Where can water be found?
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Transcript Where can water be found?
How water, gases, and
nutrients cycle throughout our
ecosystems
Cycles
Many elements in our ecosystem are never lost, but
simply recycled over and over again
Water – makes up most of living things (we are about
60% water)
Carbon – element that makes things organic (living)
Oxygen – needed for cellular respiration
Nitrogen – needed to make proteins and nucleic acids
Water Cycle Vocabulary
Hydrosphere – all the water on the Earth from oceans, creeks, streams,
rivers, lakes, ponds, etc.
Transpiration – The water that evaporates from the surface of leaves
Condensation – when water cools from its gaseous state to form a liquid
again
Evaporation – when
the surface of water
vaporizes to become a
gas
Precipitation – water
falling to the Earth over a
certain period of time
Water Cycle
Water is never lost, it is just recycled through the atmosphere
and organisms
Animals and plants are composed mostly of water, but when
these organisms are eaten or die this water is passed on to the
organism that eats it.
Much of the water we drink is recycled back into the
environment as urine or sweat.
The environment recycles water as well through a cycle of
evaporation, condensation, and precipitation.
Carbon Oxygen Cycle
Carbon dioxide is taken in by plants
During photosynthesis plants break down the carbon dioxide and
add some more elements (carbon, oxygen, and hydrogen) to
create glucose (C6H12O6)
We then eat plants and break down that glucose for energy (ATP)
in a process called cellular respiration. The carbon molecules we
take from the glucose are
then exhaled as carbon
dioxide that plants can use.
Plants also give off the
oxygen we need to perform
cellular respiration because
it is a waste product of
photosynthesis
Carbon Oxygen Cycle
It is not just plants and animals that contribute to this cycle
though . . .
Decomposers release carbon dioxide when they break down
dead matter
Anytime something is
burned carbon dioxide is
released and oxygen is
consumed
Volcanic activity also releases
carbon dioxide into the
atmosphere
The oceans do absorb some
of our atmospheric CO2
Nitrogen Cycle
All living things need nitrogen
because all living things contain
nucleic acids (DNA) and amino
acids (proteins)
Nitrogen is extremely abundant on Earth
because 72% of our atmosphere is made up of
nitrogen, but most organisms are not able to
use gaseous nitrogen (N2)
Plants need nitrogen in the form of nitrate
(No3-), ammonia (NH3), or urea (NH2)2CO2 to
be able to make proteins and nucleic acids
Nitrogen Cycle
We get our nitrogen by consuming plants and other animals
which feed on plants
So, what is converting nitrogen to its different forms?
Nitrogen fixation
Decay
Nitrification
De-nitrification
Nitrogen Fixation
Nitrogen fixation is a process
where N2 (atmospheric nitrogen)
is broken apart and the
individual nitrogen atoms are
combined with other elements
This can occur several ways
Lightning
Nitrogen Fixing Bacteria (these can
be found in the soil, living in
symbiotic relationships in the roots
of plants, or in bodies of water)
Industrially (in plants we heat up N2
and add a catalyst to create ammonia
to be used in fertilizers)
Decay
Animals consume their nitrogen
and any excess is excreted in the
form of urine and feces
Animals get their nitrogen by consuming others, so nitrogen
is passed along in the food chain
When an organism dies the
decomposers break down the dead
material and return nitrogen to the
soil in the form of ammonia
The decomposers also break down
our wastes into usable forms
Nitrification
Some ammonia
returned to the soil by
decomposers can be
taken up by plants roots,
but plants prefer
nitrogen in the form of nitrates.
Nitrifying bacteria convert ammonia to nitrates that plants
can use
These bacteria live in the soil and in bodies of water
De-nitrification
De-nitrification is the process by
which nitrates are converted
back into N2 and returned to the
atmosphere
Once again bacteria called
denitrifying bacteria are
responsible for this process
Agriculture is responsible for ½
of the nitrogen fixation on
Earth, making it very difficult
for these poor denitrifying
bacteria to keep up!