midterms Flashcards
Cycle involves life
Bio
cycle may include atmosphere,
water, rocks, and soils
Geo
because it is chemicals that
are cycled
Chemical
-the paths chemicals take through
Earth’s major systems
-complete path a chemical takes
through the four major components,
or reservoirs, of Earth’s system
Biogeochemical Cycle
Earth’s Four major Components:
Atmosphere
Lithosphere
Hydrosphere
Biosphere
5 Biogeochemical Cycles:
➢ Water Cycle
➢ Carbon Cycle
➢ Nitrogen Cycle
➢ Sulfur Cycle
➢ Phosphorous Cycle
Transfer of water from oceans to
atmosphere to land then back to
oceans
Hydrologic Cycle
process of a liquid’s surface
changing to a gas
Evaporation
gas changing to a liquid
Condensation
any liquid or solid water that falls
to Earth as a result of
condensation in the atmosphere
Precipitation
ways of liquid water to move
across land
Runoff
-produced as snow or glaciers
melt and form streams or pools
- important type of Runoff
Snowmelt
water vapor being released from
plants and soil
Transpiration
carbon is exchanged among the
biosphere, pedosphere,
geosphere, hydrosphere, and
atmosphere of Earth
Carbon Cycle
element present in all organic
substances from coal to oil to DNA
Carbon
are compressed, chemically
altered remains of plants and
microorganisms that lived millions of
years ago
Coal and oil
materials that store carbon,
includes geological formations
and standing forests
Carbon Sinks
Plants take up CO2 and convert it
into organic matter
Photosynthesis
reservoir of carbon
Terrestrial (plants and geologic
formation)
-major carbon sink (reservoir)
- contains dissolved CO2,
Carbonate and bicarbonate ions
Ocean
-Important nutrient for living
organisms
- Makes up 78% of air
Nitrogen
-only organisms that can use
nitrogen gas (N2) directly from the
atmosphere; “fix” or transform N2
into a form that plants can use
(as nutrient)
- Lives within the roots of a few
plants e.g., beans, peas, clover
and alder trees - use sugars provided by the plants
and, in exchange, produce
ammonia, a form of nitrogen that
plants can use (in a mutualistic
relationship) - Excess nitrogen fixed by the
bacteria is released into the soil
Nitrogen-fixing bacteria
-N2 enters the trophic system
- nitrogen (N2), which has a strong
triple covalent bond, is converted
into ammonia (NH3) or related
nitrogenous compounds
Nitrogen Fixation
-process of NH3 release
- Animals convert NH3 into urine,
or another chemical that is not as
poisonous as NH3
Ammonification
- Because NH3 is poisonous, most
of the NH3 which is released is
untouchable. But soil bacteria
have the ability to assimilate NH3
into proteins. These bacteria
effectively eats the NH3, and
make proteins from it.
Assimilation
Some soil bacteria do not convert
NH3 into proteins, but they make
nitrate NO3- instead.
Nitrification
- Takes NO3-, and converts it into
N2, returning nitrogen gas back
into the atmosphere. - breaks nitrate apart.
Denitrification
circulation of sulfur in various
forms through nature. Sulfur
occurs in all living matter as a
component of certain amino
acids.
Sulfur Cycle
- is also an important component of
coenzyme A, which is used to
produce energy in cellular
respiration - is essential to maintaining life
Sulfur
describes the movement of
phosphorus through the
lithosphere, hydrosphere, and
biosphere.
Phosphorous Cycle
- in unpolluted waters is imported
through dust in precipitation or via
weathering of rocks - is normally present in watersheds
in extremely small amounts as
inorganic orthophosphate,
suspended as organic colloids,
absorbed onto particulate organic
and inorganic sediments
Phosphorous
➢ Tendency of all natural
systems to go from a state
of order toward a state of
increasing disorder
➢ Law of Entropy
Second Law of Thermodynamics
the rise in global
temperatures due mainly
to the increasing
concentrations of
greenhouse gases in the
atmosphere
Global Warming
process that occurs when
gases in Earth’s
atmosphere trap the Sun’s
heat
Greenhouse Effect