LEC.173 Biogeochemical cycles Flashcards

(45 cards)

1
Q

How is the nitrogen cycle coupled with the carbon cycle?

A

Through organic matter and biological processes

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2
Q

Earth’s disequilibrium is biogenic, what is this mainly caused by?

A

The coexistence of N2 O2 and H2O(l) instead of more stable nitrate.

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3
Q

Nitrogen species: name, and oxidation state for NO3- NO2 and NO2-

A

NO3- nitrate, +5
NO2 nitrogen dioxide, +4
NO2-, +3

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4
Q

Nitrogen species: name, and oxidation state for NO N2O N2 and NH3/R-NH2

A

NO nitric oxide, +2
N2O nitrous oxide, +1
N2 nitrogen, 0
NH3/R-NH2 ammonia/amino, -3

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5
Q

NO and NO2 are important air pollutants, which one is a free radical?

A

Nitric oxide

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6
Q

Global nitrogen reservoirs?

A

Fixation, terrestrial biomass, atmosphere, river runoff, denitrification, soil, sediments, marine biomass, ocean, sedimentation

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7
Q

Global nitrogen fluxes?

A

Natural terrestrial, natural oceanic, leguminous crops, chemical fertiliser, combustion, biomass burning, weathering

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8
Q

4 nitrogen fixation reactions to convert N2 (inert) to reactive forms of N?

A

Anaerobic microbial reduction to NH3
Reduction to NH3 by Haber-Bosch process
Oxidation to NO by lightning
Oxidation to NO by anthropogenic, high T-P combustion processes

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9
Q

Anaerobic microbial reduction to NH3?

A

2N2 + 6H2O -(nitrogenase)> 4NH3 + 3O2
- done by various bacteria
- dominant fixation process over geological time

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10
Q

Reduction to NH3 by Haber-Bosch process?

A

N2 + 3H2 -(high T-P and metal catalyst)> 2NH3
- explosives and fertilisers
- helps to feed an increasing global population
- large amount of N lost to the environment via inefficient use

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11
Q

Oxidation to NO by lightning?

A

N2 + O2 + energy -> 2NO (nitric oxide)
- <5% of fixation

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12
Q

Oxidation to NO by anthropogenic, high T-P combustion processes?

A

N2 + O2 + fossil-fuel energy -> 2NO
- bi product of combustion processes

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13
Q

Ammonification? what to what

A

Organic nitrogen -> NH4+

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14
Q

Nitrification? what to what

A

NH3/NH4 -> NO2- -> NO3-

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15
Q

Denitrification? what to what

A

NO3- -> N2

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16
Q

What forms of N can be taken up by plant roots?

A

Nitrates and ammonium

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17
Q

In aerobic soil is nitrate or ammonium the dominant form of N found?

A

Nitrate

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18
Q

Assimilation by autotrophs, bacteria, archaea ?

A
  • ammonia assimilation
  • assimilatory nitrate reduction i.e. NO3- absorbed and convert to amino-N
  • e.g. algae in oceans
  • ammonia uptake is important in flood fields e.g. rice production
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19
Q

Ammonification (mineralisation)?

A
  • biological conversion of organic-N to ammonia (i.e. inorganic reactive N) under anaerobic conditions
  • part of energy production system of these organisms
  • e.g. heterotrophic bacteria
20
Q

Nitrification?

A
  • microbial step-wise conversion of Nh3/NH4+ to NO3- under aerobic conditions
  • part of the energy production system of some bacteria and archaea
  • nitrosomonas NH3 to NO2- - very efficient process in soils
21
Q

Denitrification?

A
  • microbial step-wise anaerobic respiration processes, i.e. energy yielding
22
Q

Why do mercury levels get much quicker change than e.g. nitrogen?

A

Big human health impact of mercury, so quicker reaction than to things that have environmental impacts.

23
Q

Photosynthesis eqn is actually very simplified, whats two steps that give a more detailed description of photosynthesis?

