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Oxygen is a strong , meaning it is being itself
Ozygen is a strong oxidizer, meaning it is being reduced itself
Oxidation releases…
Energy
Burning vs. respiration (differences)
Burning: Release of C in an uncontrolled way
Respiration: Release of C in a controlled way
Burning vs. respiration (similarities)
They both release C by reacting with O2
Spontenous redox reactions
Electrons move from atoms with a low affinity for electrons, to atoms with a high affinity for electrons
Zn(s) + Cu2+(aq) → Zn2+(aq) + Cu(s)
Half reaction: Zn0 → Zn2+ + 2e−
--> What happened to the zincs oxidation state and solubility
Zinc was oxidized (loss electrons) and its solubility changes in a way that it became aqueous
Zn(s) + Cu2+(aq) → Zn2+(aq) + Cu(s)
Half reaction: Cu2+ + 2e− → Cu0
--> What happened to coppers oxidation state and solubility
It was reduced (gained electrons) and its solubulity changed in a way that it became solid
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The temp increases, since energy is released during the movement of electrons
The _ changes along with the change in oxidation state
Solubility
Where do organisms collect energy from?
From carefully controlled redox reactions
Aerobic respiration
It is the reaction that most animals use to derive energy from food, starting with glucose and oxygen
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"C #1 = 0
C #2 = +4 "
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""
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C is the electron _"
Donor
Which ever molecule is the electron donor is also the source
Energy
If 1 thing is oxidized, something else must be _
Reduced
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""
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O is the electron "
Acceptor
Gibbs free energy
The potential energy that an electron can hold and therefore the energy it releases when a redox reaction occurs
Activation energy
The amount of energy needed to overcome the energy barrier that allows for a chemical reaction to occur
Gibbs free energy formula
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ΔE
The difference in electrical potential (V) between the oxidation and reduction half reactions
"ΔE formula "
"ΔEº = E cathode (reduction) - E anode (oxidation)"
The apart the electrical potential is, the ΔE is, meaning the ____ energy that is released
The further apart the electrical potential is, the higher ΔE is, meaning the more energy that is released
ΔGº vs. ΔG
ΔGº = It is under standard conditions
ΔG = It is under real world conditions, which are often not in standard conditions
Common terminal electron acceptor
O2
Electron donor in cellular respiration
Glucose
Electron transport chain
It builds up and captures energy in the form of ATP and a proton gradient
What is a terminal electron acceptor (i.e. O2)?
It's kind of like a garbage truck, such that it absorbs electrons that have already given away its energy and therefore is at a lower energy state, in order to clear them out of the way
Assimilation of carbon
Carbon to build with
Dissimilation of carbon
Carbon to burn (i.e. acts as the electron donor)
What happens if reduced carbon is not available for oxidation?
Other substances can be used as the electron donor, such as iron
Iron replacing glucose
The iron acts as the energy source, as its electrons are taken from it and given to oxygen
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Significance of distance between electron acceptor and donor "
The further away the two are from each other, the more energy that is released in the reaction
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Which reaction releases more energy?"
The red one, since the electron acceptor and donor are further apart
Aerobic respiration dominates in terrestrial environments, but not so much in aquatic environments
Why is aerobic respiration less prominent in aquatic environment
This is becayse the water acts as an effective barrier against oxygen, as the diffusion rate of oxygen in standing water is very slow
What do organisms do when O2 is not available for aerobic respiration?
They use other molecules as the terminal electron acceptor
Alternative terminal electron acceptor that is not oxygen
Nitrogen
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Energy difference between the two reactions"
The energy released is roughly the same
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If the energy difference is not that great, what is the problem with using N instead O as a terminal electron acceptor "
The constraint is the source of N and the fact that it has to be in solution
Rapid + Slow ___ = Limited amount of O2
Rapid consumption + Slow replenishment = Limited amount of O2
Adaptation that allows aquatic plants to make up for the lack of O2
They have pores that allows O2 to diffuse inside in the gas phase so that it can get to the roots, rather than it having to go through water
Dead zones that lead to fish kills
1.) This refers to areas with high decomposition, leading to a rapid consumption of O2 that causes the water to be hypoxic
2.) This kills the living organisms (i.e. the fish) in the area as a result, due to suffocation
Dead zones leading to fish kills usually occur when?
