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(1)

CHOPART J.-L.

1

& LE MEZO L.

2

[email protected]

Agroocotogy ln tropks Ground C watw ,,.,.na�nMnt

Energy from biomus Renew•bl• Enl1rge the fitld of posslbilit,es

1AGERconsult F-34090, Montpellier, France

cirad

2CIRAD, UPR 115, F-97410, Saint-Pierre, La Réunion, France

We present the findings of

a

study testing the PRER (Potential Root Extraction Ratio) mode/ (Chopart 1999,

Leifi et al., 2011) to estimate the maximum avai/able soi/ water (MASW) depending on the sugarcane root

system in a deep soi/ of La Réunion. The aim is to optimize sugarcane irrigation, especially deficit

irrigation, by adjusting irrigation rates and intervals according to root distribution in the soi/.

Methods

Measurements where done on a deep soil in La Réunion, in a R570

nine months after harvest of the previous crop.

Root distribution was studied using the trench-profile method by

mapping root intersections (RI) in four soil profiles to a depth of

four meters using a grid (5 x 5 cm mesh). From RI, we inferred

root length densities (RLD) (Chopart et al., 2008) and root distances

(RD), (Newman, 1969).

The PRER is the ratio of volume of soil potentially accessible to a root for water

uptake (Vu) and the whole volume of soil assigned to that root. Modelling Vu took

RD into account & a max distance of water movement from soil to roots (5 cm).

The conventional max. available soil water (MASWlab, cm of water in cm of soil)

had a value of 0.1cm/cm from the soil surface to the four meter depth.

Results & Discussion

../ There was a wide variability in RLD distribution between the surface and the

rooting front (4 m), with many competing roots and rootless zones (Fig.1 ).

../ PRER values ranged from 80% near the surface to values ranging from 30%

to 1% between the 1 - 3 m depth (Fig.2& 3).

../ The biological MASW (MASWbiol) depending on PRER( Fig.3) and MASWlab

ranged from 0.8 mm/cm near the surface to 0.01 mm/cm at 3 m. The total

MASWbiol was 86 mm (SD.: 14).

0.5

I 1 {; � 1.5 • u -·2S - O:ZS-04 - .... .tCM

Fig.1: RLD (cm/cm

l

)

0 0.2 0.4 0.6 1 2 ' 2.5 -PRER/5 cm muh

../ When only rooting depth and conventional MASWlab (cm/cm) were used,

value of total MASWlab was 300 mm for a 3 m rooting depth (Fig.4) .

../ MASWbiol appeared to provide a better estimate than conven_ti��al.

MASWlab for crop modelling and irrigation, especially for def1c1t 1mgat1on .

../ Deficit Irrigation requires a good estimate the soil water storage.

1

-o-

RLD

F;g.Jc 'Pmfiles of RLD (omkm') &

P

RER(O

Max Avallable Soli Water (mm/cm of soil depth)

••

I,

� 15

"

0..2 0 4

..•

-

MASWb1ol

-MASW!ab

01 10 1 2

Fig.4: Profiles of biological and conventional

MASW

(mm/cm soil depth)

References

tween SOii phys,cs root system and crops water uptake in situ methods and examples ,n trop,cs PhD Thes,s. Unrv. Grenoble France. 115 p

Chopart JL.. 1999 Relabonshrps beM Medina

c

2008 Est,mat,ng sugarcane root length dens,ty through root mapprng and onentatron modethng Plant Sort. 313 101-112

Chopart JL. Rodngues S. Azev��oMé�o L Manon o. 2010 Sugarcane Root System oepth •n Three Different Countnes Proc lnt Soc Sugar Cane Tech . Vol 27. 2010. Bp

Chopart J L , Azevedo Lérfr N. Chopart JL. Roupsard . auclrn M C.B .•

0

V

M

Aké

S

Jourdan

c

2011 Genotyp,c var of

011 P

81

1ll

root syst drstnbutron

rn

the field Consequences for water uptake PtantSorl 341 505-520

whole r�t system for a pl�nt crop of sugarcane under rarnfed and irngated envrronments

rn

Brazrl Field Crops Research 114, 351-360

Laclau P. Laclau JP. 2009 Growth of the I d plant 1 -Sor! resrstance

rn

relation to amounts of root theoret,cal est,mates

J

Appt Ecol 6 1-12

Newman El 1969 Resrstance to water flow 1n sor an

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