Aha! Chemistry with Prof Bob
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    • Chapter 02 Stuff, matter: What is it? >
      • 0200 Stuff, matter: A theory of atoms
      • 0201 Atoms: The building blocks of all stuff
      • 0202 People classifying stuffs. Why?
    • Chapter 05 Chemical reactions, chemical equations >
      • 0500 Chemical reactions vs. chemical equations. Overview
      • 0501 Chemical amount and its unit of measurement, mole
      • 0502 The Avogadro constant: How many is that?
      • 0503 The Avogadro constant: Why is it that number?
      • 0504 Chemical formulas: What can they tell us??
      • 0505 Chemical equations: What can they tell us?
      • 0506 Limiting reactants: How much reaction can happen?
      • 0507 Balanced chemical equations: What are they?
      • 0508 Chemical reactions as competitions
    • Chapter 09 Aqueous solutions >
      • 0901 What is a solution? And what is not?
      • 0902 Miscibility of liquids in each other
      • 0903 Like dissolves like? Shades of grey
      • 0905 Dissolution of ionic salts in water: A competition
      • 0906 Can we predict solubilities of salts?
      • 0907 Solution concentration
      • 0908 Chemical species, speciation in aqueous solution
      • 0909 Solutes: Electrolytes or non-electrolytes?
      • 0910 Electrolytes - strong or weak?
      • 0911 Concentrated, dilute, strong, weak
      • 0912 Species concentration vs. solution concentration
      • 0913 Weak electrolytes: Getting quantitative
    • Chapter 11: Dynamic chemical equilibrium >
      • 1100 Dynamic chemical equilibrium: Overview
      • 1101 Visualising dynamic chemical equilibrium
      • 1102 The jargon of chemical equilibrium
      • 1103 Equilibrium constants: The law of equilibrium
      • 1104 The law of equilibrium: an analogy
    • Chapter 22 Spectroscopy >
      • 2200 Spectroscopy: Overview and preview
      • 2201 Quantisation of forms of energy
      • 2202 Light: Wave-particle "duality"
      • 2203 Ultraviolet-visible spectroscopy
      • 2204 Beer’s law: How much light is transmitted?
    • Chapter 27 The greenhouse effect, climate change >
      • 2700 The greenhouse effect: overview
      • 2701 Is Earth in energy balance?
      • 2702 CO2 in the atmosphere before 1800
      • 2703 So little CO2! Pffft?
      • 2704 Does CO2 affect Earth's energy balance?
      • 2705 The "greenhouse effect"
      • 2706 Why does CO2 absorb radiation from Earth?
      • 2707 The "enhanced greenhouse effect"
      • 2708 Why doesn't CO2 absorb the radiation from the sun?
      • 2709 Why are N2 and O2 not greenhouse gases?
      • 2710 Doesn't water vapour absorb all the IR?
      • 2711 Carbon dioxide from our cars
      • 2712 The source of energy from combustion
      • 2713 Comparing fuels as energy sources
      • 2714 Methane: How does it compare as a GHG?
      • 2715 Different sorts of pollution of the atmosphere
      • 2716 "Acidification" of seawater
    • Chapter 27 Communicating chemistry >
      • 2700 Overview, preview
      • 2703 The jargon we use
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0906 Can we predict the solubilities of ionic salts?

4/2/2019

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Module 0906

Can we predict the solubilities of ionic salts?

Can we predict who will win the dissolution tug-o-war competition?

Energy used vs. energy recovered .....

But don't ignore entropy!


Rationalisation vs. prediction

​We are able to rationalise observations about the solubility (or miscibility) of molecular liquids in each other, in terms of competing "driving forces". This was the subject matter of Module 0902 Miscibility of liquids in each other. On the other hand, our ability to predict whether two particular liquids are miscible in each other is limited - See Module 0903 Like dissolves like? Shades of grey.
​
Similarly, we saw in Module 0905 Dissolution of ionic salts in water: a competition  that we can rationalise observed differences in the solubility of various solid ionic salts in water. But how well can predict the solubility of particular ionic salts in water?

That is the theme of this video .....
Aha! Aussie satisfies his curiosity, with some help from Prof Bob ..........
Picture

KEY IDEAS - Can we predict solubilities in water?

Picture
Prediction of the solubility of an ionic salt in water can be very unclear.
​In Module 0905 Dissolution of ionic salts in water, a model was proposed that the process of dissolving involves a competition for ions on the surface of a crystal in water between:
  1. forces of attraction to oppositely charged ions in the bulk of the crystal (resisting dissolution), and
  2. forces of attraction to the oppositely charged ends of water molecules (favouring dissolution).
​
If a salt is soluble in water, we can conclude that Type 2 forces dominate Type 1 forces.
If a salt is insoluble in water, we can conclude that Type 1 forces dominate Type 2 forces.


