Semester 1 Final Flashcards

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1
Q

Main parameters for measuring water quality

A

temperature - thermometer
pH - pH strip/scale
visibility/turbidity - secchi disk
oxygen concentration - oxygen meter
salinity - refractometer

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2
Q

hydrogen bonds

A

creates strong cohesion between water molecules, caused by water’s polarity

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3
Q

cohesion

A

the attraction of molecules for other molecules of the same kind; water molecules have strong cohesive forces thanks to their ability to form hydrogen bonds with one another.

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4
Q

pH of Ocean Water

A

enzymes and chemical reactions for metabolism functions only in a narrow pH range, in which they otherwise become de-natured
Dissolvability and transport of gases and ions across membranes greatly affected by pH
Biological structure such as bone shells affected by pH

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5
Q

sources of ions in ocean water

A

positive ions: from rock and soil erosion
negative ions: from magma(volcanoes/rain)

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6
Q

depth’s affect on colors

A

Violet, yellow, orange, red wavelengths don’t penetrate deep enough into the water to reflect off objects

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7
Q

Pressure under water

A

increases in seawater one atmosphere every 10 meters
BOYLE’S LAW - when pressure on a gas increases, its volume decreases

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8
Q

pH scale

A

acids are 0-6, neutral is 7, 8-14 is alkaline.
Acids have more H3O+ ions, while bases have more OH- ions

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9
Q

Nitrogen’s significance

A

essential nutrient for organisms, especially plant nutrition, part of amino acids, nitrogenous bases, ATP
limits population size in most ecosystems

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10
Q

Nitrogen cycle

A

nitrogen fixation - legumes fix into ammonia
nitrification - chemical reaction done by archaea and bacteria
ammonification - chemical reaction done by archaea and bacteria
assimilation-used in environment
denitrification-goes back into atmosphere

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11
Q

eutrophication

A

nutrients washed into water, causing algae blooms occur, algae grow on water surface absorbing all the light and oxygen, cynobacteria eat the algae

caused by nitrogen runoff from fertilizer, sewage, and animal waste, nitrogen causes algae bloom that later dies and decomposes using all oxygen making water anoxic - toxic to fish and habitats

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12
Q

excess nitrogen in plants

A

thickened and sometimes cupped leaves with atypically deep green color. Overfertilization can cause leaves to turn brown, gray, dark green, or yellow at margins and tips or overall. Affected foliage may wilt temporarily or die and drop prematurely.

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13
Q

eutrophication solutions

A

oyster farming(oysters filter water, filtering water by eating algae) + upgrading septic systems + using less fertilizer

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14
Q

bow, stern, port, starboard

A

front, back, left, right
all used in relation to ship’s bow

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15
Q

hull

A

watertight body of the ship, which provides buoyancy and protects the contents of the ship. It’s essentially the main body of the ship that keeps it afloat.

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16
Q

keel

A

backbone of the ship’s structure, running along the center of the hull bottom from the bow to the stern. It provides stability and prevents the ship from tipping over.

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17
Q

deck

A

The ‘deck’ is the top of the ship, which serves as the roof of the hull.

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18
Q

bridge

A

where the captain and the navigation officers control the ship. It’s equipped with a plethora of navigational tools, communication equipment, and control systems.

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19
Q

knot

A

unit of speed used in aviation and maritime contexts, equivalent to one nautical mile per hour. It’s worth noting that a nautical mile is slightly longer than a land-based mile.

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20
Q

draft

A

vertical distance between the waterline and the lowest point of the hull.

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21
Q

rudder

A

flat piece of metal or wood, hinged vertically at the stern, which controls the ship’s steering direction.

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22
Q

propeller

A

often found near the rudder, a rotating device that propels the ship through the water.

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23
Q

mast

A

tall, vertical pole that rises from the deck, traditionally used to support sails, rigging, and navigation lights.

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24
Q

boom

A

the horizontal pole extending from the bottom of the mast, which angles the sail to catch the wind.

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25
Q

gunnel

A

the outermost top edge of a boat hull, usually where the deck and hull come together.

