There are two officially approved methods for stable isotope analysis for wine authentication. One describes δ18O measurements of the wine water using Isotope Ratio Mass Spectrometry (IRMS), and the other one uses Deuterium-Nuclear Magnetic Resonance (2H-NMR) to measure the deuterium of the wine ethanol. Recently, off-axis integrated cavity output (laser) spectroscopy (OA-ICOS) has become an easier alternative to quantify wine water isotopes, thanks to the spectral contaminant identifier (SCI). We utilized an OA-ICOS analyser with SCI to measure the δ18O and δ2H of water in 27 wine samples without any pre-treatment. The OA-ICOS results reveal a wealth of information about the growth conditions of the wines, which shows the advantages to extend the official δ18O wine water method by δ2H that is obtained easily from OA-ICOS. We also performed high-temperature pyrolysis and chromium reduction combined with IRMS measurements to illustrate the “whole wine” isotope ratios. The δ18O results of OA-ICOS and IRMS show non-significant differences, but the δ2H results of both methods differ much more. As the δ2H difference between these two methods is mainly caused by ethanol, we investigated the possibility to deduce deuterium of wine ethanol from this difference. The results present large uncertainties and deviate from the obtained 2H-NMR results. The deviation is caused by the other constituents in the wine, and the uncertainty is due to the limited precision of the SCI-based correction, which need to improve to obtain the 2H values of ethanol as alternative for the 2H-NMR method.
Wine authenticity control is vital to protect consumers and for the proper functioning of the world market with regard to the increasing and globalized wine consumption. Because of more and more complicated and sophisticated adulteration activities during the wine-making process, stable isotope analysis has been established as a powerful method to determine such fraudulent activities. The isotopic abundance patterns, specifically those for 2H, 18O and 13C in the water and ethanol of wine, are controlled by varying degrees of isotope fractionation during grape growing and the wine-making process and are thus characteristic for authentic wine. Therefore, these stable isotope patterns can characterize the grape variety, the fermentation method and the climatic conditions related to the geographical origin and the year of vintage [1,2,3,4]. Adulteration processes, such as watering, adding sugar during the fermentation process (chaptalisation), or adding extraneous ethanol, all disturb these natural isotopic abundance patterns in one way or another. Therefore, such adulteration activities can be detected by specific isotope abundance measurements on wine components.
So far, to our knowledge, there are only two officially approved methods that use the 2H and 18O isotopes: the 18O relative abundance measurements (usually expressed as δ18O, see below) of the wine water using Isotope Ratio Mass Spectrometry (IRMS) (OIV-MA-AS2-12) and (site-specific) 2H relative abundance measurements (usually expressed as the mole ratio of 2H to 1H) of the wine ethanol using Deuterium-Nuclear Magnetic Resonance (2H-NMR) (OIV-MA-AS311-05) [5, 6]. However, the involvement of exclusive and expensive 2H-NMR equipment makes the latter method not widely applicable, and it requires strict pre-processing steps, by which wine ethanol needs to be distilled free of fractionation effects. Nevertheless, the 2H-NMR analysis of wine ethanol is the official method to detect the chaptalization of wines. The δ18O measurements of wine water by IRMS are, although also time-consuming and complex, routine in a number of laboratories, as it is the official way to prove water addition on one side, and provide information about geographic origin and year of vintage of authentic wines on the other [7, 8]. In that respect, it is worth taking note that the δ2H measurements of the wine water are not officially used, although the combination of δ2H and δ18O is more powerful in both fraud detection and characterisation of authentic wines. It must be a heritage of the past when the δ2H measurements of water were difficult and costly. With the development of infrared optical spectroscopy measurement systems for isotope ratios, δ2H of the wine water is now as easily accessible as δ18O.
The optical spectroscopy development made it generally possible to measure stable isotope ratios in water faster and using fewer consumables, but with equivalent precision and accuracy compared with IRMS [9,10,11]. Off-axis Integrated Cavity Output Spectroscopy (OA-ICOS) is one of the commercial analysers (Los Gatos Research) which has already been applied widely in studies of stable isotopes in water from hydrology and biology [12,13,14]. The OA-ICOS analyser can also be used to analyse water isotopes in organic-contaminated samples, like beverages, plant water and body fluids, thanks to the development of a spectral contaminant identifier (SCI), which is deduced from the line shapes of the absorption spectrum [15, 16]. This SCI can be used to effectively correct the measured δ18O and δ2H for some organic influences.
In our study, we have used OA-ICOS (with SCI), Pyrolysis-IRMS and chromium reduction-IRMS for analysing δ18O and δ2H in 27 European wine samples. In addition, we present Pyrolysis-IRMS analyses of close to 100 wine samples from an earlier stage of our work. Finally, we submitted the 27 wine samples to another laboratory (Isolab GmbH) for SNIF-NMR analysis of the ethanol. We report on our attempts to answer the following research questions:
Can we perform measurements on whole wine samples using the OA-ICOS with SCI, and get reliable and accurate values for both δ18O and δ2H of the wine water without preparation? Some work on this subject has been published before , and we want to continue and expand on that.
Can pyrolysis—IRMS analysis of whole wine samples produce reliable values for the δ18O of the wine water? In other words, is the influence of the oxygen in ethanol and other constituents either negligible or leading to a constant offset?
