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Materials in Civil
andConstructionEngineering土木工程材料Chapter
1BasicProperties
ofCivilEngineering Materials1.1
BasicPhysical
Properties
of
Materials1.2
MechanicalProperties
of
Materials1.3
Durability
of
MaterialsContent1.1Basic
Properties
ofCivil Engineering
Materials1.1 Basic
Physical
Properties
of
Materials1.1.1
Density,
ApparentDensity
andBulkD1.DensityDensity
isthe
mass
per
unitvolumewhenthematerial
isin
the
absolute
densestate.Itcan
beshownthat:In
thisformula:
isthe
density
(g/cm3);misthemassunderdry
conditions
(g);V
is
thevolume
underabsolutely
compactconditions
(cm3).Volume
in
the
absolute
dense
refers
to
the
volume
of
the
individual
particles
only
(no
voids).
A
lot
of
civilengineering
materials
include
voids,
such
as
brick,
stone
and
concrete.
As
for
these
materials,
it
is
required
togrind
the
materials
into
powder,
then
dry
to
constant
weight
and
measure
its
volume
using
Li
Bottle,
which
is
alsocalled
density
bottle.mV
1.1 BasicPhysical
Properties
of
Materials2.
ApparentDensityApparent
density
is
the
massper
unit
volume
when
the
material
is
in
natural
state.In
this
formula:
ρ0
is
the
apparent
density
(kg/m3);m
isthemassunder
dry
conditions
(kg);V0
is
the
volume
under
natural
conditions
(m3).The
volume
in
natural
state
includes
the
volume
of
the
solid
and
internal
pores.
The
apparentdensity
varies
with
moisture
content.
Apparent
density
generally
refers
to
apparent
density
in
dry
state.0
mV0
1.1 BasicPhysical
Properties
of
Materials3.BulkDensityBulk
density
ismassper
unit
volume
when
powdery
or
particle
materials
arein
the
stacking
condition.In
this
formula:
0
is
the
bulk
density
(kg/m3);mis
the
massunder
dry
conditions
(kg);V0
is
the
volume
under
packing
conditions
(m3).Bulk
density
isnot
an
intrinsic
property
of
a
material;
it
varies
from
how
the
material
is
handled.0V0
mstacking
stateincludesparticle
volumeinter-particle
void
volumeinternal
pore
volume1.1 BasicPhysical
Properties
of
MaterialsTable
1.1
Density,
apparent
density
andbulkdensity
of
some
civil
engineering
materialsNameDensity/(g/cm3)Apparent
Density/(kg/m3)BulkDensity/(kg/m3)Steel7.857850-Granite2.6-2.92500-2850-Limestone2.6-2.82000-2600-Gravels
or
Pebbles2.6-2.9-1400-1700Ordinary
Sand2.6-2.8-1450-1700Sintered
Clay
Brick2.5-2.71500-1800-Cement3.0-3.2-1300-1700Wood1.55-1.60400-800-Asphalt
Concrete-2300-2400-Ordinary
Concrete-2100-2600-1.1 BasicPhysical
Properties
of
Materials1.1.2 Solidity
Porosity
and
VoidagePorosity
is
afraction
of
the
volume
of
voids
over
the
total
volume.Porosity
represents
the
densification
of
material.Porosity
includes
connected
pore
andclosed
poreaccording
to
its
structure,
andit
can
beclassified
into
coarse
pore,
fine
pore
and
micropore
accordingto
its
size.Voidage
is
the
proportion
ofspacing
volume
amongtheparticlestothe
bulk
volume
of
thenon-coherent
material
in
somecontainer.Figure1.1
Sketch
map
of
poresVoidage
is
animportant
parameter
when
controlling
thegradation
of
concrete
andcalculating
sand
content.0
V0
P
1
100%
1
100%V
0
V0
0
P
1
100%
1
100%V
Thehigherporositythe
lowerdensification1.1 BasicPhysical
Properties
of
Materials(a)hydrophilic
property
θ<90
(b)
hydrophobic
property
90
≤θ≤180
Figure
1.2
Sketch
map
of
wetting
angle
(θ)Asphalt,
paraffin
wax
and
some
plasticused
in
civilengineering
are
hydrophobic
materials.1.1.3 Hydrophilic
and
HydrophobicHydrophilic
property
refers
tothe
material
property
which
can
bewettedwhen
it
contacts
with
water
in
theair
(0
≤θ≤90
).Most
civilengineeringmaterials
belong
to
hydrophilicmaterials,
such
asstone,
brick,
block,
glass
andpottery.
