GC-R-CF-MS method to determine the 13C abundance of gaseous combustion products in cigarette smoke

To determine the 13C abundance of combustion and break down products formed in cigarette smoke, especially CO and CO2, a simple and fast analytical method is needed. Taking into account the knowledge about the determination of the natural 13C abundance in air, an online method - based on gas chromatography-reaction-continuous flow mass spectrometry (GC-R-CF-MS) - has been developed, which enables the determination of the 13C abundance of CO and CO2 in the vapour phase of cigarette smoke with a relative standard deviation of< or =0.5% in one analytical run. Additionally, in a second step, the 13C abundance of total volatile carbon can be determined.     

13C Basal Abundance of Expired CO2 -Definition of Pre-Requisites for Kinetic Breath Tests

Abstract

A sufficiently stable rate of ¹³CO₂ exhalation is necessary when the diagnostic ¹³CO₂ breath tests are performed in healthy subjects and patients. The aim of the research was to define prerequisite conditions for kinetic breath tests in order to ensure a stable ¹³CO₂ background. A 3-part protocol was developed. Part I: a study of the one-day variation of ¹³CO₂ abundance in expired CO₂ confirmed that shifts of the basal ¹³C abundance in breath are inherent in nature. Part II: a study of the variations of ¹³C enrichment after the ingestion of different meals and beverages showed that ingestion of food items containing C₄ plant sugars, such as maize, induces a significant increase in isotopic abundance. Part III: a new test breakfast containing rice grain cereal, milk and orange juice was tested. This test meal induces no significant change on the basal ¹³CO₂ abundance in healthy subjects. This new finding allows to avoid the fasting period normally required prior to a breath test which is sometimes difficult for children and pregnant women.     

Towards an Inhalative 13C Breath Test Method

Abstract

Customary ¹³CO₂ breath tests—and also ¹⁵N urine tests—always start with an oral administration of a test substrate. The test person swallows a stable isotope labelled diagnostic agent. This technique has been used to study several pathophysiological changes in gastrointestinal organs. However, to study pathophysiological changes of the bronchial and lung epithelium, the inhalative administration of a stable isotope labelled agent appeared more suitable to us. [1-¹³C]Hexadecanol and [1-¹³C]glucose were chosen. Inhaled [1-¹³C]hexadecanol did not yield ¹³CO₂ in the exhaled air, but [1-¹³C]glucose did. To study the practicability of the [1-¹³C]glucose method and the reproducibility of the results, 18 inhalation tests were performed with healthy subjects. In 6 self-tests, the optimum inhalative dose of [¹³C]glucose was determined to be 205 mg. Using the APS aerosol provocation system with the nebulizer ‘Medic Aid’ (Erich Jaeger Würzburg), a 25% aqueous solution was inhaled. Then, breath samples were collected at 15 min. intervals and analysed for ¹³CO₂. 75–120min after the end of inhalation a well-reproducible maximum δ¹³C value of 6‰ over baseline (DOB) was detected for 12 healthy probands.

Speculating that the pulmonary resorption of the [¹³C]glucose is the rate-limiting step of elimination, decompensations in the epithelium ought to be reflected in changed [1-¹³C]glucose resorption rates and changed ¹³CO₂ output.

Therefore, we speculate that the inhalation of suitable ¹³C-labelled substrates will pave the way for a new group of ¹³CO₂ breath tests aiding investigations of specific pathophysiological changes in the pulmonary tract, such as inflammations of certain sections and decompensations of cell functions.     

Kinetic studies on the CO oxidation over platinum by means of carbon 13 tracer

The kinetics of the CO oxidation over polycrystalline platinum was investigated with a transient isotope tracer method. Transient CO₂ production was generated by a dosage of various gas mixtures of ¹²CO and O₂ to the surface precovered by various ratios of ¹³CO to ¹²CO. The initial ratio of ¹³CO₂ to ¹²CO₂ in the CO₂ produced transiently equaled that of ¹³CO to ¹²CO in the CO preadsorbed for all the conditions studied; CO must be chemisorbed before being oxidized, i.e. a Langmuir-Hinshelwood mechanism is operative. The ratio of ¹³CO₂ to ¹²CO₂ in CO₂ decreased more rapid than the average ratio of ¹³CO(a) to ¹²CO(a) in CO(a). This apparent inhomogeneity in the reactivity of CO(a) was explained in terms of the boundary reaction model, in which the reaction took place predominantly outside or near the boundary of the CO(a) island.     