A substantial part of the δ2H pyrolysis—IRMS analysis signal of whole wine samples is due to the hydrogen in the ethanol. Is it possible to extract reliable information about the δ2H of the ethanol from the combination of the OA-ICOS δ2H water analysis and IRMS whole wine measurement?
In case the answer to the previous question is positive, might we then be able to avoid the use of NMR for most cases, or at least select only those suspected wine samples that need the NMR analysis?
Materials and methods
Wine sample collection and preparation
27 bottles of wine were bought in a local supermarket, detailed information is listed in Table 1. Apart from their colour, they can also be divided into dry, semi-dry and sweet, based on their sugar content. Each wine sample was split into 3:500 ml for shipping to the 2H-NMR ethanol isotope measurement lab (Isolab GmbH, Germany), 30 ml for the OA-ICOS analyser water measurement, and 30 ml for the whole wine samples IRMS analysis. The headspace of the bottles was as small as practically possible, and the bottles were all kept sealed in a refrigerator at 4 °C.
In an attempt to remove the various constituents of the wine (except water and ethanol), a fraction of each wine sample was treated with activated charcoal, to study if such removal would influence the IRMS and OA-ICOS measurements. To that end, 2 ml of wine was poured into a glass tube, and then about 50 mg activated charcoal was added into the tube and agitated for 30 s; afterwards, the tube was centrifuged for 2 min, and the top 1 ml of the sample was transferred to a 2 ml sample vial. In comparison, about 1.2 ml original wine sample without activated charcoal treatment was directly transferred into a 2 ml samples vial.
IRMS measurements method 1: chromium reduction for δ2H measurement (labelled in results as “PyrOH”)
0.4 µl wine samples, from vials with a septum containing 1.2 ml, were directly injected using an auto-injector system (CTC Pal, CTC Analytics, Switzerland) into an automatic on-line sample preparation system (PyrOH, Eurovector, Milan, Italy). The injected wine was, in a He flow, reduced to H2 gas in a hot chromium reactor (1030 °C), and 2H/1H ratio of this gas was then measured by a continuous flow IRMS instrument (Isoprime, Manchester, UK).
The relative isotopic abundances are expressed in the common δ notation relative to the VSMOW-SLAP scale .
These δ values are usually small numbers, and they are commonly expressed in ‰ (per mil). For the oxygen isotopes, δ18O is expressed in an analogous way. The ratios in Eq. (1) are the actually measured ratios for the sample, and for V-SMOW and SLAP, whereas the δ2HSLAP value is defined to be − 428.0 ‰ (and δ18OSLAP is − 55.5 ‰). In practice, V-SMOW and SLAP are not used themselves, but they are represented by a series of well-calibrated local reference waters (see below).
The hydrogen content of both water, ethanol and other constituents are reduced to hydrogen gas in their reaction with chromium. The influence of especially the ethanol-hydrogen is substantial. Wine contains typically 10–14% ethanol, and the hydrogen mass percentage of ethanol is 13%, slightly higher than the 11% of water. In other words, ethanol contributes a considerable fraction of H in the whole sample. As the δ2H of the ethanol-derived H is different from that of the H2O, the measured δ2H of the wine will deviate significantly from that of the wine water. Moreover, some other substances in wine, like acids, sugars, and glycerol also have a detectable impact on the final δ2H to varying degrees.
Calibration of all isotope measurements was done using four local reference waters (which are periodically calibrated/checked using V-SMOW(2) and SLAP(2)) and the international reference water IAEA-USGS45. A series consists of these reference waters (measured in the beginning and end) and wine samples or water–ethanol mixtures (in the middle). Each sample or reference was injected six times from the same vial. The measurement sequence contained pairs of the same wine sample with and without the activated charcoal treatment. In this way, the effect of the charcoal treatment could be tested the best. The raw δ2H values from the PyrOH were corrected for memory effects using an algorithm described by Guidotti et al.. In case the reference waters showed significant drift, this drift was corrected for using an appropriate time/sample sequence dependence (either linear or LOESS-like). The uncertainty (1-sigma standard deviation) of the final calibrated δ2H values (for the average of 6 injections) was lower than 1 ‰.
IRMS measurements method 2: high-temperature pyrolysis for δ2H and δ18O measurements (labelled in results as “TC/EA”)
0.1or 0.15 µl wine samples, in vials with a septum containing 1.2 ml, were injected (using the same auto-injector system as for the PyrOH) and carried by a He flow into a high-temperature conversion analyser (Thermo, Bremen, Germany) coupled to the same continuous flow IRMS instrument as the PyrOH. The injected wine was pyrolyzed to H2 and CO gas in the presence of glassy carbon at 1400 °C. The formed gases were separated in time using a stainless steel GC column packed with Porapark Q (80/100 mesh), and subsequently first the δ2H of H2 and then δ18O of CO gas were measured by the IRMS.
