Geohazards Flashcards

1
Q

geohazard def

A

a geological condition that is dangerous/ potentially to enviro or people who live within it

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2
Q

examples of geohazards

A

earthquakes
vol eruptions
tsunamis
landslides
subsidence
avalanche
cliff fall

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3
Q

what is the focus and epicentre of an earthquake

A

focus-where movement occurred

point within the earth at which the earthquake og as movement occurs along fault plane

sesmic waves radiate away from it in all directions

epicentre point on surface above focus

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4
Q

how is stored elastic strain energy released?

A

stress = forces
strain = reaction

relative movement of rock on either side of fault applies stress

rock undergoes strain

this process transfers energy and increases elastic strain stored in rock

energy releases and elastic energy decreases

energy released due to movement

released as heat and seismic waves (greater amp greater energy)

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5
Q

amplitude def

A

maximum extent of displacement of an oscillation from the position of rest

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6
Q

what does amplitude show

A

greater the amp = greater energy released

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7
Q

what happens to amp as waves move away from focus

A

reduces as energy released and transferred to surrounding rock

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8
Q

attenuation of seismic waves

A

loss of energy experienced by a wave shown as reduction in amp as it propagates through material

waves faster through rigid as transfer is easier so attenuation is reduced in more rigid rocks

amp decreases with distance from focus

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9
Q

Mercalli scale

A

magnitude scale for measuring earthquakes

empirical

gives 12 categories earthquake can fall into based on destruction and how people felt it
instrumental to cataclysmic

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10
Q

Mercalli scale pros and cons

A

pros-
don’t need specific equation
don’t need formal training to understand

cons-
empirical (based on observation/experience )

subjective

not comparable - e.g. all observation relate to building but they are diff in each country

may not remember experience

intensity decreases from focus but mag doesn’t

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11
Q

different earthquake measurement systems in time order

earliest to oldest

A

Mercalli- Richter- moment mag

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12
Q

Richter scale

A

measures energy output of the earthquake

1-10

use seismogram:
lag time - time diff between P and S waves tells us distance from focus
height of greatest S wave

plot on richter scale graph tells mag

should give same value no matter where

log so 1= 10x amp

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13
Q

Pros and cons of Richter scale

A

Pros:
Maths equ so less subjective
but also has desc for public

Cons:
assume same rock type

larger is underrepresented and less accurate the larger it gets (seismologists only measured at certain frequencies)

outdated

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14
Q

moment magnitude scale

A

What is used now

when waves arrive at seismometer measure:
lag time - tells us distance from focus
amplitude and waves
actual displacement of rock at quake site (new, not in richter)

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15
Q

Pros of moment mag

A

interpret broader range of seismic frequencies- determines more accurate e from large earthquake

accounts for rock type and rigidity

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16
Q

moment mag equ
(given to us)

A

Mw= 2/3logE-6.1

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17
Q

different wave types

A

P- primary
S- secondary
L-love
R-rayleigh

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18
Q

features of P waves and effect on buildings

SEE BOOKLET FOR DIAGRAM

A

features-
travel through L and S

body waves

arrive first- fastest

longitudinal

effect on building-
least dangerous

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19
Q

features of S waves and effect on buildings

SEE BOOKLET FOR DIAGRAM

A

features-
can travel through S

body waves

arrive second- second fastest

shear waves - transverse

effect on buildings-
S waves more destructive than P
as greater amp

horizontal worse than vertical

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20
Q

features of L waves and effect on buildings

SEE BOOKLET FOR DIAGRAM

A

Features-
Surface waves do the most damage

shear wave where shearing motion is confined to horizontal plane at earths surface (oscillate)