Postnatal development of urea synthesis in VLBW-infants as estimated by 15N-ammonium chloride urine test: Differences between AGA- and SGA-Infants

A prototype off-axis integrated cavity output spectrometer (OA-ICOS) utilizing two identical cavities together with a near-infrared (1.63 μm) external cavity tunable diode laser is described. The two-cavity design—one for a reference gas and one for a sample gas—takes advantage of classical double-beam infrared spectrometer characteristics in reducing uncertainties due to laser scan or power instabilities and major temperature variations by a factor of three or better compared with a single-cavity scheme. This is the first OA-ICOS instrument designed to determine ¹³C/¹²C and ¹⁸O/¹⁶O ratios from CO₂ rotation/vibration fine structure in three different combination bands. Preliminary results indicate that at 0.8 Hz a precision of 3.3 and 2.8 \permil\ is obtained for δ¹³C and δ¹⁸O, respectively, over a period of 10 h and a pure CO₂ gas sample at 26 hPa. By averaging 100 spectra over a subset of the data, we achieved a precision of 1.6 and 0.8 \permil\ for δ¹³C and δ¹⁸O, respectively.     

Production of 13C Labelled Pea Flour for Use in Human Digestion and Fermentation Studies

Abstract

Stable isotope breath tests offer a new approach to the study of digestion and fermentation of carbohydrates in man. In this study, ¹³C labelled peas were grown by pulsing 250ml ¹³CO₂ into a sealed growth chamber. A second pulse was added to a portion of the peas to increase the ¹³C enrichment. This generated pea flour with an enrichment of 2.36 at.% excess (range 2.09–2.71 n = 3) and 8.64 atom % excess (range 7.37–9.78 n = 3) respectively. This represented incorporation of an absolute yield of 3.8% of the ¹³CO₂ into peas in the ‘once-labelled’ treatment and 7.5% in the ‘twice-labelled’ treatment. Ingestion of a mixture of the labelled pea flour (300 mg) by two volunteers generated measurable ¹³CO₂ excretion for breath test analysis. The profile of breath ¹³CO₂ enrichment increased to a maximum within three hours after consuming the pea flour followed by a decrease almost back to baseline by 13 hours. Breath ¹³CO₂ appeared to rise again after this apparent nadir at 13 hours until the end of the sampling period. Mathematical analysis of the data suggested that two peaks best described the profile of breath ¹³CO₂ up to 13 hours. A third peak was necessary to describe the late rise in breath ¹³CO₂ enrichment. This use of ¹³C enriched pea flour may provide a useful non invasive method for measurement of digestion and fermentation in vivo.     

The 13C bicarbonate method: an inverse end product method for measuring CO2 production and energy expenditure

We reconsider the principle of the ¹³C bicarbonate (NaH¹³CO₃) method (¹³C-BM) for the determination of the CO₂ production to obtain an estimate of energy expenditure (EE). Its mathematical concept based on a three-compartmental model is related to the [¹⁵N]glycine end product method. The CO₂ production calculated by the ¹³C-BM, R_aCO₂(¹³C) is compared to the result from the indirect calorimetry, RCO₂(IC). In an interspecies comparison (dog, goat, horse, cattle, children, adult human; body mass ranging from 15 to 350?kg, resting and fasting conditions) we found an excellent correlation between the results of ¹³C-BM and IC with RCO₂(IC)?=?0.703?×?R_aCO₂(¹³C), (R²?=?0.99). The slope of this correlation corresponds to the fractional ¹³C recovery (RF(¹³C)) of ¹³C in breath CO₂ after administration of NaH¹³CO₃. Significant increase in RF(¹³C) was found in physically active dogs (0.95?±?0.14; n?=?5) vs. resting dogs (0.71?±?0.10, n?=?17; p?=?.015). The ¹³C recovery in young bulls was greater in blood CO₂ (0.81?±?0.05) vs. breath CO₂ (0.73?±?0.05, n?=?12, p?<?.001) and in ponies with oral (0.76?±?0.03, n?=?8) vs. intravenous administration of NaH¹³CO₃ (0.69?±?0.07; n?=?8; p?=?.026). We suggest considering the ¹³C-BM as a ‘stand-alone’ method to provide information on the total CO₂ production as an index of EE.     

Field-based cavity ring-down spectrometry of δ13C in soil-respired CO2

Measurement of soil-respired CO₂ at high temporal resolution and sample density is necessary to accurately identify sources and quantify effluxes of soil-respired CO₂. A portable sampling device for the analysis of δ¹³C values in the field is described herein.