Ethanol and other substances in wine will affect both the final δ2H and δ18O in a similar manner as described above. The mass percentage of oxygen in ethanol is 35%, much lower than in water (89%). Therefore, the effect of ethanol on the final δ18O is much smaller than for δ2H, the more so since the δ18O values for wine water and wine ethanol are closer than those for δ2H. The influence of other substances to the final δ18O can likely be ignored. This is because the mass percentage of oxygen in the other substances is lower than that of water, and the concentration of other substances in wine is lower than 2%. The measurement sequences were the same as for the PyrOH analysis. Also, the correction for memory effects and drift for the TC/EA results were done using the same methods as for the PyrOH.
To test the ethanol influence on the measured δ2H and δ18O, two series of mixtures were prepared and analyzed by IRMS (method 1 and method 2). These two series were made from various natural reference waters with the same ethanol volumetric fraction (12%) added, and a single reference water with different ethanol fractions (3–19%). The measured results can then be compared to the expected ones based on the masses, the δ-values of the waters and the pure ethanol. This comparison shows whether the reduction or pyrolysis of both the water and the ethanol is complete.
2H/1H ratios of wine ethanol were measured by Site-Specific Natural Isotope Fractionation–Nuclear Magnetic Resonance (SNIF–NMR) of deuterium . The wine samples were sent to Isolab GmbH, and isotopic analyses were conducted using the official method (OIV-MA-AS311-05). (2H/H)I and (2H/H)II separately represent abundances of methyl and methylene sites of ethanol, respectively. The measurement results of (2H/H)I and (2H/H)II are expressed in ppm, calibrated in the end using the 2H abundance of V-SMOW, which is 155.7 ppm , and the analysis error of (2H/H)I and (2H/H)II are 0.3 ppm and 0.5 ppm, respectively. Conversion of these abundances to δ2H values goes according to:
where 2Fsample and 2FV-SMOW are the 2H abundances of samples and V-SMOW.
Off-axis Integrated Cavity Output Spectroscopy measurement (labelled in results as “OA-ICOS”)
δ2H and δ18O of wine samples and prepared water–ethanol mixtures were also measured by a commercial OA-ICOS Liquid Water Isotope Analyzer (LWIA, ABB-Los Gatos Research, San Jose, CA, USA). The fluid samples (size 1 µl) were introduced into the OA-ICOS instrument through an auto-injector (also a CTC Pal) into a heated injector block where the volatile fraction of the sample evaporated. This vapor expands into a high-finesse optical cavity, and δ2H and δ18O were calculated from fits to the relative transmission spectrum. Each reference or sample was injected nine times. Four to five local reference waters were measured several times each, interleaved with samples during the measurement series, and their values were used for calibration and for instrumental drift correction. Interleaving of reference waters and samples had the additional advantage of avoiding blocking the syringe by effectively rinsing wine solutes from the syringe on a regular basis.
Raw data from the instrument were analyzed using a bespoke data analysis program (programmed in R), through which memory effects and drifts were corrected, and calibration was performed. Memory effects are unavoidable in water isotope analysis, both in IRMS and laser spectroscopy, and they result from adsorption of water onto the internal surfaces of the instrument and residuals of previous water in the syringe. The standard scheme by the manufacturer addresses the memory effect by injecting samples many times and discarding the first few injections. In our data analysis program, we implemented the same algorithm as used with the IRMS measurement analysis, which actively determines and corrects for the memory effect (using a model with pools of residual water with different sizes and exchange times ), so it does not ignore the first few injections but instead uses this information to perform a reliable and accurate memory correction. Drift correction is performed using a LOESS fit to the relative deviation of the included reference waters from their average value in the series. Finally, a “two-point” calibration is carried out based on two of the local reference waters, while the other reference waters are used as quality control. The final uncertainties are based on the spread of the values for the multiple injections, with appropriate uncertainties for the memory correction, drift correction and calibration added. As wine solutes gradually accumulate in the injection block of the system, eventually blocking the syringe, it is necessary to change the septum, clean the injector block, clean the connector of the transfer tube and the syringe before every measurement series.
Wine samples contain, next to water, volatile organics, of which ethanol obviously is the most abundant one. They will also enter into the cavity and will influence the water vapour absorption spectrum, then influencing the calculated isotope ratio [15, 21]. An accurate fit to the full absorption spectrum, taking these influences into account, is virtually impossible. The approach taken by the OA-ICOS manufacturer is a quantification of the absorption influence in terms of BroadBand (BB) and NarrowBand (NB) interference. BB for wine samples is mostly caused by ethanol, whereas NB is caused by smaller molecules, mostly methanol, which is present in most wines in typically tens of ppm . Both BB and NB numbers are given in the output of the raw data of the instrument. These are then used to correct the water isotope results for these contaminants using calibration curves. To obtain these curves, we prepared two sets of mixtures: reference waters mixed with different amounts of ethanol (99.8% purity, Merck), and methanol (99.8% purity, Biosolve), and then analysed those by the OA-ICOS analyser.
