Difficulty: Easy
Correct Answer: Isotopes
Explanation:
Introduction / Context:
Mass spectrometry (MS) separates ions by mass-to-charge ratio and detects their abundances. Because different isotopes of an element have different masses, MS is exceptionally powerful for isotope identification and ratio measurements, widely used in geochemistry, nuclear science, environmental tracing, and quality control of gases and organics.
Given Data / Assumptions:
Concept / Approach:
Isotopic variants differ only in neutron number, thus mass. When ionized, their m/z values shift accordingly, producing resolvable peaks that unveil isotopic composition with high sensitivity and precision. While alloys can be studied by MS after appropriate sampling (e.g., spark source, laser ablation), the technique excels most naturally at isotope analysis due to the direct mass distinction. Bulk solids without vaporization/ionization cannot be analyzed directly; sample introduction must create ions first.
Step-by-Step Solution:
Verification / Alternative check:
Applications like isotope ratio MS (IRMS) and accelerator MS are standard for isotopic fingerprints (e.g., C-13/C-12, O-18/O-16).
Why Other Options Are Wrong:
Common Pitfalls:
Assuming MS directly “weighs” solids; all MS measurements are on ions in vacuum.
Final Answer:
Isotopes
Discussion & Comments