81 research outputs found
Application of relaxed eddy accumulation (REA) on managed grassland
Abstract. Relaxed eddy accumulation is applied for measuring fluxes of trace gases for which there is a lack of sensors fast enough in their resolution for eddy-covariance. On managed grasslands, the length of time between management events and the application of relaxed eddy accumulation has an essential influence on the determination of the proportionality factor b and thereby on the resulting flux. In this study this effect is discussed for the first time. Also, scalar similarity between proxy scalars and scalars of interest is affected until the ecosystem has completely recovered. Against this background, CO2 fluxes were continuously measured and 13CO2 isofluxes were determined with a high measurement precision on two representative days in summer 2010. This enabled the evaluation of the 13CO2 flux portion of the entire CO2 flux, in order to estimate potential influences on tracer experiments in ecosystem sciences and to compare a common method for the partitioning of the net ecosystem exchange into assimilation and respiration based on temperature and light response with an isotopic approach directly based on the isotope discrimination of the biosphere.
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Correction to Online Hydrogen-Isotope Measurements of Organic Samples Using Elemental Chromium:An Extension for High-Temperature Elemental-Analyzer Techniques
Correction to Online Hydrogen-Isotope Measurements of Organic Samples Using Elemental Chromium:An Extension for High-Temperature Elemental-Analyzer Techniques
Development and evaluation of a suite of isotope reference gases for methane in air
Measurements from multiple laboratories have to be related to unifying and traceable reference material in order to be comparable. However, such fundamental reference materials are not available for isotope ratios in atmospheric methane, which led to misinterpretations of combined data sets in the past. We developed a method to produce a suite of synthetic CH4-in-air standard gases that can be used to unify methane isotope ratio measurements of laboratories in the atmospheric monitoring community. Therefore, we calibrated a suite of pure methane gases of different methanogenic origin against international referencing materials that define the VSMOW (Vienna Standard Mean Ocean Water) and VPDB (Vienna Pee Dee Belemnite) isotope scales. The isotope ratios of our pure methane gases range between -320 and +40% for delta H-2-CH4 and between -70 and -40% for delta C-13-CH4, enveloping the isotope ratios of tropospheric methane (about -85 and -47% for delta H-2-CH4 and delta C-13-CH4 respectively). Estimated uncertainties, including the full traceability chain, are</p
Gravitational Radiation from Gamma-Ray Burst Progenitors
We study gravitational radiation from various proposed gamma-ray burst (GRB)
progenitor models, in particular compact mergers and massive stellar collapses.
These models have in common a high angular rotation rate, and the final stage
involves a rotating black hole and accretion disk system. We consider the
in-spiral, merger and ringing phases, and for massive collapses we consider the
possible effects of asymmetric collapse and break-up, as well bar-mode
instabilities in the disks. We calculate the strain and frequency of the
gravitational waves expected from various progenitors, at distances based on
occurrence rate estimates. Based on simplifying assumptions, we give estimates
of the probability of detection of gravitational waves by the advanced LIGO
system from the different GRB scenarios.Comment: 26 pages, 5 figures, accepted for publication in Ap
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