Results and discussion
Influences of ethanol, methanol and organics on the OA-ICOS wine measurements
The analyser was first tested on the ethanol/methanol mixtures to obtain its calibration curves. Figure 1 shows the results: the differences (Δδ2H and Δδ18O): the measured δ2H and δ18O values minus the assigned values of the reference water used. The a and b graphs of Fig. 1 show the results for the series of water–methanol mixtures (10–165 ppm by volume). The number on the x-axis is the value for NB as given by the instrument's analysis software. It ranges up to about 44, for the highest mixing ratio of methanol (165 ppm), and this range covers all wines that we have analysed. The Δδ2H-NB and Δδ18O-NB relations are fitted with a logarithmic curve, and the residuals are all within ± 0.2 ‰ and ± 0.15 ‰ for Δδ2H and Δδ18O, respectively. The corrections can be up to 6 ‰ and 3 ‰, respectively.
The water–ethanol mixtures made contain 6–15% ethanol (volume/volume). Unfortunately, even the purest ethanol on the market contains traces of methanol, and in our product, it was about 120 ppm. This means that the methanol (NB) influence for the water–ethanol mixtures is detectable and non-negligible. In other words, the δ-value change of the water–ethanol mixtures’ measurements results from both NB and BB. Therefore, we firstly corrected the Δδ-values based on the deduced relations (Δδ-NB) shown in the top of Fig. 1, and then established the true Δδ-BB relations. Those are shown in the c and d graph of Fig. 1. Contrary to the NB case, the BB-values provided by the instrument go down with increasing ethanol mixing ratio. We used a quadratic curve fit. The residuals are up to ± 3 ‰ and ± 0.4 ‰, and the corrections can be up to 14 ‰ and 7 ‰, for Δδ2H and Δδ18O, respectively. It is clear that for wine samples, the uncertainty in the corrections is largely determined by the ethanol influence.
The relation between the BB parameter and the actual ethanol percentage shows considerably less scatter than the Δδ relation. This good relation makes it possible to determine the ethanol concentration of wine samples from it. Figure 2 shows this relation. We used a quadratic fit, and the scatter around the fit line is below ± 0.4%. We used this relation to determine our 27 wine samples ethanol percentage. The percentage difference determined using this calibration and the quoted percentage on the labels of the wine bottles is 1% or less, and the average difference is only 0.5%. According to the wine labeling regulations, it is allowed to have 1% tolerance for the labeled alcohol content , which means the BB-% calibration in our study is suitable for determining the wine ethanol percentage. We determined an ethanol percentage of 13% this way for the wine #21 (which had no indication on the label).
In each series, several other water–ethanol mixtures made from local reference water were also measured to check the correction equations. The largest difference between assigned and corrected values for these mixtures are ± 3 ‰ and ± 0.4 ‰ for Δδ2H and Δδ18O, respectively, which are similar to the largest fit residuals of the BB-Δδ fit. It implies that the total uncertainty in our OA-ICOS wine water measurements is dominated by the limitations of this fit. So while the typical raw data processing errors are only 0.8 ‰ for δ2H and 0.08 ‰ for δ18O, the total uncertainty in the wine water amounts to 3 ‰ and 0.4 ‰ for δ2H and δ18O, respectively. This is a result similar to the findings of Gupta et al.: after corrections, their difference between actual and measured values of δ18O is within 0.42 ‰ . It is an earlier publication with the same instrument, dealing exclusively with δ18O results (although they hint at the use of δ2H measurements as well).
Apart from water and alcohol, wine also contains about 1–2% other components, like acids, sugar, tannin and various other organics. Some organics, rather small portions in these substances, have the same spectroscopic influences (BroadBand and NarrowBand) as methanol and ethanol, and their influences are included in the BB and NB shown in the SCI software. The eventual spectroscopic effects of sugar, acids and other substances cannot be corrected with SCI software. Gupta et al. tried to remove these substances with activated charcoal in their work for OA-ICOS . However, they did not explain, nor demonstrate the usefulness of this pretreatment, as they did not compare samples with and without this treatment. Therefore, we decided to examine if the activated charcoal treatment has any effect (see below).
OA-ICOS wine water measurement results
The δ2H and δ18O results for the water of 27 wine samples by the OA-ICOS method are shown in Fig. 3. The error (not shown in the figure) of δ2H and δ18O are the same for all wine samples (3 ‰ and 0.4 ‰). After organic corrections, the δ2H values range from − 25.7 to 51.8 ‰, and δ18O values from − 3.7 to 11.5 ‰. The BB and NB values are down to 1.4 and up to 44, respectively, which corresponded to Δδ change of – 14 ‰, 6.1 ‰ (for δ2H) and − 7.2 ‰, 3.2 ‰ (for δ18O). Typically, the δ-value corrections for organics, so the combination of BB and NB effects, are – 8 ‰ (for δ2H) and − 5.5 ‰ (for δ18O) for these 27 wine samples.
As expected for wine samples, all points deviate from the Global Meteoric Water Line (GMWL, defined as δ2H = 8 × δ18O + 10 ‰), clearly illustrating the effect of water evaporation from the grapes. Kinetic isotope fractionation during evaporation is well-known to lead to such "evaporation lines", with δ2H/δ18O slopes between 3 and 5, mostly depending on the relative humidity of the surrounding air . Thus, during the grape growing processes, 2H and 18O in the grape water get enriched, and the extent of enrichment depends on temperature, amount of rainfall, latitude, distance from the coast, and other geographic and climatic parameters. Some regional isotope characteristics are clearly shown in Fig. 3. All the Italian and French wine samples have higher δ2H and δ18O values than German samples, especially two of the German wine samples are far less enriched than others. The only Greek wine in our batch (#19) has a much lower δ2H than expected based on its δ18O value. Further analysis, including selected points in Fig. 3, is illustrated in Fig. 5 in comparison with IRMS values. Results in Fig. 3 immediately show the added value of δ2H-analysis in addition to δ18O: watering of wine and geographic mislabelling would be discovered more easily from the δ2H-δ18O combination (two-dimensional) than from δ18O alone (one-dimensional).
