groundwater Flashcards
importance of hydrologic cycle
without it there would be no clouds, rivers, glaciers, oceans, groundwater, plate tectonics, rock cycle, or life on Earth
in excavations and tunnels, what are some dangers of groundwater and solutions
- inflow during construction
- artificially lower water table
aquifers
saturated rock/soil layers forming a reservoir for groundwater. contains pores or open spaces to hold water and these pores are generally all connected.
4 types of aquifer
- unconfined
- confined
- semi-confined (leaky)
- perched
unconfined aquifer
water table is exposed to the atmosphere and continuous so it is free to rise and fall
confined aquifer
the groundwater is isolated from the atmosphere by less permeable layers, subject to higher than atmospheric pressure
aquitard
less permeable layer than aquifer
aquiclude
impermeable layer
semi-confined aquifer
recharge or discharge occurs through the confining layers (aquitards)
perched aquifer
water table discontinuous, exposed to atmosphere, free to rise and fall
2 aquifer properties
storage and flow
porosity
percentage of aquifer consisting of pore space. larger pore space = larger porosity = larger water holding capacity
permeability
capacity of aquifer to transmit water through its pore spaces. related to the connectivity of pores
2 forms of porosity
- primary porosity - pores space created during aquifer formation
- secondary porosity - pore space formed through fracturing and weathering of aquifer
what type of porosity dominates in sedimentary rocks?
primary porosity
hydraulic head (h)
height above a datum of a column of water that can be supported by the hydraulic pressure at a given point in an aquifer.
used to determine hydraulic gradient
hydraulic gradient (i)
rate of change in hydraulic head (h) per unit distance of flow in a given direction. equates to slope of water table ro piezometric surface
Darcy’s law (Q)
measures flow rate of water draining through porous material. Applies at macroscopic level
hydraulic conductivity (k)
rate of flow through a unit cross-sectional area of a material under a unit hydraulic gradient (1)
anisotropic
k varies with direction
isotropic
k is the same in all directions
homogenous
k is the same in all positions
heterogenous
k is different in different positions
are aquifers heterogenous or homogenous?
heterogenous
easy or hard to quantify anistropy and heterogenity in aquifer
hard because of the high degrees
groundwater is full of particle mater and polluted with sea water and NO3….
TRUE/FALSE
true apart from particles filtered out as it flows through the ground
some dangerous pollutants in groundwater
- Fe and Mn ions, from rocks , encrusts pipes and favours bacterial growth
- NO3- too much is toxic to babies and cattle.
- faeces from sewage leak
cone of depression
as groundwater is extracted, flow is induced towards well. The velocity and pressure increases towards the well and thus cone forms, centred on the well. Decreases pressure away from the well which can lead to settlement.