Chapter 2 Notes: Small Molecules and the Chemistry of Life
2.1 An Element’s Atomic Structure Determines Its Properties
All matter is composed of atoms; atoms are extremely small (more than a trillion, i.e., , could fit in the period at the end of this sentence).
Atoms have volume and mass; mass measures how much matter is present; greater mass = greater quantity of matter.
Atoms carry electric charges: - Protons are positively charged ().
Electrons are negatively charged ().
Neutrons are electrically neutral (0).
Atom structure:- A dense, positively charged nucleus contains protons and neutrons.
Electrons orbit the nucleus in regions of space called electron shells or orbitals.
The Bohr model depicts electrons moving in set distances from the nucleus; the nucleus is far smaller in diameter than the entire atom.
Mass unit: the dalton (Da), named after John Dalton. A single proton or neutron has a mass of about Da.- Proton/neutron mass Da.
Electron mass is negligible by comparison; commonly cited as about g, roughly Da.
Because electron mass is so small, atoms’ overall mass is mostly from protons and neutrons in the nucleus.
Electric charges govern bonding:- An electron has a charge of ; a proton has a charge of ; neutrons have charge 0.
Opposite charges attract; like charges repel.
Atoms are electrically neutral overall because the number of electrons typically equals the number of protons.
Element = a fundamental substance that contains only one kind of atom.- Examples: hydrogen (H), iron (Fe), etc.
The properties of an element (physical and chemical) depend on the numbers of subatomic particles within its atoms.
Natural elements and abundance:- There are more than 100 elements; 92 occur naturally (elements with ).
About 98% of the tissue of living organisms (excluding bones) is made of six elements: Carbon (C), Hydrogen (H), Nitrogen (N), Oxygen (O), Phosphorus (P), Sulfur (S).
Elemental distribution differs between living systems and the Earth:
Oxygen: ~65% of the human body (excluding bones) vs. 21% of Earth’s atmosphere and 46% of Earth’s crust.
Carbon: ~18% of the human body vs. <1% of Earth’s atmosphere/crust.
Silicon: <0.01% of the human body; absent from atmosphere; ~28% of Earth’s crust.
These differences illustrate the selectivity with which life extracts elements from the environment.
Atomic number (Z): the number of protons in the nucleus; unique to each element.- Example: Helium has (two protons); Oxygen has (eight protons).
The atomic number helps organize elements in a periodic table by similar chemical properties.
Mass number (): total number of protons and neutrons in the nucleus; isotopes differ in (neutron number) but share the same (protons).- Isotopes exist for many elements; e.g., hydrogen isotopes: , (deuterium), (tritium).
For carbon: (6 protons, 6 neutrons), (6 protons, 7 neutrons), (6 protons, 8 neutrons).
Common abundances: most carbon is ; ~1.1% is ; a tiny fraction is .
Printing symbol conventions:- Elements are often printed with the atomic number at the lower left and the mass number at the upper left: e.g., , , .
Isotopes and utilities:- Isotopes have the same chemical reactivity; they can be used as tracers in biological experiments (e.g., radioisotopes) or for isotope analysis.
Atomic weight (relative atomic mass): the average mass per atom of an element relative to the mass of a carbon-12 atom:- Defined as a dimensionless ratio (no units).
Example: Hydrogen atomic weight
Because natural isotopic abundances vary, atomic weights are sometimes listed as ranges (e.g., H: ).
Radioactivity and isotopes:- Most isotopes are stable; some are radioisotopes and decay by emitting , , or radiation.
Radioactive decay can change the number of protons, sometimes transforming the element itself (especially for Z>92).
Radioisotopes are useful as labels/tags to track molecules in experiments or in the body (e.g., imaging and tracing pathways).
Example: tagging brain activity with radioactively labeled glucose (Figure 2.4) showing different activity regions.
Radioisotopes also aid in studying biochemical pathways and dating fossils (Key Concept connections: biochemical pathways and fossil dating).
Although useful, radioisotopes can damage molecules and cells; the benefits (e.g., cancer therapy with or ) must be balanced against risks.
Applications include clinical medicine, research tracing, and forensic/isotope analysis.
