Entropy Calculators
0 calculators tagged with “Entropy”
All Calculators
No calculators found for this topic.
Thermodynamic Entropy
Boltzmann equation: S = k_B × ln(W)
k_B = 1.38 × 10⁻²³ J/K (Boltzmann constant); W = number of possible microstates. More microstates = higher entropy = more disorder. Example: 1 mol of gas has astronomically more microstates than the same gas in a crystal → S_gas >> S_crystal.
Entropy change: ΔS = q_rev/T (at constant temperature for reversible processes). Units: J/K or J/(mol·K).
Second Law of Thermodynamics
ΔS_universe = ΔS_system + ΔS_surroundings ≥ 0 for any process. Spontaneous processes increase total entropy. Reversible processes: ΔS_universe = 0. Irreversible (real) processes: ΔS_universe > 0. This explains the arrow of time — why heat flows from hot to cold, why gases expand, why ice melts above 0°C.
Shannon Entropy
H = −Σ pᵢ × log₂(pᵢ)
pᵢ = probability of outcome i. Units: bits (log₂). Maximum H when all outcomes are equally probable. Used in: ecology (Shannon diversity index, log base e); information theory (compression, communication channel capacity); genomics (nucleotide diversity, codon usage).
Entropy in Biology
Living organisms decrease local entropy (build order) at the expense of increasing environmental entropy (releasing heat, CO₂, metabolic waste). Net ΔS_universe still increases. Protein folding: apparently decreases entropy of the polypeptide chain but releases water molecules from the hydration shell (+entropy gain from water) → net ΔS_universe > 0.
Glossary
Frequently Asked Questions
Entropy (S) measures the disorder or number of accessible microstates of a system (Boltzmann: S = k_B ln W). The second law of thermodynamics states that the entropy of the universe (system + surroundings) always increases or stays constant in spontaneous processes: ΔS_universe ≥ 0. It never spontaneously decreases in isolated systems. This explains why heat flows from hot to cold (increases S), gases expand (more microstates available), and ice melts above 0°C — all increase total entropy.
ΔS_reaction = Σ S°(products) − Σ S°(reactants). Processes that increase entropy: gas formation from liquids or solids (more microstates); dissolving a solid in solvent; increasing the number of moles of gas; heating. Processes that decrease entropy: gas condensing to liquid; crystallization; highly ordered products from disordered reactants. Standard molar entropies (S°) at 298 K are tabulated in Appendix tables. ΔS alone does not determine spontaneity — ΔG = ΔH − TΔS must be < 0 for a spontaneous process.
Shannon entropy H' = −Σ pᵢ ln(pᵢ) (using natural log) is used as the Shannon-Wiener diversity index in ecology, where pᵢ is the relative abundance of species i. H' increases with more species and greater evenness. This is mathematically analogous to information-theoretic entropy — a community where all species are equally rare (equiprobable) has maximum uncertainty (entropy) about which species an individual belongs to. Converting H' to the Hill number exp(H') gives the 'effective number of species' with intuitive species-count units.
Living organisms are open systems that decrease local entropy (build ordered structures like proteins, DNA, and cells) by importing low-entropy energy (food, sunlight) and exporting high-entropy products (heat, CO₂, water, metabolic waste). The total entropy of the universe still increases: the entropy decrease within the organism is more than offset by entropy increase in its surroundings. A cell builds proteins (decreasing entropy) by coupling to ATP hydrolysis (releasing heat and entropy to the surroundings). Net ΔS_universe > 0 — the second law is never violated. This is Schrödinger's concept of life feeding on 'negative entropy' (negentropy).