Evaluation on nitrogen isotopes analysis in high-C/N-ratio plants using elemental analyzer/isotope ratio mass spectrometry

Evaluation on nitrogen isotopes analysis in high-C/N-ratio plants using elemental analyzer/isotope ratio mass spectrometry 1 first-author 1 2 corresp Corresponding author, liuwg@loess.llqg.ac.cn Corresponding author, liuwg@loess.llqg.ac.cn liuwg@loess.llqg.ac.cn State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an710075, China State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an710075, China Xi’an Jiaotong University, Xi’an710049, China Xi’an Jiaotong University, Xi’an710049, China Elemental analyzer/isotope ratio mass spectrometry (EA/IRMS) has been widely applied to analyze the 15 N/ 14 N isotope composition ( δ 15 N) of plants and soils, but the δ 15 N results may be inaccurate due to incomplete combustion of the high-C/N-ratio plant samples by EA. Therefore, it is necessary to develop a method to solve the problem of imperfect combustion. In this study, we used two methods: 1) adding copper oxide powder to the samples, and 2) increasing the O 2 flow (from 100 mL min -1 to 200 mL min -1 ) for the auto sampler inlet purge line of the EA. The δ 15 N values of the plant samples became more positive and tended to be stable after complete combustion. Also, the required blank samples for each plant sample decreased with increasing amount of the added CuO powder. However, at 200 mL min -1 of the oxygen flow in the EA, complete combustion could not be achieved without adding copper oxide, but this was done with decreased amount of CuO powder. Therefore, mixing cupric oxide into the high-C/N-ratio samples was an efficient, simple and convenient way to solve the problem of imperfect combustion in the EA. Nitrogen isotopes Cupric oxide O 2 flow of EA/IRMS High-C/N-ratio plants EA/IRMS I. INTRODUCTION 1 Continuous-flow elemental analyzer/isotope ratio mass spectrometry (EA/IRMS), which analyzes nitrogen isotopes in plant and soil samples [ 1 1 - 6 6 1-6 ], has been extensively used to study the global nitrogen cycle [ 7 7 - 11 11 7-11 ]. The EA analysis is based on flash combustion. The nitrogen content in a sample is converted to N 2 and NO x in the oxidation furnace by instantaneous and complete oxidation of the sample [ 12 12 ]. However, Wang et al. [ 13 13 ] found that natural plant samples with high C/N ratios could not be combusted completely, resulting in nitrogen isotopic compositions being less than expected. Therefore, methods should be developed to ensure complete combustion of the plant samples. In order to make sure enough N ( ≥ 100 μg) is introduced into the mass spectrometer, larger sample amounts are required for the nitrogen isotopic analysis of the high-C/N-ratio plants, but the samples are tightly loaded in Ag (or Sn) foil capsules to avoid air contamination. The plant powder in the packet core may not contact with oxygen, hence the incomplete oxidation and nitrogen isotope fractionation [ 14 14 ]. Vanadium pentoxide (V 2 O 5 ) has been added to samples to enhance combustion in sulfur stable isotope measurements by EA/IRMS [ 15 15 - 17 17 15-17 ]. This method, however, was ineffective for measuring high C/N ratios samples, because the background intensity of the m/z 28 ion even increased with the V 2 O 5 content, and the plant-V 2 O 5 mixture could not be reacted completely [ 13 13 ]. In this paper, copper oxide powder is used as a combustion-supporting reagent, aimed at finding a simple and effective way to obtain accurate isotope results for analyzing plant samples of high-C/N-ratio by EA/IRMS. II. EXPERIMENTAL 1 A. Materials 2 Copper oxide was ground into powder in particle size of <110 μg after 650 ℃ sintering for two hours. The high-C/N-ratio plant samples, i.e. Plant 1 (P1) and Plant 2 (P2), were collected from Xinjiang, China. The plant samples were soaked in deionized water for 24 hours (the deionized water was renewed every 8 hours) to remove salt in the sample surface. They were dried at 40 ℃ in an oven for 48 hours. The dried samples were ground into powder of < 74 μm in particle size. The carbon and nitrogen contents, and the C/N ratio, were determined using an elemental analyzer. The carbon content was 44.14% for the P1 samples, and 44.77% for the P2 samples, while the nitrogen content was 1.37% for P1 and 0.75% for P2. So, the C/N ratios were 32.22 and 59.69 for P1 and P2, respectively. The plant sample powders were weighed out on a fresh sheet of paper. The CuO powder was mixed with the sample powder at various mass ratios. The prepared samples were loaded into Ag and Sn