=Paper= {{Paper |id=Vol-1498/HAICTA_2015_paper47 |storemode=property |title=Inferences on Wood Density Variability in European Ash Growing in Two Different Floodplain Forest Sites |pdfUrl=https://ceur-ws.org/Vol-1498/HAICTA_2015_paper47.pdf |volume=Vol-1498 |dblpUrl=https://dblp.org/rec/conf/haicta/GiagliBGV15 }} ==Inferences on Wood Density Variability in European Ash Growing in Two Different Floodplain Forest Sites== https://ceur-ws.org/Vol-1498/HAICTA_2015_paper47.pdf

Inferences on Wood Density Variability in European Ash
Growing in Two Different Floodplain Forest Sites

Kyriaki Giagli1, Jan Baar2, Vladimír Gryc2, Hanuš Vavrčík2
1
Faculty of Forestry and Wood Technology, Mendel University in Brno, Zemĕdĕlská 3, 61300
Brno, Czech Republic, e-mail: giagli@node.mendelu.cz
2
Faculty of Forestry and Wood Technology, Mendel University in Brno, Zemĕdĕlská 3, 61300
Brno, Czech Republic

Abstract. Wood density variations in 110-year-old European ash (Fraxinus
excelsior L.) wood was examined in relation with different water regime
treatments in two floodplain forest sites of similar elevation (Lednice 161 m
a.s.l. and Tvrdonice 154 m a.s.l.) in South Moravia - Czech Republic, in order
to infer on the oven-dry wood variability. Sample logs were obtained from
breast height 1.3 m of the ground (log length 1 m) from 10 tree stems, i.e. 5
from each site. The oven-dry density was calculated along the radius of the
stem cross section per tree and was compared between sites. The average oven-
dry wood density of European ash was found significantly different for
Lednice and Tvrdonice (689.8 kgm-3 and 665.1 kgm-3 respectively).

Keywords: floodplain forests; Fraxinus excelsior L.; oven-dry density;
variability.

1 Introduction

European ash (Fraxinus excelsior L.) usually grows in mixed broadleaved forests as
well as a groupwise admixture into oak, beech and alder stands (Dobrowolska et al.
2008). It also appears as a dominant species in floodplain forests and in moist clay-
loam lowlands or even in relatively dry calcareous sites. This wide range of site types
where European ash thrives, is attributed to a generally high tolerance in relation to
water and nutrients (Střeštík and Šamonil 2006; Dobrowolska et al. 2011).
Furthermore, it tolerates short-term flooding, although stagnant water is unfavorable
for the species due to the limited oxygen supply. Vreugdenhil et al. (2006) reported
intense negative effects of flooding on European ash growth.
European ash trees cover approximately 1.4 % of forest land areas in the Czech
Republic (Ministry report 2014). The species commonly grows within the lowland
belt which includes areas adjacent to large lowland rivers (below 210 m a.s.l.)
covered mostly by floodplain forests, wetlands, inundated meadows, but also by
sandy grasslands and saline habitats (Chytrý 2012).
European ash belongs to ring-porous hardwoods with a whitish to light brown
sapwood and a dark brown heartwood, which is formed in older trees (Zeidler 2012).
Aesthetically superior with outstanding wood properties (Dobrowolska et al. 2008), it

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produces a valuable raw material for wagons, boats and ships, furniture, parquet
flooring, ladders, beams etc. (Tsoumis 1991).
Density is considered to be one of the most determinant wood characteristics,
directly related with physical and mechanical properties (Tsoumis 1991). Wood
density (or specific gravity) depends on the size of the cells, the cell-wall thickness,
and moreover on the interrelationship between the number and the different types of
cells (Panshin and de Zeeuw 1980). Wood density depends on the tree-ring structure
i.e. earlywood and latewood. Considering that latewood consists of cells with thicker
walls and smaller lumina in comparison to earlywood, the larger the latewood is, the
higher the density becomes (Panshin and de Zeeuw 1980; Tsoumis 1991). According
to the reported negative relation between the tree-ring width and the age, it is obvious
that higher density is expected to appear in the central part of a tree stem of ring-
porous species (Kollman 1951; Tsoumis 1991).
The average oven-dry wood density ranges from 650 to 687 kgm-3 for European
ash (Kollman 1951; Matovič 1984). Kollman (1951) presented that European ash
tree-ring width was narrow (less than 5 mm) by the first 10–15 years, becoming
proportionally wider up to 40 years of age, whereupon it decreased continuously.
Physical and mechanical properties of European ash also vary with the age, reaching
the highest values by 30–40 years old. The difference between the wood density
values measured in the center and the outer part of European ash stem was 22 %
(Matovič 1984).
Variations in wood density are very important for wood industry (Taylor and
Wooten 1973). These inferences can become a useful tool for estimating intra-
species and inter-species wood variability in order to indicate representative density
values for future tree selection projects. Finally, delineating the wood density profile
is likely to improve the accuracy of stem biomass estimation.
The current study aimed to infer oven-dry wood variability in European ash
(Fraxinus excelsior L.) growing in floodplain forest sites with different water regime
treatments.