The two questions posed in here are:
  • What are the factors that govern which type of force dominates?
  • Can we predict from the formula of a salt the probability that it is soluble (or insoluble) in water?
​
First of all we need to recognise that in every situation, there is a “driving force” to increase entropy – in simple terms, that means for objects (like ions) to disperse among each other.

We have encountered this “driving force” of entropy before in Module 0902 Miscibility of liquids in each other.

Objects would always intermingle (for example, ions would disperse among water molecules) if there were no forces of attraction resisting that from happening.
​
But there are forces of attraction in the system that we are considering (an ionic crystal in water): (i) between the ions of opposite charge in the crystal, and (ii) between any ions on the surface of the crystal and the polar water molecules which can rotate to point their negative end toward positively charged ions (and their positive end toward negative ions).


Forces of attraction affect the energy (as distinct from the entropy) of a system:
  • To separate two objects of opposite charge requires energy input.
  • If those two objects are allowed to come together again, energy is recovered.
​
We can compare the energy inputs and gains when sodium chloride (NaCl) is dissolved in water, with those when magnesium chloride (MgCl2) dissolves in water.

The key factor is that a sodium ion has a +1 charge, and a magnesium ion has a +2 charge.

And the key relationship that describes the force of attraction between oppositely charged ions is 
​

Picture
where q1 and q2 are the charges on the ions, and d is the distance between them.
​
The dissolution of a salt can be theoretically considered as two steps (although obviously it doesn’t happen in this way):
1.     
Separation of the ions from each other into a vacuum: for example:
Picture
2.     Aquation (or hydration) of the isolated ions: for example:
Picture
The energy required for Step 1 is called the lattice energy of a salt. Consistent with the equation (1), the lattice ergy for magnesium chloride is much greater than that for sodium chloride:
​

Picture
This data is representative of the generalisation that the higher are the charges on the ions in salt, the higher is the lattice energy.

And so a reasonable conclusion is that the forces of attractions between ions in a magnesium chloride crystal resist dissolution more than do those forces in a sodium chloride.
​

But this cannot, on its own, allow us to predict relative solubilities.

Water is not a passive receiver of ions into its midst: it is an active participant in the dissolving process by aquating the ions.

Again, we could predict that the energy “recovered” during aquation is larger for magnesium ions (compared with sodium ions). This is borne out by comparison of energies of hydration of these ions:
​
Picture
So, magnesium ions “use up” more energy of lattice separation (than sodium ions), but also they “recover” more energy in the process of hydration/aquation. Is the lattice energy of MgCl2 so large that dissolution does not happen?

We cannot answer this question from the data at this level of explanation.

But the experimental observation that magnesium chloride is very soluble in water allows us to conclude that, again, water molecules “win” the competition.
 
It seems that the energy “recovered” by aquation is enough to overcome the resistance to dissolution due to the expenditure of the lattice energy – especially since hydration energy does not have to be greater than the lattice energy to allow the natural tendency to mix due to entropy to be expressed.
​

So what to do?

The more that we are familiar with the solubilities of substances through experience, the better we can function in chemistry.
 
There are lists of generalisations that can be made about relative solubilities of ionic solids.
 
Despite common practice, it does not make sense to call these “solubility rules”: They are not rules. the word “rule” implies that the observed solubility of sodium nitrate is due to a “rule” that all nitrates are soluble. Rubbish! Sodium nitrate does not dissolve to conform with the “rule”. It does what it does.

And we have reference lists that tell us what is the solubility of salts. Let's just look it up?

So, rationalisation (explanation) after an observation is much more straightforward than prediction before an observation. Perhaps you are a little dissatisfied that we cannot predict solubilities very well? Well that is just the way it is, and appreciation of that point is an important part of learning chemistry.

Perhaps you have been conditioned to chemistry lessons that have the answer at the end ..... Well this module is a little like that: it comes to a definite conclusion - that there are limitations on how well we can predict solubilities in advance of observation (or looking it up). Suck it up!
​
Post script 1

In this module, we have focused on the charges on the ions, and ignored the influence of their sizes. The smaller are ions, the shorter can be the distance between them and, consistent with equation (1), the stronger the force between them.

In general, the higher the charge on a positive ion, the smaller it is. Indeed the diameter of +2 magnesium ions (158 pm) is smaller than that of +1 sodium ions.(196 pm).

So based on size, we would again expect that magnesium ions are more strongly attracted to oppositely charged ions in the lattice, but also more strongly held by water molecules when aquated.

On these grounds, we are also unable to predict the net outcome (Who "wins" the competition?) and whether a salt is soluble or not.
​

​
Post script 2

I have referred in this module to lattice energy and energy of hydration (or aquation). These are commonly used terms, but we will see elsewhere that the technically correct terms (approved by IUPAC) are  lattice enthalpy and enthalpy of hydration.
​
​

Picture

SELF CHECK: Some thinking tasks

Picture
We may be be aware of the opposing forces, but unable to predict who will win. Got it? Check .....