Our tests of using activated charcoal for removing “impurities” indicate that the removing effect is not significant for the OA-ICOS wine water measurements. For the δ2H measurements, the difference between with and without activated charcoal is not significant. For δ18O, the treatment leads to slightly less positive δ18O values, and at the same time the BB parameter increases, which indicates some removal of organic molecules. However, this elimination effect is very limited, and the δ18O difference between with and without activated charcoal is mostly lower than the measurement error (0.4 ‰). Moreover, the correction based on the BB parameter does not get more accurate. Therefore, we conclude that activated charcoal pre-treatment is not useful, and we have not used this treatment for our OA-ICOS measurements.
Influence of ethanol on the IRMS methods
Two series of ethanol–water mixtures were produced and measured to determine if the ethanol influence on the IRMS results is according to expectations. The pure ethanol (> 99.98%) was analyzed for its isotopic composition by the TC/EA, which resulted in δ2H = -295.3 ± 0.9 ‰, δ18O = 15.7 ± 0.6 ‰. As the δ2H value of ethanol is far more negative, and the δ18O value more positive than the chosen local reference water, the δ2H and δ18O values for the mixtures will deviate considerably from that of the reference water itself. We calculated the expected δ2H and δ18O values of the mixtures based on isotope content and the masses of the ethanol and water, assuming that the reaction process is 100% effective for both the water and the ethanol.
Figure 4 illustrates the difference between the expected and measured δ-values obtained by the two different IRMS methods. The left and middle graphs in Fig. 4 show the δ2H measured-expected differences by the PyrOH and TC/EA, respectively. The error bars represent two times the standard deviations of six injections. The differences are not statistically significant. The right graph in Fig. 4 shows the δ18O differences using the TC/EA, also there are no significant differences. In conclusion, water and ethanol are both completely pyrolyzed or reduced in these IRMS systems, and the δ2H or δ18O results of a wine IRMS measurement are the combinations of water and ethanol, which can be seen as a “whole wine” sample.
As mentioned before, the influence of ethanol on the δ2H value is much larger than on δ18O, due to the mass percentage difference of hydrogen and oxygen in ethanol (13% and 35%) and in water (11% and 89%), and due to the much larger δ2H isotopic difference between the ethanol and the water (or wine). In these two series of mixtures, the maximum δ2H change due to ethanol is about – 50 ‰ (by adding 18.9% of ethanol), whereas for δ18O the change is only + 1.2 ‰. Reasoning in the opposite way, this implies that it is probably possible to derive information about the δ2H of ethanol from the combination of the "whole wine" (with IRMS) and of the wine water (with OA-ICOS) measurements, whereas for δ18O the signal is small, and extracting useful information will be difficult (see further).
Contrary to our water–ethanol mixtures, however, wine also contains other H- and O-atom carrying molecules to a varying extent. The exact contents of these "impurities", as well as their isotopic values, are unknown. That complicates the interpretation of the "whole-wine"—wine water difference. To check if activated charcoal can remove parts of this “impurity”, the comparison of the δ-values with and without activated charcoal was also conducted by measuring 27 wine samples with the IRMS methods. However, the effect of this cleaning only occurred in a few samples, mostly the δ-value changes were lower than the average measurement error. Together with the lacking effects on the wine-water measurements by OA-ICOS, the lack of effect in the IRMS whole wine measurements shows that activated charcoal cleaning is not effective.
δ2H can be acquired both from the PyrOH and TC/EA. In this work, we compared the δ2H values of 12 wine samples by utilizing these 2 methods, and the results obtained from the PyrOH and TC/EA agree within the uncertainties. As in our laboratory the PyrOH overall performs somewhat better than the TC/EA (more stable, smaller uncertainty), we used the PyrOH to measure δ2H for the “whole wine” samples in this study.
Comparison of the δ18O values measured by the OA-ICOS and IRMS
The δ18O value of wine water is key in the official test to prove watering of wine (OIV-MA-AS2-12) [1, 24], and a previous study already shows that the OA-ICOS δ18O measurements on whole-wine samples with the spectral correction are suitable to identify wine watering levels of down to 1% when authentic wine samples from the same region are available . Alternatively, the δ18O of the wine ethanol can be used as the wine's own internal reference to detect water addition to the wine [1, 25, 26]. The δ18O values of ethanol and of water in a non-adulterated wine are closely related, so their difference is a sensitive tool for the detection of water addition, without the need for reference authentic wines [25, 26].