Asforhydrophilicmaterial,
water-proof
processingmethodcanbeused
to
improveitswater
resistance.Hydrophobic
property
refers
tothematerialproperty
which
cannotbewettedwhen
it
contacts
with
water
in
theair
(90
≤θ≤180
).1.1 BasicPhysical
Properties
of
Materials1.1.4 Water
Absorption
and
Moisture
AbsorptionWater
absorption
refers
to
the
ratio
of
the
weight
of
water
absorbed
by
a
material,
to
the
weight
ofthe
drymaterials.Specific
absorption
ofquality:Specific
absorption
ofvolume:In
this
formula:
m1
is
the
mass
of
the
materialat
water-saturated
state(g);m2
is
the
massof
the
material
under
dry
condition(g);Vis
the
volume
of
material
under
natural
condition(cm3).
m1
m2m2
100%mWW
m1
m2
100%VV1.1 Basic
Physical
Properties
of
MaterialsThe
water
absorption
is
related
to
porosity.
Water
can't
enter
into
the
dead-end
pores.
As
for
smallinterconnected
pores,
the
more
the
pores
are,
the
higher
the
water
absorption
is.
Open
pores
are
big,but
it's
difficult
to
store
water,
so
its
water
absorption
is
less.
Different
material
has
diverse
waterabsorption
for
its
different
internal
structure.Moisture
absorption
refers
to
the
ratio
of
weight
of
materials
with
absorbed
water
in
the
moist
air
tothat
of
drymaterials.In
this
formula:
m1
is
the
quality
of
material
in
the
moisture
state(g);m2
is
the
quality
of
material
under
the
dry
condition(g).
m1
m2m2
100%mW1.1 Basic
Physical
Properties
of
MaterialsSuchitemsmay
beused
in
wetenvironments
or
underwaterto
specified
depths.Waterproofingdescribesmaking
anobjectwaterproof
or
water-resistant
(suchasacamera,
watch
or
mobilephone)."Waterresistant"and
"waterproof"often
refertopenetration
of
waterin
its
liquidstate
andpossibly
under
pressure
wheredampproofrefersto
theresistance
to
humidity
ordampness.
Inbuildingconstruction,waterproofing
isafundamentalaspect
of
creating
abuilding
envelope
which
is
acontrolled
environment.
Theroof
covering
materials,
siding,foundations,
andallofthe
various
penetrations
through
these
surfaces
need
tobewater-resistant
andsometimeswaterproof.WaterresistantObjects
relatively
unaffected
bywaterorresistingtheingress
ofwaterunderspecified
conditions.1.1.5 WaterResistant
and
Waterproofing1.1 BasicPhysical
Properties
of
Materials1.1.6 Anti-permeabilityAnti-permeability
refers
to
the
property
of
something
that
cannot
be
pervaded
by
a
liquid
underpressure.
Generally,
Permeability
coefficient
or
impermeability
grade
is
used
to
describe
the
property.Permeability
coefficient
derives
from
Darcy'slaw.Darcy's
law
at
constant
elevation
is
a
simple
proportional
relationship
between
the
instantaneousdischarge
rate
through
a
porous
medium,
the
viscosity
of
the
fluid
and
the
pressure
drop
over
a
givendistance.Figure1.3
Definitions
and
directions
forDarcy's
law1.1 Basic
Physical
Properties
of
MaterialsIn
this
formula:Q
isthe
total
discharge
(m3/s);k
is
theintrinstic
permeability
ofmedium;A
is
thecross-sectional
areaof
flow
(m2);(pb-pa)
isthe
totalpressure
drop(Pa);
is
theviscosity
(Pa·s);Lis
thelength
overwhich
thepressuredrop
is
taking
place
(m).Asforconcrete
or
mortar,
impermeability
gradeisrepresented
asthe
index
of
impermeability.