effect on buildings-
responsible for most damage

greatest effect- sideways movement is more effective

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21
Q

features of R waves and effect on buildings

SEE BOOKLET FOR DIAGRAM

A

features- surface waves are most destructive

slowest

earths surface moves in a vertical elliptical path parallel to wave movement

effect on building-
worse than P and S

most movement with R- up and down so less destructive

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22
Q

effect on ground movement on built environment

A

L waves cause most damage to buildings

lose objects thrown upwards

buildings fracture
pancake

freeways collapse

brick and stonework seperate along motar

sects of utility pipes separate

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23
Q

how does rock competency affect how e is transferred and effect on buildings

A

comp rocks allow easier propergation of seismic waves and move on

less e dissipated to rock

less movement

also moves quicker through comp rock

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24
Q

liquefaction and effect on buildings

A

saturated or partially saturated unconsolidated material losing strength and rigidity in response to applied stress

e.g. Earthquake

unconsolidated and incompetent rock holds more H2O in pore spaces

when rock compressed due to seismic waves, pore spaces reduce and H2O comes up and out

loss of strength makes buildings tip and sink

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25
Q

where are developments banned

A

soft unconsol rock or incomp

on fault zone

nearby fault zones

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26
Q

earthquake engineering ideas

A

reenforce concrete with steel

base isolation

tuned mass damper- giant pendulum near top of building brings back to centre by swing in opp direction (Taipei 101)

Crossbracing- X shaped brackets transfer seismic forces back to ground reducing lateral movement

seismic damper- absorb energy

emergency shut off switch

rubber/flexi pipes

metal plates around building- easier to move through than building as more rigid reduces impact on building)

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27
Q

Taipei 101 case study

A

tuned mass damper- giant pendulum near top of building brings back to centre by swing in opp direction

used for earthquakes and hurricanes

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28
Q

what building design is used to reduce vertical + horizontal stress?

A

height

irregular + assym design is more susceptible to shaking
in sym buildings stress is dissipated equally

avoid ornamentation

think about materials- wood = more flexible = absorbs stress
brick more likely to fracture

reinforced/ deeper foundations

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29
Q

what are ground/ base isolation systems? + purpose?

A

structure is separate from base so moves independently of foundations

protects against seismic activity

e.g, rollers, rubber pads, springs, lead rubber bearings and sliders

Buildings can be retrofitted

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30
Q

what building designs are used to resist shear forces?

A

encase building in steel framework using diagonal steel cables

reduces movement in building

very ridged so doesn’t save building but does stop pancaking and increases time for evacuation

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31
Q

what building designs are used to absorb sway?

A

use mass dampers

use hydraulic systems e.g. shock absorber in car but on larger scale

flexible connections between pipes / parts of buildings

controlled rocking systems - allow to rock and be pulled back to centre after

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32
Q

how do we protect building services e.g. water pipes ?

A

gas pipes = main concern as cause fires

also worried about - water pipes, elec wiring ect

use flexible pipes or joints to prevent fracturing

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33
Q

how does the natural frequency of buildings effect them in earthquakes?
and how do we change it?

A

all structures vibrate at own seismic frequency

is similar to the frequency of the ground there will be more / amplified movement

so we should insure they are different to reduce movement

Natural frequency can be found/ changed using stiffness and mass
greater stiffness = higher frequency
greater mass= lower frequency

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34
Q

seismic risk def

A

possibility of death, injury or damage that may occur within a certain period of time

IT CAN CHANGE

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35
Q

what impacts seismic risk?

A

history of activity

frequency of seismic activity

nature of hazard

areas geology

earthquake resistant buildings- lower risk

no of people/ buildings

type of building

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36
Q

what do national governments prioritise when mitigating seismic risk?

A

maintain H20, electric, communications e.g. defence and public services ect

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37
Q

what do local governments prioritise when mitigating seismic risk?

A

protecting public buildings, emergency planning and local transport

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38
Q

what do businesses prioritise when mitigating seismic risk?

A

protecting building to avoid loss of equipment and production

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39
Q

what do householders prioritise when mitigating seismic risk?

A

pets, house, people e.g. family

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40
Q

what is a seismic risk assessment?

