Equilibrating of 15N-Gases by Electrodeless Discharge: A Method of Indirect Mass Spectrometric Analysis of 30N2 for Denitrification Studies in Soils

Abstract

The estimation of denitrification in soil by the ¹⁵N tracer technique includes isotope analysis of gas samples with a nonrandom distribution of the N₂ mole masses of 28, 29 and 30. In that case the emission of total ¹⁵N is underestimated by calculating ¹⁵N atom fractions from the ²⁹N₂/²⁸N₂ ratio if ³⁰N₂ is not considered. ³⁰N₂ can be measured indirectly in N₂ enriched with ¹⁵N with nonrandom distribution of mole masses by mass spectrometric analysis. The nitrogen fraction of gas samples was transferred to discharge tubes. Microwaves (60 sec) generated an electrodeless discharge of the gas which caused a temporary split-up of N₂ molecules and thus established an equilibrium distribution of the mole masses. The ²⁹N₂/²⁸N₂ ratio was measured in equilibrated and in untreated samples to calculate the real emission of ¹⁵N. The measurements of ¹⁵N standard gases by this method satisfactorily coincided with calculated values for ¹⁵N atom fraction above a concentration of 50 δ‰.     

Bestimmung der 15N Häufigkeit bei nichtstatistischer 15N-verteilung in N2 sowie bei N2O in Bodenluftproben mittels GC-R-IRMS-Kopplung in einem Probenlauf

Abstract

An analysis technique based on GC-R-IRMS coupling (Gas-Chromatography-Reduction-Isotope Ratio Mass Spectrometry) is demonstrated. The ¹⁵N abundance of N² and N²O in atmospheric air or soil atmosphere from nitrification or denitrification processes with nonrandom distribution is determined in one run. The 12 ml sample is separated from CO² and transported by a helium gas stream through a cooling trap. The N²O is trapped in the cooling trap while the N² passes through it and enters the GC. After GC separation and O² removal in a reduction column, part of the N² enters an isotope mass spectrometer to determine the masses m/z 28,29 and 30. The interferences on mass 30 by the formation of NO in the ion source of the mass spectrometer are eliminated by a calibration and a correction procedure. Upon removing the cooling trap, the N²O is injected into the GC, where it is separated and then quantitatively reduced to N² in a reduction column. The measurement of one sample takes 16 minutes. The detection limit of the ³⁰R_t in alteration N₂ is Δ³⁰R_t = 5 · 10^?7. The detection limit of the N₂O is 3.6 nl.     

Incorporation of 15NO2 Nitrogen into Individual Amino Acids by Sunflowers Using Gc-C-Irms

Abstract

The nitrogen isotopic composition of individual amino acids in sunflower leaves after exposures to ¹⁵NO₂ in the range of ambient NO₂ concentrations (5–37 ppb) was analysed by Gas Chromatography-Combustion-Isotope Ratio Mass Spectrometry (GC-C-IRMS). Amino acids as well as the amides glutamine and asparagine were converted with MTBSTFA (N-methyl-N-(tert.-butyldimethylsilyl)-tri-fluoroacetamid) in pyridine to their corresponding TBDMS derivatives (N, O-tert.-butyldimethylsilyl) in a simple one-step silylation reaction. The derivatized amino acids were separated by gas chromatography, combusted on-line, and the products were sent continuously to an isotope ratio mass spectrometer. Accurate measurements were obtained, when more than 7 nmol N₂ were introduced into the ion source of the mass spectrometer per gas chromatographically separated and combusted compound. No interferences of the silicate and fluor containing derivatization agents on the performance of the system were observed.

In the range of ambient NO₂ concentrations sunflower leaves predominately incorporate the nitrogen derived from atmospheric NO₂ into soluble amino acids. The highest δ¹⁵N values were measured for alanine. The ¹⁵N enrichments of the detectable amino acids increased with increasing ¹⁵NO₂ concentration.     

