The consequences of acid rain on our environment
By Barbaroux Florent and Michel Yann
| 1. Observation 2. Question 3. Hypothesis |
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| 1. Experimental protocol 2. Results 3. Interpretation |
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| Checking of the hypothesis and broadening | |
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subquestions
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- What are lichens ? - The different lichen species - We can use lichens to now quality of environnement |
1. Observation :
Acid deposition can take two forms : acid precipitations, which forms
the "acid wet deposition", or acid gases and salts, which form the "acid dry
deposition".
Precipitations are naturally acid, because of the atmospheric carbon dioxide
(CO2), which, dissolved in the water, makes some carbonic
acid (H2CO3). The natural acidity
of the precipitations is about pH=5,6. Below this value, the precipitations
are known as "acid precipitations".
Acid deposition is distributed as this world chart shows us :
But, in many industrial countries,
we can observe that the precipitations are more acid than the natural value,
for instance :
- In France, the common acidity of rains is pH=4.5 and the acidity of fogs
and drizzle can reach pH=3.
- The acidity can be higher : in the USA, the acidity reached pH=2,3 in 1978
and pH=1,5 in 1979.
The great acidity of the precipitations is due to the presence of pollutants in the atmosphere, which react with the water molecules , thanks to a catalyst, the hydroxyl (OH), to form acids : sulphuric acids (H2SO4) and nitric acids (HNO3).
The mechanism of the formation of the acid precipitations is the following
:
- Cis of the O3 molecules in the stratosphere : O3=O2+O
- Formation of the catalyst, OH : O+H2O=2OH
- Formation of the sulphuric acid H2SO4
: first O2+SO2+OH=SO3+HO2
... then H2O+SO3=H2SO4
... or 2HO2=H2O2+O2
... then H2O2+SO2=H2SO4
- Formation of the nitric acid HNO3 : either NO2+OH=HNO3
... or NO+OH2=NO2+OH ... then
NO2+OH=HNO3
These pollutants, which are sulphur dioxide (SO2) and nitrogen oxides (NOx), can come from natural sources (like volcano), but they mainly come from the human activity :
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But a part of the pollutants do not react with the water and can be transformed into gases or salts which fall on the ground by the influence of the gravity. This gases and salts formed the acid dry deposition.
By falling on the ground, acid precipitations and acid gases
and salt, form the acid deposition : 
Here is the cycle of acid precipitation :
We are about to study the acid wet depositions called "acid rains" or "acid precipitations".
2. Question :
What are the consequences of the acid deposition on our environment,
more precisely on the flora ?
3. Hypothesis :
Acid precipitations may attack the plants slowly, causing
the death of these plants.
| We will need : - Some lichens we took from the trees around the school. These lichens are from a polluted area, so they resist more to the acidity than lichens from a clean area. |
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We crushed the lichens in order to increase the exchange area between
cells and the solution. Then we put the lichens pieces in three vats
like this one : When we obtain the desired acidity, we add 7 mL of the solution in the vat, so that when we put the probe inside, there is no remaining air in the medium. We activate the agitator to facilitate the exchange between the cells and the solution. |
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Then we launched the software measuring the photosynthesis of the lichens contained in the solution which created the graph indicating the concentration of oxygen in the solutions for 10 minutes.
After the experiment, we closed the vats containing the solutions so that they would not evaporate, and therefore the solutions will be able to work on the lichens. We waited for a month.
2. Results| Solution 1 : oxygen's concentration and photosynthesis in a pure tap water solution (PH = 7.5) according to time. | ![]() |
| Solution 2 : oxygen's concentration and photosynthesis in an acid solution (PH = 4.5) according to time. | ![]() |
| Solution 3 : oxygen's concentration and photosynthesis in another acid solution (PH = 1.5) according to time. |
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Solution 1 : oxygen's concentration in a pure tap water solution (pH = 7,5) according to time. Solution 2 : oxygen's concentration in an acid solution (pH = 4,5) according to time. Solution 3 : oxygen's concentration in another acid solution (pH = 1,5) according to time. |
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3. Interpretation
In the first part of the experiment, we can explain the
decrease of the oxygen's concentration in the solutions by the lichen's breath.