A

assessment of probable max loss e.g. extent of damage to buildings in terms of finances

more linked to finance than people

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41
Q

What may we see in a seismic risk assessment

FILL IN USING TEXT BOOK

A

PML

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42
Q

probability definition

A

how likely it is something will happen

can be fraction, decimal or percentage

0-1
won’t to will

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43
Q

return period definition

A

average length of time for an earthquake of a certain mag to occur again or be exceeded

(sometimes called reoccurrence period)

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44
Q

return period calculation

NOT GIVEN IN EXAM

A

T = (n+1)/m

T= return period
n= no of years on record
m=number of recorded earthquakes

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45
Q

Case study : earthquake dills in Japanese schools

A

children get under desks- head first and hold legs of desk

wear padded head covers

lead out of building by teachers

in drills they sometimes use earthquake seismicity device ,makes special room shake

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46
Q

Case study: San Francisco resilience program

A

plan to make San Francisco more resilient to immediate and long term climate change and natural hazards

split into adaptation and mitigation

adaptation include better fire safety as well as planning for rising oceans

mitigation includes sustainable travel and renewable energy

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47
Q

Forecast definition and examples

A

calculations and data used to make a statement of probable occurrence of an event

e.g. return period calculation
forecast high probability of an earthquake on a plate boundary

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48
Q

prediction definition and examples

A

a statement about what you think will happen in the future- normally based on experience

e.g. predicting your grades

predict when, where and how

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49
Q

What data is used for forecasting?

A

historical data - produces hazard maps that can be used to forecast likelihood of earthquake in area/ where is most at risk

also use probability calculations and monitor seismic activity to do this

earthquake forecasting is a probabilistic assessment of hazard- using frequency and magnitude of damage

we can also create Venn diagram using area affected and area liable to be effected - more overlap more certain to occur

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50
Q

how do we make predictions? and why aren’t they certain?

A

ask useful questions:
what is worst case
where is nearest active fault
largest earthquake that could occur there
estimate return period
assume epicentre closest to site
calc potential ground movement

model max + use for engineering

Not currently possible to make deterministic prediction of when/ where/ how strong earthquake will be

can’t identify- seismic, biological, physical or chem changes which would indicate earthquake will happen

only say what will happen if it does occur

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51
Q

advantages of predictions

A

lives saved - people move out of dangerous areas

makes people think about safety measures e.g. escape routes

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52
Q

disadvantages of predictions

A

panic + mass movement of people leads to injury

may not happen - people stop listening

sometimes the time period is so short it may be counter productive e.g. imminent

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53
Q

what is the maximum considered earthquake? + its use?

A

earthquake that is expected to occur in given area once every 2500yrs (2% prob every 50yrs)

not necessary largest possible - insure building code is accurate

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54
Q

what is a building code?

A

set of rules that specify standards for construction of objects e.g. buildings
(can also include non buildings e.g. bridges)

different codes in diff areas

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55
Q

examples of building codes in earthquake areas

A

buildings must have steel reinforcements

buildings with more occupancy designed to withstand more seismic activity

non- structural components e.g. non load bearing walls must also be designed to withstand earthquake

old buildings must be retrofitted

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56
Q

role of a geologist in seismically active area

A

provide facts, produce hazard maps and risk assessments

decide/ advise if public warning is necessary

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57
Q

steps necessary for old buildings in seismically active areas

A

retrofitted with modern protection e.g. ground base isolation systems

plan evacuation routes to insure they don’t pass old buildings

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58
Q

what science is used to make predictions

A

physical properties

stress

animal behaviour

radon emissions

seismic gap model

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59
Q

how are physical properties used to predict earthquakes

A

large earthquakes are proceeded by smaller ones

increased frequency before event- displace strain energy

P wave velocity decreases then increases before as rock expands slightly close to fracture point

coloured lights in the sky- changes in electron properties

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60
Q

how is stress used to predict earthquakes

A

many minute cracks develop under stress -> volume increases, H20 and gas peculates in so increases elec conductivity of ground

resistivity decreases as P wave vel decreases then increases

ground may tilt due to deformation + swell slightly

H20 percolates into cracks lower water levels in wells

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61
Q

how are animal behaviours used to predict earthquakes

A

animals shows distressed behaviour just before earthquakes e.g. pig squeal

may feel waves before higher amplitude s waves or slight change in magnetic field