Bestimmung der 15N-Häufigkeit von N2O und N2 mittels emissionsspektrometrischer continuous-flow-Messung

Abstract

Tests were made for a quantitative decomposition of N₂O to N₂ and for the setting of a statistical equilibrium in mixtures with gaseous nitrogen of nonrandom distribution by emission spectrometric continuous-flow-measurements. Under high-frequency-discharge conditions a residence time of 0.5 seconds is enough for a quantitative decomposition. In this time the statistical balance in the mixture of N₂O and N₂ is reached. The determination of the relative ¹⁵N abundance in pure N₂O or N₂ gases or in mixtures of N₂O and N₂ in a continuous-flow-emissionspectrometer can directly be achieved.     

Methodische Untersuchungen zum 15N-ConFlo-IRMS-System

After installing a C-GC-IRMS-System (Elemental analyzer EA 1108 CHN + IRMS MAT 252) some problems arose with respect to the external precision of the δ¹⁵N values (standard deviation approx. 1‰ at < 50 μg N) after changeover from ¹³C to ¹⁵N measurements.

Attempts were made to determine the reasons for these effects and to eliminate them by changes of the Carlo Erba on-line combustion system (EA) and the split.

Non-quantifiable contributions, e.g., air nitrogen and/or N₂ in carrier gas helium were reduced by a blank correction.

Using Cyclohexanone-2, 4-dinitrophenylhydrazone it was shown that under the same conditions and after a common blank correction with small and large amounts of samples (60-650 μg, 20% N) an external precision of 0.2‰ (standard deviation, 10 cycles) can be reached.     

A New Approach to Determining the Content and 15N Abundance of Total Dissolved Nitrogen in Aqueous Samples: TOC Analyser-QMS Coupling

Abstract

The standard method for determining the ¹⁵N abundance of total dissolved nitrogen (TDN) in aqueous samples (e.g., soil leachate, sewage, urine) is currently Kjeldahl digestion followed by steam distillation or diffusion to isolate the ammonium, and then ¹⁵N measurement using IRMS. However, this technique is both time-consuming and laborious. One way of overcoming these disadvantages could be to couple a TOC analyser to determine the TDN with a sufficient quadrupole MS to determine the ¹⁵N abundance. The highTOC analyser (Elementar Analysensysteme Hanau, Germany), which catalytically oxidises the sample's total nitrogen with a high, constant yield to nitrogen monoxide (NO), appeared particularly suitable. The quadrupole-MS ESD 100 (InProcess Instruments Bremen, Germany) proved to be a suitable mass spectrometer for the ¹⁵N determination of NO. This combination of instruments was found to provide a workable method in numerous measurements of standard and actual samples. The detection limit concerning the N amount required per analysis is 2 μg, corresponding to an N concentration of 0.7mg/l in a maximum sample volume of 3ml. Depending on the N concentration, ¹⁵N abundances starting from 0.5 at.% can be measured with the required precision of better than 3% (simple standard deviation). For example, measuring the abundance of 0.5 at.% requires about 50 μg N, whereas for 1 at.% or more only about 5 μg N is needed per analysis.     

Conference Reports

Abstract

One purpose of new land use concepts for degraded fens (organic soils with high N content) is the reduction of the mineralization process due to very high groundwater levels. However, knowledge of nitrogen mineralization process (net and gross) in degraded fen soils affected by reflooding is very small. Therefore, the objectives of our study were (a) to evaluate the suitability of ¹⁵N pool dilution method for measurements of gross mineralization rates in degraded fen soils and (b) to investigate how the reflooding of a degraded fen affects the net and gross nitrogen mineralization in a short-term incubation experiment. The usability of the ¹⁵N pool dilution method was diminished by the low recovery of the applied ¹⁵NH₄ ^? at time zero. The recovery of the added ¹⁵NH₄ ^? in the extractable soil NH₄ ^? pool was only 13.5% for the drained soil and 59.6% for the reflooded soil. However, the gross mineralization rates were similar for both soils and exceeded always the net rates substantially. The cumulative net mineralization rate was higher for the reflooded soil (1.58 μg N?cm^?3?d^?1) than for the drained soil (-0.67 μg N?cm^?3?d^?1). Differences between the two soils were also found in the nitrification intensity and the loss of ¹⁵N. This was probably one reason for the higher net mineralization rate in the reflooded soil.     

