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Click here to request a quote Introduction to Oxygen-18 Gas (O-¹⁸O₂, O-18o2) Oxygen-18 (¹⁸O) is a stable isotope of oxygen with a nucleus containing
Introduction Zinc-68 (Zn-68) is a stable, non-radioactive isotope of zinc, accounting for approximately 18.8% of naturally occurring zinc. With 30 protons and 38 neutrons,
Carbon-13 (C-13) Stable Isotope – Introduction Carbon-13 (C-13) is a stable, non-radioactive isotope of carbon that makes up about 1.1% of all naturally occurring
Maximize your production efficiency with our high-purity Rubidium Isotopes – Rb-87 in metal form, ensuring optimal results for your applications. Superior Quality: High-purity Rb-87
High Purity Yb-176 Isotopes for optimal results in Lu-177 production. Reliable Supply Chain to support your ongoing needs. Competitive Pricing designed for bulk orders
Click here to request a quote Introduction to Oxygen-18 Gas (O-¹⁸O₂, O-18o2) Oxygen-18 (¹⁸O) is a stable isotope of oxygen with a nucleus containing
Introduction Helium-3 (He-3 , He3) is a rare and irreplaceable isotope with unique properties that make it essential across multiple industries. Its low atomic
Introduction Zinc-68 (Zn-68) is a stable, non-radioactive isotope of zinc, accounting for approximately 18.8% of naturally occurring zinc. With 30 protons and 38 neutrons,
Carbon-13 (C-13) Stable Isotope – Introduction Carbon-13 (C-13) is a stable, non-radioactive isotope of carbon that makes up about 1.1% of all naturally occurring
Introduction Magnesium-26 (Mg-26) is one of the stable isotopes of magnesium, comprising approximately 11% of naturally occurring magnesium. With 12 protons and 14 neutrons,
Calcium-44 (Ca-44) Stable Isotope – Introduction Calcium-44 (Ca-44) stands out as a highly valuable stable isotope. Its unique nuclear properties make it a critical
Please choose the element you are interested in from the periodic table below.
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These isotopes are used directly or as precursors in the production of therapeutic or diagnostic radiopharmaceuticals (e.g., n.c.a. Lu-177, Ga-68, I-123):
Used for nuclear reactions, neutron capture cross-section studies, and as target materials for accelerator or reactor-based experiments:
Used in stable isotope tracing, biogeochemistry, metabolism studies, and isotope geochemistry:
Used in semiconductors, nuclear shielding, catalysis, alloys, or as neutron absorbers:
Used for neutron detection, plasma research, or tracer gases:
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