Economic and engineering geology Flashcards

1
Q

tunnelling techniques in crystalline igneous and metamorphic rocks (hard rock)
and pros/cons

A

drilling and blasting

cons-
slow + expensive

at depth there is high confining pressure –> increased risk of rock bursts

pros-
doesn’t often require support

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

tunnelling techniques in soft rocks e.g. chalk, limestone and sandstone
and pros/cons

A

ideal
pros- cheap and easy to tunnel –> could tunnel 30m in a day

cons- require lining with concrete or steel ribs

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

tunnelling techniques in weak rocks e.g. shale, clay or unconsolidated material
and pros/cons

A

No pros listed

cons- prone to collapse –> require most support e.g. shotcrete/steel ribs

prone to H20 leaks –> require dewatering

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

best and worst material for tunnelling

A

best- soft rock
crystalline igneous and metamorphic rocks (hard rock)
worst- weak rock

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

why do changes in rock type cause problems when tunneling

A

require different equipment and techniques

every bedding plane = site of weakness

permeability differences= different dewatering techniques

some areas require support some don’t

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

types of support

A

shotcrete

steel ribs

grouting

steel bolts

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

are dipped or horizontal beds better for tunnel building

A

horizontal

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

why are dipped beds dangerous/worse in tunnels compared to horizontal

A

more changes in rock types- require diff equip and techniques and support
whereas horizontal = all same

dipped beds are subject to slippage, landslides, collapse especially is permeable/ h20 present

easier to swap beds based on what is easier/ better to tunnel in horizontal beds

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

what do we considerer before tunnelling

A

rock type

changes in rock type

dipped or horizontal bed

geological structures e.g. faults, joints, bedding planes and folds

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

how do faults pose problems for tunnelling

A

zone of weakness- fault breccia + fault gouge clay

zones of permeability- flood tunnel

different rock types either side of fault

earthquake/ slippage may cause tunnel to collapse

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

how do joints pose problems for tunnelling

A

zone of weakness + permeability - flooding and slippage

often more closely spaced than faults–> loose blocks of rock between joints
–> may fall from tunnel roof

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

how do bedding planes pose problems for tunnelling

A

bedding planes in sed rocks + foliation in met rocks

planes of weakness may allow slippage or leakage of H20

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

how do folds pose problems for tunnelling

A

folded rock sequence may have changed angles of dip + slippage may occur on fold limbs

gentle syncline
–>tunnel can follow dip of fold and stay in 1 bed

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

how are tunnels below H20 table effected by water table

A

will become flooded and require dewatering / depumping

increased hydrostatic pressure

lubricate bedding planes/joints causes slippages

may flow along joints in limestone, through unconsolidated material

or sandstone developing high pore fluid pressure

clays shrink swell

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

how is spoil from tunnelling recycled/ reused

A

millions of tons extracted from tunnels

sometimes used to build embankments
somewhere else e.g. Crossrail made new nature reserve on Essex coast

chalk from channel tunnel landscaped bottom of Shakespeare cliff

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

how to prevent flooding in tunnels

A

grout surrounding rocks
use rock drainage
pump water out

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
17
Q

how to prevent tunnel collapse

A

line with concrete segments e.g. shotcrete or steel ribs

using rock bolts to secure lose

18
Q

channel tunnel facts

A

50.5 km long

through chalk marl- gentle syncline followed same level

took longer on French side as more faults and folds

conveyers carries material out

lined with concrete and cement grouted

many water inflows on French side

19
Q

Seiken tunnel

A

volcanic rock and sedimentary rock in a syncline

intrusions and faults caused many issues

used boreholes to analyse

originally used tunnel boring machine but switched to dynamite blasting

had to pump out lots of H20 and had cave ins

steel and concrete reinforcements

20
Q

general good conditions for dams

A

impermeable rock

valley (steep)- only have to build 1 side

geologically stable - no seismic activity + faulting + folds

stable valley sides

river with low sed load- prevent build up

no toxic metals if used for drinking or agriculture

21
Q

underlying rock type suitable for dam

A

competent + strong rock - high load bearing strength e.g. interlocking crystals and impermeable I and M rock + well cemented s rock

avoid clay and shale

impermeable- prevent leakage + no joints prevent leakage

rock types- uniform so no differential leading to unstable

old mines- collapse and prevent leakage

22
Q

what strata is good/ bad for dams

A

horizontal and dipping upstream = good

dipping downstream = bad
because leakage and slippage along bedding plane–> collapse dam