Isotope measurements and real-world applications:- Isotope ratios (e.g., ) can identify the origin of biological samples (e.g., beef sources in Big Macs) and track geographic sources of water and plants.
Big Mac isotope study: different cattle feed leads to varying ratios in patties across countries, indicating local vs. common beef sources.
Mass spectrometry is a key instrument for isotope analysis; future directions include climate studies via isotopes in precipitation and hair analysis for geographic tracing.
The role of electrons in bonding and molecular geometry:- Electron arrangement determines how atoms bond and shape molecules.
The location of an electron at any instant is described as an orbital; orbitals have characteristic shapes and orientations.
An orbital can hold a maximum of two electrons.
For atoms heavier than helium, electrons occupy multiple orbitals organized into electron shells (energy levels).
First shell (innermost): holds up to 2 electrons (e.g., H: ; He: ).
Second shell: can hold up to 8 electrons (4 orbitals).
Subsequent shells: more than two electrons; farther shells have higher energy.
Valence shell and chemical behavior:- The outermost shell (valence shell) determines chemical behavior and bonding.
Atoms with unpaired electrons in the valence shell are reactive; those with completely filled valence shells tend to be inert (e.g., He, Ne, Ar).
Atoms tend to complete their outer shells to achieve the octet rule (8 electrons in the outer shell).
Hydrogen is an exception: it is stable with 2 electrons in its first (and only) shell.
2.2 Atoms Bond to Form Molecules
Types of chemical bonds and interactions (Table 2.1):- Covalent bond: sharing of electron pairs; bond energy
Ionic bond: attraction between opposite charges; bond energy
Hydrogen bond: attraction between a covalently bonded hydrogen and an electronegative atom; bond energy
Hydrophobic interaction: association of nonpolar substances in water; bond energy
van der Waals forces: transient nonpolar interactions; bond energy
Covalent bonds and molecule formation:- A covalent bond forms when two atoms attain stable outer electron configurations by sharing one or more electron pairs.
In a covalent bond, each atom contributes one electron to each shared pair.
Example: two hydrogen atoms form H–H by sharing their unpaired electrons.
A molecule is a pure substance composed of two or more atoms bonded in a fixed ratio.
Molecular weight and examples:- The molecular weight of a molecule equals the sum of the atomic weights of its constituent atoms (e.g., water, , has molecular weight ).
Methane, , forms when carbon shares with four hydrogens; carbon can form up to four covalent bonds due to four unpaired valence electrons.
Covalent bonding capabilities (Table 2.2):- H: 1 covalent bond
O: 2
S: 2
N: 3
C: 4
P: 5
Bond geometry and orientation:- Bond lengths for a given pair of elements are constant.
Bond angles around atoms are generally consistent across molecules (e.g., carbon in methane adopts a tetrahedral geometry with H–C–H angles ).
Three-dimensional geometry influences biological function.
Bond rotation and molecular flexibility:- A single covalent bond acts as an axle; around it, the bonded atoms and their substituents can rotate, giving rise to many possible conformations and functions.
Multiple bonds:- Single bond: one shared electron pair (e.g., H–H, C–H).
Double bond: two shared electron pairs (e.g., C=C).
Triple bond: three shared electron pairs (e.g., NN); these are stronger and have higher bond energies than single bonds.
Electronegativity and bond polarity:- Electronegativity measures an atom’s tendency to attract electrons in a bond.
Follows a rough trend: O (3.5), Cl (3.1), N (3.0), C (2.5), P (2.1), H (2.1), Na (0.9), K (0.8).
When electronegativity difference is small (), bonds are nonpolar covalent (e.g., O=O, H–H).
When there is a larger difference, bonds are polar covalent (electrons are drawn more toward the more electronegative atom); e.g., in H2O the electrons are drawn toward O, creating partial charges ( on O and on H).
Polar covalent bonds lead to polar molecules or polar regions within large molecules, affecting interactions with other polar molecules.
Ionic bonds and dissolution in water:- If one atom is much more electronegative, electrons can transfer completely, forming ions (cations and anions).
Example: Na (electronegativity ) donates an electron to Cl (electronegativity ), producing Na and Cl.
Ions form stable outer electron shells and can form salts (e.g., NaCl).
