Wood-water relationships 1 The technical aspects of the relationship between wood and water www.csaw.utas.edu.au Wood-water relationships 1 Content This lecture • Introduction to
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The technical aspects of the
relationship between wood and
water
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Wood-water relationships 1
Content
This lecture
• Introduction to wood-water relationships
• Water in wood
• Drying and dimensional change
• Hygroscopicity
Next lecture
• Measuring moisture content
• Drying and utility
• Moisture and production
• Moisture and service performance
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KDA503/335 Timber, its origin and characteristics
Introduction to wood-water
relationships
Water, water in wood, dimensional
change and hygroscopicity
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KDA503/335 Timber, its origin and characteristics
Wood-water relationships 1
Wood in the tree or in service contains water
• Wood in the tree or in service contains water
– Its moisture content is the weight of water in the piece as a percentage of dry wood fiber
Free water in the cell
Air dry timber
Bound water in the
cell wall
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KDA503/335 Timber, its origin and characteristics
Wood-water relationships 1
Wood, dimensional change & hygroscopicity
• Wood is hygroscopic: it loses or gains moisture
with fluctuations in environmental humidity
Air dry timber
• Wood changes in size as it loses or gaining
moisture
Bound water in the
cell wall
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KDA503/335 Timber, its origin and characteristics
Water in wood
Wood in the tree or in service contains water
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Water
• Water (H2O) is a common molecule
– Held together by electron sharing, it has an unbalanced
electrostatic charge
– The angle of the molecular bonds is 1050
• In nature, it existing in gaseous, liquid and solid forms
+
-
xnet.rrc.mb.ca/rcharney/the%20water%20molecule.htm
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Wood-water relationships 1
Water content of air
• Humidity is a general term for the presence of water vapour in air
– Absolute humidity - The amount of moisture in air
It is usually expressed as the weight of water vapour in a unit weight of dry air
– For any given temperature and pressure, there is a specific limit to the amount of water vapour that air
can hold At a given temperature, relative humidity
is the amount of moisture in air as a percentage of the maximum moisture carrying capacity of the air
– These and similar relationships can be displayed on
psychometric charts
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KDA503/335 Timber, its origin and characteristics
Wood-water relationships 1
http://www.av8n.com/physics/axes.htm
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KDA503/335 Timber, its origin and characteristics
Wood-water relationships 1
Moisture content of wood
• The moisture content of timber is expressed as
the weight of water in the piece as a percentage of the weight of oven dry wood
fiber
%
100 MC x
wood the of weight dry
wood the in water of weight
=
!!
"
#
$$
%
&
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KDA503/335 Timber, its origin and characteristics
Wood-water relationships 1
Water in wood in standing trees
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KDA503/335 Timber, its origin and characteristics
Wood-water relationships 1
Water in timber in service environments
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Water in wood and water to wood
• Free - The water
within cavities or
lumens, in the
cells of wood
• Bound - the water
weakly chemically
bound in the cell
walls of wood
From UBC 2009 Wood474 Avramidis Wood and Water
Hydroxyl group on
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Wood-water relationships 1
UBC 2009 Wood474 Avramidis Wood and Water
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KDA503/335 Timber, its origin and characteristics
Drying and dimensional change
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KDA503/335 Timber, its origin and characteristics
Wood-water relationships 1
Removing moisture
• When milled, timber has a relatively high moisture content
• It is dried to increase its utility
Free water
Air dry timber Bound water
To dry timber, a moisture gradient
has to be established in the piece
Fibre saturation point is when the
cell walls are saturated with bound water but the cell cavities are free of water It occurs at approx~ 30% moisture content
Timber shrinks as the bound water is removed
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KDA503/335 Timber, its origin and characteristics
Wood-water relationships 1
Moisture and shrinkage
0
10
20
30
40
50
60
70
80
loss of moisture with little change in size
range over which shrinkage commences
straight line portion of graph where shrinkage is proportional to moisture content
example of service conditions and
Equilibrium Moisture Content
Shrinkage
free moisture
fibre saturation point
bound moisture
Fibre saturation point
Service EMC zone
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KDA503/335 Timber, its origin and characteristics
Wood-water relationships 1