CO₂ accumulated in a soil chamber was batch sampled sequentially in four gas bags and analysed by Wavelength-Scanned Cavity Ring-down Spectrometry (WS-CRDS). A Keeling plot (1/[CO₂] versus δ¹³C) was used to derive δ¹³C values of soil-respired CO₂. Calibration to the δ¹³C Vienna Peedee Belemnite scale was by analysis of cylinder CO₂ and CO₂ derived from dissolved carbonate standards. The performance of gas-bag analysis was compared to continuous analysis where the WS-CRDS analyser was connected directly to the soil chamber.

Although there are inherent difficulties in obtaining absolute accuracy data for δ¹³C values in soil-respired CO₂, the similarity of δ¹³C values obtained for the same test soil with different analytical configurations indicated that an acceptable accuracy of the δ¹³C data were obtained by the WS-CRDS techniques presented here. Field testing of a variety of tropical soil/vegetation types, using the batch sampling technique yielded δ¹³C values for soil-respired CO₂ related to the dominance of either C₃ (tree, δ¹³C=?27.8 to?31.9 ‰) or C₄ (tropical grass, δ¹³C=?9.8 to?13.6 ‰) photosynthetic pathways in vegetation at the sampling sites. Standard errors of the Keeling plot intercept δ¹³C values of soil-respired CO₂ were typically<0.4 ‰ for analysis of soils with high CO₂ efflux (>7–9 μmol m^?2 s^?1).     

Vorwort

¹³C-enriched flour was obtained by the photosynthetic incorporation of ¹³CO₂ during the grain filling period of wheat plants. The mean atom %excess of the pooled flour obtained on two consecutive years was 2.6% and 3.9%. The ¹³C-labelled flour was used as a substrate to measure starch digestion and the effect of gelatinisation on ¹³CO₂ recovery in a healthy adult volunteer. Only 400 mg of ¹³C flour/adult were required in order to accurately measure the excretion of ¹³CO₂. The starch load could be varied by the addition of flour with natural ¹³C abundance. An increased rate of starch hydrolysis after gelatinisation was demonstrated after the ingestion of a 50 g starch load. Wheat starch can be successfully labelled with ¹³C and used as a substrate for ¹³C breath tests.     

The effect of internal Co2 conductance on leaf carbon isotope ratio

We estimated internal CO₂ conductance (g_i ) for C₃ plant species of different life forms (annual herbs, deciduous trees and evergreen trees) grown in a variety of environments to examine the effect of g i on their leaf carbon isotope ratio (i¹³C). The purpose of this study was to test the validity of using i¹³C as an index of photosynthetic water use efficiency (WUE). When comparing deciduous tree species grown in contrasting light environments, there was a strong positive relationship between i¹³C and WUE. Similarly, i¹³C was positively correlated to WUE when comparing the different species of evergreen trees. However, the difference in WUE between evergreen and deciduous tree species did not relate to that in leaf i¹³C. In addition, WUE was similar between highland and lowland herbaceous plants, although the former had a much higher i¹³C. The positive relationship between i¹³C and WUE did not hold across different life forms and different altitudes when differences in g_i did not relate to those in stomatal conductance, resulting in independence of chloroplast CO₂ partial pressure from intercellular CO₂ partial pressure.     

Interactions of D2O with CO and CO2 molecules at cryogenic temperatures

On the basis of the matrix effect of secondary-ion mass spectrometry (SIMS), the intermolecular interactions between D₂O and hydrophobic molecules have been investigated at temperature of 15 K. The D⁺ yield is found to be enhanced markedly relative to the D₃O⁺ yield when the D₂O molecule forms a complex with the CO or CO₂ molecules on the surface. The CO molecules are incorporated in the inner pores of amorphous solid water and then cover the outermost surface facing to the vacuum, which is followed by the 3D-island growth on it. A similar result is obtained for the adsorption of the CO₂ molecule but the filling of the inner pores is not complete due to the lower mobility of the CO₂ molecule. The D₂O film grows on the CO₂ layer, but a pure D₂O film is hardly formed on the CO layer due to the occurrence of intermixing.     