capsules (5 mm×9 mm), which were tightly crimped to avoid any trapping of air that would perturb the combustion. B. Sample analysis using EA/Conflo III/IRMS 2 Determination of 15 N/ 14 N isotope ratios was performed with a FLASH 1112 Elemental Analyzer (CE Instruments, Rodano, Italy) equipped with an AS200 auto sampler interfaced to a Delta PLUS isotope ratio mass spectrometer (ThermoQuest Finnigan, Bremen, Germany) via a Conflo III interface (ThermoQuest Finnigan, Germany). The elemental analyzer was composed of an oxidation furnace filled with chromium (III) oxide and silvered cobalt oxide for combustion and a reduction furnace filled with copper to reduce the nitric oxide compounds. A CO 2 adsorption trap, employed to avoid the interference of CO 2 , and a water trap to protect the GC column from humidity, were connected between the reduction reactor and the GC column. The mixed gas that flowed from the furnace was separated via the chromatographic column. The following EA conditions were used: temperatures of oxidation reactor, 1000 ℃, temperatures of reduction reactor 650 ℃, and GC column temperature 40 ℃ [ 18 18 ]. High-purity helium was used as a carrier gas at a flow rate of 85 mL min -1 . All 15 N/ 14 N isotope ratios were expressed in the conventional δ notation in per mil versus air, defined as δ 15 N()(air) = [( 15 N/ 14 N sample / 15 N/ 14 N standard )-1]× 1000. A tank of high-purity nitrogen with known δ 15 N value was used as the working reference gas. The δ 15 N standards of IAEA-NO 3 and a soil standard SN-2 were measured on a daily basis to monitor the analytical accuracy. The standard deviation for duplicate analyses was less than 0.3. C. Improvement of the oxidizing condition 2 In order to supply enough oxygen for high-C/N-ratio plant samples to be completely converted by the flash combustion in the EA, two methods were tried. The first method was to add CuO to the samples. The second method was a direct increase in the oxygen injection of the EA from 100 mL min -1 to 200 mL min -1 . Because excess O 2 would shorten lifetime of the reduction reactor [ 19 19 ], we did not continue to increase the oxygen flow. III. RESULTS AND DISCUSSION 1 A. Checks on the CuO and capsules 2 In order to determine whether the copper oxide would induce contamination, we monitored the blank of CuO reagent. Different amounts of CuO powder were used to determined N signal intensities of the blank. Also, CuO powder was mixed into the SN-2 standard and the δ 15 N data were compared with that of the SN-2 ( Table 1 Table 1 ). The results showed that the N intensity of the CuO blank was zero and the δ 15 N results of SN-2 were not affected by the added CuO. In addition, CuO and the CuO/SN-2 mixture were loaded in the Ag and Sn capsules, indicating that the Ag and Sn capsules contributed no N contamination. a No.1–4, CuO in Sn or Ag capsules; No.5–8, CuO/SN-2 mixture in Sn or Ag capsules; No.9, SN-2 standard. 1 1 Sample No. a a 1 1 Capsule type 1 1 CuO added (mg) 1 1 Ion intensity of m/z 29 (mV) 1 1 δ 15 N (% vs. air) 1 1 1 1 1 Sn 1 1 35.2 1 1 0 1 1 – 1 1 2 1 1 Sn 1 1 34.5 1 1 0 1 1 – 1 1 3 1 1 Ag 1 1 33.0 1 1 0 1 1 – 1 1 4 1 1 Ag 1 1 89.6 1 1 0 1 1 – 1 1 5 1 1 Ag 1 1 80 1 1 2476 1 1 5.43 1 1 6 1 1 Ag 1 1 80 1 1 2309 1 1 5.29 1 1 7 1 1 Sn 1 1 80 1 1 2502 1 1 5.38 1 1 8 1 1 Sn 1 1 80 1 1 2567 1 1 5.44 1 1 9 1 1 Sn 1 1 0 1 1 – 1 1 5.33±0.043( n =9) In order to examine whether Ag capsules will prevent the sample from being completely combusted, the δ 15 N values for samples wrapped in Ag capsules and Sn capsules were compared. As the results shown in Table 2 Table 2 , there was no difference between the plant samples that were loaded into Ag capsules and those in Sn capsules. a Replicate analysis in a single day. b Replicate analysis in different days. 1 1 Sample name 1 1 δ 15 N (‰ vs. air) by Ag capsules 1 1 δ 15 N (‰ vs. air) by Sn capsules 1 1 P1/CuO = 1/5 1 1 11.81 1 1 11.69 ±0.081 ( n =2) a a 1 1 P2 1 1 8.00±0.090 ( n =6) b b 1 1 8.03 1 1 P2/CuO = 1/3 1 1 8.62 1 1 8.58±0.108 ( n =3) a a 1 1 P2/CuO = 1/5 1 1 8.77 1 1 8.46±0.016 ( n =2) 1 1 SN-2/CuO = 1/4 1 1 5.36±0.099 ( n =2) a a 1 1 5.41±0.046( n =2) a a 1 1 P1/CuO = 1/1 1 1 – 1 1 11.80±0.035( n =3) a a 1 1 P2/CuO = 1/1 1 1 – 1 1 8.45±0.058( n =3) a a 3.2 The precision of EA-IRMS δ 15 N analysis 2 The precision of the EA/IRMS system must be guaranteed to study δ 15 N values, so replicate analyses, in which the plant samples mixed with different amounts of CuO were analyzed, were performed in a single day or in several days. And the results are of high precision ( Table 2 Table 2 ), with the