In water, ions become hydrated: water molecules surround and stabilize ions via dipole interactions, separating them and reducing electrostatic attraction between ions.
Hydrogen bonding and intermolecular interactions:- Hydrogen bonds occur when a partially positive hydrogen atom (attached to an electronegative atom in one molecule) is attracted to a lone pair on an electronegative atom in another molecule (or the same molecule).
Hydrogen bonds are weaker than covalent bonds but can be numerous; collectively, they strongly influence structure (e.g., DNA, proteins).
Hydrophobic interactions and van der Waals forces:- Hydrophobic interactions drive nonpolar molecules to aggregate in aqueous environments, forming micelles or protein cores.
Van der Waals forces are weak, transient attractions between nonpolar molecules that arise from momentary dipoles; they become significant cumulatively in large molecules and can contribute to enzyme–substrate interactions.
Key Concept 2.1 Recap and Assess:- Some atoms form strong covalent bonds by sharing electron pairs.
Unequal sharing leads to polarity (electronegativity differences).
Other atoms become ions via electron transfer, forming ionic bonds.
Weak forces (hydrogen bonds, van der Waals) attract atoms within or between molecules.
Bonding is dynamic; life involves continual molecular changes.
2.3 Chemical Reactions Transform Substances
Life is dynamic; atoms within molecules can break and form new bonds as they collide with sufficient energy.
Chemical reactions involve change in the bonding partners while obeying conservation of energy and matter.
Example: Combustion of propane in oxygen:-
Balanced equation:Redox (oxidation-reduction) reactions:- In redox, electron transfer occurs between species.
Oxidizing agent gains electrons (is reduced); reducing agent loses electrons (is oxidized).
Example in propane combustion: propane acts as reducing agent (loses electrons); oxygen is the oxidizing agent (gains electrons to form water).
Reactants vs. products:- The totals of each element are conserved; in a balanced equation, the number of carbon, hydrogen, and oxygen atoms on the left equals those on the right.
Reactions may release energy (exothermic) or require energy input (endothermic).
Energy and chemical change:- Energy is the capacity to do work; chemical reactions transform energy from bonds in reactants to products (some energy released as heat/light).
Relevance to biology:- Cellular reactions involve many intermediate steps to harvest and channel energy.
Key Concept 2.3 Recap and Assess:- Reactants are converted to products with different chemical compositions.
Bond breaking and forming governs the reaction; energy release or input is common.
The same fundamental chemistry underpins metabolic pathways in life.
2.4 The Properties of Water Are Critical to the Chemistry of Life
Water is the solvent of life; biological reactions largely occur in aqueous environments.
Water’s unusual properties arise from polarity and hydrogen bonding:- Water is a polar molecule (H–O–H) with partial charges: on O and on H.
Ice vs. liquid water:- In ice, each water molecule forms hydrogen bonds with four others in a rigid lattice; the lattice is more open, making ice less dense than liquid water, so ice floats.
Floating ice insulates bodies of water, protecting aquatic life in cold climates.
Specific heat and heat of vaporization:- Water has a high specific heat due to many hydrogen bonds that must be broken to raise temperature.
Water has a high heat of vaporization; much energy is required to convert liquid water to gas, which provides a cooling effect during evaporation (e.g., sweating).
Environmental relevance:- Ocean heat absorption moderates climate and coastal temperatures; this helps stabilize ecosystems and climate).
Cohesion and adhesion:- Cohesion: water molecules form hydrogen bonds with each other, enabling vertical water transport in plants via capillary action (transpiration–cohesion–tension mechanism).
Adhesion: water molecules stick to other surfaces (e.g., the sides of a straw), aiding column ascent.
Surface tension:- Surface water is difficult to puncture due to hydrogen bonding at the surface; allows events like spiders walking on water.
Aqueous solutions and solubility:- Water dissolves many polar substances (solutes) because of its polarity; however, solutes retain their identities and can participate in reactions.
Qualitative and quantitative analysis in biochemistry:- Qualitative analyses identify substances and reaction steps.
Quantitative analyses measure concentrations of substances (e.g., amount of product formed).
Moles and Avogadro’s number:- A mole is the amount of substance whose mass in grams equals its molecular weight in atomic mass units.