​Q 1
.  Are the following statements correct or incorrect?
  1. The separation of ions in a crystal from each other (the energy of which is the lattice enthalpy) is an exothermic process.
  2. Aquation of postive ions is an exothermic process.
  3. Aquation of negative ions is an exothermic process.
  4. If the lattice energy of an ionic salt is larger than the energy of hydration of both ions, we can presume that the salt is insoluble.

Q 2.  The lattice energy of calcium phosphate, Ca3(PO4)2, is very large (10 600 kJ per mol).
  1. Explain why this is so.
  2. Does this mean that we can presume that calcium phosphate is insoluble in water?
​
Answers
Q 1.
  1. Incorrect
  2. Correct
  3. Correct
  4. Incorrect. No we cannot presume this: For the salt to be insoluble, the effect of the lattice energy must overcome the effects of both the energy of hydration and the entropy (both of which "encourage" dissolving).

Q 2.

  1. ​The ions have high electrostatic charges: calcium ions have +2 charge, and phosphate ions have +3 charge.
  2. No, because the factors which contribute to the high lattice energy of the solid (ie, high charges on the ions) also contribute to high energy of hydration - maybe cancelling out the resistance to dissolution due to the high lattice energy.
​
Picture

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  • HOME
  • NAVIGATION
    • Table of contents
    • Index
    • TALK WITH PROF BOB?
  • LEARNING MODULES
    • Chapter 02 Stuff, matter: What is it? >
      • 0200 Stuff, matter: A theory of atoms
      • 0201 Atoms: The building blocks of all stuff
      • 0202 People classifying stuffs. Why?
    • Chapter 05 Chemical reactions, chemical equations >
      • 0500 Chemical reactions vs. chemical equations. Overview
      • 0501 Chemical amount and its unit of measurement, mole
      • 0502 The Avogadro constant: How many is that?
      • 0503 The Avogadro constant: Why is it that number?
      • 0504 Chemical formulas: What can they tell us??
      • 0505 Chemical equations: What can they tell us?
      • 0506 Limiting reactants: How much reaction can happen?
      • 0507 Balanced chemical equations: What are they?
      • 0508 Chemical reactions as competitions
    • Chapter 09 Aqueous solutions >
      • 0901 What is a solution? And what is not?
      • 0902 Miscibility of liquids in each other
      • 0903 Like dissolves like? Shades of grey
      • 0905 Dissolution of ionic salts in water: A competition
      • 0906 Can we predict solubilities of salts?
      • 0907 Solution concentration
      • 0908 Chemical species, speciation in aqueous solution
      • 0909 Solutes: Electrolytes or non-electrolytes?
      • 0910 Electrolytes - strong or weak?
      • 0911 Concentrated, dilute, strong, weak
      • 0912 Species concentration vs. solution concentration
      • 0913 Weak electrolytes: Getting quantitative
    • Chapter 11: Dynamic chemical equilibrium >
      • 1100 Dynamic chemical equilibrium: Overview
      • 1101 Visualising dynamic chemical equilibrium
      • 1102 The jargon of chemical equilibrium
      • 1103 Equilibrium constants: The law of equilibrium
      • 1104 The law of equilibrium: an analogy
    • Chapter 22 Spectroscopy >
      • 2200 Spectroscopy: Overview and preview
      • 2201 Quantisation of forms of energy
      • 2202 Light: Wave-particle "duality"
      • 2203 Ultraviolet-visible spectroscopy
      • 2204 Beer’s law: How much light is transmitted?
    • Chapter 27 The greenhouse effect, climate change >
      • 2700 The greenhouse effect: overview
      • 2701 Is Earth in energy balance?
      • 2702 CO2 in the atmosphere before 1800
      • 2703 So little CO2! Pffft?
      • 2704 Does CO2 affect Earth's energy balance?
      • 2705 The "greenhouse effect"
      • 2706 Why does CO2 absorb radiation from Earth?
      • 2707 The "enhanced greenhouse effect"
      • 2708 Why doesn't CO2 absorb the radiation from the sun?
      • 2709 Why are N2 and O2 not greenhouse gases?
      • 2710 Doesn't water vapour absorb all the IR?
      • 2711 Carbon dioxide from our cars
      • 2712 The source of energy from combustion
      • 2713 Comparing fuels as energy sources
      • 2714 Methane: How does it compare as a GHG?
      • 2715 Different sorts of pollution of the atmosphere
      • 2716 "Acidification" of seawater
    • Chapter 27 Communicating chemistry >
      • 2700 Overview, preview
      • 2703 The jargon we use
  • TEACHERS' CORNER
    • T01 Communicating chemistry
    • T02 Beer's law
    • T03 Professional amnesia of the chemistry teaching professio
    • T04 Law of equilibrium
    • T05 Visusalizing dynamic chemical equilibrium
    • Information vs. knowledge
  • PERSONAL GALLERY
    • Family
    • Travel
    • Playful dolphins
    • The University of Western Australia
    • Kings Park
    • Perth
    • At work
    • 999 Thermodynamics