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26
Q

freeboard

A

the distance between the waterline and the main deck or weather deck of a ship or between the level of the water and the upper edge of the side of a small boat

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27
Q

titanic

A

Royal Mail ship built Belfast Island
Left Southampton, England to NYC in April 1912, carrying 2224 passengers, weighing 46,000 tons, equipped with state of the art tech
4 days into trip hit iceberg off coast of Newfoundland, 1500 passengers died

28
Q

possible causes for Titanic sink

A
  1. travelling too fast
  2. radio operator dismissed iceberg warning
  3. ship may have taken wrong term, lack of terminology awareness
  4. titanic’s builders cut costs, rivets not strong enough
  5. mirages caused by atmospheric conditions hid iceberg
  6. no binoculars were on ship
  7. lack of lifeboats left a lot of people dead
29
Q

sonar

A

uses transmitter that emits soundwaves that reach ocean floor and bounce back, received by receiver, information interpreted by transducer

30
Q

active sonar vs passive sonar

A

passive sonar only detects sounds while active sonar uses transmitter to make sound waves, measuring time for them to return

31
Q

Bathymetric sonar

A

active sonar used to map seafloor and detect objects in watercolumn or along seafloor
gathers distance from seafloor, shape, and type of sea floor

32
Q

seismic sonar

A

active sonar determining what is under seafloor - rock layers, tectonic plate, often used for oil searching

33
Q

side scan sonar

A

used to determine what is on the bottom of the seafloor, towed behind vessel, and close to bottom of the ocean
used for identifying objects on bottom of ocean

34
Q

buoyancy

A

ability to float in water, determined if objects displace water with higher mass then object(less dense than water)

35
Q

AUV(automated underwater vehicle)

A

not tethered, battery powered, preg-programmed, used to measure water quality, bathymetric data, can be smaller and go deeper bc of no human inside, challenging to make to withstand pressure and locate after resurfacing, “swarming” work together to help navigate, can be free with no risk of human life, but can’t collect samples, only sonar, no communication, batteries decide how long it runs

36
Q

ROV(remotely operated vehicle)

A

tethered, tether powered, controlled by projection, long run times, inexpensive, no risk to human life, but limited mobility and less range

37
Q

HOV(human operated vehicle)

A

not tethered, battery-powered when small, engine when large, control is present, high mobility and range, but batteries and humans limit run time

38
Q

earth’s layers

A

core - hot center with melted nickel and iron and radioactive elements that decay and produce heat

mantle - magma

asthenosphere - molten liquid layer on which crust moves

lithosphere - plates sliding around

crust - brittle layer of rock

39
Q

convcection currents

A

generated by magma move continental plates

40
Q

convergent plate boundary

A

an area on Earth where two or more lithospheric plates collide

41
Q

divergent plate boundary

A

linear feature that exists between two tectonic plates that are moving away from each other

42
Q

transform plate boundary

A

fault along a plate boundary where the motion is predominantly horizontal

43
Q

oceanic crust will always subduct continental because

A

continental crust thicker but less dense than Oceanic Crust

44
Q

oceanic crust

A

uppermost layer of the oceanic portion of the tectonic plates

45
Q

continental crust

A

the relatively thick part of the earth’s crust that forms the large landmasses. It is generally older and more complex than the oceanic crust.

46
Q

subduction

A

the sideways and downward movement of the edge of a plate of the earth’s crust into the mantle beneath another plate

47
Q

convection

A

The density- and heat-driven cycling, transfer or circulation of energy through which material initially warms up and becomes relatively less dense, then rises, cools and becomes relatively more dense, and finally sinks.

