CHEM OF THE ATMOSPHERE Flashcards

1
Q

The atmosphere is a [] mixture of various gases. Its main composition has remarkably steady for ages with [] and [] being the main components. It is the abundance number of [] molecules in the atmosphere that makes life possible on earth.

A

homogeneous
nitrogen
oxygen
oxygen

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2
Q

Nitrogen oxide is a product of combustion through the oxidation of air. Nitrogen at high temperature and can also be produced by []. It can also oxidize into [] which is a precursor of [] and [] formation. Meanwhile, the [] is released by [] and can be converted as nitrogen oxide into the atmosphere.

A

Nitrogen oxide
lightning
nitrogen dioxide
acid rain
smog
dinitrogen oxide
soil bacteria

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3
Q

[] are produced from the oxidation of sulfur-containing fuels and dihydrogen sulfide, H2S. [] is a toxic gas that is produced from biological decay of [] and various human activities such as geothermal and industrial processes.

A

SOx
H2S
organic matter

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4
Q

[] are complex mixture of extremely small particles and liquid droplets. They are existing in different forms such as ocean salt, crystals, soil particles, minerals and metallic compounds. These small particles may come from wildfires, volcanic eruptions, incomplete combustion, mineral processing, industrial processing among others.

A

Particulates and aerosols

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5
Q

The [] is a natural process by which earth maintains the heat on its surface to make life sustainable.

A

greenhouse effect

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6
Q

The [] is the layer of atmosphere of constant temperature found between
the stratosphere and the mesosphere.

A

stratopause

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7
Q

These are light hydrocarbons and unsaturated hydrocarbons and are
precursors to smog formation and organic aerosols. They usually come from incomplete combustion processes, fugitive sources, industrial processes, petroleum processing and solvent intensive processes such as painting.

A

Volatile organic compounds (VOCs)

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8
Q

OH radical with methane and nitrogen dioxide produces [] and []

A

carbon monoxide
nitric acid

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9
Q

It is in this layer where satellites orbit the earth.

A

exosphere

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10
Q

On the other hand, O2 can be consumed if [] collides with [], the process known
as the [] reactions. This process is very slow and if it is the only means by which O3 is consumed, then the ozone layer will be [] than it really is.

A

O
O3
recombination
thicker

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11
Q

An unwanted phenomenon may occur in the troposphere, known as [] This happens when the lapse rate becomes []; hence, the reversal of the normal behavior in the troposphere wherein the cold air at the surface of the earth is overlaid by the warmer air.

A

thermal inversion
positive

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12
Q

However, in polluted environments, [] are also present which when dissolved in [], its pH goes below 5.7. This is how the
formation of acid rain occurs.

A

oxides of sulfur and nitrogen
rain droplets

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13
Q

Above the mesopause is the thermosphere with a lapse rate of [].

A

thermosphere
5 K/km

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14
Q

Processes occurring at the troposphere

The composition of the stratosphere is dependent on the properties of gases that
are present at the [] and the processes they undergo. If the trace gases in the troposphere are [] and do not react with the available [], they will be transported to the stratosphere.

Examples of these gases are
[] and []. However, there are trace gases
that readily react to free radicals and sometimes cause formation of unwanted
compounds in the atmosphere.

A

troposphere
inert
free radicals

chlorofluorocarbons (CFCs)
methyl chloride

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15
Q

refers to the thin air that is made up of a low-density fluid that extends few hundred kilometers from the surface of the earth thus surrounding the planet.

A

atmosphere

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16
Q

The greenhouse effect is primarily due to the augmented emissions of [] and other greenhouse gases into the atmosphere.

[] is the largest contributor to greenhouse effect because it absorbs infrared radiation. It helps in the maintenance of atmospheric temperature during nighttime when the earth’s surface is emitting radiation into space.

The second major contributor is the
[] due to the increase in energy production. Although [] is being absorbed by the oceans and is being used by plants during
photosynthesis, its generation is much faster than being absorbed or used.

