M.B. Esler , D.W.T. Griffith , F. Turatti , S.R. Wilson , T. Rahn , H. Zhang
{"title":"N2O浓度和通量测量和完成同位素分析的FTIR光谱","authors":"M.B. Esler , D.W.T. Griffith , F. Turatti , S.R. Wilson , T. Rahn , H. Zhang","doi":"10.1016/S1465-9972(00)00033-7","DOIUrl":null,"url":null,"abstract":"<div><p>We report the development and application of analytical techniques for atmospheric N<sub>2</sub>O based on Fourier transform infrared (FTIR) spectroscopy. Using mobile low resolution (1 cm<sup>−1</sup>) FTIR spectroscopy in the field, the technique delivers mixing ratio measurements of precision ±0.3 ppbv (0.3 nmol mol<sup>−1</sup>) N<sub>2</sub>O and in situ soil–atmosphere flux chamber measurements of fluxes less than 1 ngN m<sup>−2</sup> s<sup>−1</sup> (0.04 nmol N<sub>2</sub>O m<sup>−2</sup> s<sup>−1</sup>) with a time resolution of 30 min. The method offers the additional advantages of being simultaneously able to measure CO<sub>2</sub>, CH<sub>4</sub> and CO mixing ratios in air to high precision (±0.15 μmol mol<sup>−1</sup>, ±1 nmol mol<sup>−1</sup>, ±0.3 nmol mol<sup>−1</sup>, respectively). By a similar analysis procedure, but with laboratory-based high resolution (0.012 cm<sup>−1</sup>) FTIR spectroscopy, the N<sub>2</sub>O isotope ratios δ<sup>15</sup>N, δ<sup>18</sup>O and δ<sup>17</sup>O are determined simultaneously for a single sample, with current precision of <span><math><mtext>±1.0‰,</mtext><mspace></mspace><mtext>±2.5‰</mtext></math></span> and <span><math><mtext>±4.4‰</mtext></math></span>, respectively. FTIR also resolves the individual contributions of the <sup>15</sup>N<sup>14</sup>N<sup>16</sup>O and <sup>14</sup>N<sup>15</sup>N<sup>16</sup>O to overall δ<sup>15</sup>N. The resolution of these two isotopomers is not possible using conventional isotope ratio mass spectrometry (IRMS). We present laboratory results demonstrating precision, and N-positionally resolved δ<sup>15</sup>N and δ<sup>18</sup>O measurements of UV-photolysed N<sub>2</sub>O in which a distinct asymmetric <sup>15</sup>N positional effect is observed.</p></div>","PeriodicalId":100235,"journal":{"name":"Chemosphere - Global Change Science","volume":"2 3","pages":"Pages 445-454"},"PeriodicalIF":0.0000,"publicationDate":"2000-07-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/S1465-9972(00)00033-7","citationCount":"29","resultStr":"{\"title\":\"N2O concentration and flux measurements and complete isotopic analysis by FTIR spectroscopy\",\"authors\":\"M.B. Esler , D.W.T. Griffith , F. Turatti , S.R. Wilson , T. Rahn , H. Zhang\",\"doi\":\"10.1016/S1465-9972(00)00033-7\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>We report the development and application of analytical techniques for atmospheric N<sub>2</sub>O based on Fourier transform infrared (FTIR) spectroscopy. Using mobile low resolution (1 cm<sup>−1</sup>) FTIR spectroscopy in the field, the technique delivers mixing ratio measurements of precision ±0.3 ppbv (0.3 nmol mol<sup>−1</sup>) N<sub>2</sub>O and in situ soil–atmosphere flux chamber measurements of fluxes less than 1 ngN m<sup>−2</sup> s<sup>−1</sup> (0.04 nmol N<sub>2</sub>O m<sup>−2</sup> s<sup>−1</sup>) with a time resolution of 30 min. The method offers the additional advantages of being simultaneously able to measure CO<sub>2</sub>, CH<sub>4</sub> and CO mixing ratios in air to high precision (±0.15 μmol mol<sup>−1</sup>, ±1 nmol mol<sup>−1</sup>, ±0.3 nmol mol<sup>−1</sup>, respectively). By a similar analysis procedure, but with laboratory-based high resolution (0.012 cm<sup>−1</sup>) FTIR spectroscopy, the N<sub>2</sub>O isotope ratios δ<sup>15</sup>N, δ<sup>18</sup>O and δ<sup>17</sup>O are determined simultaneously for a single sample, with current precision of <span><math><mtext>±1.0‰,</mtext><mspace></mspace><mtext>±2.5‰</mtext></math></span> and <span><math><mtext>±4.4‰</mtext></math></span>, respectively. FTIR also resolves the individual contributions of the <sup>15</sup>N<sup>14</sup>N<sup>16</sup>O and <sup>14</sup>N<sup>15</sup>N<sup>16</sup>O to overall δ<sup>15</sup>N. The resolution of these two isotopomers is not possible using conventional isotope ratio mass spectrometry (IRMS). We present laboratory results demonstrating precision, and N-positionally resolved δ<sup>15</sup>N and δ<sup>18</sup>O measurements of UV-photolysed N<sub>2</sub>O in which a distinct asymmetric <sup>15</sup>N positional effect is observed.</p></div>\",\"PeriodicalId\":100235,\"journal\":{\"name\":\"Chemosphere - Global Change Science\",\"volume\":\"2 3\",\"pages\":\"Pages 445-454\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2000-07-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1016/S1465-9972(00)00033-7\",\"citationCount\":\"29\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Chemosphere - Global Change Science\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S1465997200000337\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Chemosphere - Global Change Science","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S1465997200000337","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
N2O concentration and flux measurements and complete isotopic analysis by FTIR spectroscopy
We report the development and application of analytical techniques for atmospheric N2O based on Fourier transform infrared (FTIR) spectroscopy. Using mobile low resolution (1 cm−1) FTIR spectroscopy in the field, the technique delivers mixing ratio measurements of precision ±0.3 ppbv (0.3 nmol mol−1) N2O and in situ soil–atmosphere flux chamber measurements of fluxes less than 1 ngN m−2 s−1 (0.04 nmol N2O m−2 s−1) with a time resolution of 30 min. The method offers the additional advantages of being simultaneously able to measure CO2, CH4 and CO mixing ratios in air to high precision (±0.15 μmol mol−1, ±1 nmol mol−1, ±0.3 nmol mol−1, respectively). By a similar analysis procedure, but with laboratory-based high resolution (0.012 cm−1) FTIR spectroscopy, the N2O isotope ratios δ15N, δ18O and δ17O are determined simultaneously for a single sample, with current precision of and , respectively. FTIR also resolves the individual contributions of the 15N14N16O and 14N15N16O to overall δ15N. The resolution of these two isotopomers is not possible using conventional isotope ratio mass spectrometry (IRMS). We present laboratory results demonstrating precision, and N-positionally resolved δ15N and δ18O measurements of UV-photolysed N2O in which a distinct asymmetric 15N positional effect is observed.