Temerdashev Zaual, Abakumov Aleksey, Khalafyan Alexan, Bolshov Mikhail, Lukyanov Aleksey, Vasilyev Alexander, Gipich Evgeniy
Analytical Chemistry Department, Faculty of Chemistry and High Technologies, Kuban State University, Krasnodar 350040, Russia.
Institute for Spectroscopy Russian Academy of Sciences, Troitsk, Moscow 108840, Russia.
Molecules. 2024 May 10;29(10):2251. doi: 10.3390/molecules29102251.
The features for assessing the authenticity of wines by region of origin are studied, based on the relationship between the mineral composition of the wine, the grapes, and the soil profile (0 to 160 cm) from the place of growth of Cabernet Sauvignon grapes. Soil, grape, and wine samples were taken from the territories of six vineyards in the Anapa district of Krasnodar Territory, Russia. Using the methods of ICP-OES, thermal, and X-ray phase analysis, the soils were differentiated into three groups, differing in mineralogical and mineral compositions. The soil samples of the first group contained up to 31% quartz, the second group up to 25% quartz and 19% mixed calcite, and the third group up to 32% calcite and 15% quartz. The formation of the elemental image of the grapes was studied, taking into account the total content and mobile forms of metals in the soil. The territorial proximity of the vineyards did not affect the extraction of elements from the soil into the grape berry, and the migration of metals for each territory was selective. According to the values of the biological absorption coefficient, the degree of transition of metals from the soil to a berry was estimated. For K, Ti, Zn, Rb, Cu, and Fe in all berries, the coefficient was higher than 1.00, which means that the berry extracts contained not only mobile-form, but also difficult-to-dissolve metal compounds. The migration of macro-components from the soil to the berry was low, and amounted to 6-7% for Ca, 0.8-3.0% for Na, and 25-70% for Mg of the concentration of their mobile forms. For all territories, the maximum correlation between metal concentrations in grapes and soil was observed for samples from a depth of 0-40 cm. The discriminant model based on concentrations of Rb, Al, K, Sr, Co, Na, Pb, Ca, and Ni showed the formation of clusters in the territories of vineyard cultivation. The developed model allow the problems of identifying wines by region to be solved with high accuracy, using their elemental image.
基于葡萄酒、葡萄的矿物质组成与赤霞珠葡萄生长地土壤剖面(0至160厘米)之间的关系,对按产地评估葡萄酒真伪的特征进行了研究。土壤、葡萄和葡萄酒样本取自俄罗斯克拉斯诺达尔边疆区阿纳帕区的六个葡萄园。采用电感耦合等离子体发射光谱法(ICP - OES)、热分析和X射线相分析方法,将土壤分为三组,它们在矿物学和矿物组成上存在差异。第一组土壤样本含石英高达31%,第二组含石英高达25%和方解石混合物19%,第三组含方解石高达32%和石英15%。考虑到土壤中金属的总含量和可移动形态,研究了葡萄元素图像的形成。葡萄园在地域上的接近程度并不影响土壤中元素向葡萄浆果的提取,且每个地域金属的迁移具有选择性。根据生物吸收系数值,估算了金属从土壤向浆果的转移程度。对于所有浆果中的钾、钛、锌、铷、铜和铁,该系数高于1.00,这意味着浆果提取物不仅含有可移动形态的金属化合物,还含有难溶的金属化合物。大量元素从土壤向浆果的迁移较低,钙的迁移量为其可移动形态浓度的6 - 7%,钠为0.8 - 3.0%,镁为25 - 70%。对于所有地域,在0 - 40厘米深度的样本中观察到葡萄和土壤中金属浓度之间的最大相关性。基于铷、铝、钾、锶、钴、钠、铅、钙和镍浓度的判别模型显示在葡萄园种植地域形成了聚类。所开发的模型能够利用葡萄酒的元素图像高精度地解决按产地识别葡萄酒的问题。