Geology 101 Quiz 11 Flashcards

1
Q

water and weathering

A

water makes dissolution possible, expanding ice widens cracks, and glaciers can pluck boulders from mountain sides and pulverize them

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2
Q

water and erosion

A

rivers and glaciers transport weathered rock great distances

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3
Q

water and rock formation: igneous rock

A

water lowers the melting temperature and influences the rate of crystal growth

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4
Q

water and rock formation: metamorphic rock

A

water facilitates exchange with dissolved ions (hydrothermal)

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5
Q

water and rock formation: sedimentary rock

A

water transports dissolved and particulate minerals, and creates depositional environments

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6
Q

water and volcanism

A

water affects viscosity of magma and gas pressure

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7
Q

water and slope stability

A

water usually decreases the stability of a slope

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8
Q

life is possible in large because

A

water is liquid in the 0-100*C temperature range

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9
Q

unique properties of water

A
  1. melting-boiling temperatures 0-100*C
  2. polar molecule
  3. solid water is less dense than liquid water
  4. unusually high heat capacity
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10
Q

water has a ? structure; its peculiar shape results in ?

A

bent; a negative and positive side

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11
Q

the polar nature of water results in

A
  1. dissolution and transport of ions
  2. creation of surface tension
  3. attraction to sediment particles
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12
Q

the polar nature of water and its dissolution and transport of ions means water

A

increases weathering and assists in moving nutrients in and wastes out of organisms

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13
Q

the polar nature of water and the creation of surface tension means water

A

reduces evaporation rates and creates an entire habitat for surface organisms

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14
Q

the polar nature of water and its attraction to sediment particles means water

A

makes sediment particles stick together and causes capillary rise

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15
Q

many nutrients and waste products in organisms are ions, which means they are

A

easily dissolved and transported into and out of organisms

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16
Q

non-polar liquids like gasoline are good at dissolving ?, but not very good at dissolving ?

A

uncharged organic molecules; charged ions found in minerals

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17
Q

polarity creates surface tension because

A

the negative and positive sides of water molecules align to form weak bonds at the surface

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18
Q

one good thing that comes from surface tension is that evaporation is slower - why?

A

water has to break free from the surface tension to pass into the vapor phase

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19
Q

one good thing that comes from surface tension is that water striders can be water striders - how?

A

surface tension will support the weight of dense objects that will sink if they break through the surface tension; water striders take advantage of surface tension to walk on water

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20
Q

capillary rise

A

water is drawn upward into unsaturated sediments

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21
Q

where groundwater is shallow, roots can get water delivered by ? even if the roots do not extend to the water table

A

capillary rise

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22
Q

ice is less dense than water, and therefore floats, because of

A

the particular arrangement of water molecules in ice

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23
Q

water has an unusually high heat capacity, meaning

A

it takes more heat energy to raise the temperature of water compared to other substances

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24
Q

the heat capacity of water plays an important role in

A

climate control

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25
Q

over large bodies of water, heat exchange between the air and water changes the temperature of the ? more

A

air

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26
Q

only about ? of the earth’s water supply is available to drink, and most of this is sitting underground

A

1%

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27
Q

despite contamination, we still have water to drink because

A

water on earth does not exist in a static condition

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28
Q

water is continuously cycled and purified through what is called the

A

hydrologic cycle

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29
Q

hydrologic cycle steps

A

evaporation, condensation, precipitation, infiltration, evapotranspiration

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30
Q

transpiration

A

transfer of water to the atmosphere through leaves

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31
Q

if water filled plant cells and stopped, the flow of nutrients would stop - what keeps the water flowing through the plant?

A

transpiration

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32
Q

does water vapor automatically precipitate?

A

no

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33
Q

for precipitation, conditions in the atmosphere have to change to cause the water vapor to condense - this generally happens by

A

b

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34
Q

there are three common ways an air mass gets cooled, but all have to do with

A

the air cooling as it expands (as an air mass rises, it expands)

35
Q

what are the three common ways an air mass gets cooled?

