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Chemistry LibreTexts

4.9: Free Radicals

  • Page ID
    97105
  • Skills to Develop

    • Recognize the structures of free radicals.
    • Understand how free radicals affect the environment and biological systems.
    • Know specific compounds that form photochemical smog.
    • Understand how photochemical smog affects the environment and people.
    • Realize that ozone in the stratosphere protects the earth from UV rays.
    • Explain the basics of the Chapman Cycle.
    • Provide sources of chemicals that deplete the ozone layer at an accelerated rate.
    • Know where areas of depleted ozone are on the planet.
    • Differentiate between CFCs, HCFC, HFC, and halons.
    • Know the meaning and environmental impact of ODS and GWP.
    • Appreciate the Montreal Protocol.
    • Understand the connection between free radicals and aging, cancer, and autoimmune disorders.
    • Provide examples of antioxidants.
    • Understand how to stop the accelerated aging of the skin.

    The majority of molecules or complex ions discussed in general chemistry courses are demonstrated to have pairs of electrons. However, there are a few stable molecules which contain an odd number of electrons. These molecules, called "free radicals", contain at least one unpaired electron, a clear violation of the octet rule. Free radicals play many important roles a wide range of applied chemistry fields, including biology, medicine, and environmental chemistry. Three well-known examples of such molecules are nitrogen monoxide, nitrogen dioxide, and chlorine dioxide. The most plausible Lewis structures for these molecules are

    In this course, you need to be concerned with identifying free radical species. It is not necessary for you to know where to place the spare electron. In addition, please focus on the problems with free radicals that are discussed in the sections below.

    Photochemical Smog

    The two nitrogen-containing compounds above are classified as being \(\ce{NO_{X}s}\). These free radicals are produced from high-temperature combustion of fuel by vehicles and industry. NOxs can also be produced by natural processes. For example, lightning and volcanic eruptions produce these species. These gases do differ from one another. Nitrogen monoxide (also known as nitric oxide) is a colorless and non-flammable gas. In contrast, nitrogen dioxide is a reddish-orange gas that is extremely flammable. Nitrogen monoxide has a slight odor, while nitrogen dioxide has a very sharp, acrid smell.

    Once \(\ce{NO_{X}s}\) are produced, they can react with ultraviolet light to produce more free radicals. After a series of reactions, these species produce ground-level ozone (\(\ce{O3}\)) which is referred to as smog. In regards to the environment, smog reduces visibility and reacts with water to produce acid rain. As for humans, \(\ce{NO_{X}s}\) can affect lung, heart, and immunity functioning. Photochemical smog is more of an issue in highly populated cities that rely heavily on transportation sources and electrical power plants. Fortunately, the United States Environmental Protection Agency (EPA) regulates \(\ce{NO_{X}s}\) amounts for vehicles and power plants.

                                                                            imageedit_1_5851676765.jpg

      Figure \(\PageIndex{2}\): Arial photograph of photochemical smog in Manhattan, New York. Documerica was a program sponsored by the Environmental Protection Agency to photographically document subjects of environmental concern in America during the 1970s.

    Consumers of American cars can review smog ratings before purchasing a vehicle. Cars and trucks produce other chemicals besides NOxs that contribute to smog formation. For a basic rating on smog-producing ability, click here and input your vehicle's information. On this website, smog ratings are assigned to mobile sources (cars, trucks, sports utility vehicles) from one to ten. A low score indicates that the vehicle produces a large number of smog precursors.

    Protective Ozone (O3)

    Ozone or O3 can be harmful or helpful depending on where it is located. In the troposphere (see image below), ozone is referred to as smog. Previously, you have learned the harmful effects of being exposed to ground level ozone. However, ozone acts as a protective shield in the stratosphere. Of the three forms of ultraviolet radiation, ozone completely screens the Earth's surface from UV-C radiation. Portions of UV-B (causes more burning of skin) and UV-A (causes more tanning of skin) still reaches the terrestrial environment.

    atmosphere types.jpg

    Figure \(\PageIndex{3}\): Levels of the atmosphere and location of the O3 layer. Image is taken from https://commons.wikimedia.org/wiki/F...5%E0%B8%81.jpg

