Panorama
The Panorama is an ultra-high resolution multiple collector mass spectrometer specifically designed to undertake stable isotope analyses, far exceeding the performance of other commercial instruments.
Product Details
The Panorama introduces a unique ion optical architecture based on the Matsuda ESA–Quadrupole–Magnet design, delivering ultra-high mass resolution while maintaining exceptional sensitivity. Utilising a large-radius 800 mm magnet and a mass dispersion figure of merit of 1400 mm, the system provides resolving power far beyond that of conventional IRMS instruments. This capability enables the separation of complex molecular interferences and the precise measurement of rare isotopologue, including species important for advanced methane, atmospheric, and Earth science research. By combining exceptional resolution with multi-collector performance, Panorama opens new opportunities for applications that were previously inaccessible using traditional stable isotope mass spectrometry.
Developed to address the growing demand for high-resolution isotope measurements, Panorama provides researchers with a platform capable of tackling some of the most challenging analytical problems in isotope science. Its innovative analyser geometry extends the boundaries of stable isotope ratio mass spectrometry, enabling new insights into atmospheric processes, methane formation pathways, and the evolution of Earth systems.
Application Area
Atmospheric Chemistry
Atmospheric gases contain a wealth of isotopic information that can be used to understand climate processes, biogeochemical cycling, and interactions between the atmosphere, oceans, and biosphere. Panorama's ultra-high resolving power allows researchers to separate and precisely measure isotopic species that cannot be resolved using conventional IRMS instruments. This capability supports studies of atmospheric transport, trace gas cycling, and the origins of greenhouse gases. By reducing spectral interferences and improving measurement precision, Panorama enables more robust investigation of complex atmospheric systems.
Application Area
Methane Formation
Methane is produced through a variety of biological and geological processes, each leaving a distinct isotopic signature. Panorama enables the measurement of rare methane isotopologues, providing powerful insights into methane formation temperatures, reaction mechanisms, and source attribution. These measurements help researchers distinguish between biogenic, thermogenic, and abiotic methane sources with greater confidence than traditional isotope techniques. The resulting data can be used to investigate methane reservoirs, migration pathways, and global methane cycling within both modern and ancient environments.
Application Area
Earth Sciences
Stable isotope measurements play a critical role in understanding the formation and evolution of Earth's systems. Panorama provides the resolution required to investigate complex isotopic signatures associated with geological, geochemical, and palaeoenvironmental processes. Applications include the study of mineral formation, fluid-rock interactions, deep carbon cycling, and ancient environmental conditions. By enabling measurements of previously unresolved isotopic species, Panorama helps researchers extract new information from geological materials and advance understanding of Earth's history and processes.
Benefits
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Markets & Applications
The Panorama has been developed for scientists pushing the boundaries of isotope research. Its ultra-high resolving power enables measurements that are not achievable using conventional IRMS instruments, opening new opportunities in atmospheric chemistry, methane formation studies, planetary science, and fundamental geochemistry.
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Methane (CH₄)
Measure rare methane isotopologues including ¹³CH₃D and ¹²CH₂D₂, enabling investigations of methane formation temperatures, source attribution, mixing processes, and reaction pathways.
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Nitrogen (N₂)
Perform high-resolution measurements of rare nitrogen isotopologues for studies of atmospheric chemistry, biological cycling, and isotope fractionation processes.
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Oxygen (O₂)
Resolve oxygen isotopologues and isotopic ordering species that are challenging or impossible to measure using conventional IRMS systems, supporting atmospheric and geochemical research.
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