Nitrogen And Phosphorus in the Atmosphere Flashcards

1
Q

Why is nitrogen important ?

A

It is the most important nutrient for plants. Nitrogen availability plays a vital role in photosynthesis

Important component of the enzyme ( rubisco) that controls the rates of biochemical reactions( photosynthesis). Nitrogen are building blocks of Amino acids and the N in the DNA

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2
Q

How much of the atmosphere is nitrogen?

A

78 %

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3
Q

What is the total mass of nitrogen in the atmosphere?

A
  1. 9 x1015 tonnes
  2. 9 x 109 megatonnes
  3. 9 x106 gigatonnes

If you convert the 78 percent into parts per millio you get 780 000 ppm in the atmosphere

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4
Q

Why is there so much nitrogen in the atmosphere?

A

N2 is an ‘even’ nitrogen molecule - it’s relatively unreactive and therefore the nitrogen is not rly available to do used by biology so builds up in the atmosphere

The two N atoms have a triple bond ( 3 pairs of electrons shared between the 2 N atoms). The nitrogen triple bond is strong. Takes a lot of energy to break.

This makes N2 almost inert, except for high energy events such as lightning

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5
Q

What are the 6 stages of the nitrogen cycle ?

A

1) Nitrogen fixation
2) Ammonia assimilation
3) Nitrification
4) Assimilatory nitrate reduction
5) Ammonification
6) Denitrification

NANA :
D

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6
Q

What is nitrogen fixation? What different types of bacteria help the process? Give examples of specific bacteria for each example and the relationship

A

1)Nitrogen fixation is any process by which N2 (gas) in the atmosphere is converted to any form of nitrogen that is more useful to organisms. Biological fixation is the enzyme catalysed reduction of ammonia ( HN3-), Ammonium (NH4+) or any other organic nitrogen
Nitrogen fixation is carried out by nitrogen fixing bacteria. They convert the nitrogen into ammonia using a reduction reaction catalysed by the enzyme nitrogenase.
Can get Bacteria that are free living and live in soil or water. Many species such as Azotobacter colonise the rhizisohere ( rioting zone) of many plant species but do not depend directly on the plants

.Some of these bacteria live in special swellings on the roots (known as root nodules) of plants called legumes. The bacterium receives water and sugars from the plant and in return supplies the plant with ammonia. The ammonia can be used later to make proteins and other nitrogen containing organic compounds which are required by the plant, such as nucleic acids. This mutually beneficial relationship between the bacteria and the plant is an example of symbiosis.

First, the atmospheric N2 diffuses into the soil air. Then it is fixed by the bacteria in the soil.

The best known examples are Rhizobium species which form root nodules on peas, bean, clover

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7
Q

What is ammonia assimilation?

A

2)The process by which HN3- or NH4+ is taken up by an organism to become part of its biomass in the form of an organic nitrogen compound like amino acids or DNA.

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8
Q

What is nitrification?

A

3)Nitrification is the oxidation of ammonia (HN3-) or NH4+ to NO2- or NO3- by an organism, as a means of producing
This process is carried out by bacteria called nitrifying bacteria. These bacteria
transform ammonium ions into nitrates.This releases energy which they use for the synthesis of organic molecules such as carbohydrates. For this reason, these bacteria are described as autotrophs.

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9
Q

What is assimilatory nitrate reduction?

A

4)Assimilatory nitrate reduction is the reduction of NO3- followed by the uptake of nitrogen by the organism as biomass ( plants). Plants can then be consumed and nitrogen flows through food webs/chains

So uptake of NO3- or nh4+ as biomass
The inorganic nitrogen is taken up by plants from the soil, largely in the form of nitrates which is then used to synthesise nitrogen-containing organic molecules such as proteins or DNA. These move into other organisms when they eat the plants, and digest and absorb the organic compounds.

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10
Q

What is ammonification?

A

5)
This is the breaking down or organic nitrogen compounds to HN3- or NH4+

Nitrogen is passed through food chains in the form of organic compounds, e.g. proteins & DNA. When organisms die, excrete urea or egest faeces, decomposers such as bacteria and fungi convert the organic nitrogen locked up in these organic compounds into ammonia.

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11
Q

What is denitrification?

A

6)

This is the reduction of NO3- ( nitrates) to any gaseous nitrogen species, generally N2 or N2O

This often happens under anaerobic conditions

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12
Q

What is fixation again generally?

A

To make N available to plants and animals, it must be fixed (combined) in the form of ammonium (NH4)

Fixation is conversion of nitrogen from a relatively stable form to something that can be used by plants

This fixation may either be natural or anthropogenic (human)

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13
Q

What is Nitrification again generally?