48
Q

earth’s continents are thought to have been once one called Pangea because of

A

puzzle like shapes and specific fossils found across oceans on different continents at same latitude

49
Q

Continental margin made up of

A

cont. shelf
cont. slope
cont. rise

50
Q

continental shelf

A

shallow submerged extension of continents, made of granite, covered by sediment, slopes gently to ocean basin but generally flat, width relates to slope of land it borders

The West Coast has a narrow shelf(bigger waves) while the east coast has a wide shelf

51
Q

continental slope

A

transition between cont. shelf+rise, begins at shelf’s break, abrupt change in landscape, contains less sediment

52
Q

continental rise

A

gentle slope of base of cont. slope

53
Q

submarine canyone

A

similar to on land, caused by river systems on earth, formed by turbidity currents, sediment and water erode slope and gain speed as sweep down. also caused by earthquakes of sediment collapses

54
Q

ocean basin

A

floor of ocean, covering more of earth’s surface than land, composed of basalite rock covered by sediments

55
Q

abyssal plain

A

bottom of ocean basins, flat expanse, formed by sediment deposited by turbidity currents, covering %40 of ocean floor

56
Q

guyots

A

flat topped sea mounts eroded by currents

57
Q

sea mounts

A

steep sided formation rising sharply from bottom, formed from underwater volcanoes, mostly in Pacific

58
Q

ridges and rises

A

divergent plate boundaries form series of large, underwater volcanic mountains, running through every ocean, stretching 68,000km, site of seafloor spreading

59
Q

trenches

A

convergent plate boundary where seafloor is being destroyed, usually associated with chains of volcanic islands

60
Q

mariana trench

A

deepest trench on earth, deepest spot 7 miles down

61
Q

biogenous sediment

A

shells of plankton

62
Q

lithogenous sediment

A

made from chemical and mechanical weathering of rocks on land

63
Q

hydrothermal vents

A

In 1977, scientists diving in HOV Alvin made a stunning discovery: openings in the Pacific Ocean seafloor with warm, chemical-rich fluids flowing out. Later trips revealed previously unknown organisms and entire ecosystems around the vents, thriving in the absence of sunlight–a phenomenon that scientists didn’t think was possible. These discoveries fundamentally changed our understanding of life on Earth.

Like hot springs and geysers on land, hydrothermal vents form in volcanically active areas—often on mid-ocean ridges, where Earth’s tectonic plates are spreading apart. In these areas, magma wells up to the surface or just below the seafloor. As ocean water percolates down through cracks and porous rocks, the super-hot magma causes chemical reactions that remove oxygen, magnesium, sulfates, and other chemicals from the water. In the process, the fluids become hotter and more acidic, causing them to leach metals such as iron, zinc, copper, lead, and cobalt from the surrounding rocks. The heated fluids rise back to the surface through openings in the seafloor, known as hydrothermal vents. The fluid temperatures can reach 400°C (750°F) or more, but they do not boil under the extreme pressure of the deep ocean.

As they pour out of a vent, the fluids encounter cold, oxygenated seawater, causing another, more rapid series of chemical reactions to occur. Sulfur and other solids precipitate–or come out of solution–to form metal-rich towers and deposits of minerals on the seafloor–some reaching over 30 feet (10 meters) tall! These minerals sometimes are visible in the gushing fluid, which is why some hydrothermal vents are called white or black “smokers.”

64
Q

hydrothermal vent communities

A

depend on chemosynthetic bacteria that convert hydrogen sulfide and other chemicals in the vent fluids into sugar for energy. These “chemosynthetic” bacteria provide food for larger organisms such as tubeworms, shrimp, and mussels.

65
Q

photosynthesis vs chemosynthesis

A

Photosynthesis occurs in plants and some bacteria, wherever there is sufficient sunlight, be it on land, in shallow water, or even inside and below clear ice. All photosynthetic organisms use solar energy to turn carbon dioxide and water into sugar (food) and oxygen: CO2 + 6H2O -> C6H12O6 + 6O2.

Chemosynthesis occurs in bacteria and other organisms and involves the use of energy released by inorganic chemical reactions to produce food. All chemosynthetic organisms use energy released by chemical reactions to make a sugar, but different species use different pathways. For example, at hydrothermal vents, vent bacteria oxidize hydrogen sulfide, add carbon dioxide and oxygen, and produce sugar, sulfur, and water: CO2 + 4H2S + O2 -> CH20 + 4S + 3H2O. Other bacteria make organic matter by reducing sulfide or oxidizing methane.