In fact, there is no reason for chimical oxydation in the water that don't
contain many oxygen molecules, so the reason for this decrease is a biochimical
one : the only one possible is the breath of the lichens. Let us recall that
the reaction which allows for breathing is the following : C6H12O6+6O2=6CO2+6H2O+energy,
and happens in the presence of enzymes catalysing the reaction of C6H12O6
molecules. Moreover this reaction can happen only in live beings, so we can
say that the lichens are still alive in all of the solutions in the first
part of the experiment.
We thought that if we did not observe any photosynthesis (except for the third
solution), this reaction being the reverse of the breath (6CO2+6H2O+energy=C6H12O6+6O2),
although there was not any light and heat, it is because the lichens were
in period of slowed down life, the normal reaction of plants in the winter
which allowed them to protect themselves from external conditions, so the
enzymes catalysing this reaction did not work, and so the reaction did not
happen.
![]() diagram of a alive lichen of thallus type |
![]() photograph of the cut of this alive lichen |
In the two acid solutions (pH=4,5 or pH=1,5) we observed that the oxygen's concentration had not increased or decreased, so the lichens did not breath, so they were died. We could deduce that the acidity of the acid solutions, contrary to the first solution, was strong enough to attack the phycosymbiote and to destroy it. Then, acidity finally reached and destoyed the cells of the mycosymbiote that allowed the lichens to breath and to produce photosynthesis. So, the acidity killed the lichens.
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More generally, in the areas concerned by acid deposition,
plants are more or less the target of the acid deposition, which cause,
with time, an attack at the cellular level, killing gradually the
plants.
Now we know that acid deposition has an impact on plants, but it also has an impact on animals and also on humans. |
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Acid deposition can increase the impact that climatic
conditions have on buildings, and particularly on old buildings built
with limestone, marble or sandstone. In fact, acid rain dissolve their
calcium carbonate, creating layers of calcium sulphate or gypsum which
are removed more easily by precipitation. Thus, in the whole world,
monuments and old buildings need continuous renovation because they
were built with these materials, that is not the case of new buildings.
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In aquatic environments, acidity in water can cause the death of some animals (first micro-organisms like insects and planktons from a PH of 6), which gradually spoils the food chain of this ecosystem. It can also cause the death of all animals when the PH is below 5. We can also observe this phenomenon for land animals, but it is less effected if these animals do not take part in the water ecosystem.
Finally, on this picture we can see the indirect effects
of the acid deposition on humans (along with also the effect of fertilizers)
: acid rain falls onto the ground which provides food to animals, and
which produces fruit and vegetables. However, meat and products from the
ground constitute the food for humans. To eat such food can induce various
bad effects on human health, amongst which magnesium deficiency :
What can we do to limit the phenomenon of acid deposition ?
As the the pollutants causing acid deposition mainly come from useless
trips in cars and excessive consumption of electricity, the first advice
we can give you is not to only use your car for small journeys and to
shut down all your apparatuses using electricity when you have finished
using them.
Then, there are a lot of things we can do :
- Only run the dishwasher and the washing machine with a full load.
- Turn off all the lights when you leave a room.
- Turn off the electricity and the hot water water tank when you will
not be at home for a long period of time.
- Turn down the heat when you are not at home.
- Do not use your air conditioner as much.
- Install fluorescent light bulbs instead of incandescent light bulbs.
- Try to reduce, reuse, and recycle as often as you can.
- Try not to burn a fire as often as you usually do.
- When you are going to work : you could walk, ride, bike or take a bus.
- Car-pool to a place with someone else.
- For alternate fuels, try ethanol, propane or natural gas.
- Take a train or a bus for long trips.
- Limit the amount of long trips you take in your car.
- Make sure that your vehicle's air conditioning system isn't leaking.
- Try not to overflow the gas tank.
- Try to respect the speed limits...
