Resolution of 176 Yb and 176 Lu interferences on 176 Hf to enable accurate 176 Hf/177 Hf isotope ratio analysis using ICP-QQQ with MS/MS
Applications | 2017 | Agilent TechnologiesInstrumentation
Accurate determination of the 176Hf/177Hf isotope ratio is critical for geological dating and understanding mineral formation processes. Hafnium isotopes serve as reliable chronometers in materials like zircon where lead mobility can compromise Pb/U and Pb/Pb age determinations. Overcoming isobaric interferences from 176Lu and 176Yb on the 176Hf signal is essential to obtain precise isotope ratios without extensive sample preparation or mathematical corrections.
This study aimed to demonstrate the direct resolution of 176Lu and 176Yb interferences on 176Hf using collision/reaction cell chemistry combined with tandem quadrupole ICP-MS (ICP-QQQ) in MS/MS mode. The goal was to eliminate isobaric overlaps and preserve true Hf isotope abundances in complex sample matrices, including mixed rare earth element standards and geological mineral extracts.
The approach employed ammonia cell gas to shift 176Hf into a characteristic ammonia‐adduct ion at m/z 258, while Lu and Yb remain unreacted. A first quadrupole (Q1) set to unit mass resolution at m/z 176 filters only ions of that mass into the collision/reaction cell, preventing other matrix species from entering. A second quadrupole (Q2) then monitors the Hf(NH)(NH2)(NH3)3+ product ion at m/z 258. Product ion scans and neutral gain scans were used to optimize cell gas flow and octopole bias, ensuring maximal yield of the desired adduct and confirmation of isotopic pattern integrity.
Comparison of three operating modes—single quadrupole without gas, single quadrupole with NH3 bandpass, and MS/MS with NH3—revealed large positive biases in the first two modes when Lu or Yb interferences were present. In contrast, MS/MS mode using ammonia fully removed isobaric overlaps and avoided formation of new ammonia‐adduct interferences, yielding 176Hf/177Hf ratios within 0.3% of the true value across all test matrices.
Advances in tandem quadrupole ICP-MS promise broader adoption of reaction chemistry approaches for challenging isobaric separations. Integration with laser ablation and automated workflows will extend precise isotope analyses to a wider range of geological, environmental, and industrial applications. Further development of novel reaction gases and cluster‐ion strategies may enable direct measurement of additional problematic isotope systems.
The MS/MS ICP-QQQ method using ammonia reaction gas provides reliable and accurate 176Hf/177Hf isotope ratio analysis by effectively resolving 176Lu and 176Yb interferences. This technique eliminates the need for extensive sample preparation or mathematical corrections, paving the way for robust isotope geochemistry studies in complex matrices.
ICP/MS, ICP/MS/MS
IndustriesEnvironmental
ManufacturerAgilent Technologies
Summary
Significance of the Topic
Accurate determination of the 176Hf/177Hf isotope ratio is critical for geological dating and understanding mineral formation processes. Hafnium isotopes serve as reliable chronometers in materials like zircon where lead mobility can compromise Pb/U and Pb/Pb age determinations. Overcoming isobaric interferences from 176Lu and 176Yb on the 176Hf signal is essential to obtain precise isotope ratios without extensive sample preparation or mathematical corrections.
Objectives and Study Overview
This study aimed to demonstrate the direct resolution of 176Lu and 176Yb interferences on 176Hf using collision/reaction cell chemistry combined with tandem quadrupole ICP-MS (ICP-QQQ) in MS/MS mode. The goal was to eliminate isobaric overlaps and preserve true Hf isotope abundances in complex sample matrices, including mixed rare earth element standards and geological mineral extracts.
Methodology
The approach employed ammonia cell gas to shift 176Hf into a characteristic ammonia‐adduct ion at m/z 258, while Lu and Yb remain unreacted. A first quadrupole (Q1) set to unit mass resolution at m/z 176 filters only ions of that mass into the collision/reaction cell, preventing other matrix species from entering. A second quadrupole (Q2) then monitors the Hf(NH)(NH2)(NH3)3+ product ion at m/z 258. Product ion scans and neutral gain scans were used to optimize cell gas flow and octopole bias, ensuring maximal yield of the desired adduct and confirmation of isotopic pattern integrity.
Used Instrumentation
- Agilent 8800 ICP-QQQ with MS/MS capability (superseded by 8900 model)
- Micromist nebulizer, quartz spray chamber, and quartz torch
- SPS 4 autosampler
- Ammonia (10% in He) as reaction gas
Main Results and Discussion
Comparison of three operating modes—single quadrupole without gas, single quadrupole with NH3 bandpass, and MS/MS with NH3—revealed large positive biases in the first two modes when Lu or Yb interferences were present. In contrast, MS/MS mode using ammonia fully removed isobaric overlaps and avoided formation of new ammonia‐adduct interferences, yielding 176Hf/177Hf ratios within 0.3% of the true value across all test matrices.
Benefits and Practical Applications
- Eliminates need for time‐consuming chemical separations in many cases
- Enables in situ analyses, including laser ablation, without matrix‐induced biases
- Facilitates multi‐element isotope measurements by rapid mode switching
Future Trends and Potential Uses
Advances in tandem quadrupole ICP-MS promise broader adoption of reaction chemistry approaches for challenging isobaric separations. Integration with laser ablation and automated workflows will extend precise isotope analyses to a wider range of geological, environmental, and industrial applications. Further development of novel reaction gases and cluster‐ion strategies may enable direct measurement of additional problematic isotope systems.
Conclusion
The MS/MS ICP-QQQ method using ammonia reaction gas provides reliable and accurate 176Hf/177Hf isotope ratio analysis by effectively resolving 176Lu and 176Yb interferences. This technique eliminates the need for extensive sample preparation or mathematical corrections, paving the way for robust isotope geochemistry studies in complex matrices.
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