One mole contains approximately molecules.
Examples:
1 mole of table sugar weighs about ; dissolving in water to make a 1 L solution yields a 1 M solution.
A 1 M solution contains , i.e., .
Acids and bases in water:- Acids release into solution; bases accept .
Examples:
Hydrochloric acid: (strong acid, fully ionizes).
Sulfuric acid: (strong acid, fully ionizes).
Acetic acid (weak acid): (partially ionizes).
Bases (strong vs weak):
Sodium hydroxide: (strong base, fully ionizes).
Bicarbonate: (base can accept H).
Ammonia: (weak base).
Acid–base reactions are often reversible:- Acetic acid example:
Reversibility depends on relative concentrations of reactants and products; the equilibrium can shift left or right.
Water as a weak acid and base:- Autoprotolysis of water:
The hydronium ion is effectively a proton bound to water: often represented as (simplified).
pH and acidity/basicity:- pH is the negative logarithm of the hydrogen ion concentration: .
Pure water has pH = 7 (neutral).
Strong acids (e.g., HCl) yield pH close to 0; strong bases (e.g., NaOH) yield pH close to 14.
Buffers stabilize pH by consuming or releasing H or OH~; example: carbonic acid/bicarbonate system in blood:
Buffers limit pH changes and are essential for maintaining homeostasis; they illustrate the law of mass action in reversible reactions.
Buffers in biology and medicine:- Biological buffering maintains internal constancy (homeostasis) of pH in tissues.
Stomach buffering can occur by ingesting bicarbonate () to relieve excess acidity.
Key Concept 2.4 Recap and Assess:- Water’s chemistry arises from hydrogen bonding and polarity; it supports life as a solvent and participant in reactions.
Aqueous solutions can be acidic or basic; buffers help maintain stable intracellular and extracellular pH.
Isotope analysis offers insights into evolutionary history, environmental sources, and climate processes.
Investigating LIFE and Real-World Connections
Isotope analysis applications mentioned in the transcript:- Dinosaur oxygen/isotope investigations and the Big Macs isotope study illustrate how isotope ratios reveal life history and origins.
Hair and body isotopes reflect geographic water sources and diet, useful in forensic and geographic tracing.
Mass spectrometry is a key analytical tool for detecting isotopes and analyzing isotope ratios.
Practical implications and cautions:- Although radioisotopes have beneficial uses in medicine and biology, ionizing radiation can damage biomolecules; risk-benefit considerations are critical (e.g., Co-60 and I-131 therapies).
Isotope analysis can inform ecological, forensic, and climate research and has future potential for understanding climate change through isotope tracking in precipitation and ecosystems.
Connections to Foundational Principles
Atomic structure and periodicity underpin chemical behavior:- Atomic number determines element identity and placement in the periodic table.
Electron configuration and valence shell determine bonding patterns and reactivity (octet rule, hydrogen exception).
Bonding types explain molecular properties and biological function:- Covalent bonds create stable molecules with defined geometries (e.g., tetrahedral carbon in methane).
Polarity and electronegativity differences drive molecular interactions in water and biological molecules.
Ionic bonds form salts and interact with polar solvents; hydration affects solubility and transport in organisms.
Hydrogen bonds and van der Waals forces shape large biomolecules like DNA and proteins, contributing to structure and function.
Water as a life-enabling medium:- Water’s polarity, cohesion/adhesion, high heat capacity, and surface tension enable transport in plants, climate regulation, and reliable biochemical environments in cells.
Chemical reactions as the engine of life:- Reactions transform matter and energy, support metabolism, and are governed by conservation laws and energy transfer across reaction steps.
Quantitative chemistry in biology:- Moles, Avogadro’s number, and molarity link molecular-scale events to measurable quantities in experiments and clinical applications.
Key Equations and Concepts (LaTeX)
Atomic weight definition (dimensionless):-
Avogadro’s number: -
Ideal gas or solute quantities (examples):- 1 mole of table sugar:
1 M solution:
Bonding and reaction examples:- Propane combustion (redox):
Polar covalent bonds and dipoles:- In water, polar covalent bonds lead to partial charges:
Autoprotolysis of water (acid-base chemistry):-
pH definition:-
Buffer equilibrium (carbonate system in blood):-
Highlights for Exam Preparation
2.1 An Element’s Atomic Structure Determines Its Properties
Subatomic Particles:
Protons: Positive charge (), in nucleus, determine atomic number ().