TEXT :
" Les lichens témoins de la pollution, by S. Déruelle and R. Lallemant
- http://crdp.ac-amiens.fr/enviro/air/air_maj6_detail_p1.htm
- http://www.atl.ec.gc.ca/msc/as/acidfaq_f.html
- http://www.senat.fr/rap/l02-215-2/l02-215-22.html
according to IFEN
PICTURES and DIAGRAMS :
- http://www.dec.ny.gov/
What are lichens?
Symbiosis :Lichens are formed from a combination of a fungal partner,
this is the fungus which is termed by scientists mycobiont, and an algal partner,
this could be an algae or cyanobacteria which is termed by scientists phycobiont.
This symbiosis can't be formed by each algae and fungus. When the symbiosis
can be formed, they make a unique type of thallus. Before the lichen is formed
the algae and fungus may lives in nature without its partner. When the thallus
is formed they can't survive without each other. The morphology from the individual
fungus is quite different from the morphology from the lichen.
Fungus / Mycobiont : The fungal partners are mostly (over 95%) Ascomycota,
and a few fungus (approximately 20 sorts) are Basidiomycota. Almost half of
the recorded fungus in the world are Ascomycota, and nearly half of these
are found only in lichens. One sort of fungus is only used by one sort of
lichen. So the names of lichens are grounded on the fungus. Only 20% of the
recorded fungus in the world are used to make lichens. The mycobiont has two
roles in the lichen symbiosis: to protect the photobiont to intense sunlight
and to absorb mineral nutrients.
Algae / Photobiont : There are only about 100 algal partners, so one
sort of algae is used to make different species lichens. Not all the algal
partners can exist in all species habitats, with these a lichen has a small
habitat. But normally a lichen has a great distribution. In alpine regions
single-celled green algae of the genus Trebouxia and Cladonia are the most
common. Trebouxia is specialised in lichen symbionts. In Mediterranean and
tropical regions especially grow green algal genus Trentepohlia. Also Cyanobacteria
can be used as algal partner. But only 10% of lichens have cyanobacteria as
partner. Sometimes a lichen exist from a green algae and a cyanobacterium,
these lichens are termed cephalodia. Only 3-4% of the recorded lichens have
this structure. The photobiont has two roles: to make organic nutrients from
carbon dioxide and to produce ammonium from N2 gas.
Reproduction : There are two different forms to reproduct. Lichens
can reproduct with non-sexual reproductive packages like soredia and isidia.
1. Soredia is a form to reproduce itself, when a cluster of algal cells wrapped
in the fungus this forms a new lichen after the disperse.
2. Isidia is like Soredia but is enclosed with a little skin, like a tissue.
To form a new lichen, fungus can produce spores, the fungal spores need new
photosynthetic partners. Some steal them from other lichens, others have partners
upon themselves.
Information : The alga will begin to use sunlight to make sugars or
food which will feed both the fungus and the alga. The fungus will create
a thallus or body that will house both organisms. Thus, through the lichen
partnership, the photobionts are protected and able to grow in conditions
in which they could not grow alone; they also benefit from the highly efficient
uptake of mineral nutrients by the lichen fungi. The fungi, in turn, obtain
sugars and in some cases organic nitrogen from the photosynthetic partner,
enabling them to grow in environments deficient in organic nutrients.
Life History & Ecology : Lichens will grow almost anywhere that a stable
and reasonbly well-lit surface occurs. This may include soil, rock, or even
the sides of trees. A lichen may absorb certain mineral nutrients from any
of these substrates on which it grows, but is generally self-reliant in feeding
itself through photosynthesis in the algal cells. Thus, lichens growing on
trees are not parasites on the trees and do not feed on them, any more than
you feed on the chair you sit in. Lichens growing in trees are simply using
the tree as a home. Lichens growing on rocks, though, may release chemicals
which speed the degradation of the rock into soil, and thus promote production
of new soils. Most lichens are temperate or arctic, though there are many
tropical and desert species. Lichens seem to do better in drier environments,
where they are not often left in standing water. What the lichen considers
dry, however, may not be what we would consider to be dry. In bayous and in
cool rainforests, large lichens known as "old man's beard" may often be seen
hanging from the branches of trees. Though there is considerable water in
these habitats, the air is not saturated, and drying breezes may serve to
dessicate arboreal organisms.
