2. Physical properties of wood
Timber is classified into hard and soft wood species. Softwoods include pine, spruce, fir, larch and others. Hardwoods include birch, oak, beech, hornbeam, maple, ash, poplar, lime, willow, fruit species and others. This classification is based upon the presence or absence of specific cellular characteristics which have no significant effect upon the pyrolysis process.
In particular, the classification «hardwood» is applied to all those species whose cellular composition includes «vessels»; long, open, tubular cells. This type of cell is absent in the softwood species. This is why e.g. balsa, a light and easily workable timber, is called a «hardwood» whereas e.g. larch, a tough and often dense timber, is a softwood.
In our activity we consider only those properties of wood that are relevant in the procurement, storage, drying and pyrolysis of wood:
- Porosity
- Specific or volumetric weight (density)
- Humidity (moisture capacity)
- Drying ability
- Heat capacity
2.1. Wood porosity
Wood consists mainly of tubular cells and therefore has great porosity. Porosity affects the specific gravity, hygroscopicity, thermal conductivity and other physical properties of wood and can be calculated based on bulk density. The degree of porosity also affects the product of wood pyrolysis – charcoal, which has a significantly higher porosity (air/water capacity by weight) compared to the wood from which it is obtained.
2.2. Specific or volumetric weight
It is important to distinguish the specific gravity of the solid matter component of wood and that of wood as it is ordinarily presented, i.e. as a cellular body.
The specific gravity of woody solid matter, regardless of species, is on average about 1.55 kg/dm3.
The specific mass (density) of wood as we see and recognise it mainly depends on the porosity and moisture of the wood. Porosity changes according to the species and age of the tree, its growing conditions and other factors.
Due to the dependence of the volumetric weight of wood on moisture content, it is usually defined in 3 ways: for absolutely dry («bone-dry»), air-dry («seasoned») and freshly cut («green») wood. The average specific gravity of different species of wood in bone-dry* condition is given in table 1.
Table 1
Bone-dry density of the most common wood species
|
Species
|
Density, g/cm3
|
|
Density range
|
Average
|
|
Fir
|
0,31—0,50
|
0,38
|
|
Spruce
|
0,30—0,56
|
0,42
|
|
Pine
|
0,31—0,65
|
0,47
|
|
Larch
|
0,43-0,82
|
0,63
|
|
Aspen
|
0,32—0,61
|
0,47
|
|
Lime
|
0,33—0,62
|
0,47
|
|
Alder
|
0,33—0,64
|
0,49
|
|
Birch
|
0,42—0,79
|
0,60
|
|
Beech
|
0,45—0,79
|
0,64
|
|
Sycamore, maple
|
0,48—0,74
|
0,65
|
|
Oak
|
0,46—0,88
|
0,68
|
*Wood dried to constant weight at a temperature of 103 ± 2 ° C
The following relationship exists between porosity and bulk density of wood in an absolutely dry state:
С = (1/х) yd
where:
С – wood density:
х — percentage porosity;
— density of timber as presented;
—density of solid woody material.
The volumetric weight of wood of the same species varies significantly depending on the growing conditions and age of the tree, resinousness and other conditions. So, for birch, it ranges from 0.51 to 0.74: for pine, from 0.31 to 0.71: for spruce, from 0.35 to 0.60 (for bone-dry wood). The specific gravity of wood taken from different parts of the same tree is not uniform: at the base of the branches it is largest, in the root greater than at the crown, and in the heartwood greater than in sapwood.
The solid biomass content of 1 m3 wood can thus be calculated. On average it is as follows: pine – 285kg, spruce — 253kg, fir – 250kg, larch – 385kg, aspen – 265kg, birch – 354 kg.
Further, a 1 m3 stack or pallet of cleft firewood has equivalent solid wood content to a single 680 kg block of wood.
2.3. Wood moisture
Water in wood is present in the cavities (lumena) of the cells and also impregnates the cell walls, where it is held by loose chemical bonding. Accordingly, free (or capillary) and bound (or colloidal) water are distinguished in wood. In general, bound water accounts for wood moisture content (MC) up to circa 28%: removing this moisture requires a relatively large input of energy. Above this MC, the water is not chemically attached to the wood structure and requires a lesser input of energy for elimination..
The MC transition betwee bound water and free water is called the fiber saturation point (FSP): it lies in the range of 23-30% of absolute humidity depending on the type of wood. In general, wood scientists would consider 27% absolute MC, or thereabouts, as being FSP in temperate species.
Moisture distribution is not uniform in different parts of the tree. Sapwood (the outer part of the stem) tends to a higher MC than heartwood. The basal trunk contains more moisture than the crown. A tree growing on marshy soil contains more moisture than a tree growing on dry soil. MC can be subject to seasonal variations.
For dry distillation (pyrolysis) of wood, the moisture content is of paramount importance. The higher the moisture content in the wood, the greater will be the process heat requirement or the lower will be the yield of valuable products.
2.3.1. The difference between Absolute and Relative Humidity of wood.
Absolute humidity of wood is the ratio of the weight of moisture contained in wood to the mass of absolutely dry wood, expressed as a percentage.
