Original article
The study of tree fine root distribution and dynamics using a combined trench and observation window method
M. Bédéneau D. Auclair
INRA, Station de
Sylviculture,
Centre de Recherches d’Orl6ans, Ardon, F 45160 Olivet, France (received 5 février 1988,accepted
6 d6cembre 1988)Summary —
Root distribution andgrowth
were studied in a natural oak-birchcoppice, by combining
the trench and observation window methods. Root
weight
was estimated whiledigging
the trench,showing
that 90 percent ofdry weight
is situated in the upper 50 centimetres of soil. Rootposition
was
analyzed, using variograms :
a cluster effect was observed, around 50 cm for old roots and 20 cm for new roots. Oak and birch appeared to have different seasonal rootelongation
patterns.The results are discussed in relation to the methods
employed.
Tree - root - distribution -
profile - spatial
distribution -coppice -
birch - oakRésumé — Etude de la distribution et de la
dynamique
des fines racines combinant les tech-niques
de tranchée et de fenêtre d’observation en forêt. Différentes méthodes ont été utilisées pour observer in situ et caractériser le système racinaire d’arbres forestiers dans un taillismélangé
de chênes et de bouleaux. La biomasse racinaire, estimée au moment du creusement de la tran-
chée, se trouve localisée en
grande partie (90%)
dans /es 50 centimètressupérieurs.
Laposition
des
racines,
étudiée à l’aide devariogrammes,
montre des phénomènesd’agrégation
de l’ordre de50 cm pour les vieilles racines et de 20 cm pour les racines
jeunes.
Chêne et bouleauprésentent
des vagues de croissance racinaire différentes. Ces résultats sont discutés en fonction des tech-
niques utilisées.
Arbre - racine - distribution -
profil -
distributionspatiale -
taillis - Betula - QuercusIntroduction
The
great majority
of studiesconcerning
forest tree root
systems
has been carried out onartificially
cultivated youngplants.
Only
a few studies have dealt with adult forest trees,mainly
due to the conside- rable technicalproblems
involved(B6hm, 1979).
However,
youngseedlings
andplantlets
have different
growth patterns
from adulttrees. Isolated
plants
inpots,
or in artificial observationchambers,
also differ from thosegrowing
in naturalconditions,
due to differences inbiological (competition)
andphysical (light,
water,soil)
environment. It is therefore hazardous to make any gene- ral conclusion from results obtained in eachlaboratory experiment.
This may also
explain why
the amountof
experimental
dataconcerning
rootdevelopment
oflarger
trees is rather scar-ce
(Persson, 1983;
Santantonio and Her- mann,1985; Ries, 1988).
In thepresent study,
various observation methods andtechniques
are discussed.A trench and an observation window
were tested in order to estimate root distri- bution and
growth
in a natural oak-birchstand in central
France,
with a view toapplying
this method to acoppicing
expe- riment(Bedeneau
andAuclair,
in prepara-tion).
Materials and Methods
Site
The
experimental
site was located at the INRAexperimental
station 20 km south of Orléans,France
(1.54°
E, 47.52°N).
The natural forest is an ancientcoppice containing mostly
Betula pendula Roth., Quercus robur L. with a few scattered Castanea sativa Mill. and Robiniapseudoacacia L. The root systems are of un- known age; the stems are 25 yrs old.
The soil is acid, of the brown crytopodzolic type with a moderate humus. It has
developed
in a terrace material
consisting
of homometric sand, essentiallyquartzic,
unstructured in the upper 40 cm andrapidly
becoming gravelly andheterometric. It can be characterized as filtering well, with a very low mineral reserve.
The study plot was situated between Quer-
cus and Betula stools, at least 1 m away from each stump in order to minimize disturbance of the
underground
system. A trench 4 mlong,
1m wide and 1 m
deep
wasdug by
hand(Fig. 1 ).