Drying mechanisms
Dryings two processes
• Water has to removed from the wood surface – With the control of temperature, humidity and air flow
• Water has to move from the woods interiors to the surface
– Through the bulk flow of vapour or liquid, or diffusion from cell to cell
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Timber dries at different rates
• Pines have a relatively porous cell
structure that allow bulk flow:
– They can be dried very quickly
– Turnaround time from saw to store can
be as low as a week
• Hardwoods have a non-porous cell
structure The moisture must diffuse
through the cell wall
– Drying can be very slow
– It must be done carefully
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Shrinkage and cell structure
• As moisture is drawn out of the cell wall, the wood fiber shrinks
This cell will shrink more than this one
Shrinkage/swelling ~ specific gravity ~ cell wall thickness
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KDA503/335 Timber, its origin and characteristics
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Shrinkage and grain direction
• As the thicker latewood cells run tangentially, shrinkage is
greatest in this direction, less radially, least longitudinally
• Rays and the irregular arrangement of cells generate constraint
and additional variability
tangential
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KDA503/335 Timber, its origin and characteristics
Wood-water relationships 1
Shrinkage rates longitudinal ~ 0.1 - 0.3%, radial ~ 2.5 - 6.5%, tangential ~ 4 - 13%
Tangential shrinkage
Radial shrinkage
Longitudinal shrinkage
Softwood
Hardwood
Shrinkage from 25% to 12% MC
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KDA503/335 Timber, its origin and characteristics
Wood-water relationships 1
Shrinkage effects
• Tangential shrinkage is almost always highest;
• This tends to shorten the growth rings as the
timber dries, distorting cut sections
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KDA503/335 Timber, its origin and characteristics
Wood-water relationships 1
Other shrinkage effects
• Simple shrinkage is complicated by other drying effects including:
– Collapse and reconditioning, – Surface and internal checking
– Grain deviation along or through the board,
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Wood-water relationships 1
Wood, dimensional change & hygroscopicity
• Wood is hygroscopic
• It loses or gains moisture to be in equilibrium with variation in environmental humidity
• As it does so, its dimensions change
Air dry timber
Bound water in the
cell wall
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KDA503/335 Timber, its origin and characteristics
Wood-water relationships 1
Moisture exchange is dynamic
environment
Dynamic exchange of heat and water
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KDA503/335 Timber, its origin and characteristics
Wood-water relationships 1
Equilibrium moisture content
• Equilibrium moisture content (EMC) is:
– the moisture content where timber neither gains nor loses moisture from the surrounding atmosphere
• There is a direct relationship between relative humidity, temperature and woods EMC
FWPA, 2009, Timber Flooring
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KDA503/335 Timber, its origin and characteristics
Wood-water relationships 1
Rate of change of MC
• The rate of MC change
in timber with changes
in the surrounding
environment varies
with species type,
density and other
characteristics
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KDA503/335 Timber, its origin and characteristics
Wood-water relationships 1
Unit shrinkage rates
Softwood
Hardwood
Unit Shrinkage (shrinkage for 1% change in MC)
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Calculations of steady state ingress of MC%
Unit width x unit movement per 1% x MC% change = total unit movement
Back sawn Radiata pine board of 85mm cover with a 3%MC change
85mm x 0.27% x 3 = 0.6885mm of movement either + or –
Back sawn Tas Oak board of 85mm cover with a 3%MC change
85mm x 0.36% x 3 = 0.918 mm of movement either + or –
Quarter sawn Tas Oak board using the same parameters
85mm x 0.23% x 3 = 0.5865 mm of movement either + or –
To calculate the total movement in the width of a floor per MC%:
Unit width x unit movement per1% x MC% change x number of units =
total movement in the width of the floor
Back sawn Radiata pine board of 85mm cover in a 6000mm wide floor
85mm x 0.27% x 3 = 0.6885mm
x (6000 / 85) = 48.59mm
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Wood-water relationships 1
Uneven moisture ingress
• Moisture ingress is often uneven
• Uneven moisture movement from one face of a board will distort the piece
Uneven moisture ingress in a bamboo floor
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KDA503/335 Timber, its origin and characteristics
Wood-water relationships 1
Summary
• Wood in the tree or in service contains
water
– Its moisture content is the weight of water in
the piece as a percentage of dry wood fiber
• Wood changes in size as it loses or
gaining moisture
• Wood is hygroscopic: it loses or gains
moisture with fluctuations in
environmental humidity
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KDA503/335 Timber, its origin and characteristics
Wood-water relationships 1