A pulsed EPR study of the catalytic oxidation of CO over Cu/SnO2

The role of the Cu(II) in the catalytic oxidation of CO over Cu/SnO₂ with low Cu(II) content was studied by continuous wave EPR, electron spin echo envelope modulation (ESEEM) and hyperfine sublevel correlation (HYSCORE) spectroscopes. Three methods were employed for introducing the copper: (i) by coprecipitation, (ii) impregnation onto SnO₂ gel and (iii) impregnation onto calcined SnO₂. Two types of Cu(II) species were identified in these calcined Cu/SnO₂ materials. Those belonging to the first type, termed B and C, exhibit highly resolved EPR spectra with well defined EPR parameters and are located within the bulk of the oxide. The other group comprises a distribution of surface Cu(II) species with unresolved EPR features and are referred to as S. While the latter were readily reduced by CO the former required long exposures at high temperatures (> 673 K). The specific interactions of the different Cu(II) species with CO were investigated through the determination of the¹³C hyperfine coupling of enriched¹³CO. The ESEEM spectra of calcined samples, generated either by coprecipitation or impregnation, show after the adsorption of CO signals at the Larmor frequencies of^{117, 119}Sn and¹³C and at twice these Larmor frequencies. Although these signals indicate that^{117, 119}Sn and¹³C are in the close vicinity of Cu(II), they cannot provide the hyperfine couplings of these nuclei. This problem was overcome by the application of the HYSCORE experiment. The 2D HYSCORE spectra show well resolved cross peaks which provide the hyperfine interaction of these nuclei. Simulations of the HYSCORE spectra yield for^{117, 119}Sn an isotropic hyperfine constant,a _iso, of ±4.0 MHz and an anisotropic component,T _?, of ±2.0 MHz. Pulsed ENDOR spectra also showed^{117, 119}Sn signals which agree with the above values. The¹³C cross peaks yielda _iso=±1.0 MHz andT _?=±2.0 MHz. Similar C cross peaks were observed in spectra of calcined Cu/SnO₂ after the adsorption of CO₂. Based on the same hyperfine couplings in the samples exposed to¹³CO and¹³CO₂ the signals were assigned to surface carbonate species generated by part of the Cu(II) S type species rather then by species B and the role of the Cu(II) in the oxidation process is discussed.     

Determination of 13C/12C-Ratios in Rumen Produced Methane and CO2 of Cows,Sheep and Camels

Abstract

Naturally produced methane shows different δ¹³C-values with respect to its origin, e.g., geological or biological. Methane-production of ruminants is considered to be the dominant source from the animal kingdom. Isotopic values of rumen methane—given in literature—range between ?80‰ and -50‰ and are related to feed composition and also sampling techniques. Keeping cows, camels and sheep under identical feed conditions and sampling rumen gases via implanted fistulae we compared δ_PDB ¹³C-values of methane and CO₂ between the species. Referring to mean values obtained from 4 or 5 samples at different times of 11 animals (n = 47) we calculated δ_PDB ¹³C-medians resulting in small but not significant differences within and significant differences between the species for CO₂ and methane. The δ_PDB ¹³C-differences between methane and CO₂ were statistically equal within and also between the species. Therefore a linear regression of methane values on CO₂ is appropriate and leads to: δ_PDB ¹³C(methane)‰ = 1,57 * δ_PDB ¹³C(CO₂)‰-47‰ with a correlation coefficient of r = 0,87.     

Compact laser difference-frequency spectrometer for multicomponent trace gas detection

2 O), carbon dioxide (CO₂), and sulfur dioxide (SO₂). Real-time detection of CO, N₂O, and CO₂ was performed in open air over a path length of 5 to 18 m. The feasibility of DFG spectroscopic measurement of the ¹³C/¹²C and ¹⁸O/¹⁷O/¹⁶O isotopic ratios in atmospheric carbon dioxide was also investigated. We report what to our knowledge is the first simultaneous spectroscopic measurement of all three isotopes of oxygen in ambient CO₂. Received: 14 August 1997/Revised version: 3 November 1997     

Laser spectroscopic monitoring of gas emission and measurements of the C/C isotope ratio in CO2 from a wood-based combustion

We report on the application of a compact and field-deployable instrument, based on a continuous-wave fiber-coupled Telecom external cavity diode laser, to measure the ¹³C/¹²C isotope ratio in CO₂ from a wood-based combustion. Carbon dioxide, the most important greenhouse gas, is a major product of combustion. The measurements of the ¹³C/¹²C isotopic ratio in CO₂ from combustion emission permit one to identify the CO₂ source and to study the temporal and spatial variations of pollution in the atmosphere. The average value of the ¹³CO₂/¹²CO₂ ratio is found to be (1.1011±0.0024)%. The corresponding δ-value relative to PDB standard is (−20.17±2.14)‰, which is in good agreement with the typical value of (−25±2)‰ for wood. Simultaneous monitoring of multiple species from gas emission has been performed using direct-absorption spectroscopy. The concentrations of C₂H₂, CO, CO₂ and H₂O were determined on the basis of integrated absorbance measured by least-squares fitting a Voigt lineshape to experimental absorption spectra.     