standard deviation being less than 0.2. C. δ 15 N linearity range of the IRMS system 2 The ion intensity of N 2 of the plant samples increases with the degree of combustion completeness of the plant samples. It is essential that the range in which the ion intensity changed was within the δ 15 N linearity range of IRMS system. The δ 15 N linearity range of IRMS system was tested by investigating the relationship between the ion intensity and the δ 15 N values [ 20 20 ]. First, the pressure controller of reference gas N 2 of the Finnigan Conflo III interface was adjusted. Eleven pulses of various amounts of N 2 were measured to achieve a diverse range of ion intensity without any change in the EA conditions. The measured δ 15 N values did not change in the ion intensity range of 500–6600 mV ( Fig. 1(a) Fig. 1(a) ). Next, different amounts of the SN-2 standard were loaded in Sn or Ag cups to examine the linearity of the EA/IRMS system. In the N 2 ion intensity range of 750–4300 mV, the measured δ 15 N value showed a linear correlation with the ion intensity. In the range of 1500–4000 mV, the δ 15 N value did not vary significant ( Fig. 1(b) Fig. 1(b) ). These results demonstrated that the increase in the δ 15 N values as a function of increasing size of plant samples was not caused by any non-linearity offset of the mass spectrometer. D. The δ 15 N values by add CuO and O increase 2 It is well known that isotope fractionation will occur if the sample is not fully oxidized using EA/IRMS [ 14 14 , 17 17 ]. The 14 N isotope can participate in the reaction more easily than 15 N, hence more negative results of δ 15 N when the samples were only partially converted. In this study, the nitrogen isotopes of the two high-C/N-ratio plant samples had a similar trend in the ion intensity at m/z 29. When the oxygen loop in the EA was set to 100 mL min -1 or 200 mL min -1 , the nitrogen isotopes of the two samples were more negative without CuO powder, indicating non-complete combustion of the samples. By adding CuO powder into the samples as shown in Fig. 2 Fig. 2 , the isotopic compositions at 100 mL min -1 increased until the ratio of CuO/plant of 5/1 for for P1 and 3/1 for P2. However, at 200 mL min -1 of the O 2 flow, the isotope results tented to be stable when the mass ratio of CuO/plant was over 3/1 for P1 and 1/1 for P2. And the nitrogen isotopes for P1 and P2 showed the same trend of variation under different experimental conditions. As mentioned above, the stable behavior means complete combustion of the plant samples, and this can be realized by adding CuO powder or increasing in the O 2 flow in the EA. E. Blank samples after each sample analysis 2 To verify complete combustion of the plant samples, blank samples were measured after analysis of each plant sample, until no appearance of the nitrogen peak. As shown in Fig. 3(a) Fig. 3(a) , the ion intensity of the first blank sample was 35–60 mV at the O 2 flow of both 100 and 200 mL min -1 . It was obvious that the nitrogen in the two plant samples was not converted completely. However, at the O 2 flow of 100 mL min -1 , four or five blank samples were required to eliminate the m/z 29 peak without adding CuO ( Fig. 3(a) Fig. 3(a) ), while this was achieved by using just two blank samples at 200 mL min -1 . Then, to some extent, increasing the O 2 flow to 200 mL min -1 promotes the sample combustion. But complete conversion of the plant samples cannot be achieved by just increasing the O 2 flow. As shown in Figs. 3(b) and 3(c) Figs. 3(b) and 3(c) , the number of blank samples decreased with increasing amount of added CuO. In the 100-mL min -1 scenario, the number of blank samples required was reduced from three to two when the mass ratio of copper oxide/plant samples increased from 1/1 to 3/1. With a 200-mL min -1 flow, the high-C/N-ratio plant samples were combusted completely when the mass ratio of copper oxide/plant samples was greater than 1/1. This indicates that copper oxide was an efficient reagent to promote combustion for N isotope analysis of the high-C/N-ratio samples using EA. IV. CONCLUSION 1 Adding copper oxide powder to the high-C/N-ratio plant samples ensures complete oxidation of the nitrogen contents in the samples by flash combustion in the EA/IRMS, so that the nitrogen isotope values of the plant samples can be accurately determined. While increasing the oxygen flow in the EA improves the nitrogen oxidation of the high-C/N-ratio plant samples, complete combustion cannot be achieved by just increasing the oxygen flow. 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