Installation
On each side of the trench 4
(1
x 1 ) m squareswere bordered with a wooden frame. Each of these
large
squares contained 400 (5 x 5) cmelementary
squares which were numberedaccording
to their horizontal and verticalposi-
tion. Coordinates were marked on the separa- tion boards.
Transparent plastic plates
werethen fixed on the boards, to observe root elon-
gation.
Each(1
x 1 ) m square was covered withan 8-cm thick
polystyrene
sheet and a blackplastic foil. The entire trench was then covered with
polystyrene.
Thisassembly
maintained anadequate
temperatureregulation.
Measurements
Several types of data were collected :
1. Root
weight
was measured whiledigging
the trench. Dead and live roots were
carefully
and
separately sampled
in each 25 cm soil hori- zon.They
were then sorted into diameter classes(<
1 mm. 1 -2 mm, > 2mm),
and oven-dried at 105°C.
2. Root
position
on each side of the trench : in eachelementary
(5 x 5) cm square, the roots cutduring
the excavation were counted and sortedaccording
to :- age : new/old (difference
appreciated
by the colour);-
species :
oak/birch (difference assessed onthe basis of
general
appearance, form, colour).For each
(x,y)
coordinate the number andquality
of roots was thus obtained. This presen- tation allowed mathematical calculations to be1 11 1
made on the variable &dquo;root density per square centimetre&dquo;.
3.
Elongation :
thepath
followedby
the rootsduring
growth was drawn on the transparentplastic plates, using
a different colour for each observation date. Totalelongation
between 2observations was obtained by
following
eachcoloured line with an
opisometer.
This type of data was recorded atirregular
intervals,depen- ding
on growth, between March and December on each (1 x 1 ) m square(4
on the&dquo;right&dquo;
side,numbered 1 - 4, and 4 on &dquo;left&dquo; side, numbered 5-8).
4. Additional data : to
simplify
tediouselonga-
tion measurements, an attempt was made to
use infrared
photography
and videorecording.
These
techniques
did not provesatisfactory, mostly
due to the outdoor environmental condi- tions.Results
Root
dry weight
tThe mean root
dry weight
excavated per cubic metre was distributedby
diameterclasses as follows :
- diameter <- 1 mm : 41
g.m-3
- diameter from 1 to 2 mm : 67
g.m-3
- diameter ! 2 mm : 395
g.m-3
- total root
weight
: 503g.m-3
Table I shows the distributionby
soilhorizon. It was observed that the
deeper
horizons were not
explored by
the roots,as > 90
percent
of thedry weight
wasfound in the upper 50 cm. This result agrees with the soil
description :
fine rootsdid not
develop
below 50 cm, whereas afew coarse roots were observed at a
depth
of 75 cm.Root distribution
The root
position
data collected on each side of the trench wasgrouped
to formtwo
(4
x1 )
mgrids. Variograms
were thencomputed
for eachgrid
in order toanalyze
the
spatial
distribution of the roots.The method used here is that of
regio-
nalized variables
developed by
Matheron(1965)
forprospecting
andevaluating
geo-logical deposits.
It consists of thestudy
ofvariables
F(X)
whose valuesdepend only
on the
supporting
coordinates X : it has been used forstudying competition
inforest
plantations (Bachacou
andDecourt, 1976),
animalpopulation
distribution(Pont, 1987)
or soilphysical
variables(Goulard et al., 1987).
F(X)
is considered as a random intrinsicfunction, thus,
for any vectorh,
the mathe- maticalexpectancy
and variance of the incrementF(X
+h) - F(X)
areindependant
of X and
depend only
on h.The
variogram g(h)
is half the second- order moment of the random functionF(X) :
g(h)
= 1 /2 E[F(X
+h) - F(X)] 2
The
shape
of the curveshowing
g as a function ofh,
inparticular
at itsorigin,
pro- vides a basis fordescribing
the randomstructure of the variable F :
- if
g(h)
isparabolic,
it shows agreat spatial regularity;
- if
g(h)
is linear theregularity
is poorer;- if
g(h)
shows adiscontinuity
at the ori-gin
there is agreat irregularity.
