APES Biogeochemical Cycles Test Questions with Verified Answers, Exams of Environmental Science

APES Biogeochemical Cycles Test Questions with Verified Answers

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2025/2026

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APES Biogeochemical Cycles Test Questions with Verified Answers
biogeochemical cycle - -cycle of matter between
biotic and abiotic things in the environment involving
biological, geologic and chemical interactions; they are
driven by energy and gravity
carbon cycle - -During photosynthesis, plants
remove carbon from the air and store it as chemical
compounds such as sugar, the carbon will be released
back into the atmosphere through cellular respiration.
Sometimes plants or animals with carbon trapped in their
body will get buried before fully decaying; over millions of
years the heat and pressure will turn them into fossil fuels
containing carbon. This carbon is then released back into
the atmosphere through combustion.
nitrogen cycle - -Consists of five steps: nitrogen
fixation, nitrification, assimilaton, ammonification, and
denitrification.
nitrogen fixation - -First step of nitrogen cycle. The
conversion of gaseous nitrogen to ammonia, a form that
organisms can use. Nitrogen fixed bacteria (Rhizobium) is
found in legumes, then this bacteria converts nitrogen gas
to ammonia (NH3) and ammonium (NH4) (NOW
USEABLE FORMS); can be done by lightning,
combustion, volcanic activity and industrially
nitrification - -Second step of the nitrogen cycle.
bacteria change ammonia (animal/plant waste) or
ammonium into nitrate; the plants then absorb it First they
turn it into nitrite, then oxidize it to form nitrate. (ammonia
into poisonous nitrites (by bacteria) and then into nitrates)
assimilation - -3rd step of the nitrogen cycle. Plants
absorb nitrate, ammonia, or ammonium and incorporate
them into plant proteins. (nitrates into protein) animals eat
the plants to make protein. it is used to make DNA, amino
acids and proteins
ammonification - -4th step of the nitrogen cycle.
conversion of animal wastes to ammonium; decomposer
bacteria convert nitrogen containing organic compounds
into simpler nitrogen containing inorganic compounds)
denitrification - -Final step of the nitrogen cycle.
anaerobic bacteria changes nitrates back into nitrogen
gas and returns to the atmosphere
phosphorus cycle - -A sedimentary cycle. Water
erodes phosphorus-containing minerals and releases
phosphorus into soil, where plant roots absorb it and
incorporate it into biological molecules. Dead organisms
decompose and release phosphorus back into the soil to
be reused. Phosphate is often carried by water into the
ocean where it remains on the sea floor for millions of
years until uplift eventually exposes the sea floor
sediments as new land surfaces, where the phosphate will
be eroded again.
sulfur cycle - -Most sulfur is underground in
sedimentary rocks and minerals, which eventually erode
and release sulfur compounds into the ocean. Many
natural abiotic occurrences release sulfur into the
atmosphere, where it combines with oxygen and hydrogen
to form sulfuric acid. Plant roots absorb sulfate from soil
and incorporate it into plant proteins. Dead organisms then
release it back into the soil.
hydrologic cycle - -Water moves from the
atmosphere to the land and ocean through precipitation.
Water evaporates from the ocean, streams, soil, to form
clouds in the atmosphere. Transpiration also adds water to
the atmosphere. Plants and animals absorb or consume
water, then decompose and release it back into the abiotic
environment.
transpiration - -water from plants evaporates into the
atmosphere as water vapor
evapotranspiration - -returns water back to the
atmosphere; faster when the temperature is hotter
infiltration - -downward movement of water through
soil
percolation - -passage of a liquid through spaces of
material (soil)
runoff - -water that flows on the earth's surface into
other bodies of water; opposite of infiltration (lot of runoff..
low infiltration), rate of precipitation exceeds rate of
infiltration, or the ground is saturated (pores are full)
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biogeochemical cycle - - cycle of matter between biotic and abiotic things in the environment involving biological, geologic and chemical interactions; they are driven by energy and gravity carbon cycle - - During photosynthesis, plants remove carbon from the air and store it as chemical compounds such as sugar, the carbon will be released back into the atmosphere through cellular respiration. Sometimes plants or animals with carbon trapped in their body will get buried before fully decaying; over millions of years the heat and pressure will turn them into fossil fuels containing carbon. This carbon is then released back into the atmosphere through combustion. nitrogen cycle - - Consists of five steps: nitrogen fixation, nitrification, assimilaton, ammonification, and denitrification. nitrogen fixation - - First step of nitrogen cycle. The conversion of gaseous nitrogen to ammonia, a form that organisms can use. Nitrogen fixed bacteria (Rhizobium) is found in legumes, then this bacteria converts nitrogen gas to ammonia (NH3) and ammonium (NH4) (NOW USEABLE FORMS); can be done by lightning, combustion, volcanic activity and industrially nitrification - - Second step of the nitrogen cycle. bacteria change ammonia (animal/plant waste) or ammonium into nitrate; the plants then absorb it First they turn it into nitrite, then oxidize it to form nitrate. (ammonia into poisonous nitrites (by bacteria) and then into nitrates) assimilation - - 3rd step of the nitrogen cycle. Plants absorb nitrate, ammonia, or ammonium and incorporate them into plant proteins. (nitrates into protein) animals eat the plants to make protein. it is used to make DNA, amino acids and proteins ammonification - - 4th step of the nitrogen cycle. conversion of animal wastes to ammonium; decomposer bacteria convert nitrogen containing organic compounds into simpler nitrogen containing inorganic compounds) denitrification - - Final step of the nitrogen cycle. anaerobic bacteria changes nitrates back into nitrogen gas and returns to the atmosphere phosphorus cycle - - A sedimentary cycle. Water erodes phosphorus-containing minerals and releases phosphorus into soil, where plant roots absorb it and incorporate it into biological molecules. Dead organisms decompose and release phosphorus back into the soil to be reused. Phosphate is often carried by water into the ocean where it remains on the sea floor for millions of years until uplift eventually exposes the sea floor sediments as new land surfaces, where the phosphate will be eroded again. sulfur cycle - - Most sulfur is underground in sedimentary rocks and minerals, which eventually erode and release sulfur compounds into the ocean. Many natural abiotic occurrences release sulfur into the atmosphere, where it combines with oxygen and hydrogen to form sulfuric acid. Plant roots absorb sulfate from soil and incorporate it into plant proteins. Dead organisms then release it back into the soil. hydrologic cycle - - Water moves from the atmosphere to the land and ocean through precipitation. Water evaporates from the ocean, streams, soil, to form clouds in the atmosphere. Transpiration also adds water to the atmosphere. Plants and animals absorb or consume water, then decompose and release it back into the abiotic environment. transpiration - - water from plants evaporates into the atmosphere as water vapor evapotranspiration - - returns water back to the atmosphere; faster when the temperature is hotter infiltration - - downward movement of water through soil percolation - - passage of a liquid through spaces of material (soil) runoff - - water that flows on the earth's surface into other bodies of water; opposite of infiltration (lot of runoff.. low infiltration), rate of precipitation exceeds rate of infiltration, or the ground is saturated (pores are full)

condensation - - gas into liquid; makes clouds; relative humidity must be saturated (100%) which means that air temperature must equal dew point and then condensation occurs when temperature goes below dew point; must stick to something to form which is called condensation nuclei, or dust particles surface water - - precipitation that does not infiltrate the ground or return to the atmosphere groundwater - - water that sinks into the soil and is stored and renewed in underground reserves called aquifers how do humans alter the hydrologic cycle - - withdrawing large amounts of freshwater at rates that are faster than nature can accommodate (unsustainable), clearing vegetation because trees increase the amount of infiltration and transpiration, and increasing flooding when wetlands are drained; releasing pollutants into the water Glaciers - - store water (u shape) abilities of water - - water can shape and erode rocks, valleys are V shaped properties of water - - (due to hydrogen bonds between water molecules) exists as a liquid over a range of temperatures (high specific heat), changes temperature slowly, has a high boiling point (100 C), melting point (0 C), in between 0 and 100 water is liquid, adhesion (water to other molecules), cohesion (water sticks to water), expands as it freezes, solvent, filter out harmful UV what is carbon the basic building block of? - - carbohydrates, lipids, proteins, and nucleic acids, it makes up organic material how is carbon absorbed from the atmosphere? - - through photosynthesis, plants release CO2. how is carbon found in the ocean (a sink) - - phytoplankton carry photosynthesis; carbon is found as carbonate and bicarbonate how is carbon present in rock? - - present in Limestone (a sedimentary rock) how is carbon trapped? - - can be sequestered in tree wood for 100s of years, an as fossil fuels for millions of years carbonic acid - - CO2 + H20 together is carbonic acid and it lowers pH causing the shells of organisms to dissolve, produce H+ ions and release calcium Sinks of Carbon - - oceans (dissolved CO2 and living and nonliving shells), old growth forests (terrestrial biosphere stores most of the above ground soil and carbon), plant matter (photosynthesis), sedimentary deposits (limestone rock and carbon trapped in fossil fuels) How is carbon released back into the atmosphere - -

  1. cellular respiration (aerobic releases CO2 and anaerobic releases CH4) 2. Decay by decomposers 3. livestock produce CH4 when they digest 4. Burning fossil fuels 5. slash and burn forests 6. weatherization of rocks which breaks down CO2 and H2CO3 7. volcanic erruption
  2. combustion 8. release of Co2 by warmer oceans what does additional CO2 added to the atmosphere do? -
    • tree clearing, burning of fossil fuels, and warms the atmosphere nitrogen/ nitrogen sink - - component of proteins, vitamins and nucleic acids/ atmosphere how much of atmosphere does nitrogen gas make up -
    • 78%, N2 is very stable and unusable to living organisms, must be converted for use human intervention in the nitrogen cycle - - additional NO (nitric oxide) and N2O (nitrious oxide) in atmosphere from burning fossil fuels causes acid rain; N20 to atmosphere from bacteria acting on fertilizers and manure; destruction of forests, grasslands and wetlands; add excess nitrates to bodies of water; remove nitrogen from