Lecture 18 - Dynamic Equilibrium

Thursday, March 14, 2024

9:00 AM

"The solvent is the most disregarded reactant in solution chemistry. It participates, it influences, and it shapes the reaction, yet it is rarely accounted for with the respect it deserves." Henry Eyring
Class notes (1-16): https://bricejurban.github.io/CHEM101/ 
Assignments this week:
﷟HYPERLINK "https://boisestatecanvas.instructure.com/courses/28698/assignments/1005442"HW 11 - Aqueous Solutions, Molarity, Aqueous Reactions
﷟HYPERLINK "https://boisestatecanvas.instructure.com/courses/28698/assignments/1008080/edit?quiz_lti"Reading Quiz on Chapter 6
Reminders:
Midterm 2 is published on Gradescope and the answer key is outside SCNC 336. If you notice any errors in grading, please make a regrade request through Gradescope.

CIC (EDUC 107) Hours: Friday 11AM - 1PM
Office Hours (SCNC 314 or Zoom): ﷟HYPERLINK "https://calendly.com/bricejurban/office-hours"By appointment
Today (3/14)
Equilibrium
Le Chatelier's Principle
CO2/Bicarbonate Buffer System
Ocean Acidification

Looking Ahead
Spring Break (3/18 - 3/22)
Tuesday (3/26)
﷟HYPERLINK "https://boisestatecanvas.instructure.com/courses/28698/assignments/967940"Midterm 3

Irreversible versus Reversible Reactions
 
Irreversible reactions: 

Proceed until a reactant runs out and the reaction reaches completion

Reversible reactions:

Both the forward and reverse reaction occur at the same time

A reaction appears to stop when:

 When it reaches equilibrium

 When a reactant is used up

 When a reaction is very slow

We know a system is at dynamic equilibrium when we can observe constant properties such as:
 



          [M]





                  
                                             time

 Dynamic equilibrium does not mean equal amounts

 Dynamic equilibrium happens when the forward and reverse reactions  take place at equal rates
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We know a system is at dynamic equilibrium when we can observe constant properties such as:

Constant volume
Constant pressure
Color
pH
conductivity


Equilibrium Expression
Given a reversible reaction:  aA + bB ⇌ cC + dD
where a, b, c, and d are the balanced coefficients 
and A, B, C, and D are the chemical formulas            
 We can write an expression that represents the equilibrium:
 
Keq = 


The equilibrium constant (Keq) is constant at a specific temperature.

Only gases and dissolved substances are included in the Keq expression since their concentrations vary in a reaction. 

Solids and liquids are not included in Keq since their concentrations are relatively constant. 

Include: (g), (aq) 
Do not include: (s), (ℓ)

The equilibrium expression (Keq) describes the extent of a reaction.

If Keq >> 1, at equilibrium, the reaction is product favored.

If Keq ≈ 1, at equilibrium, approximately equal reactants and products

If Keq << 1, at equilibrium the reaction is reactant favored.


Examples:

HCN (aq) ⇌ H+ (aq) + CN‒ (aq)                              [HCN] = 1.3 × 10–5 M, [H+] = 9.0 × 10–8 M, [CN–] = 9.0 × 10–8 M
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HCN (aq) ⇌ H+ (aq) + CN‒ (aq)                              [HCN] = 1.3 × 10–5 M, [H+] = 9.0 × 10–8 M, [CN–] = 9.0 × 10–8 M











2 NO (g) + O2 (g) ⇌ 2 NO2 (g)                                 [NO] = 1.0 × 10–8 M, [O2] = 5.0 × 10–3 M, [NO2] = 1.0 × 10–3 M











Al(OH)3 (s) ⇌ Al3+ (aq) + 3 OH‒ (aq)                        [Al3+] = 5.2 ×10–9 M, [OH–] = 1.6 × 10–8 M







Le Chatelier's Principle
 
When a stress is added to a system at equilibrium, the system will shift to reduce that stress 

The Rules:
Add a reactant, shift to the products. Add a product, shift to the reactants.
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Add a reactant, shift to the products. Add a product, shift to the reactants.
Increase temperature, shift away from heat. Decrease temperature, shift toward heat.
Reactions that are exothermic ΔH < 0 (release heat); heat is a product
Reactions that are endothermic ΔH > 0 (absorb heat); heat is a reactant
Increase pressure (reduce volume), shift toward side with fewer moles of gas. 
Decrease pressure (increase volume), shift toward side with more moles of gas.
Concentration of solids and liquids cannot change, adding a solid of liquid will not shift the equilibrium.
Adding a catalyst will speed up the reaction in both directions equally, not affecting the equilibrium (only the rate)


﷟HYPERLINK "https://www.youtube.com/watch?v=_jypU3FvS_o"Chromate Dichromate Ion Equilibrium

Chromate Dichromate Ion Equilibrium - LeChatelier's Principle Lab Part 2 Press enter to activate, Machine generated alternative text:
a%nlfie 

2H+(aq) + 2CrO42–(aq) ⇌ Cr2O72–(aq) + H2O(ℓ) 
(yellow)         (orange)



Observed Change   
Stress 
H+
CrO42–
Shift 
Cr2O72–
Add HCl
 (Add H+)
Yellow -> Orange
Too much H+




Add NaOH
 (remove H+)
Orange -> Yellow
Not enough H+





﷟HYPERLINK "https://www.youtube.com/watch?v=ScWBj0hqOLE"Effect of Temperature on conversion of NO2 to N2O4

