Part 1: Water, Soil, Mineral and Rock, and Energy Flashcards

(72 cards)

1
Q

the proportion of void space in the material (holes or cracks),
unfilled by solid material, within or between individual mineral grains and is a
measure of how much fluid the material can store

A

porosity

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2
Q

measure of how readily fluids pass through the material. It is
related to the extent to which pores or cracks are interconnected, and to their
size—larger pores have a lower surface-to-volume ratio so there is less frictional
drag to slow the fluids down

A

permeability

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3
Q

is a volume of rock or soil above the
impermeable material that is water-saturated, in which water fills all the
accessible pore space

A

saturated zone

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4
Q

water in the saturated zone

A

ground water

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5
Q

rock or soil above the saturated zone in
which the pore spaces are filled partly with water, partly with air

A

unsaturated zone

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6
Q

water in the unsaturated soil

A

soil moisture

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7
Q

is all of the water occupying pore space below the ground
surface this includes ground water, soil moisture, and water in unsaturated
rocks.

A

subsurface water

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8
Q

is the top surface of the saturated zone, where the saturated
zone is not confined by overlying impermeable rocks

A

water table

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9
Q

is the processes of infiltration and migration or percolation by which
ground water is replaced

A

recharge

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10
Q

occurs where ground water flows into a stream,
escapes at the surface in a spring, or otherwise exits the aquifer

A

groundwater discharge

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11
Q

is a rock that holds enough water and transmits it rapidly enough to be
useful as a source of water

A

aquifer

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12
Q

is a rock that may store a considerable quantity of water, but in
which water flow is slowed, or retarded

A

aquitard

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13
Q

was used to describe an extreme aquitard, a rock that is essentially
impermeable on a human timescale

A

aquiclude

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14
Q

when the aquifer is directly overlain only by permeable
rocks and soil

A

unconfined aquifer

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15
Q

is bounded above and below by low permeability rocks
(aquitards)

A

confine aquifer

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16
Q

If a well is drilled into a confined aquifer, the water can rise
above its level in the aquifer because of this extra hydrostatic (fluid) pressure

A

artesian system

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17
Q

represents the height to which the water’s pressure would raise
the water if the water were unconfined

A

potentiometric surface

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18
Q

is a circular lowering of the water table immediately
around the well in an unconfined aquifer.

A

cone of depression

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19
Q

If the aquifer rocks are no longer saturated with water, they may become
___________ from the weight of overlying rocks. This decreases their porosity,
permanently reducing their water-holding capacity, and may also decrease their
permeability

A

compacted

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20
Q

Fresh water falling on land does not mix so readily with saline ground water at
depth because water in the pore spaces in rock or soil is not vigorously churned
by currents or wave action

A

saltwater intrusion

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21
Q

is a common way to provide more land for construction.
This practice can interfere with recharge, especially if surface runoff is rapid
elsewhere in the area.

A

filling in wetlands

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22
Q

are a partial solution to the problem of areas where
groundwater use exceeds natural recharge rate, but they are effective only
where there is surface runoff to catch, and they rely on precipitation

A

recharge basins

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23
Q

Rock types such as carbonate rocks or beds of rock salt or gypsum, chemical
sediments deposited in shallow seas, are extremely soluble in water.
Dissolution of these rocks by subsurface water, and occasional collapse or subsidence of the ground surface into the resultant cavities, creates a
distinctive terrain known as ________

A

karst

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24
Q

Rainwater is not considered
as ____________ because it contains dissolved chemicals of various kinds,
especially in industrialized areas with substantial air pollution