A

step 1 - a photolytic reaction involving capture of photons by chlorophyll and resulting oxidation of O in water

H2O(-II) + hn -> 2H+ + 2e- + ½O(0)2

step 2 – series of reactions, e.g. Calvin cycle - can be regarded as reduction of C by the electrons released

C(IV)O2 + 4H+ + 4e- -> C(O)H2O

23
Q

Photosynthesis eqn?

A

6CO2 + 6H2O + hv = C6H12O6 + 6O2

24
From a chemical perspective whats a more meaningful representation of photosynthesis?
6C(IV)O2 + 12H2O(-II) -> C(0)6H12O6 + 6O(0)2 + 6H2O
25
What are the main environmentally important biochemical reactions associated with creation and destruction of OM?
photosynthesis and respiration
26
Autotroph?
Primary producer Utilises inorganic C sources such as CO2 and HCO3-
27
Heterotroph?
Secondary producer Utilises complex C sources - C from pre-formed organic compounds - diverse range of organisms
28
Oxygenic photosynthesis?
CO2 + H2O + hv → Ch2O + O2 - dominant source of biomass today and much of geological time - e.g. plants, algae, cyanobacteria - not first to evolve, end product - light limitation - generates O2
29
Anoxygenic photosynthesis
6CO2 + 12H2S (source of electrons) + hv → C6H12O6 +12S +6H2O - globally very minor source of biomass today - e.g. purple sulphur bacteria - evolved before oxygenic photosysnethis
30
Chemoautotroph?
- inorganic C source, independent of light - energy from oxidising reduced inorganic compounds - productivity independent of light - important in soils, sediments, hydrothermal vents - mainly bacteria and archaea (single cells, no nucleus - prokaryotes) e.g. nitrification
31
Photoheterotrophs?
energy from sunlight, e.g. purple non-sulfur bacteria (cannot use CO2 as sole carbon source)
32
Chemoheterotrophs
energy from oxidation of pre-existing reduced compounds – normally organic compounds (organotrophs). But can be inorganic compounds (lithotrophs) - many bacterial examples. (do not use CO2 e.g. cyanobacteria N2 fixing producing NH3)
33
Aerobic respiration?
CH2O + O2 → CO2 + H2O - O2 is external or terminal electron acceptor (oxidising agent) - preferred energy yielding reaction, as maximum energy yield per mole of glucose - e.g. animals, plants, algae, bacteria, protozoa, fungi - Gibbs = -2880kJ per mole C6H12O6
34
Anaerobic respiration?
- use various terminal electron acceptos, other than O2 - occupy hypoxic/suboxic (<~0.1 mg/L or 3 M O2) and anoxic environments - e.g. some bacteria, archaea, protozoa e.g. denitrification is a type of anaerobic respiration
35
Fermentation?
- anaerobic, energy yielding rxns, involves redox changes to C in large organic molecules but with no external oxidising agent. - e.g. bacteria and fungi (yeast) - limited environmental importance
36
Methanogenesis?
(previously regarded as a form of fermentation) e.g. acetic acid - small entitle molecules, methane produced (important GHG), archaea e.g. in digestive tract of cows
37
Weathering: dissolution?
- water as a medium to break a mineral down into its constituent elements - water not active in the reaction
38
Weathering: hydrolysis?
- Rxn with water, generally leading to an excess of H+ or OH-
39
Weathering: acid-base rxns?
Faster than dissolution and hydrolysis, and generally more important. Weathering as a global acid-base rxn.
40
Weathering: redox rxns?
Oxidation fog minerals by O2 OILRIG
41
Weathering: example of dissolution?
CaCO3, one of the fastest weathering rxns CaCO3(s) -> Ca2+(aq) + CO32-(aq) Apatite dissolution (most common P mineral)
42
Weathering: example of hydrolysis?
Alumino-silicate weathering
43
Weathering: example of acid-base rxns?
CaCO3 + H2CO3 -> Ca2+ + 2HCO3-
44
Globally significant effects of weathering?
- atmospheric CO2 concs - soil development - water chemistry - economic mineral deposits