23
Q

should you build a dam on an anticline or syncline

A

syncline = good
because stable
but H20 can pass under dam through permeable layers (cut off curtain)

anticline = bad
because slippage can occur along bedding planes on fold limbs and tension joints on crest = leakage

faults + joints = permeable
reopening of old faults increase sesmic activity

24
Q

Type of dams

A

Arch dam

gravity dam

arch-gravity

embankment or earth dam

25
Arch dam
curves upstream - pushes the hydrostatic pressure from the H20 and dam to the valley side--> strengthens it thinner than other types--> less construction suitable for narrow gorges with steep sides
26
Gravity dam
Held in place by gravity due to immense mass of concrete best type for impermeable and high load bearing sometimes they are hollow as it is more economical may be supported by inflexible buttresses downstream
27
arch-gravity dam
combines strength of arch and force of gravity basically thick arch dam doesn't have to be massive good for high flow low material for building- economic
28
embankment or earth dam
sort of like a mound have an impermeable clay or concrete held in place by piles of rock, earth, sand and clay with an impervious covering the material binds itself together by friction-cement unnecessary built in broad shallow valleys- mass of dam spread over large area so foundations don't need to be a strong require very large quantities of filler material
29
what are Ground improvement methods for dams?
grouting- drill holes unto rock + fill with liquid cement fills joints and porespaces ect. reduce permeability + increase strength clay/plastic lining- prior to filling line with impermeable material prevent leakage cut of curtain- impermeable barrier (extension below dam) e.g. concrete prevents leakage on synclines + slippage + strengthens foundations
30
environmental impacts of dam
Habitat loss- upstream- lose grassland downstream- lose fresh water creates microclimate- High Specific heat capacity- absorbs heat - prevents extreme temps nutrient + mineral block- nutrients settle out a dam - less downstream migration blocker- aquatic organisms and people in boats increased evap and precip- effect water cycle build up of pollution-e.g. heavy metals or pathogens - leak into ground H20 resivour induced sesmicity
31
Social impacts of dams
increased energy security- cheaper displacement of people recreational use microclimate increased seismic activity- damage to buildings possible increased water security better flood control
32
What is reservoir induced sesmicity?
earthquakes/sesmic activity caused by the overlying mass + pressure of the dam and reservoir on underlying rock
33
Examples of suspected resiviour induced seismic activity
Hoover dam- 600 earthquakes in 10 years tibet- 3 gorges dam - 6.8mag oroville-6.1 mag Ulley,Rotheram 2007- Cracks appeared in the dam - emergency services pumped out millions of gallons to ease pressure
34
What indicates reservoir induced sesmicity?
tremors while/ soon after filling when previously not sesmically active
35
why is it difficult to link dam construction and seismicity
little reasearch funded historic sesmic records = inadequate each dam has different geological characteristics = not comparable some earthquakes occur years after construction- can't prove due to dam
36
What recommendations are in place to reduce RIS
More research + monitoring necessary- in view of disastrous consequences model changes in pore pressure + rock mechanics build no new high dams- until research complete design to account for RIS monitor seismic activity as reservoir filled- stop if increases possible seismic activity could occur in previously void of activity - buildings not prepped
37
HEP case study
Hydroelectric power Chinas 3 gorges dam + largest HEP dam contain 32 generators H20 turns turbines which turns generator producing energy
38
Causes of land contamination
extraction of geological resources- Acid mine drainage heavy industry accidental spills or naturally occurring pollution salt water encroachment oil and gas extraction- fracking- fracking fluid toxic can contaminate pores in rock spaces leachate from spoil heaps agriculture-organic waste + hazardous chem + inorganic waste disposal of domestic + commercial --> leachate brown field sites contain pollutants
39
why is bioavailability of a pollutant important than amount
bioavailability- ability of toxins to enter living things potential for bioaccumulation if not taken up then not an issue
40
explain how metal ions become mobile
when they enter solution- more easy in acidic conditions changes in H2O make more mobile + exposed to 02 become oxidised and go into solution
41
what causes resivoir induced sesmicity
- due to H20 + mass of dam creating stress in rocks and increased hydrostatic pressure --> H20 infiltrates pores and fissures increasing pore pressure (leads to fractures) + lubrication --> slippage