PreCon: A Fully Automated Interface for the Pre-Gc Concentration of Trace Gases on Air for Isotopic Analysis

Abstract

For the high precision isotope analysis of atmospheric trace gases a computer controlled concentration interface has been developed. From small air samples it collects either N₂O or CO₂ derived from CH₄ at their respective concentrations (0.3 ppm for N₂O, 1.7 ppm for CH₄) into a small diameter cold trap (?196°C) and interfaces via GC and open split to an isotope ratio mass spectrometer (Finnigan MAT 252) for on-line isotope evaluation. External reproducibilities for repeated measurements of 100 ml air samples from the same source of < 0.2° (δ-notation) have been achieved for ¹³C/¹²C from CH₄ and for ¹⁵N/¹⁴N and ¹⁸O/¹⁶O from N₂O. The precision is adequate to monitor the isotopic changes in these gases during a day's course.     

Aufnahme von 15NO2 und Einbau des 15NO2-Stickstoffs in verschiedene Stickstofffraktionen bei Sonnenblumen (Uptake of 15NO2 and Metabolic Transfer of the 15NO2 Nitrogen to Various Nitrogen Fractions of Sunflowers)

Abstract

Sunflowers were exposed to ¹⁵NO₂ at a range between 4,9 and 42,0 ppb. The ¹⁵NO₂ uptake was quantified and the fate of the ¹⁵N in different parts and pools of nitrogen was investigated. The very high δ¹⁵N-values of the free amino acid pool can't give an answer to the question whether the NO₂-nitrogen is incorporated by a different pathway, compared to the nitrogen which derives from root uptake. Or does a compartmentation of the nitrate pool in the plant cell cause a dilution of the ¹⁵N enrichment in the mineral nitrogen pool during sample preparation?     

Dinitrogen Fixation of Microbe-Plant Associations as Affected by Nitrate and Ammonium Supply

Abstract

The dinitrogen fixation activity of Azospirillum sp., and Pantoea agglomerans strains was determined by ¹⁵N₂ incorporation after incubation with ¹⁵N₂ labeled air or/and by acetylene reduction. These bacterial strains were able to fix N₂ both in pure culture and in association with wheat plants in hydroponics. Nitrogenase activity of Azospirillum sp., in pure culture was more rapidly inhibited by the addition of NH₄ ⁺ than NO₃ ^?. The N₂ fixation of P. agglomerans decreased only by NH₄ ⁺ -addition, but was stimulated by NO₃ ^?. Nitrogen fixation in association with wheat plants remained unaffected by both N compounds. However, nitrogen derived from the atmosphere (N_dfa) contributed only very little to the overall nitrogen nutrition of the plants.     

Estimation of Urea Production Rate With [15N2]Urea and [13C]Urea to Measure Catabolic Rates in Diabetes Mellitus

Abstract

For verifying catabolic states in insulin-dependent patients and dogs the method estimating urea production rates with ¹³C and with doubly ¹⁵N labeled urea, respectively, has been established. For a fast steady state of urea tracer dilution, a prime of 600 times the continuous infusion rate had to be injected. Urea was isolated from plasma samples by protein precipitation and cation exchange chromatography with a consecutive derivatization of the dried urea fraction (trimethylsilyl derivatives). The masses of the fragment ions m/z 189 (¹⁴N¹⁴N), 190 (¹⁴N¹⁵N) and 191 (¹⁵N¹⁵N) urea are monitored to estimate the [¹⁵N₂]urea frequency in the overall body urea pool in mol percent excess (MPE). 1 to 15 ng of derivatized urea were measured efficiently. An excellent correlation between expected standard and measured MPE (r = 0.9977) was achieved from solutions containing 1 to 7% [¹⁵N₂]urea. The interassay coefficient of variation amounted to < 10% for a [¹⁵N₂]urea portion of ≥ 3%.

Normoglycemic diabetic patients who were treated with insulin overnight showed significantly higher urea production compared to healthy controls (9.22 ± 2.07 vs. 5.4 ± 0.32 μmol·kg^?1 · min^?1; p < 0.05). Measurements in chronic diabetic dogs proved an increased rate of amino acid catabolism (+ 20% urea production) in systemic versus portal application of insulin in paired studies. This increased nitrogen load in diabetics may accelerate progression of diabetic nephropathy. - Thus, the established stable isotope technique may serve as a sensitive and useful indicator of amino acid catabolism in clinical and experimental research.     