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62
Q

how are Radon emissions used to predict earthquakes

A

Radon = decay product of uranium
easy to detect + short half life

so it is sensitive to short term flux

it is a heavy gas an accumulates in H2O wells

increased radon suggests microcracks that allow it to escape so earthquake is imminent

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63
Q

how are seismic gap models used to predict earthquakes- more used for forecasting

A

2 plates slip past each other

every section of fault slips but not at same time

different section are in different stages of cycle

next big earthquake is expected in gap between recent slipped sections as strain has built

64
Q

what is a tsunami? + how do they work?

A

large wave caused by the displacement of water, normally due to shallow focus earthquakes (submarine)

as the approach land and slow the amplitude increases (especially is in narrow area)

65
Q

what can trigger tsunamis

A

shallow focus submarine earthquakes

release of glacial lake

landslide

submarine volc eruption

meteorite impact

66
Q

Early warning systems for tsunamis?

A

used to save lives + protect:

phone + television alerts

siren/radio/loudspeaker

signs showing evac routes

educate about signs

prohibit building on coast + maintain coral reefs + costal trees –> reduce wave + impact

seismologist monitor- earthquakes focus and mag + type of crustal movement, tsunamis associated with high mag - evac

67
Q

tsunami case studies

A

2011 - Tohoku
20000 deaths
9-9.1 mag earthquake
several waves over 12 hr period

uk:
Storegga slide- caused tsunami off coast
Lisbon earthquake- caused tsunami

68
Q

What is clay? + examples

A

very fine grained sedimentary rock made up of flat platy particle- malleable and plastic
e.g. Kaolinite, montmorillonite, vermiculite and illite

69
Q

how does clay form?

A

from the chemical weathering of carbonate minerals e.g. quartz and feldspar

mostly feldspar (exposed to air and H20)

70
Q

why is Britain covered in clay

A

clay deposits post glacial retreat

71
Q

kaolinite information

A

non-expanding and low shrink swell capacity

1:1

used in ceramic and porcelain

used for glossy high finish paper

72
Q

montmorillonite information

A

expanding structure and high shrink swell capacity

2:1

used for:
protective linings
catalytic processes
facial powder
cat litter

73
Q

vermiculite information

A

limited expansion and medium shrink swell

2:1

used for:
when hot expands to low density medium
gardening
cat litter

74
Q

Illite information

A

non expanding and low shrink swell capacity

2:1

uses:
ceramics
fillers

75
Q

1:1 clays chemistry

A

1:1 clays are made up of alternating Al octahedra and Si tetrahedra sheets

these are joined by Hydrogen bonding = very strong

this prevents hydration and therefor shrink swell

76
Q

2:1 clays chemistry

A

2:1 clays are made up of layers

each layer is made of 2 silica tetrahedra surrounding 1 Al octahedra (like a sandwich)

these are joined by van der walls forces allowing hydration and shrink swell between the layers

e.g. smectite

77
Q

silica tetrahedra in clays

A

many silica tetrahedra join together to partially satisfy charge via bonding oxygens and form a sheet

the left over change is used to bond to the next sheet by bonding to charged ions between sheets

shown as a trapezium

78
Q

Aluminium octahedra in clays

A

many octahedra share 2 o atomso partially satisfy charge via bonding oxygens and form a sheet

the left over change is used to bond to the next sheet by bonding to charged ions between sheets

shown as a rectangle

79
Q

problems with building on clay

A

shrink swell-
likely to be vertical movement which effects foundations

leads to subsidence (shrinking, downward) then hardens and crack pipes

swells and rises causing tilt

doesn’t necessarily be pure clay can be high clay soil

80
Q

How can engineers mitigate problems with building on clay

A

understand water table fluctuation -
monitor + maintain WT by pumping out or in H2O - useful drainage system

build super deep foundations - pass through clay (pile foundations)

add/ remove trees - add/ remove H20

reinforced raft foundations (concrete slabs + steel mesh)–> larger than building –> spreads weight and ‘floats’

81
Q

How can we change the properties of clay

A

smectite 2:1 can shrink swell 1500%/15x vol

often contains Na+ forms ionic bonds that hold sheets together

add lime –> Ca+ ion –> displaces Na+ –> only shrink swells 100%/2x vol

OR

add bacteria which changes Fe3+ to Fe2+ –> reduces shrink swell

82
Q

subsidence def

A

vertical downward movement of ground ( and building) due to the shrinking of soil, clay or clay rich soil

83
Q

why does subsidence occur?

