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Agroforestry: Can trees change aggregate stability ?

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HAL Id: hal-02793200

https://hal.inrae.fr/hal-02793200

Submitted on 5 Jun 2020

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Agroforestry: Can trees change aggregate stability ?

Yogan Monnier, Jean-Luc Maeght, Yves Le Bissonnais, Catherine Roumet, Alexia Stokes

To cite this version:

Yogan Monnier, Jean-Luc Maeght, Yves Le Bissonnais, Catherine Roumet, Alexia Stokes. Agro-forestry: Can trees change aggregate stability ?. Climate Smart Agriculture 2015, Mar 2015, Mont-pellier, France. 2015. �hal-02793200�

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Agroforestry: Can trees change

aggregate stability ?

Why ?

Then… what next ?

How ?

Soil erosion in farmlands is a major cause of water quality degradation and

reduced crops production potential throughout the European countries.

In agroforests, if the role of tree lines as physical barriers to runoffs is easily

understanding, processes involving rooting systems and soil erodilbility are still unknown.

Objectives

- 

Do the presence of a tree line improve soil aggregate stability

?

- 

What are the mecanisms underlying ?

Y. Monnier

1

, J.L. Maeght

2 1

, Y. Lebissonais

3

, C. Roumet

4

, A. Stokes

1

10 m. 7m. Tree 1 Tree 2 7m. Zone sampling (x4) Tree line Crops

A

re there effects of the tree line on soil aggregate stability ?

W

hat factors drive the soil aggregate stability ?

OUT

(in tree line) IN

***   *  

Crown presence (MB)

(c) (t) Out (in tree line)

. Most of sites are too young to reveal a distance effect to the line => new sampling design with hedges

-  From mature hedges

-  Progressive sampling from 0 to 9 m. - Several depths: from 0 to 2.10 m.

. Next analysis to better explain our results : Soil organic matter content /Root morphological traits / Microbial activity &

metabolic diversity Soil erodibility = the ability of soils to resist erosion, assessed

by measuring soil aggregate stability (Le Bissonnais 1996).

1, INRA, UMR AMAP, Bld de la Lironde, 34298, Montpellier cedex 5, France / 2. IRD, UMR  IEES-Paris, Paris, France / 3. INRA, UMR LISAH, 2 Place Pierre Viala, F-34060, Montpellier, France / 4. C.N.R.S., UMR CEFE, 1919 route de Mende, 34293, Montpellier Cedex 5, France

No difference between soil aggregate stability in

tree-line and crops field in 3 sites (ED, LB & PS)

Higher soil aggregate stability in 5 sites =>

increment from critical to good levels of stability

MWD

1.  Graf F, Frei M, (2013) Soil aggregate stability related to soil density, root length and mycorrhiza using site-specific Alnus incana and Melanogaster variegatus s.l. Ecol. Eng. 57: 314-323. 2.  Le Bissonnais Y, (1996) Aggregate stability and assessment of soil crustability and erodibility: I. Theory and methodology. European Journal of Soil Science, 47: 425–437

3.  Pérès G, Cluzeau D, Menasseri S, Soussana JF, Bessler H, et al. (2013) Mechanisms linking plant community properties to soil aggregate stability in an experimental grassland plant diversity gradient. Plant Soil 373: 285–299.

Soil aggregate stability can be positively correlated to soil organic matter

content, roots presence and soil biota (Graf and Frei 2013, Pérèz et al. 2013).

ED : No effect

Root proportion

MWD

Root proportion (g.g-1)

(root fresh biomass / soil fresh biomass)

Aggregate stability (Mean Weight Diameter, MWD) in different sites and different treatments (crop field (c) & tree line (t))

***  

***  

For each sample we measured : -  soil aggregate stability (Le

Bissonnais, 1996)

-  microbial metabolic activity and diversity (microresp ©)

-  root biomass and root trait diversity

-  characteristics of the vegetation structure and soil properties.

PS

MB

ED

LB

VP

CH

SJ

SM

4 zones were sampled in each 8 sites.

By zone, three samples in the tree line, at

different distances from the tree, and two

composite samples in the crop, at ¼ and ½ of the distance between two tree lines. VP MB PS LB

0

1

2

3

L B

V P

M B

C H

S M

S J

P S

E D

ED CH SM SJ Good Critical Different ranges of stability

Sites

 

MWD

*** *** ** *** *** PC1 : 63 % PC2 : 1 5 % MWD Herbaceous cover Height of vegetation Number of species Litter cover Tree line

PCA

The root proportion in the soil is positively linked with the aggregate stability. The strength of the relationship differ between sites

The aggregate stability is positively corelated with all the indicators

of a perennial vegetation cover Aerial descriptors of vegetation

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