Effect of Temperature on conversion of NO2 to N2O4 (Le Chatelier's Principle) Press enter to activate, Machine generated alternative text:
N2fa(g) + he 
red-br 
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Effect of Temperature on conversion of NO2 to N2O4 (Le Chatelier's Principle) Press enter to activate, Machine generated alternative text:
N2fa(g) + he 
red-br 

2 NO2(g) ⇌ N2O4(g) + heat
(amber)       (colorless)


Observed Change   
Stress 
NO2
Shift 
N2O4
Increase Temperature

Amber -> Dark Amber
Too much heat



Decrease Temperature

Amber -> colorless
Not enough heat





﷟HYPERLINK "https://www.youtube.com/watch?v=cWr3UDo-WeU"Cobalt Complex Ion Equilibrium

Cobalt Complex Ion Equilibrium - LeChatelier's Principle Lab Part 3 Press enter to activate, Machine generated alternative text:
Onl%e 

heat + Co2+(aq) + 4 Cl–(aq) ⇌ CoCl42–(aq)
(pink)                             (blue)



Observed Change   
Stress 
Co2+
Cl–
Shift 
CoCl42–
Add HCl
 (Add Cl-)






Add AgNO3
 (remove Cl-)






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 (remove Cl-)
Increase Temperature







Decrease Temperature








﷟HYPERLINK "https://www.youtube.com/watch?v=1_HoWz5Kxfk"The Haber Process

GCSE Chemistry - The Haber Process Explained  #76 Press enter to activate, Machine generated alternative text:
THE 
HABER PROCESS 

N2(g) + 3H2(g)  ⇌ 2NH3(g) + heat

Identify what's changing
Determine the stress (too much ____or not enough ________)
State which direction the system will shift  ←  or →
State whether each component of the system will increase (↑) or decrease (↓) or remain unchanged (—)
N2(g) + 3H2(g)  ⇌ 2NH3(g) + heat

Stress 
[N2]
[H2]
Shift 
[NH3]
Add N2

Too much N2




Add H2

Too much H2




Add NH3

Too much product




Remove N2

Not enough N2




Remove H2

Not enough H2




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Remove NH3

Not enough NH3




Increase Temperature

Too much heat




Decrease Temperature

Not enough heat




Increase Pressure

Not enough space




Decrease Pressure

Too much space




Add a catalyst

No stress


no shift



Example of a reversible reaction: CO2/Bicarbonate buffering system
Untitled picture.png Machine generated alternative text:
C02 + H20 
61 
1.2 [TIM 
HC09 
Carbon dioxide- 
bicarbonate buffer 
24 mM 
Untitled picture.png 
"The most important buffer in the blood is the CO2/bicarbonate buffer. This consists of water, carbon dioxide (CO2, the anhydride of carbonic acid H2CO3), and hydrogen carbonate (HCO3–, bicarbonate). The adjustment of the balance between CO2 and HCO3– is accelerated by the zinc-containing enzyme carbonate dehydratase (carbonic anhydrase). At the pH value of the plasma, HCO3– and CO2 are present in a ratio of about 20 : 1. However, the CO2 in solution in the blood is in equilibrium with the gaseous CO2 in the pulmonary alveoli. The CO2/HCO3– system is therefore a powerful open buffer system. Faster or slower respiration increases or reduces CO2 release in the lungs. This shifts the CO2/HCO3– ratio and thus the plasma pH value (respiratory acidosis or alkalosis)." (Source: Color Atlas of Biochemistry, Koolman)

 

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HC03 e 
C02 + H 20 
ung 
ung influences 
H value by C02 
xcretion 

Ocean Acidification and the impact on coral and shellfish
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CO2​(g) + H2​O(l) ⇌ H2​CO3​(aq) ⇌ HCO3−​(aq) + H+ (aq) ⇌ H+ + CO32−
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sequestration of carbon by the ocean forms carbonic acid (reversible)
carbonic acid breaks apart into bicarbonate and hydrogen ions (reversible)
(forward) bicarbonate can break apart into carbonate and hydrogen ions
(reverse) carbonate from shellfish can react with hydrogen ions to form bicarbonate.

"The oceans absorb excess carbon dioxide from the atmosphere as part of the global carbon cycle. As atmospheric CO2 levels increase from the burning of fossil fuels, excess CO2 dissolves in the oceans and forms carbonic acid. This is the process of ocean acidification—a lowering of the ocean pH. A more acid ocean causes certain marine organisms such as corals, plankton, and shellfish to have difficulty maintaining external calcium carbonate structures. The ocean’s average pH today is 8.1, down from 8.2 at the beginning of the Industrial Revolution. Scientists estimate that ocean pH could decrease by 0.4 to 0.5 units this century as atmospheric CO2 increases. The pH scale is logarithmic, so a decrease of 0.1 equals a 30% increase in acidity. Oceanic biodiversity and food webs will respond to this change in unknown ways." (Source: Elemental Geosystems, Christopherson)
Figure-7_OceanAcidity-ChartREV1_Final-e1460747846316-750x522.png 
Source: Oregon Conservation Strategy
﷟HYPERLINK "https://www.youtube.com/watch?v=7h08ok3hFSs&t=357s"Ocean Acidification - Changing Waters On The Oregon Coast

 

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