Since IRMS measures δ18O of the “whole wine" sample (combination of water and ethanol) and OA-ICOS only measures δ18O of water, it is theoretically possible to obtain the δ18O of ethanol from the difference between these two methods. Given the tight relation between the δ18O in the ethanol and water, the relation between the OA-ICOS and IRMS results must be characterized by a rather constant difference. A calculation, using a 12% ethanol concentration, and a δ18O value for the wine ethanol that is 25 ‰ higher than that of the wine water , leads to an expected difference of 1.0 ‰. Therefore, in this study, we compared the δ18O values measured by the IRMS and OA-ICOS to see if the δ18O difference between these two methods is detectable with significance, and of a constant nature.
In Fig. 5 we compare δ18O results of the OA-ICOS and TC/EA measurement for 21 wine samples. The OA-ICOS uncertainty is the aforementioned 0.4 ‰. The uncertainty for each sample measured by the TC/EA is equal to the standard deviation of six wine injections, and the average measurement standard deviation is 0.25 ‰. Figure 5 shows the y = x + 1 line next to the 1:1 line, and it is expected that the results are near this higher line. However, most of the results are closer to the 1:1 line, and only one point (#12) is significantly off both lines. As said, the δ18O value of TC/EA is expected to be ≈ 1 ‰ higher than the value of OA-ICOS for a wine sample, and this deviation is linearly dependent on the ethanol percentage of the wine. The extra ethanol adding of wine samples #15, 16 and #19 causes different effects shown in the Fig. 5. Sample #21, a German ice wine, is also higher than the lines and also at a very low δ18O value. Interestingly, #15, 16, 19, 21 are all the wine samples with higher sugar content (see Table 1), therefore, sugar maybe also contributes to the questionable OA-ICOS values.
Wine sample #12 shows an extreme deviation for the lines. Peculiar for this wine is the high narrowband parameter of 43 (which points at a methanol concentration of ≈ 160 ppm, if it is indeed caused by methanol). This causes an δ18O correction of about 3.2 ‰ (see Fig. 1), which is far more than for any other wine sample. Nevertheless, the correction would have to be more than twice that amount to bring the point close to the lines in Fig. 5. In our experiment, most NB parameters are lower than 3, causing a correction of less than 1.4 ‰ for δ18O. We determined the NB correction line using water–methanol mixtures (10–165 ppm), up to about 44 for the NB parameter (see Fig. 1). Still, the δ18O correction for #12 is apparently inadequate, because either the substances causing the high NB parameter in #12 are not (only) methanol, or, in spite of our correction determination, the correction only works well for low NB parameter samples. This wine has the highest values for both δ18O and δ2H of all the wines in our batch. However, the position in Fig. 3 of this wine is according to expectations.
In summary, the difference between the δ18O values measured by the OA-ICOS and TC/EA-IRMS unfortunately cannot be used directly to acquire information about the δ18O of ethanol. This is partly caused by the lack of precision of the ethanol (and methanol) correction, and partly by the influence on the TC/EA IRMS results of other constituents in the wine. On the other hand, the OA-ICOS method, and to some extent even the TC/EA-IRMS method, seem well capable of measuring the δ18O values of wine water without pre-treatment. Both are easier to perform than the water-CO2 equilibration method, which is at the moment the official δ18O wine water measurement. The OA-ICOS method has the additional important benefit that in a single measurement the δ2H of the wine water is available as well (see Fig. 3, and below). Some caution is necessary for wines with high sugar content and wines that show a high NB parameter in the measurements. For these cases, the software might need "training" , or better still, the spectral fitting algorithm must be upgraded.
The δ2H and δ18O relation measured by the OA-ICOS and IRMS methods
As mentioned before, the measurement of δ2H would be an important addition to the official method for measuring δ18O of wine water. δ2H is strongly correlated with δ18O for natural 'meteoric' water, but the δ2H–δ18O relation of wine water is influenced by the fermentation process, and more importantly, by the evaporative loss of water from the grapes during growth and ripening. The combination of δ18O and δ2H therefore reveals the true climatic and geographical characteristics more comprehensively. The OA-ICOS measurements with spectral correction offer this combined measurement directly on wine. The IRMS δ2H measurements on whole wine, however, are heavily influenced by the ethanol. This is shown in Fig. 6, where the δ2H results of 21 wine samples measured by the IRMS and OA-ICOS are plotted against their accompanying δ18O values (complete OA-ICOS points have been shown earlier in Fig. 3). The GMWL is also given as comparison. The standard errors (not visible in the plot) are typically 0.5 ‰ for δ2H (PyrOH) and for 0.25 ‰ for δ18O (by TC/EA).
As expected, the IRMS δ2H values are much more negative than those from OA-ICOS, caused by the far more negative δ2H values of ethanol [1, 5]. All the points in Fig. 6 are below GMWL, following the δ2H-δ18O relations known as "evaporation lines" . Whereas the δ2H-δ18O slope for meteoric water is ≈ 8, the relation for (kinetic) evaporative behaviour can be 3–6, depending on (micro) climatic conditions . The values of the individual wines can thus be thought of to start from the values on the GMWL that represent the local ground and rain water, and then moving from there along an evaporation trajectory to their final values. Two of these tracks have been indicated in Fig. 6. The Evaporation Fit Line for Italy (EFL-Italy) starts from – 5 ‰ (δ18O) and goes through all the Italian wine points, and the slope of this fitted line is 5.9 . The fitted evaporation line of Germany (EFL-Germany) starts from – 7 ‰ with a slope of 5.6 . The starting points correspond to, respectively, Italian and German precipitation and ground water . The Italian and German slopes do not differ much, and that is possibly because the Italian wines are from locations near the sea, while the German ones grow in a more arid place. In spite of the strong shift in the δ2H-values, the basic features of the water origin and evaporation effects are also conserved in the IRMS measurements (see the IRMS-Italy and IRMS-Germany line in Fig. 6). Moreover, from Fig. 6, and the ethanol/water H-amount ratio, one can deduce that the average δ2H-value for ethanol must be about – 270 ‰ (see further).
