Precise determination of the lithium isotope ratio in geological samples using MC-ICP-MS with cool plasma

2013 ◽  
Vol 28 (4) ◽  
pp. 505 ◽  
Author(s):  
Min Seok Choi ◽  
Jong-Sik Ryu ◽  
Ha Yan Park ◽  
Kwang-Sik Lee ◽  
Youngwoo Kil ◽  
...  
2019 ◽  
Vol 34 (6) ◽  
pp. 1256-1262 ◽  
Author(s):  
Qian Ma ◽  
Ming Yang ◽  
Han Zhao ◽  
Noreen J. Evans ◽  
Zhu-Yin Chu ◽  
...  

We describe protocols for highly reproducible analysis of Lu and Hf contents and Hf isotopic composition at sub-nanogram levels in geological samples by MC-ICP-MS.


2018 ◽  
Vol 34 (6) ◽  
pp. 667-674 ◽  
Author(s):  
Masaharu TANIMIZU ◽  
Kazuya NAGAISHI ◽  
Tsuyoshi ISHIKAWA

2016 ◽  
Vol 31 (8) ◽  
pp. 1673-1679 ◽  
Author(s):  
Ting Zhang ◽  
Lian Zhou ◽  
Lu Yang ◽  
Qian Wang ◽  
Lan-ping Feng ◽  
...  

A new MC-ICP-MS approach is reported for highly precise and accurate determination of the Ga isotope ratio in geological samples.


Author(s):  
Ferrari Colin ◽  
Resongles Eléonore ◽  
Freydier Rémi ◽  
Casiot Corinne

Thiol-functionalized silica powder allowed single-step purification of antimony for exploring stable Sb isotope signatures in the environment.


2021 ◽  
Author(s):  
Seung-Gu Lee ◽  
Tsuyoshi Tanaka

<p></p><p>Eu has only two isotopes (151Eu and 153 Eu). Eu and Gd are one of the rare earth elements that are very difficult to completely separate from each other. Eu isotope ratio can be determined by MC-ICP-MS using internal Sm or Gd spikes to correct for mass discrimination. NIST3117a ultrapure chemical reagent shows almost no Eu isotope fractionation regardless of the kind of normalization isotope pair. However, Eu isotope ratio in the silicate rocks was effected by Gd matrix during MC-ICP-MS measurement if a trace amount of Gd impurity remains in the purified Eu fraction. In this report, we tried to determine optimizing conditions for precise and accurate Europium isotope ratio measurements in geological samples using MC-ICP-MS. The pure Eu fraction with almost no Gd matrix separated from geological samples and NIST3117a ultrapure chemical reagent show almost same degree of Eu isotope fractionation regardless of the kind of normalization isotope pair. However, Eu isotope ratio in the silicate rocks was effected by Gd matrix during MC-ICP-MS measurement using if 154 Gd interference relative to 154 Sm as internal standard is more than ca. 0.1%. Particularly, highly fractionated granite and high silica volcanic rock with extremely low Eu concentration compared to Gd require high – purity Eu separation with a high recovery rate to obtain the true value of the Eu isotope fractionation in the geological rocks. <br></p><br><p></p>


Author(s):  
Colin Ferrari ◽  
Eléonore Resongles ◽  
Rémi Freydier ◽  
Corinne Casiot

Correction for ‘A single-step purification method for the precise determination of the antimony isotopic composition of environmental, geological and biological samples by HG-MC-ICP-MS’ by Colin Ferrari et al., J. Anal. At. Spectrom., 2021, 36, 776–785, DOI: "https://doi.org/10.1039/D0JA00452A">10.1039/D0JA00452A.


2019 ◽  
Vol 31 (2) ◽  
pp. 262-270 ◽  
Author(s):  
Lüyun Zhu ◽  
Ganglan Zhang ◽  
Yongsheng Liu ◽  
Jie Lin ◽  
Xirun Tong ◽  
...  

2020 ◽  
Vol 92 (24) ◽  
pp. 16097-16104
Author(s):  
Jakub Karasiński ◽  
Andriy Tupys ◽  
Lu Yang ◽  
Zoltan Mester ◽  
Ludwik Halicz ◽  
...  

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