A

lots of clay - shrink swell

mineshafts below

damaged drain-> water escapes -> softens ground

non cohesive soil e.g. sand = washed away

soil decomposition e.g. plant matter

trees - add/remove H2O

84
Q

how does longwall mining cause subsidence

A

traditional+ current coal mining method

move forward allowing material behind to collapse into cavity - subsidence

not all the subsidence occurs at once 10,50,100 yrs later

10m of mining doesn’t mean 10m subsidence necessary

fault and fractures in rock weaken it, can happen yrs later

85
Q

how does shallow mining cause subsidence

A

old bell pits + pillar and stall –> unstable voids underground

no records of old mines = surprise collapses

86
Q

how does deep mining cause subsidence

A

bigger operation -> bigger voids–> large amounts of subsidence

however better recorded so less surprise

87
Q

how does salt mining cause subsidence

A

drill and pump in hot H2O -> leaves large caverns e.g. under Cheshire

often pump water down to hold them up but if water escapes pressure drops leading to subsidence

88
Q

how does crown holes cause subsidence

A

anthropogenic- mad made

circular depression –> causes vertical downward movement

often due to mines

89
Q

how does sink holes cause subsidence

A

natural circular depressions that cause vertical downward movement

90
Q

common causes of subsidence

A

mining - deep, shallow and salt

crown and sink holes

clay shrink swell

91
Q

how can we avoid subsidence

A

avoid karst terrain- limestone (dissolves)

reinforced raft formations - isolate foundations from movement

monitor subsidence using ground surveys or satellite radar (expensive)

can use concrete pining

92
Q

how can subsidence be corrected

(FILL IN WITH TEXTBOOK)

93
Q

what are the causes of mass movement basics?

A

increasing mass - H2O or building

increased slope angle-due to e.g. river erosion, building roads or tectonic uplift

decreasing friction- lubrication with H2O

94
Q

which types of dipping beds are best and worst for causing mass movement

A

dipping in direction of slop is most likely to cause mass movement - worst

horizontal beds are okay

dipping away from slope = best

95
Q

what kind of mass movement do competent rocks undergo?

A

steep slope–> so transitional slides –> all moves at once breaking up into scree (talus)

96
Q

what kind of mass movement do incompetent rocks undergo?

A

shallow slopes –> low shear strength –> rotational slide

97
Q

types of mass movement

A

flow - H2O major component

mudslide- H2O and clay

soil creep - very slow

landslide- slow

mud/debris flow- medium

rock fall- fast

98
Q

how are mass movements classified

A

velocity and type of material
e.g.
soil creep - very slow
rock fall- fast
flow - H2O major component

99
Q

what triggers mass movement

A

addition of H2O –> heavy rain

earthquakes

building on slope- adds mass

deforestation

sudden drop in H2O table

100
Q

how does deforestation tigger mass movement

A

deforestation- increases H20 flow and decreases root binding

101
Q

how does changes in water table tigger mass movement

A

sudden drop in H2O table- change pore pressure in rocks –> cause break up of rock

102
Q

how does addition of H2O trigger mass movement

A

Adds mass and increases lubrication increasing friction

103
Q

How does bullion on slopes trigger mass movement

A

Adds mass and can also increase slop angle

104
Q

How do we stabilize material to prevent mass movements

A

slope modification - decrease angle

build retaining wall of concrete

use gabbons or mash wire - steel cages of rock

use rock bolts - drill into rock and cement

rock drains- drain H2O decreasing mass and lubrication

shotcrete- sprayed at high pressure and reinforces

add plants - root binding rocks in place

105
Q

Mass movement case studies

A

blubberhouses landslide -
used mesh wire and rock bolts to stabilize
originally caused by heavy rain

youngay landslide-
peru
killed 20,000 people
triggered by ancash earthquake

106
Q

How is rock strength defined

A

ability to resist stress without large scale failure

107
Q

what does rock strength depend on?

