Atomic Number, Isotopes & Average Atomic Mass of Chlorine
Atomic Number (Z) – The Element’s Fingerprint
Definition: The count of protons in the nucleus of an atom.
Z = \text{number of protons}
Determines elemental identity:
Z=1 \Rightarrow \text{Hydrogen}
Z=6 \Rightarrow \text{Carbon}
Z=17 \Rightarrow \text{Chlorine}
Periodic-table convention:
Small, whole number above/beside the symbol (e.g., the circled numbers the narrator refers to).
Connection to previous lecture: Earlier videos established that changing Z changes the element entirely (e.g., adding a proton to carbon turns it into nitrogen).
Mass Number (A) – Counts Nucleons
A = Z + N where N = neutrons.
Written in isotope notation at the upper-left of the element symbol: ^{A}{Z}\text{Cl}, ^{35}{17}\text{Cl}, etc.
Represents the total of massive nuclear particles; electrons are excluded because their mass is (<10^{-3}) of a nucleon and usually neglected for atomic-mass discussions.
Isotopes – Multiple Versions of the Same Element
Definition: Atoms with identical Z (protons) but differing N (neutrons).
Significance:
Chemically similar (same electron configuration when neutral) because chemistry is governed by proton count/electron structure.
Differ in mass, affecting density, diffusion rates, and nuclear stability.
Two stable chlorine isotopes discussed:
Chlorine-35
Notation: ^{35}_{17}\text{Cl} or “Cl-35.”
Z = 17 ⇒ Chlorine.
A = 35 ⇒ N = 35-17 = 18 neutrons.
Chlorine-37
Notation: ^{37}_{17}\text{Cl} or “Cl-37.”
Z = 17.
A = 37 ⇒ N = 37-17 = 20 neutrons.
Key take-away: Same Z (chlorine identity), different N (18 vs 20) ⇒ distinct isotopes.
Atomic Mass vs. Mass Number
Mass Number (A) is an integer count of nucleons.
Atomic Mass (m) is a measured mass expressed in unified atomic mass units (u, also “amu”).
1 u ≈ mass of a single ^{12}\text{C}/12 atom.
Protons & neutrons ≈ 1 u each, but not exactly.
Why m ≠ A exactly:
Individual proton mass \neq 1.000\text{ u}; same for neutrons.
Mass defect: When nucleons bind, the system’s mass drops (energy released, E = \Delta m c^2).
Example: Cl-35’s actual atomic mass is slightly below 35 u.
Natural Abundance & Weighted Average Atomic Mass
Periodic-table “35.45” for chlorine is not any single isotope’s mass; it’s a weighted mean.
Given natural abundances:
Cl-35: 75.77\% = 0.7577 fraction.
Cl-37: 24.23\% = 0.2423 fraction.
Formula:
\bar m{\text{element}} = \sumi wi\, mi
where $wi$ = fractional abundance, $mi$ = isotopic atomic mass.Chlorine example (symbols explained inline):
\bar m{\text{Cl}} = (0.7577)(m{\text{Cl-35}}) + (0.2423)(m_{\text{Cl-37}}) \approx 35.45\ \text{u}Practical use: Chemists use this average for molar-mass calculations (e.g., grams-per-mole numerics in stoichiometry).
Mass Defect ((\Delta m)) – Brief Mention
Combined nucleus mass is less than sum of isolated nucleons:
\Delta m = \big(Z mp + N mn\big) - m_{\text{nucleus}} \gt 0Significance: The “missing mass” is binding-energy credit, foundational for nuclear physics and applications (e.g., fission, fusion).
Linked concept: Even stable isotopes (Cl-35, Cl-37) exhibit a measurable mass defect despite chemical stability.
Key Take-Home Bullet List
Element identity = proton count (atomic number).
Isotopes: same Z, different N ⇒ different mass numbers.
Chlorine’s two stable isotopes: Cl-35 (18 n), Cl-37 (20 n).
Periodic table lists average atomic mass, not mass number.
Weighted average uses natural abundance: 35.45 u for chlorine.
Atomic mass slightly deviates from integer values due to nucleon mass differences and mass defect.
For routine chemistry, electrons’ mass is negligible in atomic-mass calculations.