ch 9 - Solutions Flashcards

1
Q

solutions

A

homogeneous throughout - same phase. All of them are mixtures but not all mixtures are solutions

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2
Q

solute

A

dissolved or dispersed in a solvent

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3
Q

solvent

A

component of solution that remains in the same phase after mixing, in which solute is dissolved; if already in same phase as solute, the solvent is that which is present in greater quantity

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4
Q

Solvation

A

the electrostatic interaction between solute and solvent molecules; also called dissolution; when water is solvent called hydration

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5
Q

when solvation is exothermic

A

when new interactions between molecules are stronger than the original ones; favored at low temps

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6
Q

when solvation is endothermic

A

when the new interactions formed are weaker than the original ones; favored at high temps; most dissolutions are this

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7
Q

ideal solution

A

enthalpy of dissolution is equal to zero; solutions get close to this when overall strength of new interactions is approximately equal to overall strength of original interactions

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8
Q

entropy of dissolution

A

second property (along with enthalpy) that contributes to whether a dissolution is spontaneous or not - at constant temp and pressure, entropy always increases upon dissolution

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9
Q

solubility of a substance

A

the max amount of that substance that can be dissolved in a particular solvent at a given temp

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10
Q

saturated solution

A

when the max amount of solute has been added and the dissolved solute is in equilibrium with its undissolved state

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11
Q

if more solute is added to an already saturated solution

A

solute will not dissolve but precipitate to the bottom

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12
Q

dilute solution

A

solution in which proportion of solute to solvent is small ; still unsaturated

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13
Q

concentrated solution

A

solution in which proportion of solute to solvent is large; still unsaturated

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14
Q

when is a solute considered soluble

A

when Gibbs free energy is negative and reaction will proceed spontaneously

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15
Q

sparingly soluble salts

A

those solutes that dissolve minimally in a solvent (molar solubility under 0.1 M)

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16
Q

aqueous solution

A

solvent is water

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17
Q

hydronium ion

A

H3O+

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18
Q

solubility rules for aqueous solutions (know rules one and two)

A
  1. All salts containing ammonium (NH4)+ and alkali metal (group 1) cations are water-soluble; 2. all salts containing nitrate (NO3)- and acetate (CH3COO-) anions are water-soluble; 3. Halides (Cl-, Br-, I-) except fluorides, are water soluble except those formed with Ag+, Pb2+, and (Hg2)2+; 4. All salts of sulfate ion (SO4)2- are water soluble, except those formed with Ca2+, Sr2+, Ba2+, and Pb2+; 5. all metal oxides are insoluble except ones formed with alkali metals, ammonium, and CaO, SrO, and BaO; 6. all hydroxides are insoluble except ones formed with alkali metals, ammonium, and Ca2+, Sr2+, and Ba2+; 7. all carbonates (CO3)2+, phosphates (PO4)3-, sulfides S2-, and sulfites (SO3)2- are insoluble except ones formed with alkali metals and ammonium
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19
Q

complex ion - or coordination compound

A

refers to a molecule in which a cation is bonded to at least one electron pair donor (which could include the water molecule) [complexation reactions]

20
Q

ligands

A

electron pair donor molecules

21
Q

coordinate covalent bonds

A

bonds that hold complexes together, in which an electron pair donor (a Lewis base) and an electron pair acceptor (a Lewis acid) form very stable Lewis acid-base adducts

22
Q

chelation

A

central cation of a complex is bonded to the same ligand in multiple places; usually requires large organic ligands that can double back to form second or third bond with the central cation

23
Q

concentration

A

denotes the amount of solute dissolved in a solvent

24
Q

percent composition by mass

A

mass of solute/mass of solution x 100

25
Q

mole fraction (X)

A

XsubA = moles of A/total moles of all species; used to calculate the vapor pressure depression of a solution

26
Q

molarity (M)

A

M = moles of solute/liters of solution

27
Q

molality (m)

A

m = moles of solute/kilograms of solvent; for dilute aqueous solutions at 25 degrees C, the molality is approx equal to molarity because the density of water at this temp is 1 kg per L. situations where it is required are boiling point elevation and freezing point depression

