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Vol. 35 – 2009 - Ecologia Mediterranea - Université d'Avignon et des ...

Vol. 35 – 2009 - Ecologia Mediterranea - Université d'Avignon et des ...

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MUSTAPHA DADDI BOUHOUN, LOUHICHI BRINIS, MOHAMED LAKHDAR SAKER, MARC COTE, JACQUES RABIER<br />

42<br />

hydro-édaphique sur l’enracinement du palmier<br />

dattier Dégl<strong>et</strong> Nour dans les périmètres phœnicicoles<br />

de la cuv<strong>et</strong>te d’Ouargla.<br />

Les résultats obtenus montrent que 53,9 % <strong>des</strong><br />

exploitations phoenicicoles présentent une<br />

nappe phréatique ayant une profondeur comprise<br />

entre 29 <strong>et</strong> 119,4 cm. L’étude de l’enracinement<br />

du palmier dattier, à 80 cm du tronc, a<br />

montré que 56,9 % <strong>des</strong> palmeraies présentent<br />

un enracinement compris entre 27 <strong>et</strong> 119 cm de<br />

profondeur, dont 3 % à cause <strong>des</strong> croûtes gypseuses<br />

<strong>et</strong> gypso-calcaires, 10,8 % à cause de la<br />

nappe <strong>et</strong> <strong>des</strong> croûtes gypseuses <strong>et</strong> gypso-calcaires<br />

<strong>et</strong> enfin 43,1 % à cause de la nappe<br />

phréatique. La conductivité électrique <strong>des</strong> eaux<br />

phréatiques varie de 10 à 39,7 dS.m-1 .<br />

L’étude <strong>des</strong> corrélations montre que la faible<br />

profondeur de la nappe phréatique ainsi que<br />

<strong>des</strong> croûtes gypseuses <strong>et</strong> calcaires diminuent la<br />

profondeur d’enracinement. Les racines fuient<br />

la zone de saturation en eau <strong>et</strong> la résistance<br />

mécanique <strong>des</strong> croûtes pour se développer dans<br />

le sens latéral. La salinité <strong>des</strong> eaux phréatiques<br />

présente moins d’eff<strong>et</strong> sur l’enracinement du<br />

palmier dattier comparée au niveau de la nappe<br />

phréatique.<br />

Introduction<br />

Excess water in soils is a global environment<br />

problem and contribute to the degradation of<br />

595 millions km 2 of soil, corresponding to<br />

approximately 5% of non-productive grounds.<br />

Soil clogging is caused by bad water irrigation<br />

management, nature of soil and, water<br />

table rise (Robert & Cheverry 1996).<br />

Rise of subsoil water, produced by bad drainage,<br />

causes edaphic degradation of agricultural<br />

ecosystems and shortening of crop root<br />

depths (Hatton & Nulsen 1999). Lowering<br />

water table depths trigger harmful consequences<br />

in the sub-Saharan (Bertrand <strong>et</strong> al.<br />

1993) and Saharan environment (Durand<br />

1958).<br />

The phreatic groundwater table is close to the<br />

soil surface in some Algerian south-east areas,<br />

like Oued Righ and Ouargla; it varies from 0<br />

to 1.2 m depth (Dubost <strong>et</strong> al. 1983; Dubost<br />

1991; Saker 2000; Hamdi Aïssa 2001).<br />

Problem of groundwater rise in the Ouargla<br />

basin developed over the last few years as a<br />

result of the anarchic multiplication of<br />

drillings, bad drainage of agricultural water<br />

and bad management of worn water. According<br />

to Côte (1998), after the XXth century<br />

drillings made it possible to double the planted<br />

surfaces; but waste waters contributed to<br />

the groundwater rise, in parts of the basin. The<br />

drainage remains partly ineffective caused by<br />

absence of discharge system.<br />

Surface ground water, in hyper-arid climate<br />

supports capillary increase of soluble salts and<br />

accumulation of gypsum in the water table<br />

(Durand 1958; Halitim 1988). This situation<br />

causes harmful root asphyxiation and limits<br />

crop rooting at the Saharan oasis level (Dutil<br />

1971; Bahri 1987). This malfunction of the<br />

date palm crop heritage leads to drop in date<br />

yields quality.<br />

Degl<strong>et</strong> Noor dates, produced on South-East<br />

Algerian palm (Phoenix dactylifera L.) plantations,<br />

are very sensitive to the bayoud<br />

disease but until now, they have been leaved<br />

unscathed. That seems to be related to different<br />

param<strong>et</strong>ers such as salinity (Amir <strong>et</strong> al.<br />

1996). However, particular nature of salted<br />

soils of these palm plantations also seems to<br />

contribute to resistance (Laville & Lossois<br />

1963; Kada <strong>et</strong> al. 1972).<br />

Date palm grows badly in compact soils and<br />

areas of bad drainage (Monciero 1961) which<br />

presents harmful consequences on soil structure,<br />

ventilation, biological activity, assimilation<br />

of some mineral nutrients and consequently<br />

date palm growth (Djerbi 1994).<br />

According to Dutil (1971), rooting of the date<br />

palm in soils of Ouargla is subjected to a<br />

stressful environment caused by soil salinity,<br />

bad groundwater drainage and gypseous or<br />

calcareous encrusting. High root activity of<br />

date palm favours concentration of soil solution<br />

and precipitation of less soluble salts.<br />

In the Maghreb, studies on tree rooting are<br />

rare, especially for the date palm (Phoenix<br />

dactylifera L.). Most of studies are American<br />

and were carried out using pot cultures or on<br />

soil profiles next to date palms; search were<br />

related to root systems and impact of moisture<br />

on rooting (Went and Darley 1953), water<br />

table (Simmons 1926; Weeks 1957; Furr<br />

1975; Dubost 1991) or irrigation and soil<br />

(Armstrong & Furr 1959).<br />

In this context, our study investigated the<br />

impact of hydro-edaphic environment in the<br />

Ouargla basin on root system of the Degl<strong>et</strong><br />

Noor date palm. Degl<strong>et</strong> Noor is a very wi<strong>des</strong>pread<br />

cultivar in this area and it is of important<br />

economic interest for Algeria.<br />

ecologia mediterranea <strong>–</strong> <strong>Vol</strong>. <strong>35</strong> <strong>–</strong> <strong>2009</strong>

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