Release of nitrous oxide and dinitrogen from a transition bog under drained and rewetted conditions due to denitrification: results from a [15N]nitrate–bromide double-tracer study

Denitrification is well known being the most important nitrate-consuming process in water-logged peat soils, whereby the intermediate compound nitrous oxide (N₂O) and the end product dinitrogen (N₂) are ultimately released. The present study was aimed at evaluating the release of these gases (due to denitrification) from a nutrient-poor transition bog ecosystem under drained and three differently rewetted conditions at the field scale using a ¹⁵N-tracer approach ([¹⁵N]nitrate application, 30?kg N ha^?1) and a common closed-chamber technique. The drained site is characterized by a constant water table (WT) of –30?cm (here referred to as D30), while rewetted sites represent a constant WT of –15?cm, a constant WT of 0?cm (i.e. waterlogged), and an initial WT of 0?cm (which decreased slightly during the experiment), respectively, (here referred to as R15, R0, and R0_d, respectively). The highest N₂O emissions were observed at D30 (291?µg N₂O–N m^?2 h^?1) as well as at R0_d (665?µg N₂O–N m^?2 h^?1). At the rewetted peat sites with a constant WT (i.e. R15 and R0), considerably lower N₂O emissions were observed (maximal 37?µg N₂O–N m^?2 h^?1). Concerning N₂ only at the initially water-logged peat site R0_d considerable release rates (up to 3110?µg N₂–N m^?2 h^?1) were observed, while under drained conditions (D30) no N₂ emission and under rewetted conditions with a constant WT (R15 and R0) significantly lower N₂ release rates (maximal 668?µg N₂–N m^–2 h^?1) could be detected. In addition, it has been found that natural WT fluctuations at rewetted peat sites, in particular a rapid drop down of the WT, can induce high emission rates for both N₂O and N₂.     

Tree species of the central amazon and soil moisture alter stable isotope composition of nitrogen and oxygen in nitrous oxide evolved from soil

The use of stable isotopes of N and O in N₂O has been proposed as a way to better constrain the global budget of atmospheric N₂O and to better understand the relative contributions of the main microbial processes (nitrification and denitrification) responsible for N₂O formation in soil. This study compared the isotopic composition of N₂O emitted from soils under different tree species in the Brazilian Amazon. We also compared the effect of tree species with that of soil moisture, as we expected the latter to be the main factor regulating the proportion of nitrifier- and denitrifier-derived N₂O and, consequently, isotopic signatures of N₂O. Tree species significantly affected δ ¹⁵N in nitrous oxide. However, there was no evidence that the observed variation in δ ¹⁵N in N₂O was determined by varying proportions of nitrifier- vs. denitrifier-derived N₂O. We submit that the large variation in δ ¹⁵N-N₂O is the result of competition between denitrifying and immobilizing microorganisms for NO 3 m . In addition to altering δ ¹⁵N-N₂O, tree species affected net rates of N₂O emission from soil in laboratory incubations. These results suggest that tree species contribute to the large isotopic variation in N₂O observed in a range tropical forest soils. We found that soil water affects both ¹⁵N and ¹⁸O in N₂O, with wetter soils leading to more depleted N₂O in both ¹⁵N and ¹⁸O. This is likely caused by a shift in biological processes for ¹⁵N and possible direct exchange of ¹⁸O between H₂O and N₂O.     

Analysis of the coexisting pathways for NO and N2O formation in Chernozem using the 15N-tracer SimKIM-Advanced model