Electrons: Negative charge (), orbit nucleus in shells, negligible mass.
Neutrons: Neutral charge (0), in nucleus, contribute to mass number ().
Element Identity: Atomic number () is unique to each element (number of protons).
Isotopes: Atoms of the same element () but with different numbers of neutrons (), thus different mass numbers ().
Radioisotopes decay, useful as tracers but can be damaging.
Valence Shell: Outermost electron shell; determines an atom's chemical reactivity and bonding behavior.
Atoms tend to complete their valence shells (octet rule, 8 electrons; Hydrogen is stable with 2).
Essential Elements for Life: Carbon (C), Hydrogen (H), Nitrogen (N), Oxygen (O), Phosphorus (P), Sulfur (S) make up ~98% of living tissue.
2.2 Atoms Bond to Form Molecules
Chemical Bonds: Interactions that stabilize atoms by achieving stable electron configurations.
Covalent Bonds: Sharing of electron pairs between atoms.
Can be single, double, or triple bonds.
Electronegativity: Atom’s attraction for shared electrons.
Nonpolar Covalent: Small or no electronegativity difference (e.g., C–H, O=O).
Polar Covalent: Larger electronegativity difference, leading to partial charges ($\delta^+$ and $\delta^-$) (e.g., O–H in water).
Ionic Bonds: Complete transfer of electrons, forming ions (cations and anions) that attract each other (e.g., NaCl).
Hydrogen Bonds: Attraction between a partially positive hydrogen (bonded to an electronegative atom) and another electronegative atom with a lone pair. Weaker than covalent but collectively strong; crucial for biological structures (DNA, proteins).
Hydrophobic Interactions: Tendency of nonpolar molecules to aggregate in water.
Van der Waals Forces: Weak, transient attractions due to momentary dipoles in nonpolar molecules.
Molecular Geometry: Fixed bond lengths and angles give molecules specific 3D shapes, which are critical for biological function.
2.3 Chemical Reactions Transform Substances
Definition: Processes involving the breaking and forming of chemical bonds, converting reactants into products.
Conservation Laws: Matter and energy are conserved in chemical reactions.
Redox Reactions: Involve the transfer of electrons.
Oxidation: Loss of electrons.
Reduction: Gain of electrons.
Energy Changes: Reactions can be exothermic (release energy) or endothermic (require energy input).
2.4 The Properties of Water Are Critical to the Chemistry of Life
Polarity: Water ($\text{H}_2\text{O}$) is a polar molecule with partial negative charge on oxygen and partial positive charges on hydrogen, enabling extensive hydrogen bonding.
Key Properties due to Hydrogen Bonding:
Cohesion: Water molecules stick to each other.
Adhesion: Water molecules stick to other surfaces.
High Specific Heat: Absorbs/releases large amounts of heat with small temperature change.
High Heat of Vaporization: Requires much energy to evaporate, creating a cooling effect.
Ice Floats: Less dense than liquid water due to open, rigid hydrogen-bonded lattice; insulates aquatic environments.
Excellent Solvent: Dissolves many polar and ionic substances (hydrophilic).
Acids and Bases:
Acids: Release $\text{H}^+$ ions into solution.
Bases: Accept $\text{H}^+$ ions (or release $\text{OH}^-$).
pH Scale: Measures hydrogen ion concentration: $\text{pH} = -\log [\text{H}^+]$.
Neutral: pH 7 (e.g., pure water).
Acidic: pH < 7.
Basic (Alkaline): pH > 7.
Buffers: Systems that resist changes in pH by accepting or donating $\text{H}^+$ ions.
Crucial for maintaining homeostasis in biological systems (e.g., the carbonic acid/bicarbonate system in blood: $\text{HCO}3^- + \text{H}^+ \rightleftharpoons \text{H}2\text{CO}_3$).
Key Equations and Concepts
Avogadro’s number:
Molarity: (moles per liter).
Autoprotolysis of water (simplified):
pH Definition: