Hydrologic, carbon-oxygen, and nitrogen cycle Flashcards

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1
Q

Matter

A

-anything that has mass and occupies space.
-cannot be created nor destroyed.
-must be recycled on Earth!

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2
Q

Biogeochemical

A

the pathways matter is able to move through biosphere to be recycled.

They are made up of various biological, geological, and chemical processes (both natural and anthropogenic)

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3
Q

cohesive

A

water molecules stick to each other

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4
Q

adhesive

A

water molecules stick to other things

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5
Q

percolation

A

the movement of water through a porous material (eg. soil) to enter as ground water

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6
Q

Causes of Acid Rain (Deposition)

A

Emissions from burning fossil fuels in vehicles
Emissions from factories

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7
Q

Wet Deposition

A

sulfur and nitrogen compounds combine with water droplets in atmosphere to form acidic compounds; fall as acidic precipitation

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8
Q

Dry Deposition

A

sulfur and nitrogen compounds settle as dry compounds and form acids when contact water (eg. in respiratory tract, on surface of water)

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9
Q

Effects of Acid

A
  • Corrison
  • damage lung / skin
  • trees defoliated and die
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10
Q

Preventing Acid Deposition

A

-Scrubbers in smokestacks to remove sulfur compound emissions
-Remove sulfur compounds from coal

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11
Q

Polar molecule

A

molecules that have a dipole or an uneven distribution of charge across their geometry resulting in one side being positive and the other side negative. ex) Water (H2O), Ammonia (NH3), Sulfur dioxide (SO2), Hydrogen sulfide (H2S)

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12
Q

Carbon-Oxygen Cycle

A

Mainly involves the circulation of carbon dioxide (CO2) and oxygen (O2) between organisms and the atmosphere

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13
Q

Where in the biosphere is carbon found? (Biotic)

A

-Key element in living organisms (organic)
-Trapped in plants in photosynthesis (glucose)
-Released by respiration (CO2)

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14
Q

Fast cycle

A

Decay and Assimilation, Decomposers break down dead organisms and release phosphates (PO43-) into the soil.

Producers can absorb phosphates via root uptake and assimilation can occur. The plant is able to use the phosphates to make their own proteins, DNA, etc.

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15
Q

Slow Cycle

A

Sedimentation and Erosion:
Rocks are a major sink (storage) for phosphorus.

Plate tectonics causes land masses to rise (geologic uplifting), exposing ancient rock. The phosphorus can then be released slowly from weathering and erosion processes.

Weathering of phosphate can be carried by water into bodies of water. Phosphates that are in the soil can leach into water.

These phosphates can sink in the water (sedimentation) and over time will become new rocks to start the slow process again.

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16
Q

Carbon is released into the atmosphere from sources:

A

Cellular respiration from ALL living things
Combustion
Weathering
physical/chemical breakdown of calcium carbonate of rock
Decomposition
Volcanic Activity

17
Q

Carbon is stored into the atmosphere from sinks:

A

Photosynthesis in photosynthetic organisms
Biosphere
Makes up bodies of all living organisms
Oceans
Dissolved carbon dioxide
Lithosphere (land)
Carbonate rock, fossil fuels, diamonds, graphite
Atmosphere

18
Q

Forming Fossil Fuels

A

Decomposers cannot break down organic matter in acidic or anaerobic conditions in bogs and swamps
Partially decomposed plant material accumulates as peat
Over time, peat is crushed into coal

19
Q

Oil & Gas

A

Anaerobic conditions at the bottom of silty oceans prevents complete decomposition of organic matter
Over time, silt turns into shale and the organic matter becomes oil or gas trapped in the shale

20
Q

Greenhouse gases are found

A

atmosphere and act like a blanket that traps radiant energy (heat). This is referred to as the natural greenhouse effect.

Important greenhouse gases are carbon dioxide, water, and methane.

Combustion of fossil fuels releases carbon dioxide into the atmosphere, where it traps more heat! (Enhanced greenhouse effect)

21
Q
A