Brazilian AMS Radiocarbon Laboratory (LAC-UFF) and intercomparison of preliminary results with Sample Preparation Laboratory (LAPA14C - UFBA)

被引:0
作者
dos Santos, Tarcio Henrique Ribeiro [1 ]
Zucchi, Maria do Rosario [2 ,3 ]
Costa, Alexandre Barreto [2 ,3 ]
de Oliveira, Fabiana Monteiro [4 ,5 ]
Macario, Kita Chaves Damasio [4 ,6 ]
Lopes, Jose Marques [2 ,3 ]
dos Santos, Naiana Dias [3 ]
de Azevedo, Antonio Expedito Gomes [2 ]
Barioni, Adriana [7 ]
Gomes, Doriedson Ferreira [8 ]
机构
[1] Inst Fed Educ Ciencia & Tecnol Bahia IFBA, Campus Valenca, BR-45400000 Valenca, Brazil
[2] Univ Fed Bahia UFBA, Dept Fis Terra & Meio Ambiente, Inst Fis, BR-40170115 Salvador, Brazil
[3] Univ Fed Bahia UFBA, Programa Posgrad Geoquim Petr & Meio Ambiente POSP, BR-40170110 Salvador, Brazil
[4] Univ Fed Fluminense, Lab Radiocarbono, LAC UFF, Ave Gal Milton Tavares de Souza S-N, BR-24210346 Niteroi, RJ, Brazil
[5] Univ Fed Fluminense UFF, Programa Posgrad Quim, BR-24020141 Niteroi, RJ, Brazil
[6] Univ Fed Fluminense UFF, Programa Posgrad Ciencia Informacao, Niteroi, Brazil
[7] Univ Fed Sao Paulo Unifesp, Dept Ciencias Mar, BR-11015020 Santos, Brazil
[8] Univ Fed Bahia UFBA, Inst Biol, Lab Paleoecol EcoPaleo, BR-40170115 Salvador, Brazil
关键词
accelerator mass spectrometry; carbon isotopes; laboratory intercomparison; Latin American radiocarbon network; C-14; GRAPHITIZATION; PROTOCOLS; EXERCISE; BONES;
D O I
10.1017/RDC.2024.104
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
This study presents the initial results of carbon-14 dating after performing sample preparation and graphite production processes at the Federal University of Bahia (UFBA) in an intercomparison with the same processes performed at the Radiocarbon Laboratory of the Fluminense Federal University (LAC-UFF). Both laboratories are located in Brazil. The accelerator mass spectrometry (AMS) system at LAC-UFF was used for radiocarbon measurements. To verify any possible contamination sources during sample preparation, we initially performed swipe tests at UFBA, which were subsequently processed and the graphite samples were produced at LAC-UFF. After UFBA, several reference materials (IAEA-C1, -C2, -C6, -C9, and OXII standards) were prepared and converted into graphite. In addition, the sample material was first partially prepared at UFF and UFBA and then analyzed with the AMS system at LAC-UFF. Subsamples were prepared for additional measurements of the delta 13C composition with an elemental analyzer coupled to an isotope ratio mass spectrometer (EA-IRMS) in LFNA-UFBA to study the isotopic fractionation and yield of the graphitization reaction. The obtained values closely aligned with the reference values, demonstrating reproducibility and quality and indicating minimal contamination during chemical and graphitization processes. In the future, samples from different matrices will be prepared at UFBA for application in paleoenvironmental and archaeological studies.
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页数:9
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