It often occur after winter, due to the long duration of ice cover
ASK PROF
Flux in = Local production or transfer from atmosphere
Flux out = Consumption by respiration
Determining O2 concentration in a soil aggregate (how)
Penetrate into the soil aggregate to measure the O2 levels
Determining O2 concentration in a soil aggregate (results)
The amount of O2 decreases the deeper we go, meaning that the deeper we go, the more that rates of consumption exceeds replenishment
O2 levels in microbial colonies
The area at the surface has the highest concentration, but the deeper you go into the colony, the less O2 there is
Aerobic respiration vs. photosynthesis reaction
Their reactions are the complete inversion of each other
Input of energy in photosynthesis
Sunlight
Why is it weird that we have so much O2 in our atmosphere
Geochemical forces usually want O2 to react with other chemicals and form oxides
Two mechanisms for the generation of O2
1.) Use of solar energy
2.) Photosynthesis
Generation of O2: using solar energy
This invovles the photolysis of water vapour into O2 (but it's only a small source of O2)
Photolysis
The process of breaking something apart using light
Generation of O2: photosynthesis
Oxygen is a byproduct of photosynthesizers making chemical energy
Photosynthesis reaction
It involves using water and CO2 as substrates, resulting in O2 and CH2O products
Seasonal dynamics of O2
This refers to the fact that O2 levels are directly proportional to the amount of actively growing plants
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What is the graph showing us "
Dotted line = Capacity of O2 that water can hold
Above line = It represents the level of O2 being ejected from water, coming from photosynthesizers in the water
Banded iron formations
It represents the transition of earth from a low oxygen environment to a high oxygen environment, based on the massive amounts of iron that precipitated out of ancient oceans
Atmosphere then vs. now (in relation to oxygen + iron)
Then = Atmosphere used to be anoxic, therefore most/all of the iron was reduced in water
Now = As O2 became more available because of photosynthesizers, the iron became oxidized, which is less soluble, causing the iron to precipitate out of the water
1.) Photosynthetic organisms acted as the source of oxygen, allowing it to flux out into the environment
2.) It started off as being in a steady state, as it was constantly being used up by iron so that it can be oxidized, all while the photosynthesizers continued to make more
Reverse
Significance of aerobic respiration being the reverse reaction of photosynthesis
In order for photosynthesis to drive the accumulation of molecular oxygen, some of the reduced carbon that is formed by photosynthesis must be stored as organic matter
"""In order for photosynthesis to drive the accumulation of molecular oxygen, some of the reduced carbon that is formed by photosynthesis must be stored as organic matter"" --> WHY? "
1.) If the reduced carbon made in photosynthesis is immediately oxidized, the formation of O2 is just reversed, before it could be utilized in aerobic respiration
2.) Therefore, it must first be stored in/as organic matter
Negative vs. positive feedback
Negative feedback has a dampening/countering effect, while positive feedback has a re-inforcing effect
Negative feedback example
When the temperature in a room drops, it is sensed by the thermostat, which brings the temperature back up
Negative and positive feedback are esssential for what?
They are essential for maintaining balance/stability
Feedback example involving oxygen
As O2 levels increase in the atmosphere, the penetration of O2 into the ocean is deeper, allowing respiration to happen in more places, which allows O2 to be used up at a faster rate
1.) It has made Earth's surface a highly oxidizing environment
2.) Which in turn, helps in the formation of the shield against UV radiation
Earth's surface is now a highly environment, due to the splitting of via _
Earth's surface is now a highly oxidizing environment, due to the splitting of water via photosynthesis
Ozone
A thick layer O3 that shields the earth from UV radiation
High altitude
Stratospheric ozone
Low altitude
Tropospheric
Ozone in the lower atmosphere
It contributes to air pollution
Ozone creation & destruction is a continuous and dynamic process
Production of ozone
1.) UV radiation (light) splits O2 into individual oxygen atoms
2.) The individual oxygen atom can then react with O2 to form O3
Destruction of ozone
1.) UV radiation splits O3 into O2 and an individual atom
2.) The individaul atom can then react with another O3 molecule and form two O2 molecules
UV radiation splitting O2 or O3 is similar to…
The formation of O2 from the photolysis of water
Ozone is only created when…
When O2 levels become enriched in the atmosphere
Ozone is the primary constituent of the atmosphere that absorbs incoming light in the ultraviolet wavelengths.
What makes O3 so good at acting as a barrier against UV radiation
Because it is able to absorb UV very well
Pollutant
What impacts the fate of the ozone in the stratopheric vs. troposcheric atmosphere
It depends on the prescence of water
Water availability in the lower vs. upper atmosphere
Stratosphere = Low water
Troposphere = High water
What happens to the ozone in the trophospheric region
1.) There are lots of water, which can interact with an excited oxygen atom to form a hydroxyl radical
2.) A series of reactions then occur that result in the formation of O2 from O3
Significance of high water availability in the tropospheric region
The water helps clean up the air, as it forms O2, which helps control the fact that ozone is a pollutant in this region
Hydroxyl radicals
1.) The main source of oxidizing power in the troposphere
2.) It has a lifespan of seconds
More ozone is formed in the ___
Stratosphere
Ozone in the stratosphere (stability)
It is more stable and therefore has a longer residence time in the stratosphere
What happens to the ozone when other chemicals are present in the atmosphere
They can accelerate ozone destruction, as many of them act as catalysts that can be regenerated during intermediate reactions
Example of chemical that acts can as a catalyst to accelerate ozone destruction
Chlorine
What causes chemicals to be present in the atmosphere
It is caused by human activity, such that it causes chemicals to be in the atmosphere that are not usually there
Chlorine significance to the ozone
It can react with O3, convering it into O2
CFC significance to the ozone
1.) UV light causes one of its chlorine to be cleaved
2.) The chlorine can now reaction with O3 to form O2
How does chlorine act as a catalyst
It does not get used up, it can be used again to react with O3 again
NaCl vs. CFC residence times
NaCl = Short RT
CFC = Long RT
Tropopause
The barrier that separates the stratosphere and troposphere from mixing
Is there stratification in the atmosphere
Yes, via the tropopause