Growth and Development : Like all living things lichens need nutrients
and energy to grow. Nutrients they obtain from the air (including dust), water
and some from the substrate they are growing on. Energy they obtain through
photosynthesis, which is the role of the algal partner. They can also be incidentally
fertilised by bird and insect dung. Lichens will and do grow on just about
everything, natural or manmade. Different species of lichens prefer, or only
grow on different substrates. Thus some species will be found on smooth barked
trees, some on rough barked and some on only one species of tree. Also some
lichens grow on basic rocks while others only grow on acidic rocks and some
have particular mineral requirements, thus Acarospora sinopica only grows
on rocks with a high iron content. However where ever they grow lichens grow
slowly so what ever it is they are growing on, the 'substrate' needs to have
been around for a few years. Lichens grow differently at different times in
their lives. When young and very small they grow slowly, then once they are
reasonably well established they grow much more quickly, obviously when they
are dying, for what ever reason they grow more slowly again, or not at all.
Lichens grow by extending their thallus outwards, from either its tips or
edges. They grow very slowly, some species more slowly than others. Rates
of growth can vary from 0.5mm per year to 500mm per year. Their slow growth
rate equates with their long life. However the question "How long does a lichen
live?" is difficult to answer. The reasons for this are twofold. Firstly because
they can reproduce vegetatively, and because any part of the thallus that
becomes detached from the main plant can continue growing as new part of the
same plant (genetically they are the same individual) it is hard to define
the limits of an individual lichen. Secondly, in some cases, when two members
of the same species meet they simply merge together to become one plant, again
this make identifying an individual lichen difficult. Interestingly not all
lichens respond to meeting another member of their species in this way, in
some cases they fight for their own individuality. This also occurs between
different species and you can often see a mosaic of lichens on a rock all
sharply defined by black lines where their individual borders are demarcated.
In theory then, some lichens are immortal, and some famous Ascomycetes hold
to the truth of this theory. Certainly they can live for a long time and their
lives can often be measured in hundreds rather than tens of years. Lichens
live all across the world, in Antarctica they can be found living just below
the surface of rocks, in deserts, providing there is a permanent substrate
they can be found surviving the hottest sun, they can also be found in rock
pools on the sea shore and on the roofs of our buildings. Lichens survive
in an extremely wide range of temperatures. They have been known to survive
temperatures as low as -190C for several hours and as low as -78C for several
days. Going to the other extreme they can also survive temperatures as high
as 100C if they are dried out, and even when moist temperatures of 40C-50C
do not worry them. However because they depend on their Algal partners to
photosynthesise in order to obtain energy for growth all lichens need light.
There are therefore no subterranean or deep cave dwelling lichens. Generally
speaking lichens like areas where their is plenty of light, such as the exposed
surfaces of alpine rocks, and the rooves of our houses...
Like all plants lichens like water, and most of them like a regular supply
of it. Optimum humidity fro growth is between 40% and 70%. However some species
can survive for up to 9 months without water and obviously those that live
in rockpools or streams and ponds survive, and even need constant moisture.
Lichens have no special water storage organ, however they can trap and hold
for a short while a considerable amount of water in their thalli. This can
amount to initially 300 times their dry weight. During their growth lichens
tend to absorb and store metallic ions in their thalli. It is unknown quite
why they do this or what benefit they derive from it. However it is known
that some lichens can tolerate much higher concentrations of metals than other
plants or fungi. They also have a high tolerance for radioactivity and can
be the first organisms to colonise, or the longest to survive in areas of
high radioactive contamination. Lichens produce a strange group of various
metabolic biproducts called 'Lichen Products'. These include esters and organic
acids and are produced, or at least stored, externally to the fungal and algal
cells. They occur in a crystalline form. There are over 350 'Lichen Products'
currently known to science, nearly all of which are totally unique to lichens.