A

rock type- competence
composition- e.g. quartz = hard
texture and Fabric e.g. crystalline or clastic
foliation
crystal/grain shape
cracks or fractures

(diff section of small rock can have diff strength)

108
Q

stress definition

A

force per unit area acting on rock

shear, compressive or tensional

109
Q

Fabric definition

A

spacial and geometric configuration of all the components in a rock

e.g crystal and void shapes,sizes and orientations

also know as texture

110
Q

strain definition

A

Response of a system to applied stress

when material is loaded with stress it produces strain e.g. deformation

111
Q

what is rock stress measured in

112
Q

what is ductile deformation + where is it seen

A

malleable- changes shape

occurs at deep depths and high temps

when rock suffers large strain without large scale fracturing

113
Q

what is brittle deformation + where is it seen

A

shatters

near surface and cold

when stress causes rock to fracture (possibly some elastic deformation first)

114
Q

what does UCS stand for

A

uniaxial compressive strength

115
Q

when is UCS used

A

before construction

to design rock crushers in mining

and determine strength of concrete

116
Q

UCS test method

A

1) sample of rock extracted
2)sample prepped- flat,smooth and cylindrical
3)sample placed in test machine
4)gradual compressive load is applied
5)load increased till sample fails
6)max compressive load is recorded as UCS

117
Q

why is the UCS test class as unconfined

A

No where for stress to be transferred from rock

118
Q

confining pressure def

A

combined lithostatic and hydrostatic pressure (at depth all principal stress is =)

119
Q

how does confining pressure change way rock behaves under pressure

A

would be able to transfer stress to surrounding rock so would have higher USC

120
Q

how does mineral composition effect overall strength of rock

A

Different mineral have different strengths

for example quartz is very strong as it has a hardness of 7 whereas micas only have a hardness of 3 and have a strong cleavage that makes them weak

121
Q

how does cementation effect overall rock strength

A

rocks with the same composition can have different cementations that make them stronger or weaker

for example sandstone is weaker than metaquartzite as it inly has a weak cement whereas metaquartzite has interlocking crystals

122
Q

lithostatic pressure def

A

vertical pressure due to mass of overlying rock only

also called overburden pressure

123
Q

density definition and units

A

mass found in a set volume of a material

gcm-3 or kgm-3

124
Q

density calculation

A

density = mass/volume
p=m/v

125
Q

how does rock density change with depth

A

increased depth, increased pressure –> particles more tightly packed = more dense

126
Q

why is it important to know the lithostatic pressure

A

if high it can be dangerous and lead to rock burst (rock explodes inward) at depth

important for mining and tunnelling

at depth (below 1km) it = hydrostatic pressure

127
Q

lithostatic pressure calculation

A

p x g x h

p=density
g= acceleration due to gravity
h=depth

units: likely kgm-3

128
Q

what are the disadvantages with testing rock strength in a lab

A

unconfined - not in situ may be stronger when it can transfer stress

rock sample- large vol of rock may not be
homogenous so may not be representative

doesn’t account for temp increase with depth

also doesn’t account for faults or fractures in other parts of rock

129
Q

homogenous def

A

same/ similar nature throughout

130
Q

how are rocks not always homogenous

A

magmatic differentiation

different composition = different hardness

131
Q

where is weakness present in rock

A

bedding planes
fractures
joints
discontinuities
foliation
lamination

132
Q

what happens when stress is applied to a discontinuity

A

rock is liable to fracture as weakest here

stress builds at discontinuity, then will reach peak strength and fail causing movement and strain –> then returns to residual strength

