Difficulty: Easy
Correct Answer: Nitrogen (N2)
Explanation:
Introduction / Context:Greenhouse gases (GHGs) absorb and re-emit infrared radiation, reducing the efficiency with which Earth loses heat to space. The major naturally occurring GHGs include water vapour, carbon dioxide, methane, nitrous oxide, and ozone; human activities have increased several of these concentrations.
Given Data / Assumptions:
Concept / Approach:Molecules absorb IR when their vibrations change the dipole moment. Linear homonuclear diatomics such as N2 and O2 lack a permanent dipole and have vibrational modes that are IR-inactive, making them negligible greenhouse contributors despite their abundance. Conversely, CO2 (asymmetric stretch/bend), CH4 (multiple vibrational modes), N2O, and O3 have strong IR absorption bands and contribute to the greenhouse effect.
Step-by-Step Solution:
1) List candidate gases and recall their IR activity.2) Identify N2 as a homonuclear diatomic with IR-inactive fundamental vibrations.3) Recognize CO2/CH4/N2O/O3 as established GHGs.4) Select N2 as the non-greenhouse gas in this set.Verification / Alternative check:Atmospheric spectroscopy data and climate texts consistently classify N2 (and O2) as non-GHG for IR absorption; any greenhouse influence is indirect (e.g., pressure broadening), not primary absorption.
Why Other Options Are Wrong:
CO2: strong 15 μm band and others; key anthropogenic GHG.CH4: potent GHG with absorption near 7.6 μm and others.N2O: long-lived GHG with strong IR bands.O3: absorbs in IR and UV; contributes to greenhouse effect.Common Pitfalls:Assuming abundance alone (N2) implies greenhouse effect; confusing UV absorption (O3) with lack of IR activity—ozone does both.
Final Answer:Nitrogen (N2)
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