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（意大利南部）的地质溯源性：初步矿物学和同位素数据。

Geotraceability of (South Italy): Preliminary mineralogical and isotopic data.

作者信息

Mercurio Mariano, Cappelletti Piergiulio, Di Renzo Valeria, Grifa Celestino, Guarino Carmine, Izzo Francesco, Magliulo Paolo, Mercurio Vincenzo, Tranfa Piergiorgio, Zuzolo Daniela, D'Antonio Massimo, Langella Alessio

机构信息

Department of Science and Technology, University of Sannio, Via dei Mulini 59/A, 82100 Benevento, Italy.

Department of Earth Sciences, Environment and Resources, University of Naples Federico II, Via Vicinale Cupa Cintia 21, 80126 Naples, Italy.

出版信息

Data Brief. 2024 Jun 26;55:110686. doi: 10.1016/j.dib.2024.110686. eCollection 2024 Aug.

DOI:10.1016/j.dib.2024.110686
PMID:39071958
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC11282966/
Abstract

The present study gathers mineralogical and isotopic geochemical data of 45 soil samples collected from the and wineries (Southern Italy) in order to provide useful information for the geotraceability of white wine . Mineralogical analyses show the ubiquitous presence of quartz, frequent and moderate contents of feldspars and phyllosilicates (i.e., illite/mica, kaolinite, and smectite). Rhizosphere soils from vineyards show a strontium isotope signature (Sr/Sr) ranging from 0.708604 to 0.711234 (average 0.710334; 1σ = 0.000943; = 7) for the total fraction and a narrower range (from 0.706907 to 0.708807; average 0.708120; 1σ = 0.000641; = 7) for the bioavailable one. For the rhizosphere soils collected from the vineyards of winery, Sr/Sr ratios range from 0.708268 to 0.712413 (average 0.710145; 1σ = 0.001622; = 8) and from 0.707968 to 0.709157 (average 0.708384; 1σ = 0.000409; = 8) for the total and the bioavailable fraction, respectively. Actually, the bioavailable Sr fraction shows a narrower range of Sr/Sr ratios compared to that of the total fraction, making the former more suitable for any study of wine traceability.

摘要

本研究收集了从意大利南部的[酒庄名称1]和[酒庄名称2]酒庄采集的45个土壤样本的矿物学和同位素地球化学数据，以便为[白葡萄酒名称]白葡萄酒的地质溯源提供有用信息。矿物学分析表明，石英普遍存在，长石和层状硅酸盐（即伊利石/云母、高岭石和蒙脱石）含量频繁且适中。[酒庄名称1]葡萄园的根际土壤中，总部分的锶同位素比值（(^{87}Sr/^{86}Sr)）范围为0.708604至0.711234（平均值0.710334；1σ = 0.000943；(n = 7)），生物可利用部分的范围较窄（从0.7

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c3c0/11282966/6e91c5c2e96a/gr7.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c3c0/11282966/de4785d72ea3/gr1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c3c0/11282966/08c64e477457/gr2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c3c0/11282966/5846e7c3dea8/gr3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c3c0/11282966/25407a4a30f9/gr4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c3c0/11282966/ee34a74f6c1f/gr5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c3c0/11282966/6844f60f7a61/gr6.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c3c0/11282966/6e91c5c2e96a/gr7.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c3c0/11282966/de4785d72ea3/gr1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c3c0/11282966/08c64e477457/gr2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c3c0/11282966/5846e7c3dea8/gr3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c3c0/11282966/25407a4a30f9/gr4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c3c0/11282966/ee34a74f6c1f/gr5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c3c0/11282966/6844f60f7a61/gr6.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c3c0/11282966/6e91c5c2e96a/gr7.jpg

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本文引用的文献

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2
Archaeometric data from the ceramic workshop in Pompeii (Southern Italy).来自意大利南部庞贝陶瓷工坊的考古测量数据。
Data Brief. 2020 Dec 30;34:106706. doi: 10.1016/j.dib.2020.106706. eCollection 2021 Feb.
3
From soil to grape and wine: Variation of light and heavy elements isotope ratios.从土壤到葡萄和葡萄酒：轻、重元素同位素比值的变化。
Food Chem. 2016 Nov 1;210:648-59. doi: 10.1016/j.foodchem.2016.04.108. Epub 2016 Apr 23.
4
ATR-FT-IR spectral collection of conservation materials in the extended region of 4000-80 cm⁻¹.4000 - 80厘米⁻¹扩展区域内保护材料的衰减全反射傅里叶变换红外光谱采集
Anal Bioanal Chem. 2016 May;408(13):3373-9. doi: 10.1007/s00216-016-9411-5. Epub 2016 Mar 11.