28
Q

normality (N)

A

equal to the number of equivalents of interest per liter of solution; equivalent is measure of the reactive capacity of a molecule (equal to a mole of the species of interest); how many moles of electrons an ion will accept in a certain solution

29
Q

equation for concentration of solution after dilution

A

M sub i (V sub i) = M sub f (V sub f); M = molarity, V = volume and subscripts i and f = initial and final values

30
Q

saturation point

A

in process of creating a solution, this is the equilibrium, where the solute concentration is at its max value for the given temp and pressure; rates of dissolution and precipitation are equal, and concentration of dissolved solute reaches a steady state (constant) value; neither is favored thermodynamically

31
Q

reaction example that represents dissociation of such a solute in solution

A

A sub m (B sub m) ->

32
Q

solubility product constant (K sub sp) for example formula A sub m B sub n

A

K sub sp = [A^(n+)]^m[B^(m-)]^n; where concentrations of ionic constituents are equilibrium (saturation) concentrations

33
Q

Ion product (IP)

A

used to determine where the system is with respect to the equilibrium position; analogous to the reaction quotient, Q, for other chemical reactions: IP = [A^(n+)]^m[B^(m-)]^n; concentrations used here are the ionic constituents at that given moment in time, which may differ from equilibrium concentration

34
Q

unsaturated solution

A

if a salt’s IP is less than the salt’s Ksp; dissolution is thermodynamically favored over precipitation

35
Q

supersaturated solution

A

IP is greater than Ksp, solution is beyond equilibrium; thermodynamically unstable and any addition or further cooling will cause spontaneous precipitation (achieved by dissolving more solute and then cooling solution)

36
Q

molar solubility

A

molarity of a solute in a saturated solution

37
Q

common ion effect

A

the reduction in molar solubility that occurs to solubility of salt when it is dissolved in a solution that already contains one of its constituent ions

38
Q

colligative properties

A

physical properties of solutions that are dependent on the concentration of dissolved particles but not on the chemical identity of the dissolved particles: vapor pressure depression, boiling point elevation, freezing point depression, osmotic pressure

39
Q

Raoult’s law

A

accounts for vapor pressure depression caused by solutes in solution; as solute is added to a solvent, vapor pressure of the solvent decreases proportionately: P sub A = X sub A x P, degree sign, sub A; P sub A = vapor pressure of solvent A when solutes are present; X sub A = mole fraction of the solvent A in the solution; P, degree sign, sub A = vapor pressure of solvent A in its pure state

40
Q

formula for which the boiling point of a solution is raised relative to that of the pure solvent

A

delta T sub b = iK sub b (m); delta T sub b = increase in boiling point; i = van’t Hoff factor; K sub b = proportionality constant characteristic of a particular solvent; m = molality of the solution

41
Q

boiling point

A

temperature at which the vapor pressure of the liquid equals the ambient (incident) pressure; higher in solutions than pure solvents

42
Q

Van’t Hoff factor

A

corresponds to the number of particles into which a compound dissociates in solution

43
Q

causes of freezing point depression

A

presence of solute particles interferes with formation of lattice arrangement of solvent molecules associated with the solid state causing a need for a greater amount of energy to

44
Q

formula for freezing point depression

A

delta T sub f = i(K sub f)m; delta T sub f = freezing point depression; i = van’t Hoff factor; K sub f = proportionality constant characteristic of a particular solvent; m = molality of solution

45
Q

osmotic pressure

A

refers to a “sucking” pressure generated by solutions in which water is drawn into a solution: pi symbol = iMRT; where pi = osmotic pressure; i = van’t Hoff’s factor; M = molarity of the solution; R = ideal gas constant; T = temp

46
Q

boiling point of water

A

100 C; 212 F, 273.2 K

47
Q

ideal solutions

A

solutions that obey Raoult’s law which holds only when the attraction between the molecules of the different components of the mixture is equal to the attraction between the molecules of any one component in its pure state.