2 Materials and Methods

Two sites along the middle and lower course of the Morava river and lower
courses of other rivers (Dyje) in southern Moravia in the Czech Republic were
chosen for obtaining the sampling material. The first site (A) was a floodplain forest
mixed stand of English oak and European ash (60 % of oak and 40 % of ash) in
Lednice (161 m a. s. l.) and the second (B) was another floodplain forest mixed stand
of similar mixture (70 % of oak and 30 % of ash) in Tvrdonice (154 m a.s.l.) (Fig. 1).
Floodplains of these rivers have been strongly modified by floods and associated
accumulation of loamy sediments. The emergence of floods increased after the
deforestation of sub-montane and montane areas occurred in the medieval period
(Ložek 2011). Typically the rivers flood after snowmelt in March–April and
occasionally after heavy rainfall, mostly during summer but also randomly during the
year. The incidence of floods has declined during the last decades as a result of
regulating the course of the rivers by diverting and deepening the riverbed, as well as

388
by constructing protective dikes (Prax et al. 2005). The site A was successfully
regulated during ‘70s in order to lower the level of the water during floods. On the
contrary, in the site B the water regime treatments were not successful enough to
decrease the level. The mean annual temperature in the research area is 9.0–9.5°C
and the annual precipitation amount is 500 mm (Chytrý 2012).
Five 110-year-old healthy European ash trees were selected randomly per site
i.e. 10 trunks. Sample logs were obtained from breast height 1.3 m of the ground (log
length 1 m). The mean diameter of the trunks ranged from 39.5 to 53.5 cm (site A)
and from 44.0 to 56.5 cm (site B). Specimens 20 × 20 × 30 mm for oven-dry density
testing were obtained radially from bark to pith (A – J) and prepared as shown on
Fig. 1. The specimens were dried up to 0 % of moisture content in a program oven (at
103 ± 2˚C). Each oven-dried specimen was measured in three anatomical directions
and specimens were weighed. Oven-dry wood density of specimens was calculated
as:
!!
𝜌𝜊 = , (1)
!!

where: m0 – the oven-dry weight (kg)
V0 – oven-dry volume (m3)

R-program was used for statistical analysis (Students t-test, Tuckey’s range test).

a b
Fig. 1a. Sampling sites (Lednice-black arrow and Tvrdonice-grey arrow) in the Czech
Republic, b. Sampling method.

3 Results and Discussion

The average oven-dry density of the specimens obtained from both sites (A and B)
was found to be 677.3 kgm-3 (CV = 8.7 %), which is in line with the literature for
European ash oven-dry density (Kollman 1951; Matovič 1984). Lexa et al. (1952)
resulted to 680 kgm-3, which was the closest to our finding.
The successful water regime treatment regulations in the site A resulted to a
higher average oven-dry density in European ash, which was found to be in average
689.8 kgm-3 (CV = 8.9 %) and ranged from 495.4 to 814.2 kgm-3. The average oven-

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dry density of the specimens obtained from the site B was found lower (665.1 kgm-3,
CV = 8.2 %) ranging from 508.8 to 773.3 kgm-3 (Fig. 2a,c).

Lednice Tvrdonice
Oven-dry density (kg.m )
900
-3

800
700
600
500
400

1 2 3 4 5 1 2 3 4 5
Tree no. a
900
Oven-dry density (kg.m )
-3

800
700
600
500
400

A B C D E F G H I A B C D E F G H I J
Lednice Tvrdonice b
Position along radius
800
Oven-dry density (kg.m )

Oven-dry density (kg.m )
-3

-3

800
750

750
700

650 700
650
600

600
550

550
500

500

A B C D E F G H
Lednice
Position along radius d
Tvrdonice c
Fig. 2. a. Average oven-dry density per tree, b. Horizontal oven-dry wood density distribution,
along radius from bark to pith (Lednice: A–I, Tvrdonice: A–J) per tree, c. Average oven-dry
density per site, d. Horizontal oven-dry wood density distribution (both sites together).

390
The difference between the two sites was significant (F = 1.3, p < 0.001). The
result of this study is in line with Matovič (1984) describing the negative relation
between the oven-dry density of European ash wood and the level of the water during
flooding.
The horizontal wood density variation analysis along radius (from bark to pith)
differed significantly among the trees within the same or between two sites (Fig. 2b,
d). In the site A, the highest average oven-dry density was found 732.6 kgm-3 (CV =
5 %) approximately 80 mm away from the pith (A–I), while in the site B, the highest
average oven-dry density (739.3 kgm-3, CV = 1.7 %) was located approximately 20
mm closer to the pith (A–I). Finally, in both sites (A + B) together, the highest
average oven-dry density reached 718.0 kgm-3 (CV = 5 %), measured approximately
80 mm away from the pith. In all cases (A, B, A + B sites), the outer margins of the
radial sections (close to bark and pith) presented significantly lower average oven-
dry density than the central parts, which is in accordance with Matovič (1984).
Furthermore, lower oven-dry density was observed to the specimens obtained closer
to the bark in comparison with the samples that came from the parts closer to the
pith, probably due to the sapwood area.

4 Conclusions

In this study, the highest average oven-dry density was found approximately 80
mm away from the pith. The margins of the radial sections (bark and pith) presented
significantly lower average oven-dry density than the central parts in accordance also
with Kollman 1951. Furthermore, in line with Matovič (1984), it was concluded
during this research that the successful water regime treatment regulations in the site
A resulted to a higher average oven-dry density in European ash.

Acknowledgments. This article was supported by the European Social Fund and the
state budget of the Czech Republic, project "The Establishment of an International
Research Team for the Development of New Wood-based Materials" reg. no.
CZ.1.07/2.3.00/20.0269 and the CZ.1.07/2.3.00/30.0031 project, Postdoc contracts at
MENDELU technical and economic research, with the financial contribution of
EC and the state budget of the Czech Republic.

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