D UK aquifers Flashcards
Mendips geology
series of periclines
Jurassic sediments have been eroded on the west side so limestone on west has been exposed to weathering for longer
Karst hydrology features
sinking and gaining streams
network of caves, diffuse infiltration
autogenic recharge
rain which falls on the limestone and immediately percolates
auto meaning self
allogenic recharge
rain falls on impermeable rock and runs along surface till it reaches the permeable rock
Limestone Mendips water pathway
down the bedding plain, up the joint
Data quality and quantity
sparse & variable normally
core data is biased towards
lithologies sufficiently consolidated to be sampled
Sandstone
large pores- good storage
good core scale, limited scale dependence
affected by grain size variations and cementation
Gouge
smear of clay or broken up rock (found in sandstones)
lower greensand- found in surrey
intergranular flow, minor fracturing
ironstone hard bands locally impede vertical flow
Permo-Triassic sandstone aquifer
large pores so drains easily
very high permeability
weakly cemented
good quality yield but in coastal areas seawater intrusion occurs
Matrix properties controlled by
lithology and degree of cementation
Permo-Triassic sandstone matrix
mostly isotropic
heterogeneity in K from inter-bedding of fine and coarser
Permo-Triassic sandstone fracture flow
bedding plane fractures and inclined joints, solution enlarged fractures
permeable faults shown as
recharge boundaries during a pumping test