D UK aquifers Flashcards

1
Q

Mendips geology

A

series of periclines
Jurassic sediments have been eroded on the west side so limestone on west has been exposed to weathering for longer

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2
Q

Karst hydrology features

A

sinking and gaining streams
network of caves, diffuse infiltration

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3
Q

autogenic recharge

A

rain which falls on the limestone and immediately percolates
auto meaning self

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4
Q

allogenic recharge

A

rain falls on impermeable rock and runs along surface till it reaches the permeable rock

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5
Q

Limestone Mendips water pathway

A

down the bedding plain, up the joint

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6
Q

Data quality and quantity

A

sparse & variable normally

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7
Q

core data is biased towards

A

lithologies sufficiently consolidated to be sampled

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8
Q

Sandstone

A

large pores- good storage
good core scale, limited scale dependence
affected by grain size variations and cementation

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9
Q

Gouge

A

smear of clay or broken up rock (found in sandstones)

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10
Q

lower greensand- found in surrey

A

intergranular flow, minor fracturing
ironstone hard bands locally impede vertical flow

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11
Q

Permo-Triassic sandstone aquifer

A

large pores so drains easily
very high permeability
weakly cemented
good quality yield but in coastal areas seawater intrusion occurs

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12
Q

Matrix properties controlled by

A

lithology and degree of cementation

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13
Q

Permo-Triassic sandstone matrix

A

mostly isotropic
heterogeneity in K from inter-bedding of fine and coarser

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14
Q

Permo-Triassic sandstone fracture flow

A

bedding plane fractures and inclined joints, solution enlarged fractures

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15
Q

permeable faults shown as

A

recharge boundaries during a pumping test

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16
Q

why are we so dependent on the chalk aquifers

A

high population
low rainfall and few site can be used for surface reservoirs

16
Q

composition of Chalk

A

fined grained
very high porosity but small pore size so limited permeability

17
Q

what dominates flow in Chalk aquifers

A

flow through disolusionally enlarged fractures and bedding planes

18
Q

vertical variations in Chalk

A

weathered at the surface that is more porous and permeable
as you go further into the saturated zone the amount of open fractures decreases

19
Q

Lateral variation in chalk

A

could be covered with glaciers or rock