Hydro-geology and aquifer properties Flashcards
The emergence of groundwater is determined by?
- Lithology
- Regional geological structures
- Geomorphology of landforms
- Availability of recharge sources
How much of earths water is groundwater?
- 97.25 of earths water is in the sea
- 74.9 of fresh water is locked up in ice
- most of water left is ground water
Lithological factors are related to:
Physical properties of the material:
- Porosity
- Permeability
- Transmissivity
What do the physical properties of a rock affect? And what are they referred as?
The ability, and ease at which groundwater can pass through the subsurface.
- Aquifer properties
Define porosity:
The fraction of a given volume of material occupied by void space.
What is the equation for porosity?
n = 1 - known bulk mass density / particle mass density
void ratio (e) = Volume of void / Volume of solid
n = e / (1 - e)
n = Sy + Sr
What is primary porosity?
Determined by the inherent character of a soil/rock matrix, formed during rock formation
What is secondary porosity?
Develops from physical and chemical weathering along cleavage planes and in surface weathering.
Name the factors affecting porosity in sedimentary rock and sediments
- Packing (Cubic,0.48 and Rhombic, 0.26)
- Grain sorting
- Grain shape/orientation
- Diagenesis (compaction, removal/addition of material, mineral replacement/phase changes)
What is specific yield (Sy)?
ratio of water that drains from a saturated rock owing to the attraction of gravity to the total volume of rock - like water out of a sponge due to gravity.
What is specific retention (Sr)?
ratio of the volume of water in a rock can retain against gravity drainage to the total volume of the rock.
Sr increases with:
decreasing grain size
Coarse grain rocks have large pores therefore:
capillary films occupy very small proportion of n such that Sy is almost = n
n =
Sy + Sr
Fine grain rocks have small pores therefore:
capillary forces dominate such that Sr will almost = n
Particularly in fine grained aquifers:
Not all water contained in pores is viewed as available to groundwater.
Total porosity relates to:
the storage capability of the material
Effective porosity relates to:
the transmissive capability of the material (drainable)
Darcy studied the flow of water through porous material contained in a column and found:
the total flow, Q, is proportional to the difference in water level and the cross sectional area of flow; and inversely proportional to column length.
What is transmisivity?
the degree to which a medium allows something to pass through it.
Darcy’s law equation:
Q = -KA(dh/dl)
Q = Flow rate A = cross sectional area K = hydraulic conductivity dh/dl = hydraulic gradient dh = change in head between two points separated by small distance dl
What is the hydraulic conductivity (K or coefficient of permeability)?
Measure of the ease of movement of water through a porous medium. (Length/Time)
Whats the hydraulic conductivity (K) equation?
K = -Q / [A(dh/dl)] [L^3/T[L^2(L/L)] = L/T]
Whats specific discharge
A.K.A. Darcian velocity.
V = Q/A = -K(dh/dl)