A
  1. orographic lifting
  2. frontal lifting
  3. convective lifting
36
Q

orographic lifting

A

caused by an air flow over mountains

37
Q

rain shadow

A

dry region on downward side of mountain range because air rising on the upwind side rains out as it rises; as air travels down the far side, it compresses and warms so no more water condenses

38
Q

frontal lifting

A

caused by moving cold or warm fronts

39
Q

cold front

A

cold air is more dense, so it ploughs its way underneath warmer air in front of it; as the warmer air rises, it expands, cools, and precipitates

40
Q

warm front

A

warm air is less dense, so it slides up over the top of the colder air in front of it; as the warmer air rises, it expands, cools, and precipitates

41
Q

convective lifting

A

caused by heating air near the ground

42
Q

convective lifting is often associated with

A

cities where building and pavement absorb sunlight and radiate it out as heat

43
Q

water that stays in the ground is known as

A

groundwater

44
Q

groundwater can be divided into two regions

A

the saturated zone and the unsaturated zone

45
Q

unsaturated zone

A

contains air and water in pores (a well in the unsaturated zone will be dry)

46
Q

saturated zone

A

pores are completely filled with water (a well completed in the saturated zone will fill with water)

47
Q

water table

A

top of unconfined saturated zone

48
Q

aquifer

A

a geologic unit that transmits water in sufficient quantity to supply a well

49
Q

confined aquifer

A

aquifer bounded on top by an impermeable layer

50
Q

artesian well

A

water rises in a well above the top of the aquifer

51
Q

flowing artesian well

A

water rises above the ground surface

52
Q

potentiometric surface

A

the height to which water will rise in a cased well

53
Q

influences on groundwater flow: porosity

A

ratio of pore volume to total volume (ex: if solid particles fill half the total volume, the porosity is 0.5 or 50%)

54
Q

influences on groundwater flow: permeability

A

ability of a medium to transmit a fluid (water)

55
Q

we tend to think that higher porosity always leads to higher permeability - is this true?

A

often, but not always

56
Q

poorly sorted sediments have (lower/higher) porosity and (lower/higher) permeability

A

lower; lower

57
Q

more compacted, more tightly packed sediments have (lower/higher) porosity and (lower/higher) permeability

A

lower; lower

58
Q

tightly packed sand has a (lower/higher) porosity than loosely packed clay, and a (lower/higher) permeability

A

lower; higher

59
Q

if the shape and packing are the same, different grain sizes (do/do not) change the porosity

A

do not

60
Q

smaller particles will (decrease/increase) permeability and why?

A

decrease; because of attraction between the water and solid surfaces

61
Q

good aquifers (high porosity and permeability) examples

A

sand, gravel, sandstone, karst limestone

62
Q

karst

A

lots of dissolved caves and passageways

63
Q

intermediate to poor aquifers

A

silt, glacial till, fractured rock, unweathered limestone

64
Q

not aquifers

A

clay, shale, unfractured crystalline rock

65
Q

one way a spring can form: if water accumulates on an impermeable layer intersected by a slope, water will

A

eventually seep out the side of the hill slope

66
Q

one way a spring can form: fractures cutting through a confined aquifer will

A

provide conduits for pressurized water to reach the surface

67
Q

when we start to pump water from a well, what happens to the water table or potentiometric surface?

A

a cone of depression (drawdown cone) forms

68
Q

if pumping from multiple wells exceed annual recharge, the entire water table will begin to ?, which increases pumping costs and can cause ?

A

lower; wells to go dry and the ground surface to subside

69
Q

subsidence

A

decrease in surface elevation due to collapse or compression of underlying material

70
Q

subsidence in unconfined aquifers: draining water from unconsolidated sediments often causes ?, so the ground surface settles downward

A

compaction (compacted sediments take up less space)

71
Q

subsidence in confined aquifers: confined aquifers are ?, but pumping relieves pressure, which allows the aquifer to ?

A

pressurized; compress (the ground surface drops)

72
Q

subsidence in caves

A

a cave with a thin or weak roof may collapse if pumping drops the water level below the top of the cave

73
Q

a depression or hole caused by a collapsed cave roof is called

A

a sinkhole

74
Q

total dissolved solids (TDS)

A

the total mass of all dissolved ions and molecules per liter of solution

75
Q

we divide water into different types based on TDS:

A

fresh, brackish, saline, brine

76
Q

water in quartz sand (SiO2) tends to have (low/high) TDS< with dissolved ? as primary ion

A

low; silica

77
Q

water in limestone (CaCO3) is fresh, but tends to have (lower/higher) TDS, with ? and ? as primary ions

A

higher; calcium and bicarbonate

78
Q

water in halite (NaCl) forms a brine, (very low/very high) in TDS, with ? and ? as primary ions

A

very high; sodium and chloride

79
Q

contaminants come in a variety of different forms

A

salts, metals, bacteria, agricultural and pharmaceutical chemicals, radioactive waste, organic liquids

80
Q

organic liquids are divided into two groups

A

LNAPL and DNAPL

81
Q

LNAPL

A

light non-aqueous phase liquid (floats on water)

82
Q

DNAPL

A

dense non-aqueous phase liquid (sinks in water)

83
Q

Which are harder to clean up and why? (LNAPL or DNAPL)

A

DNAPL because they continue moving downward in an aquifer and get hung up in little pools wherever the permeability is slow