CO2/CO2 isotopic ratio measurements with a continuous-wave quantum cascade laser in exhaled breath

A laser spectrometer based on a continuous-wave thermoelectrically-cooled distributed feedback quantum cascade laser at ∼2308 cm⁻¹ has been evaluated for measurement of ¹³CO₂/¹²CO₂ isotopic ratio (δ¹³C) changes in exhaled breath samples and in CO₂ gas flows in the concentration range 1-5%. Mid-infrared CO₂ absorption spectra were measured in a 54.2-cm long optical cell using balanced detection whereby the beam passing through the cell was ratioed against a reference beam split-off from the main beam before the cell. Signal-to-noise ratios (SNR) were estimated for CO₂ concentration measurements determined from either absorption peak amplitude or absorption peak area. The highest SNR were achieved in the measurements based upon a fitted absorption peak area. Typical short-term δ¹³C precisions of 1.1⁰/₀₀ (1-s integration time) and 0.5⁰/₀₀ (8-12-s integration time) were estimated from the two-sample (Allan) variance plots of data recorded in the optical cell at a pressure of 20 Torr and with no active temperature stabilization of the cell and gas flow. The best precision of 0.12⁰/₀₀ was achieved for averaging 80 successive 1-s integration time measurements.     

Relative intensities in x-ray photoelectron spectra

An experimental determination of the relative intensities of X-ray photoelectron lines corresponding to the inner levels of elements with Z ? 20, and calculations of the total photo-ionization cross-sections for all shells of these elements with the Hartree—Fock—Slater potential are reported. The experimental and theoretical values agree well for the 1s levels while marked discrepancies are revealed for the 2p levels. The theoretical values of the cross sections for the atomic valence levels are used to calculate the relative intensities of molecular levels in CF₄, BF₄^?, BeF₄^2?, LiF, NO₃^?, CO₃^2?, CO, N₂, CO₂, H₂O and C₄H₅N. The results of the calculations agree satisfactorily with experiment.     

Relative intensities in X-ray photoelectron spectra

An experimental determination of the relative intensities of X-ray photoelectron lines corresponding to the inner levels of elements with Z ? 20, and calculations of the total photo-ionization cross-sections for all shells of these elements with the Hartree—Fock—Slater potential are reported. The experimental and theoretical values agree well for the 1s levels while marked discrepancies are revealed for the 2p levels. The theoretical values of the cross sections for the atomic valence levels are used to calculate the relative intensities of molecular levels in CF₄, BF₄^?, BeF₄^2?, LiF, NO₃^?, CO₃^2?, CO, N₂, CO₂, H₂O and C₄H₅N. The results of the calculations agree satisfactorily with experiment.     

Kinetic Carbon Isotope Effects in the Decarbonylation of Lactic Acid of Natural Isotopic Composition and of [1-14C] Lactic Acid

Studies of carbon-13 and carbon-14 kinetic isotope effects (K. I. E.) in the decarbonylation of lactic acid (L. A.) in sulphuric acid and in phosphoric acids media have been summarized and compared with earlier studies of ¹⁴C and ¹³C K. I. E. in the decarbonylation of formic and oxalic acids in concentrated sulphuric acid. Supplementary data concerning the decarbonylation of L. A. in sulphuric acid diluted with water and in pyrophosphoric acid are presented and discussed. The observed temperature dependences of ¹³C and ¹⁴C K. I. E. in concentrated H₂SO₄ and in concentrated phosphoric acids media have been rationalized by invoking a change of the mechanism of decarbonylation of L. A. in concentrated sulphuric and phosphoric acids with temperature. Preliminary calculational results concerning ¹³C and ^1??C K. I. E. in decarbonylation processes are also presented. In H₂SO₄ diluted with water and in H₃PO₄ diluted with water the temperature dependence of ¹³C and ¹⁴C K. I. E. is normal and well reproduced by one frequency approximation. In concentrated sulphuric acid and in concentrated phosphoric acids besides the C—OH bond rupture the rupture of a C—C bond had to be considered also to reproduce the observed ¹³C K. I. E. in selected temperature regions.     

Use of the optogalvanic effect (OGE) for isotope ratio spectrometry of 13CO2 and 14CO2

The use of isotopic carbon dioxide lasers for determination of carbon (and oxygen) isotope ratios was first demonstrated in 1994. Since then a commercial device called LARA^?, has been manufactured and used for Helicobacter pylori breath tests using ¹³C-labelled urea. The major advantages of the optogalvanic effect compared with other infrared absorption isotope ratio measurement techniques are its lack of optical background and its high sensitivity resulting from a signal gain proportional to laser power. Continuous normalisation using two cells, a standard and sample, lead to high accuracy as well as precision. Recent advances in continuous flow measurement of ¹³C/¹²C ratios of CO₂ in air and extensions of the technique to ¹⁴C, which can be analysed as a stable isotope, are described.