基于矿物元素指纹图谱技术的武夷岩茶产地溯源研究

    Study on the Origin Traceability of Wuyi Rock Tea Based on Mineral Element Fingerprinting Technology

    • 摘要: 武夷岩茶由于外形、工艺的一致性,无法通过外观特征来识别其产地,茶叶中元素组成因产地环境不同而有所差异,形成茶叶产地特有的元素指纹。通过测定武夷岩茶不同产区的多种元素含量,借助化学计量统计方法建立产地判别模型,为武夷岩茶的产地判别提供技术参考。从武夷岩茶3个主要产区采集茶青样品共55件,采用电感耦合等离子体发射光谱法(ICP-OES)和电感耦合等离子体质谱法(ICP-MS)测定矿物元素含量,对数据进行主成分分析,同时采用正交偏最小二乘法判别(OPLS-DA)和Fisher线性判别(FLDA)2种判别方法对武夷岩茶进行产区判别。结果表明:武夷岩茶3个主产区茶叶样品中元素表现出不同的特征,对样品中元素的含量进行巴特利特球形检验,得出取样适切性量数( KaiserMeyer-Olkin,KMO)值为0.650,KMO>0.5说明分组聚类效果较好。通过主成分分析,成功提取了5个主成分,其特征值均超过1,且累计方差贡献率为71.560%。正交偏最小二乘法判别模型累积解释能力参数R2X=0.652,R2Y=0.752,预测能力参数Q2为 0.590,均大于0.5。Fisher线性判别模型对模型构建样本回代验证的正确判别率和交叉验证率均在90.9%以上。2种模型均能实现对3种不同产区采集的茶青样品进行准确判别。研究认为通过3个不同产区采集的武夷岩茶样品中矿物元素指纹分析结合化学计量统计方法,可以有效地进行产地判别,为武夷岩茶原产地保护提供了鉴别理论基础。

       

      Abstract: Due to the consistency of appearance and processing, the place of origin of Wuyi rock tea can not be identified by its appearance characteristics. The elemental composition of tea leaves is different due to the different environment of producing area, forming the unique elemental fingerprint of tea producing area. By measuring the contents of various elements in different producing areas of Wuyi rock tea, the origin discrimination model was established by means of stoichiometric statistical method, which provided technical reference for the origin discrimination of Wuyi rock tea. A total of 55 tea green samples were collected from three main producing areas of Wuyi rock tea. The contents of mineral elements were determined by inductively coupled plasma optical emission spectrometry (ICP-OES) and inductively coupled plasma mass spectrometry (ICP-MS), and the data were analyzed by using the principal component analysis. At the same time, two discriminant methods, including the orthogonal partial least squares discriminant analysis (OPLS-DA) and Fisher linear discriminant analysis (FLDA), were used to discriminate the producing areas of Wuyi rock tea. The results showed that: the elements in the tea samples from the three main producing areas of Wuyi rock tea showed different characteristics. The content of the elements in the samples was tested by Bartlett’s sphericity test. The Kaiser Meyer-Olkin (KMO) value was 0.650, and KMO > 0.5 indicated that the grouping clustering effect was better. Through the principal component analysis, five principal components were successfully extracted, and their eigenvalues were more than 1, and the cumulative variance contribution rate was 71.560%. The cumulative interpretation ability parameters of the orthogonal partial least squares discriminant model were R2X = 0.652, R2Y = 0.752, and the predictive ability parameter Q2 was 0.590, all exceeding 0.5. The correct discrimination rate and cross-validation rate of the Fisher linear discriminant model were more than 90.9%. Both models could accurately discriminate the tea green samples collected from three different producing areas. This study demonstrated that the mineral elemental fingerprints of Wuyi rock tea samples from three different producing areas, combined with stoichiometric statistical methods, could effectively identify their origin, providing a theoretical basis for the protection of place of origin of Wuyi rock tea.

       

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