Higher
the
gradeis,
better
the
impermeability
is.Q
kA
(
pb
pa
)L
Higherthegradeisbetter
theimpermeability
isThenegative
signisneeded
because
fluid
flowsfrom
highpressuretolowpressure.1.1 Basic
Physical
Properties
of
MaterialsFreezing
ResistanceFreezing
resistance
refers
to
the
property
of
materials
that
can
endure
repeated
freezing
and
thawing
cyclewithout
damage
and
its
strength
can't
be
obviously
reduced.
Generally,
Dn
is
taken
as
frost
resistance
grade,
inwhich
n
is
themaximum
times
of
freezing
and
thawing
cycle
when
materials
reachtheregulated
damage
extent.Both
the
anti-permeability
and
the
freezing
resistance
are
related
to
voidage
of
materials.
Materials
with
lessvoidage
or
end
voidage
has
higher
anti-permeability
and
the
freezing
resistance.
The
small
and
connected
poresaredisadvantageous
to
these
properties.ThermalConduction
and
Specific
HeatThermalconduction
is
the
transferofheat
from
one
part
of
abodytoanother
or
from
onebodytoanotherthroughits
physical
contact.
Nonmetalshavealow
coefficient
ofthermalconductivity.
Metals
haveamuchhigherone
because
their
freeelectrons
transferthevibrations
much
more
rapidly.
Thus,
metalsare
goodconductors
ofheat.1.1 Basic
Physical
Properties
of
Materials1.1.8 Thermal
Conduction
and
Specific
HeatThe
rate
of
heat
transfer
by
conduction
is
dependent
on
the
temperature
difference,
the
size
of
the
area
incontact,
thethickness
of
thematerial,
and
thethermalproperties
of
thematerial(s)
in
contact.Thequantity
ofheattransferred
by
conduction
isdefined
as
follows:
Qd
At(T2
T1
)In
this
formula:λ
isthe
coefficient
of
thermalconductivity
of
thematerial[W/(m·K)];Qis
theconducted
heatquantity
(J);A
istheheat-transfer
area
(m2);t
isthe
time
for
theheattransfer
(s);T1
isthe
temperature
on
warmer
side
(K);T2
is
thetemperature
on
thecolderside
(K);d
is
thethickness
of
a
material
(m).1.1 Basic
Physical
Properties
of
MaterialsThe
specific
heat
is
the
amount
of
heat
per
unit
mass
required
to
raise
the
temperature
by
one
degree
Celsius.The
relationship
between
heat
and
temperature
change
is
usually
expressed
in
the
form
shown
below
where
c
isthe
specific
heat.
The
relationship
does
not
apply
if
a
phase
change
is
encountered,
because
the
heat
added
orremoved
during
a
phase
change
does
not
change
the
temperature.Table
1.2
lists
afew
construction
materials
andtheirthermalproperties
atnominalroom
temperature.Table
1.2Construction
material
thermal
properties
at
room
temperatureMaterialThermal
Conductivity
/[W/(m·K)]Specific
Heat/[J/(kg·
C)]Density/(kg/m3)Brick0.78401600Concrete–cast
Dense1.48402100Concrete–cast
Light0.410001200Granite1.7-3.982026001.1 Basic
Physical
Properties
of
MaterialsGlass
(window)0.88802700Hardwoods
(oak)0.161250720Softwoods
(pine)0.121350510Polyvinyl
Chloride0.12-0.2512501400Paper0.041300930Acoustic
Tile0.061340290Particle
Board
(low
density)0.081300590Particle
Board
(high
density)0.1713001000Fiberglass0.04700150Expanded
Polystyrene0.031200501.2Mechanical Properties
ofMaterials1.2 Mechanical
Properties
ofMaterialsThemechanical
properties
of
amaterial
describehow
itwillreact
toexternal
loads.Mechanical
propertiesoccuras
aresultof
thephysical
properties
inherent
toeachmaterial,
andaredeterminedthroughaseries
ofstandardized
mechanical
tests.1.2.1 StrengthStrength
is
the
material
capacity
of
resisting
breakage
by
the
external
force.
