yvan capowiez (inra avignon) and colleaguesbrandenburg.geoecology.uni-potsdam.de/users/... · (inra...
TRANSCRIPT
![Page 1: Yvan CAPOWIEZ (INRA Avignon) and colleaguesbrandenburg.geoecology.uni-potsdam.de/users/... · (INRA Avignon) and colleagues: - Chris Moran (univ. Canberra) Alain Pierret (IRD, Laos)](https://reader034.vdocuments.site/reader034/viewer/2022042802/5f3f1f47a367bb1c93409e9a/html5/thumbnails/1.jpg)
Yvan CAPOWIEZ
(INRA Avignon)
and colleagues:
- Chris Moran (univ. Canberra)
Alain Pierret (IRD, Laos)
- S. Sammartino and E. Michel
(INRA Soil Science Avignon)
- H. Boizard (INRA Agronomy Mons)
radiotracking
3D reconstructions
![Page 2: Yvan CAPOWIEZ (INRA Avignon) and colleaguesbrandenburg.geoecology.uni-potsdam.de/users/... · (INRA Avignon) and colleagues: - Chris Moran (univ. Canberra) Alain Pierret (IRD, Laos)](https://reader034.vdocuments.site/reader034/viewer/2022042802/5f3f1f47a367bb1c93409e9a/html5/thumbnails/2.jpg)
Main topic :
Physical effects of earthworms behaviour (burrowing and
casting) on the soil functionning
… the most accepted and known effects but rarely
quantified due to the lack of adapted tools.
Scientific areas :
- soil ecology (interactions between earthworms)
- agronomy (soil regeneration, water infiltration)
- ecotoxicology (a link between effects at the individual
level and soil functions)
![Page 3: Yvan CAPOWIEZ (INRA Avignon) and colleaguesbrandenburg.geoecology.uni-potsdam.de/users/... · (INRA Avignon) and colleagues: - Chris Moran (univ. Canberra) Alain Pierret (IRD, Laos)](https://reader034.vdocuments.site/reader034/viewer/2022042802/5f3f1f47a367bb1c93409e9a/html5/thumbnails/3.jpg)
METHODS
* Burrowing
- X-ray tomography (snapshots)
- radiotracking (dynamical)
- 2D terraria (easy and cheap)
} Simulation
model
* Cast
Production
- X-ray tomography (underground casts)
- sieving -> a new
biomarker (ecotox.)
Not all these tools are relevant at the field scale…
![Page 4: Yvan CAPOWIEZ (INRA Avignon) and colleaguesbrandenburg.geoecology.uni-potsdam.de/users/... · (INRA Avignon) and colleagues: - Chris Moran (univ. Canberra) Alain Pierret (IRD, Laos)](https://reader034.vdocuments.site/reader034/viewer/2022042802/5f3f1f47a367bb1c93409e9a/html5/thumbnails/4.jpg)
SCALE : Example 1 (field study)
Can earthworm regenerate compacted soil under natural
(crop) conditions (if yes, at which rate ?)
![Page 5: Yvan CAPOWIEZ (INRA Avignon) and colleaguesbrandenburg.geoecology.uni-potsdam.de/users/... · (INRA Avignon) and colleagues: - Chris Moran (univ. Canberra) Alain Pierret (IRD, Laos)](https://reader034.vdocuments.site/reader034/viewer/2022042802/5f3f1f47a367bb1c93409e9a/html5/thumbnails/5.jpg)
CONTROL COMPACTED
M+
1 (
03
/20
05
) M
+8
(11
/20
05
)
Soil core
(Diameter
= 16 cm
Height
= 35 cm)
![Page 6: Yvan CAPOWIEZ (INRA Avignon) and colleaguesbrandenburg.geoecology.uni-potsdam.de/users/... · (INRA Avignon) and colleagues: - Chris Moran (univ. Canberra) Alain Pierret (IRD, Laos)](https://reader034.vdocuments.site/reader034/viewer/2022042802/5f3f1f47a367bb1c93409e9a/html5/thumbnails/6.jpg)
M+
24
(0
3/2
00
7)
Functional consequences (water infiltration - Beer Kan method)
0
100
200
300
400
500
1 8 24
Months after compaction
Infi
ltrati
on
rate
(m
m h
-1)
Control
Compacted
*
*
![Page 7: Yvan CAPOWIEZ (INRA Avignon) and colleaguesbrandenburg.geoecology.uni-potsdam.de/users/... · (INRA Avignon) and colleagues: - Chris Moran (univ. Canberra) Alain Pierret (IRD, Laos)](https://reader034.vdocuments.site/reader034/viewer/2022042802/5f3f1f47a367bb1c93409e9a/html5/thumbnails/7.jpg)
SCALE : Example 2 (laboratory conditions)
Do burrows of endogeic species influence water
infiltration ? (if yes, what are the most effective burrows?)
![Page 8: Yvan CAPOWIEZ (INRA Avignon) and colleaguesbrandenburg.geoecology.uni-potsdam.de/users/... · (INRA Avignon) and colleagues: - Chris Moran (univ. Canberra) Alain Pierret (IRD, Laos)](https://reader034.vdocuments.site/reader034/viewer/2022042802/5f3f1f47a367bb1c93409e9a/html5/thumbnails/8.jpg)
1ew
(3ew)
7ew
1 week 3 weeks 4 weeks
NB : 2 replicates => 32 soil cores
5ew
(2 weeks)
![Page 9: Yvan CAPOWIEZ (INRA Avignon) and colleaguesbrandenburg.geoecology.uni-potsdam.de/users/... · (INRA Avignon) and colleagues: - Chris Moran (univ. Canberra) Alain Pierret (IRD, Laos)](https://reader034.vdocuments.site/reader034/viewer/2022042802/5f3f1f47a367bb1c93409e9a/html5/thumbnails/9.jpg)
Step1 :Burrow volume in function of time and ew number
Step 2: Burrow system characterisation and rain simulation
-> time for breakthrough of water
0
10
20
30
40
50
60
70
80
90
0 1 2 3 4 5
Time (weeks)
Vo
lum
e (
cm
3)
1 ew
3 ew
5 ew
7 ew
Scale1
Effluent
Rainfall simulator
Scale2 0
50
100
150
200
0 0.5 1 1.5 2
Core
wei
ght
vari
ati
ons
(g)
time (hour)
![Page 10: Yvan CAPOWIEZ (INRA Avignon) and colleaguesbrandenburg.geoecology.uni-potsdam.de/users/... · (INRA Avignon) and colleagues: - Chris Moran (univ. Canberra) Alain Pierret (IRD, Laos)](https://reader034.vdocuments.site/reader034/viewer/2022042802/5f3f1f47a367bb1c93409e9a/html5/thumbnails/10.jpg)
Step 3: regression between breakthrough time and the
characteristics of the burrow systems in each core
Continuity of the
burrow system
But this is only a correlative approach ….
![Page 11: Yvan CAPOWIEZ (INRA Avignon) and colleaguesbrandenburg.geoecology.uni-potsdam.de/users/... · (INRA Avignon) and colleagues: - Chris Moran (univ. Canberra) Alain Pierret (IRD, Laos)](https://reader034.vdocuments.site/reader034/viewer/2022042802/5f3f1f47a367bb1c93409e9a/html5/thumbnails/11.jpg)
To go deeper into processes …
Water (50-70%) in
macropores
Scale1
Effluent
Rain simulator
Flux
Scale 2
Core weight dynamics Breakthrough time
Q1: which macropore are active ?
Q2: what kind of flux (laminar, droplets, …) ?
The core is scanned 20 times during a one-hour rain simulation