    If all the ozone in the atmosphere were combined, it would have a thickness of less than 0.5 cm (.20 inches). Ozone is most concentrated in the lowest 15 km portion of the stratosphere. NASA and other atmospheric scientists utilize the Dobson scale to represent the concentration of ozone molecules. One Dobson Unit (DU) is the number of ozone molecules that could create a 0.01 mm layer of thickness (conditions of 0ºC and 1.0 atm). NASA reports the average thickness of the ozone layer to be 300 DU which translates to 3 mm. A depleted ozone layer would register as being equal to or less than 100 DU or a thickness of 1 mm. The NASA image below depicts a purplish-blue region that corresponds to the largest area of ozone depletion. First detected in 1985, the ozone hole has grown to a maximum of 7.6 million square miles (or 2.5 times the size of the United States. NASA reported this peak value on September 11, 2017.

    imageedit_6_9147527758.jpg

    Figure \(\PageIndex{4}\): NASA image of Dobson units that correlates to O3 concentration. Image used with permission (Public Domain; NASA)

    Ozone is made and decomposed naturally via the Chapman cycle. In the stratosphere, ultraviolet light breaks the double bond of the diatomic oxygen molecule. From this reaction, spare oxygen (O) atoms encounter more diatomic oxygen (O2) molecules to produce ozone. Ultraviolet light can attack ozone molecules BY CLEAVING ONE oxygen bond in the structure. This natural cycle of ozone production and decomposition repeats in the Chapman Cycle.

    Figure \(\PageIndex{5}\): Production and decomposition of ozone via the Chapman Cycle. The image is taken from https://upload.wikimedia.org/wikiped..._cycle.svg.png

    Understanding Stratospheric Ozone

    Watch The following video and then answer the questions below:

    1. What is the formula for ozone? what types of bonds does this molecule have (you will need to draw)?
    2. How many ozone molecules are present per 10 million molecules of air?
    3. What percentage of UV rays does ozone layer absorb?
    4. What chemicals are responsible for depleting ozone?
    5. What are the uses of the chemicals in question #4?
    6. When UV light hits ozone-depleting chemicals, what atom is liberated? How many valence electrons does this atom have?
    7. Where are the areas on the earth that have ozone holes or patches?
    8. Why is the largest area of depletion over Antartica?
    9. At this time, is the ozone hole growing or shrinking?
    10. What protocol banned the production of ozone-depleting chemicals?
    Answer a

    Ozone (\(\ce{O_3}\)), which this molecule has a single and a double bond. The single bond is much weaker and longer. It would be easier to break this bond.

    Answer b

    3

    Answer c

    98%

    Answer d

    CFCs are organic compounds that contain different combinations of carbon, chlorine, fluorine, and sometimes hydrogen. The chlorine portion is particularly toxic to the ozone layer.

    Answer e

    Chlorine gas or chlorine that is used to disinfect drinking water is not a CFC.

    Answer f

    When ultraviolet light hits a CFC, chlorine is freed and becomes a free radical. This reactive species attacks the ozone molecule at the single bond location. Chlorine atom has seven valence electrons.

    Answer g

    Both poles contain areas that are lacking in \(\ce{O3}\).

    Answer h

    The CFCS used in northern hemisphere eventually migrated to the cold areas of Antarctica. The temperatures in this area catalyze (speed up) the free radical reactions. This produces more chlorine atoms that will attack ozone molecules.

    Answer i

    The hole is shrinking!

    Answer j

    Montreal Protocol

    Causes of Depletion

    Before the 1920's, the mechanism of chemical refrigeration required such toxic chemicals as ammonia or sulfur dioxide. Frigidaire scientists focused on synthesizing safer compounds to be used in this industry. This research lead to the production of CFCs or compounds that contained a combination of chlorine, carbon, and fluorine. Chemists found these colorless liquids to be very volatile and inert. By the 1970's, the chemical industry was producing one million tons a year of these chemicals to be used as refrigerants, propellants, and foaming agents.

    asthmacfc.jpg

    Figure \(\PageIndex{6}\): Asthma inhaler with CFC propellant. Image taken from: https://www.flickr.com/photos/fdaphotos/5532092795

    Perhaps the most common CFC made was dichlorodifluoromethane. This CFC is also known as Freon-12 and was used as a refrigerant for cars, commercial, and industrial air conditioning systems. Today, the United States is no longer able to make this compound and distributors must have a Freon license to distribute existing supplies. Even though you might use the term "freon" to describe air conditioning coolant, you are not using this particular chemical due to environmental restrictions.

