CO2 causes global warming.
Environmental Chemistry
Greenhouse gases are CO2, CH4, Water vapour, Nitrous oxide, CFCs and ozone.
The breakdown of ozone in the stratosphere largely involves a series of reactions often initiated by free radicals, such as chlorine (Cl), bromine (Br), or nitric oxide (NO) radicals.
In particular, chlorine atoms, which can come from substances like chlorofluorocarbons (CFCs), can catalyze the destruction of ozone.
The first three reactions listed are all part of the ozone breakdown process: Option A: This is the photodissociation of a chlorofluorocarbon, which releases a chlorine atom (a free radical) that can participate in ozone destruction.
Option B: This reaction shows a chlorine atom catalyzing the destruction of ozone, forming ClO and O2.
Option D: This reaction shows a ClO radical reacting with a single oxygen atom to regenerate the Cl radical and form O2.
The regenerated Cl radical can then go on to catalyze more ozone destruction, making this a catalytic cycle.
However, option C:
This reaction is not typically part of the ozone breakdown process.
Chlorine monoxide (ClO) radicals generally react with atomic oxygen (O), not with another ClO radical, to regenerate the chlorine radical and produce oxygen (O2).
The product of this reaction, ClO2, does not commonly appear in the standard ozone depletion mechanisms.
Biochemical oxygen demand (BOD) is amount of oxygen required by bacteria to break down organic waste in a certain volume of water sample.
Freons are a family of chlorofluorocarbon (CFC) compounds, which are chemicals that contain chlorine, fluorine, and carbon atoms.
They are used in a variety of applications, including refrigeration and air conditioning, as well as in aerosol spray cans.
Photochemical smog contains oxides of nitrogen, ozone and hydrocarbons.
The F
ions make the enamel on teeth much harder by converting hydroxyapatite, [3Ca3(PO4)2] .
Ca(OH)2], the enamel on the surface of the teeth into much harder fluroappatite.
[3Ca3(PO4)2 .
CaF2]
The radical that mainly causes ozone depletion in the presence of UV radiation is .
The chloro radical reacts with ozone molecules to form chlorine monoxide and oxygen:
This reaction depletes the ozone layer, as the chlorine monoxide can then go on to react with another ozone molecule:
Thus, , is the correct answer.
The formation of photochemical smog depends on several factors, including sunlight, temperature, and the presence of pollutants such as nitrogen oxides and volatile organic compounds.
Option (A) Mumbai in May may also have some possibility of photochemical smog formation because the temperature and sunlight are relatively high in May.
Option (B) Kolkata in October may have some possibility of photochemical smog formation because the temperature and sunlight are still relatively high in October.
Option (C) New-Delhi in August (Summer) is more likely to have photochemical smog formation because the temperature and sunlight are at their peak in the summer months, and there is a high level of air pollution in the city due to various anthropogenic activities.
Option (D) Srinagar, Jammu and Kashmir in January is less likely to have photochemical smog formation because the winter season typically has less sunlight and lower temperatures, which are not conducive to the formation of photochemical smog.
Therefore, the answer is (D) Srinagar, Jammu and Kashmir in January, as it is the option with the least possibility of photochemical smog formation.
Clean water would have BOD value of less than 5 ppm whereas highly polluted water could have a BOD value of 17 ppm or more.