Strength
includes
compressivestrength,
tensile
strength,shearingstrength
and
bending
strength
accordingto
thedifferent
formof
external
force.Thecompressivestrength
is
thecapacity
of
amaterial
orstructuretowithstandloads
tendingtoreduce
size.
Itcan
bemeasured
by
plotting
applied
forceagainstdeformationina
testing
machine.
Some
material
fracture
attheir
compressive
strength
limit;
othersdeform
irreversibly,
soagiven
amountofdeformationmay
beconsideredas
the
limit
forcompressive
load.Compressive
strength
isa
key
valuefor
design
ofstructures.1.2 Mechanical
Properties
ofMaterialsTensile
strength
is
not
the
same
as
compressive
strength
and
thevalues
can
be
quite
different.
Some
materials
will
break
sharply,without
plastic
deformation,
in
what
is
called
a
brittle
failure.
Others,whichare
more
ductile,
including
most
metals,will
experience
someplastic
deformation
and
possibly
necking
before
fracture.Shear
strength
is
the
maximum
shear
stress
which
a
material
canwithstand
without
rupture.
In
structural
and
mechanicalengineering
the
shear
strength
of
a
component
is
important
fordesigning
the
dimensions
and
materials
to
be
used
for
themanufacture/construction
of
the
component
(such
as
beams,
plates,or
bolts).The
flexural
strength
represents
the
highest
stress
experiencedwithin
the
material
at
its
moment
of
rupture.
It
is
measured
in
termsof
stress.
Three
and
four
points
bend
tests
are
commonly
used
todetermine
the
flexural
strength
of
a
specimen.the
maximum
stress
that
amaterialcan
withstand
while
beingstretched
orpulled
before
failingor
breakingTensilestrengtha
material's
ability
toresistforcesthat
can
causetheinternal
structure
of
thematerialtoslideagainst
itselfShearingstrengtha
material's
ability
to
resistdeformationunder
loadBendingstrengthorflexuralstrength1.2 Mechanical
Properties
ofMaterialsTable
1.3FormulaofstrengthClassificationSketchmapFormulaAnnotationsCompressive
strengthfcfc=F/Af—Strength(MPa)F—Failure
load(N)A—Loaded
area(mm2)Tensilestrengthftft=F/AShearing
strength
fvfv=F/ABendingstrengthfmfm=3FI/2bh2fm=FI/bh21.2 Mechanical
Properties
ofMaterials1.2.2 Elastic
and
Plastic
DeformationIn
materials
science,
deformation
is
a
change
in
the
shape
or
size
of
anobject
due
to
an
applied
force
or
a
change
in
temperature.
A
temporary
shapechange
that
is
self-reversing
after
the
force
is
removed,so
thatthe
objectreturns
toits
original
shape,
is
called
elastic
deformation.
Elastomers
and
shapememory
metals
such
as
nitinol
exhibit
large
elastic
deformation
ranges,
as
doesrubber.
However,
elasticity
is
nonlinear
inthese
materials.Normal
metals,ceramicsand
most
crystalsshow
linear
elasticityand
a
smallerelasticrange.When
amaterial
distorts
under
pressure
butdoesnotreturnto
its
originalshape
afterthe
pressure
isreleased,
itiscalled
plasticdeformation.Figure1.4 Deformationcurve1.2 Mechanical
Properties
ofMaterialsThis
type
of
deformation
is
irreversible.
However,
an
object
inthe
plastic
deformation
range
will
first
have
undergone
elasticdeformation,
which
is
reversible,
so
the
object
will
return
part
wayto
its
original
shape.
