BGC quiz cards Flashcards

1
Q

calcium carbonate

A

CaCO3

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2
Q

bicarbonate

A

HCO3-

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3
Q

carbonic acid

A

H2O + CO2 = H2CO3
(water and carbon make carbonic acid)

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4
Q

carbonate

A

CO3(2-)

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5
Q

ocean acidification

A

the oceans are becoming more acidic every year because they’re absorbing so much excess CO2

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6
Q

carrying capacity

A

how many people our planet can support (food is a major variable)

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7
Q

sequestrating CO2

A

“storing away” CO2 over decades to millions of years in rocks, oceans, fossil fuels, etc.

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8
Q

carbon sources

A

wild fires, combustion of fossil fuels, orogenic uplift (mountain making) because it exposes carbonates to surface processes, acid rain (released pent-up carbon in rocks), decomposition, respiration, volcanism

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9
Q

carbon sinks

A

biosphere, atmosphere, hydrocarbons (coal, oil, carbonate sedimentary rocks) ground litter, oceans

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10
Q

tests

A

microscopic creatures (phytoplankton) whose shells are made up of calcium carbonate

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11
Q

ocean acidification and calcium carbonate issue

A

carbonic acid dissolves calcium carbonate:

H2CO3 <=> HCO3- + H+

the H+s go and start synthesizing with CO3(2-), kicking Ca(2+) out, so its harder to form calcium carbonate

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12
Q

ocean acidification issues

A
  1. carbonic acid is decomposing into bicarbonates and hydrogens, the hydrogens then go and bond with carbonates, stealing them from calcium (so breaking apart calcium carbonate): this is bad because it weathers down test shells that are made of calcium carbonate
  2. new tests cannot find the calcium carbonate needed to develop their shells
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13
Q

coral bleaching

A

rising temperatures, turbidity, and sunscreen stress out coral reefs, driving them to essentially go into hibernation, getting rid of the algae that live on them (hence the removal of color)… if they stay in hibernation for too long, they die

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14
Q

orogenic uplift

A

“mountain building”

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15
Q

leaching

A

water seeping into the ground, taking salts, irons, minerals, etc. from the surface down with it (think of sponge with salt on top example)

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16
Q

phosphorous short-term cycle

A

similar to nitrogen cycle, animals get their phosphorous from plants, then release it back into the environment when they die

17
Q

phosphorous long-term cycle

A

note: NOT a gas
similar to nitrogen cycle

18
Q

how do humans use phosphorus?

A

fertilizer, detergent
also P is a major food for plants
humans are removing up the long-term, sequestered C and P

19
Q

lagtime

A

the amount of time it takes for water to flow from a precipitation event to the nearest lake, creek, stream, etc.

20
Q

phosphorous significance in deforestation

A
  1. cutting of flora in tropical areas w/ high productivity reduces P in soil
  2. w/o root systems, the soils and nutrients are washed away by runoff
  3. this leads to turbidity in the lakes the runoff pools into
21
Q

eutrophication (meaning “too much food”)

A
  1. runoff water containing excess phosphates, nitrates, other plant food collects into ponds with algae
  2. these algae blooms rapidly feed on the nutrients, growing quickly and soon covering the surface of the lake
  3. sunlight to the bottom of the lake is blocked out, so subatomic vegetation (SAVs) die because they can’t photosynthesize
  4. without SAVs, the water is not being oxygenated (hypoxic “lack of oxygen” conditions)
  5. dead algae suck up oxygen as well
  6. these things kill off animals in the water, such as fish (anoxic “no oxygen” conditions)
22
Q

biogeochemical cycle

A

~ earth is an open system w/ respect to energy, but a closed system w/ respect to matter
~ components that contain matter (air, organisms, water, etc.) are called “pools”
~ processes that move matter between pools are “flows”

23
Q

atmosphere composition

A

78% Nitrogen, 21% Oxygen, 1% Carbon & others

24
Q

Nitrogen importance

A

nitrogen is a major component for life-sustaining molecules:
~ proteins: structure of enzymes, cells, etc.
~ DNA/RNA
~ animo acids

25
Q

Nitrogen cycle

A
  1. start with atmospheric nitrogen (N2) which is either split apart by lighting or mixed into the soils where nitrifying bacteria split it apart
  2. nitrogenase enzymes converts N2 to ammonia (NH3):
    N2 + 3H2 + energy = 2NH3
  3. ammonification: when ammonia reacts with water (through bacteria), it becomes ammonium:
    2NH3 + H20 = NH4+
  4. erobic bacteria oxidize ammonia/ammonium (which can both be used by plants) into nitrite, NO2-, which is toxic for plants
  5. aerobic bacteria oxidize the nitrite ions further into nitrate, NO3-, which plants can use
  6. assimilation: plants take in nitrates, make proteins, molecules, etc.
  7. denitrification: denitrifying bacteria convert nitrate back into nitrogen gas, N2, and put it back in the atmosphere
26
Q

nitrifying bacteria

A

~ usually aerobic (N and O)
~ found in most soils
~ take N2 and split it apart
~ found in legumes, roots filled with sacks of N-fixing bacteria called rhizobia

27
Q

legumes & rhizobia

A

Legumes (corn, soy beans, lentils, etc.) form a symbiotic relationship with nitrogen-fixing soil bacteria called rhizobia

28
Q

nitric oxide

A

chemical formula: NO
combine with water and you get acid rain

29
Q

nitrous oxide

A

chemical formula: N2O
~ is a greenhouse gas
~ destroying the ozone layer

30
Q

environmental concern: lack of N in soils

A

crops going through fields and after a couple seasons, nutrients have been sucked up or leached out