IBCH4 definitions

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14 Terms

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thermodynamics

  • law of cons. of energy → E can be converted from 1 form to another but not destroyed/created (total E remains constant)

  • heat (Q) in (J) → form of thermal E, transferred between objects because of temp. diff. 

    • conduction, convection, radiation

  • temp. (T) in (K) → measure of avg. kinetic energy of particles

    • how much heat has been transferred → measured by temp. change

  • heat capacity (c) in (J/kg K) → amt. of E needed to raise temp. of substance by 1 degree

    • specific heat capacity → amt. of heat E needed for 1 unit of mass of substance to cause inc. of one unit in temp.

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open/closed/isolated systems

  • open → allows transfer of heat/matter in/out of system

  • closed → allows transfer of only heat 

  • isolated → doesn’t allow transfer of heat/matter

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endo/exo

  • exothermic reaction gives out heat, warming mixture (heat lost to surroundings) (ΔH<0)

  • endothermic reaction takes in heat, cooling mixture (heat gained from surroundings) (ΔH>0)

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standard enthalpy change of combustion/formation

  • standard enthalpy change of combustion (∆Hc) is heat E released when 1 mol of pure substance is completely burnt in excess O2 under standard conditions

  • standard enthalpy change of formation (∆Hf) is heat change at constant production of 1 mol of pure substance from its elements in standard states under standard conditions

  • can see these values in data booklet + when writing reaction equation can use fractions

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measurement uncertainty in calorimetry

  • heat transfer due to calorimeter not being 100% insulated

  • reactions rarely immediate → heat lost while reaction takes place

  • heat absorbed by calorimeter (e.g. can)

  • standard heat capacity not exactly same for sol. and water

  • experiment not under standard conditions

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fossil fuels

  • crude oil → HC + sulfur, nitrogen etc, refined to petroleum etc

  • coal → combustible sedimentary rock with high amt. C, HC

  • natural gas → naturally occurring mixture of gaseous HC (mainly methane, little bit of other higher alkanes)

  • cheap/efficient, found in large amounts, reliable, infrastructure exists alr

  • non-renewable, produces GG → global warming, pollution (NOx, SOx), isn’t found everywhere

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biofuel

  • = fuel produced over short timespan from biomass (renewable E source)

  • biological carbon fixation → production of organic compounds from CO2 (photosynthesis)

  • bioethanol → ethanol produced by fermentation of glucose/biomass, used as fuel/fuel additive

  • biodiesel → produced in transesterification reaction

  • renewable, reduced GG, sustainable (many plant mats+waste can be used), economic security (reduced dependency on imported oil)

  • high cost, possible deforestation as demand inc., monoculture may result in reduced biodiversity, food products diverted to produce biofuel, use of agricultural land/water/fertiliser/pesticides for growing crops

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specific energy

  • = amt of heat E released per mass of fuel (kJ/kg) (enthalpy/molar mass)

  • larger HC → lower volatility bc stronger dispersion forces

    • affects how HC interact with oxygen + type of combustion 

    • longer HC chain → greater tendency of fuel to undergo incomplete combustion, which releases poisonous CO and produces less specific E when compared to same HC’s complete combustion

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collision theory

chem. reaction only occurs when → collisions between molecules have enough E to break bonds in reagents, molecules collide w/ proper orientation, new bonds form

  • change in concentration (c) or amount (n) of reactant/product with time (t)

    • r/v = ∆/c∆t (absolute value) in  mol/dm3 s

    • if half mass → half volume produced

    • if less V but same c → slower but reaches same volume

  • avg rate measures over particular time interval (usually slower)

  • instantaneous rate measures at particular time from gradient (e.g. initial, 10hr…)

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factors affecting RoR

  • concentration / mixing

    • mixing or inc. c inc. freq. of collisions between particles → greater RoR 

  • pressure

    • inc. pressure forces particles closer tog. → inc. collision rate → inc. RoR (only gases)

  • temperature

    • inc. in temp. → inc. velocity of particles → greater Ek → more collisions → greater RoR

  • catalyst (= inc. RoR but remains chemically unused at end of reaction)

    • provide alt. pathway for reaction w/ lower Ea

      • temp. has no effect on Ea. slower tend to have greater Ea

  • light

    • VIS/UV radiation breaks bonds in reactant molecules (some rates can be inc.)

    • silver halides…are photosensitive + undergo partial decomp. in light

  • particle size

    • dec. size inc. SA of solid substance → more freq. collisions → greater RoR

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dynamic equilibrium + equilibrium constant

  • only in closed systems!

  • macroscopic properties don’t change → amt./concentrations/densities of reactants/products same

  • at microscopic lvl → particles continue to take part in forward/reverse reaction (rates of these equal)

  • aA + bB ⇌ cC + dD

  • Kc (equilibrium constant) expression  = [C]^c[D]^d/[A]^a[B]^b is constant at given temp. 

    • [] = concentration

    • only for homogeneous equilibrium!

    • if Kc<1 → equilibrium at reactant’s side (more reactants)

    • if Kc=1 → equal amt. of reactants/products

    • if Kc>1 → equilibrium at product’s side (more products)

  • deduce Kc equilibrium, use it to find expression for reactions w/ diff. coefficients

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le chatelier’s principle

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arrhenius + BL acids/bases

Arrhenius acids and bases:

  • acid → any species that inc. concentration of hydrogen ions/protons in (aq) sol.

  • base → any species that inc. concentration of hydroxide ions in (aq) sol.

  • doesn’t take into account reactions w/o water

Bronsted-Lowry acids and bases

  • acid → any species capable of donating a proton

  • base → any species capable of accepting a proton

  • conjugate acid of BL base → species formed after base accepts a proton

  • conjugate base of BL acid → species formed after acids donates a proton

    • e.g. NH3 + H2ONH4+ OH⁻ 

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strong/weak acids/bases

  • strong acids/bases dissociate/ionise completely (irreversible)

    • result in weak conjugate bases/acids

    • strong acids → HCl, HNO3, H2SO4 (diprotic acid, donates 2H), HI (hydroiodic), HBr (hydrobromic)

    • strong bases → group 1 hydroxides e.g. NaOH, KOH

  • weak acids/bases dissociate/ionise partially (equilibrium)

    • result in stronger conjugate bases/acids

    • weak acids → organic acids, salicylic acid, ethanoic acid

    • weak bases → NH3 (ammonia), amines e.g. aminoethane, CO22- (carbonates), HCO3- (hydrogen carbonates)

  • if dissociation not complete → less OH ions produced

    • check pH, conductivity, amt. of H3O ions produced to distinguish strong/weak