Example: If a raw 300 g sample weighs 200 g after drying to constant mass, then its absolute moisture content (300-200) / 200 * 100% = 50%)
Relative humidity of wood is the ratio of the weight of the moisture contained in the wood to the weight of the raw wood, expressed as a percentage.
Example: If a raw 300 g sample weighs 200 g after drying to constant mass, then its relative humidity (300-200) / 300 * 100% = 33%
It is very important to define which expression of MC is in use. As a generality, wood producers, traders and processors will speak of MC as relative humidity: researchers and wood scientists prefer to use absolute humidity.
2.3.2. Degrees of Absolute Wood Moisture
| Name |
Absolute MC, % |
Preparation conditions |
| Wet wood |
More than 100 % |
prolonged exposure to water |
| Freshly cut |
50—100 % |
variable by season of harvesting |
| Air-dried |
15—20 % |
Prolonged period in exposure to warm, dry natural air |
| chamber-dried |
6—10 % |
Dried in artificially controlled environment |
| Absolutely dry |
0 % |
Dried by excess heat until stable mass is reached |
2.4. Natural (atmospheric) drying of wood.
During natural drying, the wood loses moisture through contact with circulating natural atmospheric air of relative humidity < 100%,. The speed of natural drying is greater, the higher the temperature of the air, the lower its relative humidity and the faster its movement. Moisture release per surface area of wood is variable, according to the exposed dimension of the wood: most of all from a transverse section of wood (across the grain), less from a longitudinal split (along the grain) and even less from a surface covered with bark.
Evaporation from wood proceeds at a lower rate than evaporation from an open source of water. The more cell walls the water molecules encounter when passing from the inside of a piece of wood to the outside surface, the slower this process. On a path parallel to the axis of the trunk, the cell walls are fewer than on a path perpendicular to the axis of the trunk. Therefore, through a cross-section of wood, more water vapor is released per unit of drying time from a cross-sectional than from a lateral surface of the wood.
The relative humidity and air temperature have a very large effect on the speed of drying viz:
- It has been shown that under conditions, for example, of the Urals, the most intensive drying of wood is observed in the period April — July;
- during the first year post-felling, coniferous industrial firewood does not dry as completely as firewood cleared of bark;
- In the autumn months, due to the easier absorption of moisture by firewood without bark, the humidity of both types of firewood differs only slightly;
- Coniferous firewood not de-barked dries slightly during the first year, the bark is shed during the second year and the wood becomes air-dry;
- Birch dries slower than conifers. De-barked birch firewood reaches its maximum dryness only in the second year of storage, and birch remaining in the bark dries out less.
- Split firewood, bark on, dries faster than de-barked roundwood.
- The average moisture content in freshly cut birch is 56.2% (from 54% to 59%), in pine — 49.9% (from 46% to 53%), in spruce — 50.2% (from 44% to 55%) ) (percentage of relative humidity), in oak – 55%. (from 52% to 58%)
- With natural drying, no matter how long it lasts, the wood will never attain a completely dry state. Accordingly, the temperature and relative humidity of the outdoor air will only achieve equilibrium humidity.
- In natural drying for 1.5 years after felling, the relative humidity of air-dried firewood reaches approximately 20%.
- When lying (in woodpiles in a forest or in a warehouse), firewood gradually loses moisture. The speed of this natural drying depends on the type of wood, its initial moisture content, method of cutting, relative humidity, temperature and air velocity.
How to dry firewood 1 m long, harvested in January, at storage under a canopy is shown in table 2.
Drying a piece of wood, due to its low thermal conductivity, is non-uniform. The outer layers of wood dry much faster than the inner ones. With fast drying of thick and damp logs, the outer layers are dry, while the inner layers are just starting to lose moisture. As a result, wood shrinkage is anisotropic (differential by dimension); this causes the formation of cracks in the wood, extending from the outer surface inward along the radius. Cracks in the wood may also occur as a result of faster drying of the core compared to sapwood.
2.5. Heat capacity
The heat capacity of absolutely dry wood of all species is 0.324 kcal / kg, and resinous substances – 0.5 kcal / kg.
When wood is heated by 1 ° (within 0 ° – 100 °), it expands by 0.040 mm/metre in the transverse direction and by 0.005 mm/metre in the longitudinal direction.
Wood is a poor conductor of heat. Its thermal conductivity depends on the conditional density of the wood (variable by species), the direction of the heat flux relative to the axis of the wood fiber, temperature and humidity. The coefficient of thermal conductivity of dry wood ranges from 0.1-0.4 W / m². An increase in the density of dry wood, i.e., an increase in the proportion occupied by wood substance per unit gross volume, leads to an increase in thermal conductivity. This is due to the fact that the wood substance has a 20 times greater thermal conductivity than air. The thermal conductivity of wood along the fibers is 3 times greater than across the fibers. In the radial and tangential directions, the thermal conductivity of wood may differ slightly because the zones of late wood of annual layers are elongated in the tangential direction. Late wood, especially coniferous, is denser and therefore more thermally conductive. Moistening of wood, i.e. replacing the air contained in it with water, which has 23 times greater thermal conductivity, leads to an increase in the thermal conductivity of wood. An increase in the temperature of wet wood leads to an even greater increase in thermal conductivity.