Ground Water 2 Flashcards

1
Q

well efficiency

A

ratio of theoretical specific capacity to the measured one

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2
Q

well loss

A

energy dissipation from turbulent flow in the vicinity of the well

forms due to the convergence of streamlines, leads to increased velocity

significant for large Q

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3
Q

deployable output
- definition
- factors

A

well water levels during drought period, should allow supply and demand balance

depends on
- licences
- environment
- water quality
- physical aquifer/well characteristics

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4
Q

drought curve
- use
- cons

A

used to determine deployable yield, at the intersection of the curve and DAPWL
- curve defined such that all observed data is to the right
-DAPWL = deepest advisable pumped water level

cons
- curve is subjective
- doesnt consider well interactions
-lack of data

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5
Q

baseflow separation
- aim
- techniques

A

Aim: measuring GW discharge into rivers

Techniques
- channel water budget
- seepage water, point measurement
- tracers
- numerical modelling

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6
Q

measuring GW recharge
- techniques

A

chloride mass balance
- for arid/semi-arid climates
- assumes a SS thus chloride flux at surface same as at root zone due to insignificant plant capture

modelling: Penman Grindley
- based on root constant = max soil moisture deficit without an effect on ET
- above leads to decreased with AE -> P as SMD -> FC

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7
Q

rapid recharge

A

high rainfall leads to fracture flow in unsaturated zone, can cause flow into boreholes

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8
Q

measuring hydraulic head

A

deep jacking tensionometer

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9
Q

GW protection approaches
- approach selection

A
  • do nothing
  • control/modify hazard
  • remove hazard

selected based on: risk = hazard * vulnerability
- no pathway means no risk
- hazard is the prob of event, assumed 1
- vulnerability = damage

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10
Q

aquifer vulnerability factors

A
  • geological (major aquifer?)
  • overlying soil ( leaching ability ?)
  • depth of water table (deep ?)
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11
Q

DRASTIC
- use
- weighting

A

for aquifer vulnerability, all sored 1-10 with 10 being highest polluting potential

Depth of GW - 5
Recharge - 4
Aquifer media - 3
Soil media - 2
Topology - 1
Impact of unsaturated zone - 5
Conductivity (hydraulic) - 3

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12
Q

well zone of contribution

A

are with pathways to the well
- Time related capture zone (area branded by isochrone, below is UK)
— zone 1, t = 50 days for biological contamination
—- zone 2, t = 400 days for slow degrading pollutants
— zone 3 = well catchment

  • well catchment, t= Inf
  • source protection zone, has a specific level of protection determined by models
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13
Q

source protection zone model steps

A
  • conceptual model
  • data collection
  • mathematical model
  • test against observations
  • sensitivity analysis = find parameters most likely to control models behaviour
  • perform simulation
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14
Q
A
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