A

CO2, NOx, water vapor
Water vapor
carbon dioxide

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17
Q

These may consist of hazardous particulate matter or vapors of metals such
as [] that are generated by combustion and
incineration processes, engine wear, lubricating oil components, lamp
wastes, and mineralization of geologic formations.

A

Metal and metalloid compounds and vapors
Pb, Hg, As, Ni, Be, and Cu

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18
Q

lowest part of the atmosphere. It is where the planet Earth’s weather and air pollution takes place.

A

troposphere

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19
Q

Above the stratopause is the [] with a temperature profile that is like the [], that is the temperature increases as the altitude increases until it reaches the mesopause at an altitude of [] from the surface of the earth.

A

mesosphere
troposphere
85 km

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20
Q

[] are products and by-products of different process such as combustion, industrial activities, natural resource processing and commercial services.

They can be classified as [] (those that are directly emitted to the atmosphere) and [] (those that are products of various chemical reactions in the atmosphere). There are [] groups of air pollutants according to the US EPA (Environment Protection Agency) official Hazardous Air Pollutants (HAPs) list:

A

Air pollutants
primary pollutants
secondary pollutants
10

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21
Q

The [] is the layer of atmosphere of constant temperature found
between the thermosphere and the exosphere.

A

thermopause

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22
Q

These are aromatic compounds of at least three fused aromatic rings and
are hazardous. They are products of incomplete combustion of fossil fuels and vegetable matters, petroleum products and petroleum refineries.

A

Polycyclic aromatic hydrocarbons and derivatives (PAHs)

23
Q

Above the tropopause, is the []. It has a temperature profile that increases with the altitude up to a maximum of about [] and it reaches at around [] from the surface of the earth. The layer’s temperature profile is what suppresses air to undergo vertical motions.

A

stratosphere
273K
50 km

24
Q

the layer of the atmosphere
that contains about 80 percent of the total mass of air and practically all of
the atmosphere’s water vapor.

A

troposphere

25
Q

the term used to describe the homogeneous mixture of gases that makes life on earth sustainable due to its dioxygen molecule component

A

air

26
Q

Major sources of OH is the [] with [] during
daytime, producing excited oxygen atom which rapidly reacts with water vapor.

During nighttime, the [] radical
NO2 reacts with ozone (O3) to produce the
[] radical NO3

Moreover, when the compound [] (PAN, CH3COOONO2) thermally decomposes in the presence of NO also produce OH radicals and convert NO2

A

ozone photolysis
ultraviolet (UV) radiation

nitrite
nitrate

peroxyacetyl nitrate

27
Q

Volcanic eruptions are natural sources of [], while lightnings are natural sources
of []. [] processes remain as the top anthropogenic sources of SOx and NOx.

A

SOx
NOx and ozone
Combustion

28
Q

Under normal conditions, the pH of rain is slightly [] at [] due to the dissociation of dissolved carbon dioxide in water:

A

acidic, 5.7

29
Q

The temperature change within the troposphere with respect to altitude
(known as lapse rate) decreases at a rate of []. The troposphere is the
occurrence of earth’s [] and []

A

troposphere
5 to 6 K/km
weather
air polution

30
Q

Hazardous compounds volatile chlorinated hydrocarbons and polychlorinated dibenzo compounds dioxins and furans belong to this category. They usually come from incineration processes and car emission.
The ozone layer destructing chlorofluorocarbons (CFCs) are also included in this category.

A

Halogenated hydrocarbons and polychlorinated organic compounds

31
Q

[] is a consequence of photochemical reactions based on primary pollutants discharged into the atmosphere. [] has many deleterious effects on human health as well as on plants and materials. Nitrogen oxides and hydrocarbons emitted from vehicles with sunlight and oxygen produce pungent nitrogen dioxide and toxic ozone.

A

Photochemical smog

32
Q

[] oxidants are considered as [] as they are
products of chemical reactions from other pollutants. The common photochemical oxidants are [] (which can be produced through lightning or photochemical reactions), peroxybenzonyl nitrate (PBzN),
peroxyacyl nitrate (PAN), hydroxyl radicals (OH) and nitrogen oxide derivatives.