A

It is the bacterial conversion of NH4+ intro nitrites NO2–) then nitrates (NO3-)which is a form than can be used directly by plants

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14
Q

Describe the anthropogenic nitrogen fixation

A

Main human processes ( 1/3 of total -2/3 is natural processes) are fertiliser production and combustion

Driven by our desire to increase agricultural production

Fertilisers ( planned fixation) 
Ammonium sulphate -21
Ammonium nitrate -33.5
Urea (NH2)2CO - 45
Liquid ammonia -82

Trace amount of accidental fixation which occurs due to combustion

Some N in fuel is oxidised to NO or NO2
Some of the N2 in the fuel is oxidised to NO or NO2

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15
Q

How much non biological N and biological N is fixed Global, MT:year

A

Non biological - 80

Biological -175

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16
Q

What is the rate of use per year of nitrogen ? Why doesn’t nitrogen run out?

A

200 Mt per year

Total N in atmosphere = 4 x109 Mt

Should all have been used up since should only take 20million years Nd earth is 5000 million years

Because denitrification!

Bacterial process which converts nitrates into N2 and returns it to the atmosphere)

This also produces N2O and NO

17
Q

Why doesn’t the N2O concentration keep increasing?

A

N2O has a long lifetime in the troposphere (the lowest region of the atmosphere, extending from the earth’s surface to a height of about 6–10 km (the lower boundary of the stratosphere)

Eventually it diffuses up into the stratosphere
In the stratosphere there is a high UV flux density and the N2O Is bombarded with UV radiation

( above stratospheric ozone layer) Interacts with photons less than 250 nm ( UV-C light) and this high amount energy can break up the N2O molecule into N2 and O

18
Q

What are odd nitrogen in the atmosphere ?

A

Present both in gases and particles

The particles may be solid or liquid, and they may be small enough to remain suspended in the air for days ( aersols), or large enough to fall out

Nitric oxide ( gas)- N2O IMPORTANT
Nitrogen dioxide (gas)
HNO2 - nitrous oxide (gas/liquid)
HNO3 - nitric acid (gas/liquid)

19
Q

How does the odd nitrogen get back out of the atmosphere? What are the different types of these and describe them

A

Diffusion - diffusion of gas molecules and particles from the atmosphere to surfaces ( area of high concentration to low) down a concentration gradient

Note this is dry deposition:

Turbulent diffusion: the bulk movement of large number of molecules; cannot operate close to surfaces - close to sources or in remote areas

Molecular diffusion; important close to surfaces, but only for gases deposition of particles by impactation from the wind onto surfaces ( leaves etc)

20
Q

Describe wet deposition

A

Deposition by incorporation into cloud droplets and then rain drops

Gases can be dissolved into the cloud water droplets

Particles can be the nuclei around which cloud droplets form

Falling raindrops can collect particles and dissolve more gases

Cloud droplets May impact onto surfaces ( e.g leaves) without forming raindrops

21
Q

How are nitrogen compounds involved in climate change?

A

N2O is a very potent greenhouse gas

GWP ( greenhouse warming potential) of 109 years, compared to GWO of 30 for methane

Most N2O is derived from bacterial denitrification so its associated with land use and agricultural practices

22
Q

Discuss stratospheric ozone destruction with nitrogen oxide

N2O = nitrous oxide
NO = Nitric oxide
A

O3 + NO = O2 + NO2

NO2 + O = NO + O2

O3 + O = 2O2

Chemistry don’t rly need to go over?

NO is derived from the photolysis of N2O

However, not all the NO is reacted with O3 some reacts to with the hydroxyl radical (•OH) to produce nitrous acid ( HNO2)

This is not involved in O3 ( ozone destruction) so overall there is a reduction in O3 removal by NO

Not a fully closed system - NO used up so not a perfect catalyst

23
Q

Polar stratospheric clouds?

A

They form in high altitudes.

You have CLOx —-> NO2 (dioxide
|
CH4
Outside stratospheric clouds which can reacts to form ClONO2 (chloro-nitrate) which is relatively stable and inert and HCl which is relatively soluble and rapidly rains out on the system.
So no real build up of chlorine in atmosphere when outside of the polar stratospheric clouds

In Winter the atmosphere in Antarctica gets really cold which leads to the formation of high altitude of polar stratospheric clouds

Within these clouds you have the process of denitrification. Where the chloronitrate and HCl denitrify yo give you HNO3 ( nitric acid) which forms as ice crystals on the surfaces of the clouds. And the denitrification liberates chlorine

24
Q

Discuss stratospheric ozone destruction with nitrogen oxide

N2O = nitrous oxide
NO = Nitric oxide
A

O3 + NO = O2 + NO2

NO2 + O = NO + O2

O3 + O = 2O2

Chemistry don’t rly need to go over?