Exactly what their use is to the lichens remains a mystery, however they are
often responsible for giving lichens their attractive colours and may serve
to protect the lichen from slugs, snails, psocids and caterpillars, all of
which feed on lichens. They are useful to man in the identification of similar
looking species, though it may be that some species produce different 'Lichen
Products' in different habitats so their taxonomic use is limited.
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The most of what you see when you look to a lichen is the thallus. The form of the thallus is a result of the different characters. The lichen exists from a fungal part and a algal part. Normally the top of the lichens is a crust called cortex. Below the cortex lives the photobiont. Below this is the medulla, in this area the lichen store his feed. |
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Crustose lichens grow mainly on rocks and
pavements, also on trees. They can't be removed without damaging the
substrate. These lichens make a crust on the top of the substrate on
which they are growing. This crust can be thick and granular. At the
picture you first see a substrate, up to this substrate grow the crust.
At the crust grow the fruiting body and finally grow the cortex.
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Squamulose lichens : By this lichens a bit
of the thallus lifted up from the substrate to form squamules. Squamules
are scale-like components that are usually small and overlapping. The
only difference with crustose lichens is that squamulose lichens have
no lower cortex but only an upper cortex, crustose lichens possess both.
At the picture you see that the tallus lifts up from the substrate.
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Foliose lichens have an upper and lower cortex
as the crustose lichens. They have a leaf-like structure. They are easy
to remove because they are very low attached, usually by rhizines. These
are the two connections with the substrate when you look at the picture.
At this rhizines grow leaf-like components which have lower and upper
sides and usually grow parallel to the substrate.
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Fruticose lichens exists of little bushes and
they are the most three-dimensional. They are attached to their substrate
by one point and rise from this. The bushes can grow upward or they
can hang down from the point of their attachment. The difference with
foliose lichens is that at foliose lichens the algal part only exists
on one side of the thallus and at a fruticose lichens the algal part
exists as a ring around the thallus. At the picture you see the attachment
with the substrate and the bushy structure.
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Leprose lichens are the same lichens as crustose
lichens, the only difference is that the leprose lichens have no upper
cortex. At the picture you see the same as the crustose lichens but
without upper cortex.
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We can use lichens to now
the quality of the environnement
Lichens can be used for many different things:
- From lichen substances drug stores can make antiobiotics.
- Some lichens make feed for plants for example nitrogen.
- Lichens are homes for insects for example spiders.
- Lichens can be used as a natural tint to color wool.
- People eat lichens, but only some sorts because a few are poisonous.
- Lichens can be used as indicator for the pollution in the air, they can
tell us if the air is clear.
We like to tell more about the last point of the enumeration
:
In 1976, Hawksworth and Rose expose in Britain and Europe that lichens were
recognized as potential indicators of air pollution. Since their exposure
lichens have a very great influence, at air pollution studies. Because of
their sensitivity to pollutants, for example sulfur dioxide (SO2),
sulfur (S) and radioactive elements.
Lichens show varying degrees of sensitivity to pollution, because some sorts
of lichens grow only were it's a highly polluted and some sorts where no pollution
is. Scientist can use the differences of the sensitivity of lichens as a bio-indicator
for pollution. In some cases the presence or absence of lichens is recorded
and there at different times in the past. At these recording there are prominent
differences at the species of lichens from the past until now. The conclusion
of this phenomenon is that the quality of the air is changed.
In the 1970's studies in Europe were able to create a plan of 10 zones were
the pollution is different. There are indicator species for each zone, these
are varying form highly polluted zones to unpolluted zones. At the first zone
there were no lichens, the second contained algae only, the third zone contained
Hypogymnia physodes and Parmelia caperata. The last zone contained rare species
like Usnea articulata.
The colouring and patchiness in the centre of the thallus is also an indicate
for the pollution.
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High polluted
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Moderate polluted
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A little bit polluted
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Minimal or no polluted
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Hypogymnia physodes
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Evernia prunastri
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Parmelia caperata
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Usnea subfloridana
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Xanthoria parietina
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Foraminella ambigua
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Grahis scripta
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Parmelia perlata
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Lecanora dispersa
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Lecanora chlarotera
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Bryoria fucescens
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Degelia plumbea
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