Soft
thermoplastics
have
a
rather
large
plasticdeformation
range
as
do
ductile
metals
such
as
copper,
silver,
goldand
steel,
but
cast
iron
does
not.
Hard
thermosetting
plastics,rubber,
crystals,
and
ceramics
have
minimal
plastic
deformationranges.1.2 Mechanical
Properties
ofMaterials1.2.3 Ductility
andBrittlenessDuctility
and
brittleness
are
two
of
the
most
important
physicalproperties
of
materials
in
construction
engineering.
Brittleness
is
theproperty
of
a
material
that
will
fracture
without
appreciable
prior
plasticdeformation.
Brittleness
is
lack
of
ductility
and
for
a
brittle
material
thereis
no
plastic
deformation.
Theelastic
stage
is
followed
by
immediatefracture.
Typical
brittle
materials
include
glass,
concrete,
ceramics,
stone,and
cast
iron.
Ductility
is
the
property
of
a
material
that
can
be
plasticallydeformed
by
elongation
without
fracture.
Ductile
materials
can
typicallybe
plastically
elongated
with
more
than
15%
before
they
fracture.
Typicalductilematerials
includecopper,mild
steel,
and
thermoplastics.Figure1.5 Stress-straincurvesforbrittleandductilematerials1.2 Mechanical
Properties
ofMaterialsDuctility
of
a
material
is
its
ability
to
deform
when
a
tensile
force
is
applied
upon
it.
It
is
also
referred
toastheability
of
asubstance
to
withstand
plasticdeformation
without
undergoing
rupture.
Brittleness,
on
theother
hand
is
exactly
an
opposite
property
of
ductility
as
it
is
the
ability
of
a
material
to
break
without
firstundergoing
any
kind
of
deformation
upon
application
of
force.1.2.4 HardnessHardness
is
a
measure
of
how
resistant
solid
matter
is
to
various
kinds
of
permanent
shape
change
whenacompressive
force
is
applied.Hardness
isdependenton
ductility,
elastic
stiffness,
plasticity,
strain,
strength,
toughness,
viscoelasticity,and
viscosity.1.2 Mechanical
Properties
ofMaterialsCommon
examplesof
hard
matter
are
ceramics,
concrete,
certain
metals,
andsuper-hard
materials.
Thereare
three
main
types
of
hardness
measurements:
scratch,
indentation,
and
rebound.
Within
each
of
theseclasses
of
measurement
there
are
individual
measurement
scales.
Scratch
hardness
tests
are
often
used
todetermine
the
hardness
of
natural
mineral.
Steel,
wood
and
concrete
is
usually
determined
by
means
ofindentation
hardness
test.
Rebound
hammer
measures
the
surface
hardness
of
the
concrete.
The
surface
ofconcrete
gets
harder
as
concrete
gains
strength;
thus,
the
strength
of
concrete
can
be
estimated
using
thismethod.Figure
1.6
Concrete
test
hammer1.2 Mechanical
Properties
ofMaterialsStress
is
defined
as
force
per
unit
area.
It
has
the
same
units
as
pressure,
and
in
fact
pressure
is
one
special
variety
ofstress.
However,
stress
is
a
much
more
complex
quantity
than
pressure
because
it
varies
both
with
direction
and
with
thesurface
it
acts
on.
Strain
is
defined
as
the
amount
of
deformation
an
object
experiences
compared
to
its
original
size
andshape.It
is
unique
for
each
material
and
is
found
by
recording
the
amount
of
deformation
(strain)
at
distinct
intervals
oftensile
or
compressive
loading
(stress).
A
lot
of
useful
information
about
the
material
can
be
revealed
by
plotting
thestress-strain
diagram.
Figure
1.7
shows
the
typical
uniaxial
tensile
or
compressive
stress-strain
curves
for
severalengineeringmaterials.(a)
glass
and
chalk(b)
steel (a)
glass
and
chalk (d)
concreteFigure
1.7
Typical
uniaxial
stress-strain
diagrams
for
someengineering
ma
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