Our lab did close to 100 δ2H and δ18O "bulk" wine samples measurements using TC/EA between 2012 and 2014 (before we had an OA-ICOS instrument to our disposal) and Fig. 7 plots the results, in which the δ2H-values have already been shifted to correct for the ethanol influence. In Fig. 6, it can be seen that the IRMS-OA-ICOS δ2H difference for high δ18O-values is larger than the difference for low δ18O-values. Therefore, we shifted the δ2H of the 100 "bulk" wine samples based on the difference between the two German δ2H–δ18O slopes in Fig. 6. The wine samples are from 22 countries worldwide, and Fig. 7 indicates 6 representative countries. The differences between the wine-making countries are obvious in Fig. 7, and the δ2H and δ18O for South African wine samples are the most enriched ones, due to the warm and dry climatic conditions giving rise to both high values for the ground water and important evaporation effects. On the other hand, the German wines are from the northern-most climatic regions where grapes can grow, and we see the least enriched values from there. The French and Italian wine samples are in between. The Chilean and Californian wines show a strange deviation from most of the other ones, as they are relatively more enriched in δ18O than in δ2H. We attribute this effect to the fact that in these regions very often irrigation takes place with water originating from higher, colder mountainous regions nearby, water thus having far more negative isotope values than local water would have, but at the same time the evaporation characteristics belong to the warmer growing climate.
As the main features are thus conserved even in the IRMS "whole-wine" measurements, this means that suspicion of wine watering would also be visible in these simple and straightforward measurements. Nevertheless, since OA-ICOS (and similar laser techniques) are now mature, such measurements (with spectral correction) are to be preferred. They are even simpler and cheaper than TC/EA-IRMS. The spectral correction still offers room for improvement. The fact that one acquires both isotopes at the same time is very valuable, and needs to be brought into official methods, as this increases the sensitivity of wine watering detection.
Calculating δ2H for ethanol by combining the IRMS and OA-ICOS methods
As mentioned in the introduction, δ2H measurements of the wine ethanol using 2H-NMR is an official method to detect chaptalization. The hydrogen in the methyl group of ethanol is mostly (≈85%) transferred from the sugars, whereas the methylene group gets its hydrogen predominantly (≈75%) from the water. This leads to a characteristic difference in the D/H ratios of these two groups, denoted as (D/H)I and (D/H)II, respectively . Till now, site-selective 2H-NMR analysis ("SNIF-NMR") of wine ethanol is the only official way to prove chaptalization or sweetening of a wine. However, it is time-consuming and laborious, because of the necessary complete, fractionation-free distillation of ethanol, and the availability of a suitable NMR installation.
Both the IRMS method for the “whole wine” samples analysis and the OA-ICOS method with spectral correction for wine water isotopes are quick and simple methods for wine isotope analysis that require no pretreatment. Consequently, the δ2H difference between both methods must reflect the (average) δ2H of the ethanol (provided that the influence of the other constituents in the wine is not significant). If we further assume that the hydrogen in the hydroxyl group is in equilibrium with the wine water, and thus its δ2H equal to the δ2H of the wine water, we can deduce the sum of (D/H)I and (D/H)II in ethanol from the D/H ratio difference between IRMS and OA-ICOS.
The (D/H)I and (D/H)II of ethanol in our wine samples have been measured (by Isolab GmbH) via 2H-NMR methods, and they were reported to us as isotope abundances in ppm. The reported uncertainties for (D/H)I and (D/H)II were 0.3 ppm and 0.5 ppm, respectively, which are equivalent to 1.9 ‰ and 3.2 ‰. The average of (D/H)I and (D/H)II, defined as Fa, is equal to:
where FCH3, FCH2 are (D/H)I and (D/H)II, respectively.