In the
present study
the variable is the number of rootsoccurring
at coordinates(x,y).
Avariogram
can be obtained for each rootparameter : old,
new,birch, oak,
on each side of the trench
(left, right).
Thestep
of thevariogram (h)
is 5 cm.All
variograms (Fig. 2)
show that thecurve starts at
approximately
half the linedetermined
by
the &dquo;apriori
variance&dquo;. This indicates a clustereffect, varying
with roottype
and side of the trench = 50 cm for old roots and 20 cm for new roots(value
readat the
starting point
of thevariogram).
To have a clearer view of this
phenome-
non, we
computed
amoving
average of each square with the 8surrounding
squares. The smoothed curves obtained
(Fig. 3)
outline the clusterpoints.
This canbe
clearly
observed atapproximately
50-cm
intervals,
inparticular
for old oak roots on the left side and at a lesserdegree
for new roots.Elongation
Returning
to each(1
x1 )
m square, we measured thelength
of all new rootsappearing
at each observation.During
one
growing
season we thus obtainedtotal root
elongation
per square, on each side of the trench(Fig. 4).
On the
right side,
rootgrowth began
inMarch and reached a
peak
inearly July.
Growth ceased in
August
and a secondgrowth
flushappeared
fromSeptember
toDecember.
On the left
side,
severalelongation
flushes were observed :
- square 7 showed intensive
growth
until
June,
followedby
agradual growth
inhibition until
November;
- squares 5 and 6 showed a
pattern
similar to that observed on theright side;
- square 8 was intermediate.
Square
7 wasmostly occupied by
birchroots and square 8
by
a mixture of birch andoak,
whereas the other squares containedonly
oak roots : thissuggests
that birch has a differentgrowth pattern
from that of oak.
Discussion
Root
systems
of mature trees can be stu- died in different ways, but all methods arecomplex
andtime-consuming.
Thestudy
of
underground system architecture, by excavation,
which has some disadvan-tages (necessarily destructive,
time- andpower-consuming; Pages, 1982)
can. pro- vide someinteresting
information on grow- th in different situations(Bedeneau
andPages, 1984). However,
thestudy
of coar-se roots
gives
insufficient information aboutdynamics.
Fine root
dynamics
may be studied with varioustechniques, involving
core sam-pling
or morecostly methods,
such asendoscopy (Maertens
andClauzel, 1982)
or video
recording (Upchurch
andRitchie, 1984).
The environmental conditions in the forestwould, however,
entail additionalequipment
at an excessive cost.The trench method used here has its drawbacks
(B6hm, 1979) :
it causes dis-turbances in both the soil
dynamics (late-
ral water
movements)
and the rootdyna-
mics(cutting
of rootsduring
thedigging
ofthe
trench).
In thisstudy
we thereforecombined the static
description
of root dis-tribution with a root observation window
technique
in order to follow thegrowth
offine roots in situ.
In the
dynamic experiment
with observa- tionwindows,
we assumed that:-
damage
to soil remainsslight
becauseof the careful
digging by hand;
- root
growth capacity,
as describedby
Sutton(1980)
remainsunchanged;
- the
edaphic
factorssubject
tochange
are the
following :
lateral waterrunoff,
andhence mineral runoff
(Callot et al., 1982),
as well as gas
exchange (0 2 )-
Our
assumption
that we observed nor-mal
growth
rather than tree or rootsystem
response to the trench issupported by
thefact that we observed no
major change
inabove-ground parts
of the trees.Results relative to root
weight
are simi-lar to those
reported by
others(Duvi- gneaud
et al.,1977;
Gholz etaL, 1986).
However,
our results are somewhat bia-sed,
for we collected the roots more than 1 metre away from any stem. Thus weexcluded from our estimations the main structural roots
accounting
for themajor part
of theunderground
biomass.Above-ground
biomass amounts here to= 80-100 t.ha-!
