Regional Groundwater Flow Flashcards

1
Q

subsurface flow in a groundwater basin is considered to be _______ in nature

A

regional

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2
Q

groundwater recharge is about _____ times the lake’s catchment area

A

1.5x

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3
Q

movement of water is a ________ phenomenon

A

three-dimensional

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4
Q

what is the heterogeneity and anisotropy of the Philippine lithology?

A

heterogenous and anisotropic

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5
Q

the primary method through which water enters an aquifer

A

recharge

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6
Q

an area in which groundwater is discharged to the land surface

A

groundwater discharge zone

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7
Q

an area in which water enters an aquifer

A

groundwater recharge zone

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8
Q

recharge areas are usually located in _______ and with _______ water table

A

topographic high places ; deeper

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9
Q

discharge areas are usually located in __________ and with ________ water table

A

topographic low places ; shallow

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10
Q

manifestations of discharge areas

A

spring, seep, lake, or streams

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11
Q

manifestation of discharge in densely vegetated areas

A

wet soil

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12
Q

manifestation of discharge in arid areas

A

thicker vegetation cover or salt deposit

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13
Q

in the presence of fractures, recharge rate will _____

A

accelerate

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14
Q

water moves from the wetland into the groundwater

A

recharging wetland

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15
Q

water moves from groundwater into the wetland

A

discharging wetland

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16
Q

_______ can cause wetlands to shift back and forth from discharging to recharging

A

fluctuating water table

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17
Q

groundwater availability map of the Philippines was created in what year?

A

1977

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18
Q

a line in two-dimensional groundwater flow field such that the total hydraulic head is the same everywhere on the surface

A

equipotential line

19
Q

t or f: equipotential line is 2D

20
Q

t or f: in an equipotential line, hydraulic head is equal everywhere on the surface

21
Q

represents the height of the water table or potentiometric surface of a confined aquifer, above a datum plane

A

equipotential lines

22
Q

connects points or equal head

A

equipotential lines

23
Q

idealized paths followed by particles of water as they move through the aquifer

A

flow lines

24
Q

plays a role in the settlement pattern of many lands

25
__________ and __________ are though to have therapeutic value
mineralized and thermal
26
mineralized and thermal springs are found along:
inactive volcanoes or surface with residual heat
27
springs can be _______ or _________
permanent or ephemeral
28
provide simple mechanism of springs
topographic low spots
29
forms when water table reaches the surface
depression spring
30
where do swamps naturally form?
in depression springs where water table is shallow and reaches the surface. over time, trees and shrubs begin to fill in the land.
31
these springs are formed when relatively permeable rocks overlie rocks of low permeability
contact spring
32
t or f: depression springs are only formed in unconfined aquifer
T
33
are formed when faulting causes groundwater under hydrostatic pressure (such as in confined aquifers) can move up along such faults
fault springs
34
are formed at topographic lows when water table reaches the surface due to topographic undulations
depression spring
35
are formed when large quantities of water move through the cavities, channels, conduits and other openings developed in limestones.
sinkhole springs
36
occur due to existence of jointed or permeable fracture zones in low permeability rocks
joint springs
37
are formed whene fractures intersect the land surface, movement of groundwater is mainly through fractures that may tap shallow as well as deep aquifers.
fracture spring
38
some of the largest spring are found on
limestone bedrocks
39
springs on limestone bedrocks can either be:
diffused flow in pores and fractures; channelized flow in caverns
40
a river that runs wholly or partly beneath the ground surface
subterranean river
41
a ___________ has a channelized flow in caverns
subterranean spring
42
example of subterranean river in the Philippines
Puerto-Princesa Subterranean River
43
t or f: all surface water interact with groundwater
T