The nitrogen (N) cycle consists of a variety of microbial processes. These processes often occur simultaneously in soils, but respond differently to local environmental conditions due to process-specific biochemical restrictions (e.g. oxygen levels). Hence, soil nitrogen cycling (e.g. soil N gas production through nitrification and denitrification) is individually affected through these processes, resulting in the complex and highly dynamic behaviour of total soil N turnover. The development and application of methods that facilitate the quantification of individual contributions of coexisting processes is a fundamental prerequisite for (i) understanding the dynamics of soil N turnover and (ii) implementing these processes in ecosystem models. To explain the unexpected results of the triplet tracer experiment (TTE) of Russow et al. (Role of nitrite and nitric oxide in the processes of nitrification and denitrification in soil: results from ¹⁵N tracer experiments. Soil Biol Biochem. 2009;41:785–795) the existing SimKIM model was extended to the SimKIM-Advanced model through the addition of three separate nitrite subpools associated with ammonia oxidation, oxidation of organic nitrogen (N_org), and denitrification, respectively. For the TTE, individual treatments with ¹⁵N ammonium, ¹⁵N nitrate, and ¹⁵N nitrite were conducted under oxic, hypoxic, and anoxic conditions, respectively, to clarify the role of nitric oxide as a denitrification intermediate during N₂O formation. Using a split nitrite pool, this analysis model explains the observed differences in the ¹⁵N enrichments in nitric oxide (NO) and nitrous oxide (N₂O) which occurred in dependence on different oxygen concentrations. The change from oxic over hypoxic to anoxic conditions only marginally increased the NO and N₂O release rates (1.3-fold). The analysis using the model revealed that, under oxic and hypoxic conditions, N_org-based N₂O production was the dominant pathway, contributing to 90 and 50 % of the total soil N₂O release. Under anoxic conditions, denitrification was the dominant process for soil N₂O release. The relative contribution of N_org to the total soil NO release was small. Ammonia oxidation served as the major pathway of soil NO release under oxic and hypoxic conditions, while denitrification was dominant under anoxic conditions. The model parameters for soil with moderate soil organic matter (SOM) content were not scalable to an additional data set for soil with higher SOM content, indicating a strong influence of SOM content on microbial N turnover. Thus, parameter estimation had to be re-calculated for these conditions, highlighting the necessity of individual soil-dependent parameter estimations.     

Elemental Analyzer-Quadrupole MS Coupling—A Low Cost Equipment for the Simultaneous Determination of Carbon/13C and Nitrogen/15N in Isotopically Enriched Soil and Plant Samples

Abstract

Since the end of the 80s elemental analyzer-isotope ratio mass spectrometer connections have been used for the fast, automatic and highly precise determination of carbon and nitrogen content as well as their isotopic composition in one run. But for artificially enriched stable isotopes as tracer in biological processes and since these processes have a high biological variability anyway (e.g. soil processes) the use of these highly precise but also sophisticated and expensive instruments is not required. In this case the use of a quadrupole mass spectrometer connected with an elemental analyzer can offer a low cost alternative. As shown, such coupling is suitable for automatic simultaneous routine analysis of total nitrogen and carbon and their isotopic enrichment (¹⁵N, ¹³C) in plant material and soils. The relative standard deviation for ¹⁵N and ¹³C determination is 2% To meet this precision a careful sample homogenization by grinding is very important. The duration of one measurement is 6–8 min. depending on whether nitrogen alone or both nitrogen and carbon are determined. This enables a high sample throughput.     

15N natural abundance of non-fixing woody species in the Brazilian dry forest (caatinga)

Foliar δ¹⁵N values are useful to calculate N₂ fixation and N losses from ecosystems. However, a definite pattern among vegetation types is not recognised and few data are available for semi-arid areas. We sampled four sites in the Brazilian caatinga, along a water availability gradient. Sites with lower annual rainfall (700 mm) but more uniform distribution (six months) had δ¹⁵N values of 9.4 and 10.1 ‰, among the highest already reported, and significantly greater than those (6.5 and 6.3 ‰) of sites with higher rainfall (800 mm) but less uniform distribution (three months). There were no significant differences at each site among species or between non-fixing legume and non-legume species, in spite of the higher N content of the first group. Therefore, they constitute ideal reference plants in estimations of legume N₂ fixation. The higher values could result from higher losses of ¹⁵N depleted gases or lower losses of enriched ¹⁵N material.     

