2">nationallicence</subfield>
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  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">H : Heat content (Jmol−1)</subfield>
   <subfield code="2">nationallicence</subfield>
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  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">k : Reaction rate constant (Τ−1)</subfield>
   <subfield code="2">nationallicence</subfield>
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  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">K b : Boltzmann constant (JK−1 mol−1)</subfield>
   <subfield code="2">nationallicence</subfield>
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  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">K : Affinity (half-saturation concentration) (M)</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">S : Entropy content (JK−1 mol−1)</subfield>
   <subfield code="2">nationallicence</subfield>
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  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">t : Time (T)</subfield>
   <subfield code="2">nationallicence</subfield>
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  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">T : Absolute temperature (K)</subfield>
   <subfield code="2">nationallicence</subfield>
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   <subfield code="a">NRMSE : Normalized root mean square error (-)</subfield>
   <subfield code="2">nationallicence</subfield>
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  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">R : Correlation coefficient (-)</subfield>
   <subfield code="2">nationallicence</subfield>
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   <subfield code="a">Maggi</subfield>
   <subfield code="D">Federico</subfield>
   <subfield code="u">Laboratory for Advanced Environmental Engineering Research, School of Civil Engineering, The University of Sydney, 2006, Sydney, NSW, Australia</subfield>
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   <subfield code="a">Riley</subfield>
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   <subfield code="u">Earth Systems Division, Climate and Carbon Department, Lawrence Berkeley National Laboratory, 94720, Berkeley, CA, USA</subfield>
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   <subfield code="t">Biogeochemistry</subfield>
   <subfield code="d">Springer International Publishing</subfield>
   <subfield code="g">124/1-3(2015-05-01), 235-253</subfield>
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   <subfield code="a">Metadata rights reserved</subfield>
   <subfield code="b">Springer special CC-BY-NC licence</subfield>
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