(Auclair
andMetayer, 1980).
Theunderground parts
we have measuredrepresent
6percent
of this bio-mass. This
figure is, however,
an underes- timation of totalunderground
biomass as itdoes not account for the coarse roots close to the stems and the
stumps.
Wemust also be cautious in
generalizing
onan area
basis,
as oursampling technique
was not intended for that
(small sampling
area, not
random,
noreplicates, etc.).
The statistical data showed that the roots were not
randomly
distributed in the soil : inparticular,
birch roots were inter-mingled
with oak roots. Thismight
be dueto different
growth
behaviour andphenolo-
gy of the 2
species :
- root
elongation
in birchbegan
earlierand decreased when oak root
elongation
was
initiated;
- the horizons
occupied
were different : near the soil surface forbirch, deeper
inthe soil for oak..
The
position
of the new rootssuggested
that root
growth
was derived from older ramifications. The distance between new roots and old rootsalways
remained short.The section of each side of the trench dis-
played
&dquo;channels&dquo; leftby
dead roots, andoccupied by growing
roots, aphenomenon previously
describedby
others(B6hm, 1979).
New roots were also found to deve-lop
from the sectioned area of cut roots : thisability
to form ramifications has beenreferred to as &dquo;root
growth capacity&dquo; by Sutton (1980).
This
suggests
thatelongation
of thepri-
mary axes was followed
by
ramification andelongation
of severalsecondary
axes,and that the disturbance induced
by
thetrench did not inhibit root
growth.
A
strong
rootgrowth activity during Spring
and Summer was demonstrated(Fig. 4).
This agrees with otherinvestiga-
tions
suggesting
arelationship
betweenroot
growth
and accumulation of the pre- viousyear’s photosynthates (Bonicel
andGagnaire-Michard, 1983).
Thissuggests
thatcutting during
thevegetation period prevents
the rootsystem
fromexpanding
and new roots from
growing,
thus hinde-ring
thegrowth
of thefollowing coppice cycle.
Conclusions
The
present study
was aimed atperfecting
methods for root observation in natural forest
stands,
andinterpretation
tech-niques.
The excavation method
gives
staticresults on root
biomass,
and its distribu- tion in different diameter classes. Itis, however,
insufficient for totalunderground production
studies which entail agreater
number of observations.The root observation window
gives
adynamic
view of rootdistribution,
but itsinterpretation
is most delicate. Root grow- th has been describedby
mathematical models(Rose, 1983; Belgrand
etal., 1987).
Thegeostatistical approach
usedhere should be considered as an
attempt
to describe the
spatial
distribution of rootsystems.
A cluster effect has beenshown,
but itsinterpretation
in relation to the structure andgrowth
of roots, and to soilheterogeneities
wouldagain require
agreat
number ofreplications.
The limitations underlined here
join
thegeneral
views(B6hm,
1979; Santantonio andHermann, 1985), stating
how time-consuming precise
root studies can be. Animprovement
of the methods described heremight
be toprovide
for thepossibility
of
taking samples
at variousprecise
deve-lopmental stages, giving
access to studieson root turnover and
productivity,
and tothe
study
of nutrientcycles.
The
present
dataonly
concerns onegrowing
season, and to have a reliableinterpretation
of the difference between oak and birchgrowth behaviour,
morefrequent
observations should be underta- ken at severalimportant
dates in relation tophenology (budbreak, budset, fall).
Acknowledgments
We wish to thank A. Riedacker, J.
Gagnaire-
Michard and L.
Pages
for their advice concer-ning
root observation and biometrics, J.Roque
(INRA - SESCPF) for the soildescription,
M. Bariteau, L. Bouvarel and the technical staff of the Orl!ans INRA
Sylviculture
and Biomass laboratories for their hard work. Thisstudy
waspartly
supported by the French Energy Manage-ment
Agency (AFME).
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