NO is derived from the photolysis of N2O

However, not all the NO is reacted with O3 some reacts to with the hydroxyl radical (•OH) to produce nitrous acid ( HNO2)

This is not involved in O3 ( ozone destruction) so overall there is a reduction in O3 removal by NO

Not a fully closed system - NO used up so not a perfect catalyst

25
Q

Polar stratospheric clouds?

A

They form in high altitudes.

You have CLOx —-> NO2 (dioxide
|
CH4
Outside stratospheric clouds which can reacts to form ClONO2 (chloro-nitrate) which is relatively stable and inert and HCl which is relatively soluble and rapidly rains out on the system.

So no real build up of chlorine in atmosphere when outside of the polar stratospheric clouds

In Winter the atmosphere in Antarctica gets really cold which leads to the formation of high altitude of polar stratospheric clouds

Within these clouds you have the process of denitrification. Where the chloronitrate and Hcl denitrify to give you Nitric acid (HNO3) and this forms as ice crystals on the surfaces of the clouds and the denitrification liberated chlorine. So you get a build up of chlorine on these cloud surfaces

Come the Antarctic spring you have daylight arriving in the system and this drives photo dissociation and acts upon the chlorine and this liberates vast amount of chlorine that had been built up in the winter to drive ozone depletion and form this catalytic conversion of ozone into oxygen.

So polar stratospheric clouds low key drive ozone depletion

So outside stratospheric clouds clox reacts with NO2 to form ClONO2 and CLOx reacts with ch4 to produce HCl

26
Q

How do the northern and Southern Hemisphere differ in ozone depletion?

A

The northern hemisphere does have ozone decline but much less sporadic and less pronounced than the Southern Hemisphere

This is driven by climate. Southern Hemisphere has high production of polar stratospheric clouds. Northern hemisphere has far fewer polar stratospheric clouds as temperatures in winter in artic nowhere near as could as Antarctic. Far less denitrification and far less chlorine being stored

Polar stratospheric clouds lead to the production of free radicals Pf chlorine in stratosphere which directly destroy ozone molecules

27
Q

How are nitrogen compounds involved in photochemical smog and what is photochemical smog ?

A

Photochemical smog is ozone formation in the troposphere ( so in atmosphere we interact with on a daily basis so it is bad ozone). This bad ozone is highly reactive and can cause cell death in plants. Decrease in yield and seed mass . A way to combat this is the use of nitrogen fertiliser onto soil but that is broken down through denitrification which produces these compounds which can drive further smog

Good ozone and ozone layer is usually found in the stratosphere

It’s driven by photolysis ( in presence of sunlight) of nitrogen compounds

NO2 + hv NO + O

O + O2 O3

You get a brown haze across cities.

Net reaction: NO2 + O2 NO + O3 ( cancel out the Os)

28
Q

Where is photochemical smog usually found?

A

They develop in areas of high urban density. In India and China. Lots of combustion and photochemical reactions

29
Q

Tell me about the occurrence of phosphorus

A

Phosphorus = light bringing - white phosphorus spontaneously combusts in Air, burning to pentoxide. It is insoluble in water

Not found free in the natural environment. Natural occurrence - phosphate rock

Large deposits in Russia, Morocco and USA and very toxic

50 Mg fatal by ingestion

0.1 mg m-3 inhalation limit

30
Q

What are the uses of phosphorus

A

One set of used based on reactivity: matches, pyrotechnics, smoke bombs

General chemical properties: steels; specialised glass

Essential component of all cell protoplasm, nerve tissue and bones

Major production is based on importance as a plant nutrient, I.e. fertiliser

Used to make a superphosphate fertiliser ( e.g ammonium phosphate)

31
Q

Talk about phosphorus in the atmosphere

A

No significant gaseous component

The main sources to the atmosphere are dust from weathering/ soil erosion

Dust from industrial processing ( e.g fertiliser production)

Sea spray

Total atmospheric flux small compared to water and soul fluxes

32
Q

Compare nitrogen with phosphorus

A

Whereas most of the nitrogen pool is in the atmosphere, most of the phosphorus pool is in rock

There is no biological route for recycling

Renewal of the supply needs plate tectonics I.e the phosphate ion in soils and lakes are sedimented and phosphate in rocks are eroded

Timescale for P cycling is therefore 10^8 years