A

Photochemical
secondary pollutants
ozone

33
Q

is the uppermost layer of the atmosphere. The rise in temperature in this region is the result of the bombardment of molecular oxygen and nitrogen and atomic species by energetic particles, such as electrons and protons, from the sun

A

thermosphere, or ionosphere

34
Q

The ozone is not [] and the UV radiation is converted into []. This is the reason behind the positive lapse rate profile of the stratosphere. Because the stratosphere is warmer compared to the troposphere, an inversion between the two layers occurs. This traps the molecules found in the troposphere.

A

consumed
heat

35
Q

Their presence is due to natural gas or particulate emissions from natural
deposits of uranium where radon is liberated, as well as emissions from
uranium processing, nuclear reactors, and fuel-reprocessing wastes.

A

Radionuclides

36
Q

[], on the other hand, refers to the
effect of global warming to the winds and ocean currents in ways that can cool
some areas and warm others.

A

Climate change

37
Q

The presence of these [] in the troposphere are crucial to the formation of compounds that are responsible to pollution.

A

free radicals

38
Q

The [] is the thinnest layer of the atmosphere (10 km), but it is where all the dramatic events of weather—rain, lightning, hurricanes—occur. Temperature decreases almost linearly with increasing altitude in this region.

A

troposphere

39
Q

The [] is the layer of atmosphere of constant temperature found between
the troposphere and the stratosphere.

A

tropopause

40
Q

In this layer, the gases are thick enough to slow down the meteors hurtling to the atmosphere, which when burn up leave fiery tails in the night sky.

A

mesosphere

41
Q

[] changes the dynamics of air movement resulting in air pollutants to be trapped near the earth’s surface. Prolong occurrence can have several adverse effects on the population’s health such as lung inflammation.

A

Thermal inversion

42
Q

which consists of nitrogen, oxygen,
and ozone. This warming effect is the result of exothermic reactions triggered by UV radiation from the sun

A

stratosphere

43
Q

[] is produced from complete combustion of fuels and metabolic processes while [] is derived from the incomplete combustions processes and from the photochemical transformation of volatile organic compounds (VOCs) by the free hydroxyl radical (OH) generated in the atmosphere such as methane.

Carbon dioxide is considered toxic because it can replace [] by hemoglobin.

A

Carbon dioxide
carbon monoxide

oxygen uptake

44
Q

Combustion of [] leads to the production of main primary pollutant CO, NOx, VOCs and SO2.

A

fossil fuel

45
Q

Another way by which O3 is consumed is catalysis of the recombination reactions
by available [] such as NO*
, NO2 H* OH, HO2 Cl* ClO* and ClO2

The thickness of the ozone layer is therefore due to the competition among these three reactions.

A

free radicals

46
Q

The [] is the layer of atmosphere of constant temperature found between
the mesosphere and the thermosphere.

A

mesopause

47
Q

It is not only the gaseous compounds that have impact to the atmospheric
conditions. Solid and liquid particulates, known as [], also have consequences in atmospheric temperature and climate because they can alter the [] processes of the Earth. An example of which is the [] as a product from the burning of fossil fuels.

A

aerosols
radiative
soot

48
Q

The [] layer of the atmosphere is the exosphere which extends from the
[] to about [] from the surface of the earth.

A

exosphere
outermost
thermopause
10000 km

49
Q

It extends from the ground level to
1- to 15 km.

A

troposphere

50
Q

the concentration of ozone and other gases is low, and the temperature decreases with increasing altitude

A

mesosphere

51
Q

dioxygen molecules are abundant in the atmosphere, they are not considered as the principal oxidative species in the troposphere. This is because
reactions of dioxygen molecules require [] energy compared to that of the free radicals such as the hydroxyl radical,

A

higher activation

52
Q

the concentration of greenhouse gases in the atmosphere is gradually increased. This is trapping more heat from earth resulting for the earth’s temperature to rise. The phenomenon known as the []

A

global warming.

53
Q

Processes occurring at the stratosphere

The stratosphere is where the ozone layer can be found. Stratospheric ozone
protects life in the surface of the earth by screening the harmful ultraviolet rays
from the sun through the [] mechanism.

A

photodissociation