A

pure water

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25
is one of the parameters used in describing water quality, the sum of the concentrations of all dissolved solid chemicals in the water.
total dissolved solids (TDS)
26
simply contains substantial amounts of dissolved calcium and magnesium
hard water
27
DENR A.O. 2016-08 also known as
water quality guidelines and general effluent standards
28
3 ways of extending the water supply
conservation interbasin water transfer desalination
29
Water is wasted in home use every day by long showers, inefficient plumbing, insistence on lush, green lawns even in the heat of summer, and in dozens of other ways
conservation
30
__________ of seawater would allow parched coastal regions to tap the vast ocean reservoirs.
desalination
30
involves heating or boiling water full of dissolved minerals. The water vapor driven off is pure water, while the minerals stay behind in what remains of the liquid
distillation
30
People persist in settling and farming in areas that may not be especially well supplied with fresh water, while other areas with abundant water go undeveloped.
interbasin water transfer
31
the water is passed through fine filters or membranes to screen out dissolved impurities
filtration system
32
those materials capable of supporting plant growth. It also implies little transportation away from the site at which the soil formed.
soil
33
the loose material on the lunar surface, it encompasses all unconsolidated material at the surface, fertile or not
regolith
34
indicates matter that has been transported and redeposited by wind, water, or ice.
sediment
35
soil is produced by _______
weathering
36
is the physical breakup of rocks without changes in the rocks’ composition.
physical weathering
37
involves the breakdown of minerals by chemical reaction with water, with other chemicals dissolved in water, or with gases in the air
chemical weathering
38
plays a major role in the intensity of chemical weathering. Most of the relevant chemical reactions involve water, the more water, the more chemical weathering
climate
39
effects can be either mechanical or chemical. Among the mechanical effects is the action of tree roots in working into cracks to split rocks apart.
biological weathering
40
between bedrock and atmosphere is the formation resulted from mechanical, chemical, and biological weathering, together with the accumulation of decaying remains from organisms living on the land and any input from the atmosphere.
blanket of soil
41
soil horizons
O horizon A " E " B " C "
42
consisting wholly of organic matter, whether living or decomposed—growing. plants, decaying leaves, and so on
O HORIZON
43
below O horizon, consists of the most intensively weathered rock material, being the zone most exposed to surface processes, mixed with organic debris from above.
A HORIZON
44
below the A horizon, is also known as the zone of leaching. Fine grained minerals, such as clays, may also be washed downward through this zone.
E HORIZON
45
is also known as the zone of accumulation
B HORIZON
46
below the B horizon, is a zone consisting principally of very coarsely broken-up bedrock and little else.
C HORIZON
47
tends to reflect compositional characteristics. Soils rich in organic matter tend to be black or brown, while those poor in organic matter are paler in color, often white or gray
soil color
48
3 types of soil texture
sand, silt, and clay
49
describes a soil that is a mixture of all three particle sizes in similar proportions (10 to 30% clay, the balance nearly equal amounts of sand and silt). Soils are named on the basis of the dominant grain size(s) present.
loam
50
relates to the soil’s tendency to form lumps or clods of soil particles
soil structure
51
from the Latin root pedo- meaning “soil”, is the term use for clumps
Peds
52
can indicate something of a soil’s composition and perhaps its origins, which in turn may have implications for its suitability for agriculture or construction, or its vulnerability to degradation
soil classification
53
comes from the prefix pedo - and the Latin words for aluminum (alumium) and iron (ferrum)
pedalfer
54
is for the soil of a dry climate.
pedocal
55
The U.S. comprehensive soil classification, known as the _________________________ has twelve major categories (orders), which are subdivided through five more levels of classification into a total of some 12,000 soil series.
seventh approximation
56
may be regarded as an extreme kind of pedalfer.
laterite
57
tend to be rich in accumulated organic matter, reduced because the decaying organic matter consumes dissolved oxygen, and soft.
wetland soils
58
is caused by the action of water and wind
soil erosion
59
______________ in the fields after a crop has been harvested and planting cover crops in the off-season between cash crops. In either case, the plants’ roots help to hold the soil in place, and the plants themselves, to some extent, shield the soil from wind and rain
leaving stubble
60
Surface runoff may be slowed on moderate slopes by ______________
contour plowing
61
a single slope is terraced into a series of shallower slopes, or even steps that slant backward into the hill.
terracing
62
Wind can be slowed down by planting hedges or rows of trees as ___________________ along field borders or in rows perpendicular to the dominant wind direction or by erecting low fences, like snow fences, similarly arrayed
windbreaks
63
alternating crops of different heights, slows near-ground wind by making the land surface more irregular.
strip cropping
64
main cause of soil degradation
deforestation
65
is a rock in which a valuable or useful metal occurs at a concentration sufficiently high, relative to average rocks, to make it economically worth mining.
ore
66
is the term given to unusually coarse-grained igneous intrusions. In some _______, single crystals may be over 10 meters (30 feet) long.
pegmatite
67
They are mined primarily from igneous rocks called
kimberlites
68
Ordinary table salt, known mineralogically as _____________ is one mineral commonly mined from evaporite deposits
halite
69
The deposits mechanically concentrated by water are called
placers
70
They are rarely the sites of primary formation of ore minerals.
streams