Infrared spectroscopy of closed s-shell gas-phase M+(N2O)n (M = Li,Al) ion-molecule complexes*

ABSTRACT

We present the results of a combined experimental and computational study of the structures of gas-phase M⁺(N₂O)_n (M?=?Li, Al) complexes. Infrared spectra were recorded in the region of the N₂O asymmetric (N?=?N) stretch using photodissociation spectroscopy employing the inert messenger technique. Unlike in our previous studies on M⁺(N₂O)_n (M?=?Cu, Ag, Au and M?=?Co, Rh, Ir) complexes, N– and O–bound isomers in this case are near isoenergetic and are not distinguished spectroscopically at this resolution. In the case of Li⁺ complexes, there is, however, evidence for the presence of bound N₂ moieties, indicating the presence of inserted, OLi⁺N₂(N₂O)_n–type structures. The weak N₂ band lies to the blue of the signature of molecularly N– and O–bound ligands and is well–reproduced in the simulated spectra of energetically low-lying structures computed from density functional theory. No such inserted isomers are observed in the case of Al⁺(N₂O)_n complexes whose infrared spectra can be understood on the basis of molecularly-bound N₂O ligands. The differences in M⁺(N₂O)_n structures observed for these closed–shell, ns², metal centres relative to other metal cations are discussed in terms of the likely bonding motifs.     

Structural Characterization of RF‐Sputtered a‐C:N Thin Films by Raman,IR, and X‐ray Reflectometry Spectroscopies

Abstract

Amorphous carbon nitride thin films (a‐C:N) were deposited from a carbon target, at room temperature onto silicon substrates, by reactive RF sputtering in a gas mixture of argon and nitrogen. The structural properties of these films have been studied by Raman, infrared (IR), and X‐ray reflectometry spectroscopies. Both the IR and Raman spectra of the a‐C:N films reveal the presence of C–C, C?C, C?N, and C≡N bonding types. The Raman spectra analysis shows, an increase of the C≡N triple bonds content when the concentration of nitrogen C(N₂) in the gas mixture is increased. The Raman intensities ratio between the disorder (D) and graphitic (G) bands increases with C(N₂) suggesting an increased disorder with the incorporation of nitrogen in the carbon matrix. The effect of C(N₂) on the density of a‐C:N films was also investigated by X‐ray reflectometry measurement. The increase of the nitrogen concentration C(N₂) was found to have a significant effect on the density of the films: as C(N₂) increases from 0 to 100%, the density of the a‐C:N films decreases slightly from 1.81 to 1.62 g/cm³. The low values of density of the a‐C:N films were related (i) to the absence of C–N single bonds, (ii) to the increase of disorder introduced by the incorporation of nitrogen in the carbon matrix, and (iii) to the presence of the bands around 2350 cm^?1 and 3400 cm^?1 associated with the C–O bond stretching modes and the O–H vibration, respectively, suggesting a high atmospheric contamination by oxygen and water. The presence of these bands suggests the porous character of the studied samples.     

Utilization by maize of phosphonitrilic hexamide labelled with 15N at cyclic and at amino positions

Abstract

The phosphonitrilic hexamides (PNH) [¹⁵N₆] hexamino-phosphatriazine and hexaminophospha-[¹⁵N₃] triazine were synthesized. Vegetation experiments showed that PNH has a favourable effect on the maize growth. Also the results demonstrated that the major part of PNH is mineralized during the following days. This process diminishes after 60 days. The total N-fertilizer uptake is about 46%, 29% of which came from amino-N and 17% from cyclic N, respectively. PNH behaved as a slow releasing N-fertilizer.     

GC-MS-gestützte Synthese und Qualitätskontrolle von 15N-markiertem Stickstoffmonoxid mit hoher 15N-Häufigkeit für umweltrelevante Tracer-Untersuchungen

Abstract

[¹⁵N]nitric oxide for investigations on the effect of nitric oxide in biological systems can be synthesized economically from the commercially available [¹⁵N]nitric acid. Difficulties arise, however, for the preparation of highly enriched ¹⁵N-labelled nitric oxide on a lower mmol scale. These difficulties are caused by oxygen and result in both, yield depression and insufficient long-time stability of the NO-containing gas mixture due to its oxidation to NO₂. Therefore, a sensitive in situ oxygen detection during synthesis was carried out by on line coupling of the synthesis apparatus with a GC-MS. Additionally, this equipment offers the advantage that both, conversion and ¹⁵N enrichment may be measured almost continuously and simultaneously. In this way, the yield can be increased up to 85% without increasing by-products. The gas mixture prepared from this [¹⁵N]nitric oxide showed an adequate stability for several months at a concentration of about 100 ppm(v) NO.