133
Q

asperity def

A

roughness of the surface of a discontinuity

134
Q

how does asperity effect rock

A

as asperity decreases rock is more likley to fail/ easier for it to fail

135
Q

residual strength def

A

remaining resistance to movement after rock has failed and been displaced

136
Q

joint def

A

fracture in a competent rock where there has been no observable displacement

137
Q

joint sets def

A

see multiple joints that often look sub-parallel (but can cross) formed as a result of regional stress e.g. folding

138
Q

how do joints react to tensional stress

A

pull apart

producing angular discontinuity which may resist shear stress

139
Q

how do joints react to shear joints

A

move past horizontally

smoother and less likely to resist stress

140
Q

how to jointed rocks become stronger again

A

compressive forces=close fractures/voids

intrusion into void

secondary precipitation of mineral into voids

narrow and tight joints = stronger

fewer joints are also stronger

141
Q

how does water in joints decrease rock strength

A

freezes - frost shattering = accelerate weathering + widen joint

hydrolysis and carbonation weather rock

142
Q

unloading joints def

A

rock is compressed by overlying mass–> mass removed–> competent rock expands in direction of pressure release –> causes fractures perpendicular to direction of release

143
Q

why are unloading joints problematic

A

form dangerous joint sets which are unpredictable and need grouting to fill in spaces/voids

144
Q

how do faults reduce rock strength

A

rock is ground producing fault gouge (incompetent and contains clay) which may shrink swell and reduces rock strength

especially is saturated

145
Q

bedding plane def

A

mark in time where dep temporarily ceased

usually between rock types

146
Q

why are bedding planes points of weakness

A

clay rich material settles out –> weak

can lead to unexpected failure

sudden change in permeability = water percolates down and accumulates

147
Q

Malpassat dam case study

A

built on gneiss with foliation -> 30-50 degree angle

a huge block of the rock was lifted and released all the water

presence of fault and force of water compressed the gneiss which increased pressure which dislodged block leading to failure

148
Q

Tebay case study

A

lots of folding + joint sets + changes in rock type + bedding planes

used extensive rock bolting to hold contorted cutting sides together

rock bolting = drilling steel rods into rock

149
Q

stages of geological site investigation

A

Desk study
site surface mapping
geophysical surveys
site subsurface mapping
Rock and soil property measurements
geohazard mapping
integration of data

150
Q

desk study

A

BGS mapping of UK show drift, bedrock and structures - available to consult

+ previous borehole data is available-shows geology changing with depth

aerial and satellite photos

look how water table changes

151
Q

Site surface mapping

A

large scale + cleared sites

all changes in earth material are mapped

not just about rock type and weathering but also subsoil e.g. may contain clay

also maps structures e.g. faults + frequency + openness + other discontinuity

152
Q

geophysical surveys on site

A

small sites - include ground penetrating radar to detect near surface anomalies

larger areas- use resistivity survey

seismic surveys required for deeper changes

simple data e.g. depth of weathering
lager use seismic refraction surveys

153
Q

site subsurface mapping

A

test pits dug to sample all critical areas

cheaper to excavate a shear sided pit large enough to climb in to extract samples

some soil mech properties can be tested in site –> deeper than 1m may collapse (health and safety)

cored metals drilled in samples

154
Q

rock and soil property measurements

A

samples of rocks and soil analysed for strength and composition

soils: simple penetration test –> test strength

rocks: carry out compressive and shear strength testing –> established how rocks react

test very important on weathered rock

permeability and porosity assesses to see effect on strength

155
Q

Geohazard mapping

A

gradient mapping –> slope stability
and how this would effect work and what would need to be done to stabilise

use contour maps and aerial photos and ground surveys —> tell-tale signs of landslides

heavy duty programs do calculations

ground surveys necessary if can be affected

alert of hazard

156
Q

integration of data

A

analysis of all data

GIS enabled to look at all information needed to plan the work in map form with data represented as a layer

157
Q

stress equation

A

stress= amount of deformation in direction of applied force ÷ initial length/vol/shape