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How's my Ozone section? (1 Viewer)

.ben

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" identify the origins of chlorofluorocarbons (CFCs) and halons in the atmosphere

CFCs (as the name suggests, consists of the elements carbon, fluorine and chlorine) and are a subset of the group of compounds known as the haloalkanes. Haloalkanes consist of carbon based compounds which contain one or more halogen atom (fluorine, chlorine, bromine or iodine). Chlorofluorocarbons (CFCs) were first invented in 1928, and began to be used for their favourable properties such as inertness, non-toxicity and the fact that they were readily liquefied upon compression. By the 1950s they had been begun to be mass produced. After widespread use in applications such as refrigerators, aerosol can propellants, and air conditioners, they entered the lower atmosphere (troposphere) in large quantities.

Halons were another ozone destroying substance used in applications such as computer systems and fire extinguishers. They are bromofluorocarbons (consisting of the elements bromine, fluorine and carbon only).

 discuss the problems associated with the use of CFCs and assess the effectiveness of steps taken to alleviate these problems

CFCs are highly unreactive compounds and do not destroy ozone molecules directly. It is however the fact that they slowly diffused (tropopause barrier) into the stratosphere which was the problem. In the stratosphere, CFCs are subject to intense bursts of high to medium energy UV rays which cause them to decay. This decay eventually brings about the formation of chlorine radicals. These chlorine radicals readily attack ozone molecules to produce chlorine oxide and oxygen gas of which the former combines with oxygen free radicals to produce more oxygen gas and another chlorine free radical. This process is known as photodissociation.

[instert equantiosns]

As it is obvious from the process of photodissociation, that the destruction of ozone molecules produce 'catalysts' (chlorine free radicals) for the destruction of more ozone molecules. In this way, a single CFC molecule decomposed by UV radiation can destroy thousands of ozone molecules before being removed by external forces. This can be classified as a positive feedback system. This system of destruction of the ozone in the stratosphere has caused ‘holes’ in the ozone layer allowing high to medium energy UV radiation to reach the earth’s surface. This is particularly dangerous as UV radiation can potentially cause cancers in humans as they mutate living tissue. Statistics show an alarming increase in skin cancers with just 1% decrease in ozone level enough to cause an 8% jump of cancer cases. Environmental damage associated with ozone depletion includes the melting of the poles (attributed to the large ozone hole over Antarctica) which contributes to the increased sea levels and temperatures. Thus measures have been taken to reduce the amount of ozone depletion.

In 1987 the Montreal Protocol was introduced, gradually phasing out halon and CFC production by 1996. Plans to terminate HCFCs by the early 21st Century were also drawn out. Scientists have researched the destruction of the ozone and as a result of the termination of ozone destroying compounds, have predicted the damage to the ozone to begin to reverse and the ozone to begin its recovery process from the early 21st century.


 present information from secondary sources to identify alternative chemicals used to replace CFCs and evaluate the effectiveness of their use as a replacement for CFCs

The discovery of this immense destruction of ozone in the stratosphere prompted many measures such as replacement haloalkanes such as HCFCs and HFCs. The principle of the former was to allow any haloalkane escaped into the troposphere to react with hydroxyl free radicals and thus eliminate the chlorine entering the stratosphere. This was unsuccessful as much HCFC still escaped into the stratosphere. Upon further investigation it was found that HCFCs destroyed ozone at a faster rate than its CFC predecessors. HCFCs were used only as a stopgap measure until a more favourable alternative could be found. The latter, HFCs, contained no chlorine at all and thus posed no danger upon entering the stratosphere. Due to this many HFCs are still in use in refrigerators and other appliances despite their increased economic cost."

Do my answers fulfill the requirements of these dps? do i need to +/- anything to improve this? thankyou
 

Riviet

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 discuss the problems associated with the use of CFCs and assess the effectiveness of steps taken to alleviate these problems
You need to provide an assessment of how effective these steps have been, e.g "These steps have been effective because... [insert reason(s) + explanation here]".
 present information from secondary sources to identify alternative chemicals used to replace CFCs and evaluate the effectiveness of their use as a replacement for CFCs
You need to clearly state whether these alternative chemicals are effective or not and include reasons to support your judgement, a bit like the previous dotpoint.
 

.ben

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mmm, do you think i've done this in my summary?
 

Riviet

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You have the sufficient discussion of the issues etc. but just need to polish it off with a clear statement saying whether they have been effective or not (for both dotpoints that I referred to above). This is why alot of students miss out on that mark or two in those longer response questions. They have all the info and equations but not the assessment or evaluation.
 

royy

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Hey can any 1 help me with this outcome, is this right? What needs changin?

Analyse the information available that indicates changes in atmospheric ozone concentrations, describe the changes observed and explain how this inform

• Ozone thinning is greatest in spring (late October) over Antarctica
• During the preceding winter, HCl and ClONO2 molecules react on the surfaces of atmospheric ice crystals to form chlorine molecules (Cl2)
ClONO2 + HCl HNO3 + Cl2
• Following the long, dark Antarctic winter there is a rapid increase in UV in the stratosphere over Antarctica
• Ozone loss is worst in the world’s coldest region because of polar stratospheric clouds (PSCs) which form when temperatures fall below -80°C. It is suggested that these clouds are necessary for the chemical reactions to occur late in the Antarctic winter. Once spring appears and light shines on the PSCs, rapid ozone destruction occurs
• The increase in UV causes photodissociation of the chlorine molecules to produce additional chlorine free radicals that begin the ozone destruction process
• With a rise in temperature, the PSCs are reduced and the ozone destruction stops
• Several months later, the supply of Cl molecules is exhausted and ozone levels gradually return to normal as lower latitude air mixes with polar air
• Ozone concentration is measured in Dobson units. One unit represents one molecule of ozone to every billion molecules of air
 

.ben

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ill edit it thanks

royy ur one seems pretty complete in terms of info
 

.ben

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Do wehave to know about greenhouse and NOx effects?
 

tennille

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If you look at this

http://hsc.csu.edu.au/chemistry/core/monitoring/chem944/944net.html

it doesn't specifically say that you need to know about the greenhouse effect or NOx effects. But, when it comes to CFC's, these enhance the greenhouse effect. The greenhouse effect is mainly related to the second last dot-point. So, it would be a good idea to have an understanding of each.
 
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