    512px-Trichlorofluoromethane-2D.svg.png

    Figure \(\PageIndex{7}\): Chemical structure of Freon-12. Chlorine (dark green) and fluorine atoms (light green)

    In the early to late 1970's, many international studies determined CFCs and other halons (once used as fire retardants), particularly those containing bromine, contributed to the destruction of the ozone layer.  It was not until the mid-1980's that an international treaty was formulated to reduce the production of certain ODS (ozone depleting substance). In 1987, over 190 countries signed the Montreal Protocol. Upon signature, countries would agree to reduce and then eliminate ODS chemicals that contained chlorine or bromine. Countries that could not afford to find suitable replacements for ODS would be given time extensions and funding.

    CFCfriendly.jpg

    Figure \(\PageIndex{8}\): Label indicating ozone friendly packaging. Picture courtesy of Elizabeth R. Gordon

    Operation Cool breeze

    Even though freon production in the United States has halted, this chemical is still used in refrigeration systems that cannot switch to ozone-friendly replacements. This has opened an illegal smuggling of freon into countries that have signed the Montreal Protocol. In the United States, freon smuggling is an environmental crime. Violators that have been prosecuted have paid fines and/or served time in prison. Read the article in this link and record main ideas regarding EPA/s Operation Cool Breeze.

    The United States and several other countries replaced many CFCs with HCFC compounds. By adding hydrogen, this allowed a CFC compound to retain its chlorine atoms. In other words, ultraviolet light would not be able to break the C-Cl bond releasing a chlorine free radical. Unfortunately, HCFCs were found to have higher global warming potentials (GWP) and would need to be phased out as well. For most countries, this HCFC reduction would occur in 2010. During this time, countries substituted HFCs for both HCFC and CFC compounds. HFCs have the lowest OD potential but still, have high GWP. Today, countries are focusing on finding more environmentally friendly replacements for these chemicals as well. Keep in mind, each chemical substitution that has been mentioned is costly and still affects the environment.

    Table \(\PageIndex{1}\): Comparing CFCs, HCFCs, HFCs, and halons.
    Chemicals Formula Classification Atmospheric lifetime (years) ODP GWP
    CF2Cl3 CFC 69 1.0 4660
    CF2Cl2 CFC 195 1.0 10,200
    CF3Br Halon 65 13 6300
    CF2ClBr Halon 20 5.0 1750
    CHClF2 HCFC 13 .055 1760
    CHCl2CF3 HCFC 1.4 .02 80
    CH2F2 HFC 5 0 677
    CHF2CF3 HFC 29 0 3170

    Free radical formation from the cleavage (breaking) of the C-Cl bond by ultraviolet light can be seen in the reactions below. It is not important for you to memorize these series of reactions. However, it should be noted that chlorine and bromine cause ozone depletion when they are freed from ozone-depleting substances.

    Ultraviolet radiation, denoted by \(h\nu\), breaks the carbon chlorine bond to form two free radicals

    \[ \ce{CF_2Cl_2 + h \nu \rightarrow CF_2Cl^{\cdot} + Cl^{\cdot} }\label{i}\]

    Chlorine atom being highly reactive reacts with ozone (\(\ce{O3}\)).

    \[ \ce{Cl^{\cdot} + O_3 \rightarrow ClO^{\cdot} + O_2}\label{ii}\]

    The monoxide of chlorine further reacts with another molecule of \(\ce{O3}\)

    \[ \ce{ClO^{\cdot} + O_3 \rightarrow Cl^{\cdot} + 2O_2 } \label{iii}\]

    The chlorine atom so obtained reacts with another ozone molecule. Hence, steps \ref{ii} and \ref{iii} are repeated again and again and, leads to the depletion of concentration of ozone.

    Free Radicals and Disease

    Free radicals can be generated by a number of processes. For example, combustion of any material will produce OH (not hydroxide) free radicals. Once inhaled, OH can enter the body and affect cells. Watch the video below to see how free radicals affect biological systems.

