| Literature DB >> 31993161 |
María Isabel Sánchez-Rodríguez1, Elena M Sánchez-López2, Alberto Marinas2, Francisco José Urbano2, José M Caridad1.
Abstract
Extra virgin olive oil (EVOO) is very appreciated by its taste, flavor, and benefits for health, and so, it has a high price of commercialization. This fact makes it necessary to provide reliable and cost-effective analytical procedures, such as near-infrared (NIR) spectroscopy, to analyze its traceability and purity, in combination with chemometrics. Fatty acids profile of EVOO, considered as a quality parameter, is estimated, firstly, from NIR data and, secondly, by adding agro-climatic information. NIR and agro-climatic data sets are summarized by using principal component analysis (PCA) and treated by both scalar and functional approaches. The corresponding PCA and FPCA are progressively introduced in regression models, whose goodness of fit is evaluated by the dimensionless root-mean-square error. In general, SFAs, MUFAs, and PUFAs (and disaggregated fatty acids) estimations are improved by adding agro-climatic besides NIR information (mainly, temperature or evapotranspiration) and considering a functional point of view for both NIR and agro-climatic data.Entities:
Keywords: NIR spectra; agro‐climatic curves; extra virgin olive oil; functional data analysis; regression models
Year: 2019 PMID: 31993161 PMCID: PMC6977507 DOI: 10.1002/fsn3.1312
Source DB: PubMed Journal: Food Sci Nutr ISSN: 2048-7177 Impact factor: 2.863
Figure 1NIR spectra of EVOO
Fatty acid composition (in % m/m methyl esters) as determined by GC
| Group | Fatty acid | Carbon number | % m/m methyl esters |
|---|---|---|---|
| SFA | Myristic | C14:0 | ≤0.03 |
| Palmitic | C16:0 | 7.50–20.00 | |
| Heptadecanoic | C17:0 | ≤0.40 | |
| Stearic | C18:0 | 0.50–5.00 | |
| Arachidic | C20:0 | ≤0.60 | |
| Behenic | C22:0 | ≤0.20 | |
| Lignoceric | C24:0 | ≤0.20 | |
| MUFA | Palmitoleic | C16:1 | 0.30–3.50 |
| Heptadecenoic | C17:1 | ≤0.60 | |
| Oleic | C18:1 | 55.00–83.00 | |
| Eicosenoic | C20:1 | ≤0.50 | |
| PUFA | Linoleic | C18:2 | 2.50–21.00 |
| Linolenic | C18:3 | ≤1.00 |
Source: International Olive Council (2012).
Abbreviations: MUFA, monounsaturated fatty acids; PUFA, polyunsaturated fatty acids; SFA: saturated fatty acid.
Automatic Weather Stations (AWSs)
| Province | Station | Code |
|---|---|---|
| Cadiz | Villamartín | 1 |
| Cordoba | Adamuz | 2 |
| Baena | 3 | |
| Belmez | 4 | |
| Cabra | 5 | |
| Córdoba | 6 | |
| El Carpio | 7 | |
| Hinojosa del Duque | 8 | |
| Hornachuelos | 9 | |
| Palma del Río | 10 | |
| Santaella | 11 | |
| Granada | Loja | 12 |
| Pinos Puente | 13 | |
| Jaen | Alcaudete | 14 |
| Chiclana de Segura | 15 | |
| Jaén | 16 | |
| Higuera de Arjona | 17 | |
| Mancha Real | 18 | |
| Marmolejo | 19 | |
| Pozo Alcón | 20 | |
| San José de los Propios | 21 | |
| Santo Tomé | 22 | |
| Malaga | Antequera | 23 |
| Archidona | 24 | |
| Pizarra | 25 | |
| Sierra de Yeguas | 26 | |
| Seville | Écija | 27 |
| Osuna | 28 |
Figure 2Agro‐climatic spectra for the 28 AWSs
Figure 3Phenological cycle of the olive grove
Optimal number of components by considering classical and actual criteriaa
| N. comp in PCA regression | N. Comp in FPCA regression | ||||
|---|---|---|---|---|---|
| Spectral information | Kaiser's rule | Cross‐validation | Kaiser's rule | Cross‐validation | |
| NIR | NIR | 4 | 7 | 3 | 6 |
| NIR + AGR | NIR + TEMP | 7 | 6 | 7 | 7 |
| NIR + HUM | 9 | 10 | 9 | 8 | |
| NIR + WSPE | 10 | 11 | 10 | 11 | |
| NIR + RAD | 8 | 10 | 8 | 10 | |
| NIR + PRECIP | 11 | 10 | 11 | 8 | |
| NIR + ETo | 10 | 11 | 10 | 9 | |
In all cases, the percentage of variability of data explained by the selected components is greater than 85%.
Figure 4DRMSE in SFA, MUFA, and PUFA estimations by PCA* and FPCA** regression models from NIR data
Figure 5RMSE in SFA estimations by PCA* and FPCA** regression models from NIR and agro‐climatic data
Figure 6RMSE in MUFA estimations by PCA* and FPCA** regression models from NIR and agro‐climatic data
Figure 7RMSE in MUFA estimations by PCA* and FPCA** regression models from NIR and agro‐climatic data