The OA-ICOS measurement provides the deuterium abundance of the wine-water, and in addition the ethanol percentage (pe) based on Fig. 2. If, for the time-being, we neglect the other constituents of the wine, the percentages of water and ethanol (pw + pe) add up to 1. Therefore, the deuterium abundance in ethanol can be expressed as:
where Fw represents the water deuterium abundance and Fpyr the total wine deuterium abundance. mHw and mHe are the hydrogen masses in water and ethanol, respectively, calculated from pw and pe, the densities of water and ethanol, and the necessary atomic weights. As a result, the sum of (D/H)I and (D/H)II in ethanol using the PyrOH and OA-ICOS methods (F’a) is equal to:
(where the subtraction of Fw in the nominator is due to the hydroxyl group). Finally, we transfer the Fa and F’a abundances to δ2H (using the abundance of V-SMOW = 155.7 ppm). The comparison of δa and δ’a is shown in Fig. 8. It is directly visible that the scatter in the IRMS-OA-ICOS results is much larger than in the 2H-NMR ones. This is caused by the substantially higher uncertainty in the former, due to the fact that the measured difference must be multiplied by about a factor of 8–9 (according to Eq. (4) and (5) to get the value for the ethanol). Therefore, the measurement uncertainties of ± 3 ‰ in the OA-ICOS results lead to uncertainties around 25 ‰ for the ethanol value. In comparison, the uncertainties in the results of 2H-NMR are around 2 ‰. Still, it is visible that most of results deduced from the combination of IRMS and OA-ICOS are lower than those of 2H-NMR. Furthermore, the NMR results are rather constant, contrary to the IRMS-OA-ICOS ones. Only wines #19 and #21 (respectively: the sweet Greek whine that is possibly fortified, and the sweet German wine with the lowest δ-values) are higher than the NMR values, and there may be some non-detectable substances affecting the OA-ICOS value.
The likely explanation for the significant difference between the combination results and measured results by 2H-NMR is that the other constituents are not taken into account. The amounts of sugar, acids and glycerol varies from wine to wine, as does their isotopic content. Prior studies indicate that δ2H of these constituents are always negative [5, 31]. As an example, glycerol in wine has similar δ2H-values as ethanol , and (D/H)I of sugar-derived ethanol ranges from 93 to 110 ppm (equal to − 400 to − 294 ‰) . If we assume that the other constituents have the same δ2H value as the ethanol, we get the best overlap between our combination results and the NMR ones when we put their concentration at 2%. Those are the purple points in Fig. 8. This exercise shows that the impact of the other constituents is significant for using the combination of OA-ICOS and IRMS results to deduce the ethanol deuterium content.
The information that we have gathered using our various wine measurements can be wrapped up by answering our original research questions:
- The OA-ICOS method, in conjunction with the spectral contaminant identification software to correct for organic effects, provides the δ2H and δ18O values of wine water without any pre-treatment. It offers a fast (no pretreatment necessary) and cheap (no chemicals needed, the instrument is much cheaper than an IRMS) method for wine water isotope analysis with acceptable measurement uncertainties (in our study 3 ‰ and 0.4 ‰, respectively, for δ2H and δ18O). Especially the "automatic" addition of δ2H is an asset. Together, δ18O and δ2H are more powerful in pointing at the geographic origin of the wine and the growing season peculiarities. Wine watering is also much more clearly visible on the two-dimensional δ18O -δ2H surface than on the one-dimensional δ18O "line". As such, it is our recommendation to extend the official wine testing methods by δ2H of the wine water, and add OA-ICOS as an authorized measurement tool. Some caution must be taken when analyzing wines with high sugar content or high amounts of other impurities (methanol). The spectral parameters provided by the instrument, however, give a clear warning for these kinds of samples.
- For wine measurements with IRMS, δ2H and δ18O results represent the combination of water and ethanol, which can be seen as “whole wine” samples. The differences between the δ18O results measured by IRMS and OA-ICOS are mostly negligible. In other words, IRMS analysis of whole wine samples produce reliable values for the δ18O of the wine water, because the influence of the oxygen in ethanol and other constituents is small. This means, TC/EA-IRMS can be used as a fast screening tool for wines, to select potential suspicious wines for further testing.
The δ2H difference of IRMS and OA-ICOS results mostly comes from wine ethanol, so it provides in principle a possibility to analyse wine ethanol without distillation (and without 2H-NMR). However, the comparison of the ethanol deuterium results from 2H-NMR and the combination of methods (IRMS and OA-ICOS) shows that the combination results have large uncertainties, and do not correspond well with the 2H-NMR results. The former is caused by the relatively large uncertainty of the OA-ICOS spectral correction, and this uncertainty needs to be multiplied by 8–9 to arrive at the ethanol δ2H uncertainty. The latter is caused by the influence of the other constituents in the wine.
Improvements to the present work are to be found in the first place is a better, more accurate spectral correction mechanism. This would ideally lower the uncertainty in δ2H from the present ± 3 ‰ down to close to the ± 0.3 ‰ (or better) that we can achieve for δ2H measurement of pure waters with this instrument. An effective way to remove all other constituents but water and ethanol from the wine will be helpful as well. Together, this removal plus the lower uncertainty will definitely allow the deduction of the ethanol δ2H value from the IRMS-OA-ICOS combination. Of course, for site-specific analysis 2H-NMR will still remain the sole technique available, but fast and cheap screening of wine ethanol would then become possible for many laboratories. If the uncertainties can be brought down, even δ18O of ethanol would then be measurable, with the possibility of offering an internal standard for wine watering detection.
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Xing Wang gratefully acknowledges support by the Chinese Scholarship Council.
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Wang, X., Jansen, H.G., Duin, H. et al. Measurement of δ18O and δ2H of water and ethanol in wine by Off-Axis Integrated Cavity Output Spectroscopy and Isotope Ratio Mass Spectrometry. Eur Food Res Technol 247, 1899–1912 (2021). https://doi.org/10.1007/s00217-021-03758-2
- Stable isotopes
- Optical spectroscopy