    How do antioxidants keep you healthy? Our body is under constant attack from oxidative stress. By wrong lifestyle choices, we make billions of free radicals in our body leading to oxidative stress. This can also increase when we are physically and/or emotionally stressed. Oxidative stress occurs when there is an imbalance of free radicals and antioxidants (too many free radicals and too few antioxidants). It is a condition that results when our body does not have enough antioxidants to counter free radicals in our body.

    Free radical exposure has been linked to cancer, aging, and a number of autoimmune diseases. One way of fighting free radicals is to consume or apply antioxidants. By providing sources of electrons, antioxidants can detour free radicals from attacking healthy cells in the body. The word wall below displays a variety of foods that are rich in antioxidants. Foods and beverages that are rich in vitamins A, C, and E provide sources of electrons for free radicals. Minerals like selenium are also antioxidants. For a more comprehensive list of foods are labeled as being antioxidants, click here.

    antioxy.png

    Figure \(\PageIndex{9}\): Word wall art displaying antioxidants. Image is taken from https://pixabay.com/en/cloud-concept...dants-18527

    Free Radicals and Aging

    Some studies have linked biological free radical production to aging. In a cell's mitochondria, reactive oxygen species are naturally made. These substances damage fats, proteins, and mitochondria DNA. During this process, more free radicals are produced in the cell. Two of these destructive free radicals are superoxide (\(\ce{O2-^{}}\)) and nitrogen monoxide (\(\ce{NO}\)). These radicals have been linked to cancer, skin aging, heart disease, stroke, and other chronic diseases.

    By eating more fruits and vegetables, many nutritionists believe the free radical effect can be reduced in regards to chronic disease. As for aging, many scientists believe that not just one theory can explain why aging occurs. For care of skin, dermatologists recommend that you reduce UV exposure. Ionizing radiation is a source of free radicals that can be minimized. Once the skin has been exposed to UV radiation, there is very little that can be done to counteract its effects.

     roldanfields.jpg

     Figure \(\PageIndex{10}\): Skin comparison of a younger to an older person. Images are taken from: https://commons.wikimedia.org/wiki/F...Hand_aging.jpg and Elizabeth R. Gordon

    Dermatologists and nutritionists recommend a diet rich in antioxidants (vitamins C, E, selenium, and coenzyme Q) to protect skin from damaging free radicals. Lotions, moisturizers, and sunscreens can contain these ingredients as well. 

    Skin Care products

    Watch the following video to understand how to care for your skin

    1. What are the purposes of the Epidermis and dermis in your skin?
    2. What do GAGS do:
    3. How can UVB help the body?
    4. What do the letters ROS represent?
    5. How do free radicals affect DNA, proteins, Fats, and the Dermis?
    6. What types of chemicals help repair damaged skin?
    7. When should the chemicals in question #6 not be used?
    8. How does Salicylic acid make skin appear more youthful?
    9. What is the purpose of applying hyaluronic (it is a humectant) acid to skin?
    10. Why are peptide products useless?
    11. According to this video, what is the best anti-aging product you can purchase?

    Figure \(\PageIndex{11}\) Retinol

    Manufacturers of anti-aging lotions or creams might use the scientific chemical names for the antioxidant ingredients. When purchasing these products, remember to translate them accordingly. Consumers often spend excessive amounts of money on anti-aging creams and lotions. The best way to reduce advanced aging is to protect your skin from ultraviolet exposure. In addition, selecting a skin-care product that contains a combination of some of the antioxidants below is helpful. Lastly, there is no need to pay a large amount of money for an anti-aging product.

    Table \(\PageIndex{2}\): Antioxidants and their effect on skin
    Antioxidant Effect on skin
     Vitamin E ( also known as Alpha-lipoic acid, 3-5%) protects skin from sun damage
     Vitamin A (also known as Retinoic acid, 0.01-0.1%) treats fine wrinkles, age spots, and rough skin
    Flavonoids (extracts from green tea or chocolate) reverses sun damage
    Vitamin B6 treats fine wrinkles and protects skin from sun damage
    Lycopene (a carotene that is present in tomatoes, watermelon, asparagus, and grapefruit) protects skin from sun damage

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