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

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density which are respectively 0.5 and 0% of<br />

its initial level at the end of the experiment<br />

(Amir <strong>et</strong> al. 1996). Rooting of the date palms<br />

in the Ouargla basin is subjected to a salinity<br />

of phreatic origin, above 1.5 to 6 times the<br />

threshold of disappearance of the pathogen,<br />

which confers to this area a resistance to the<br />

bayoud disease.<br />

The plant root system cannot easily pen<strong>et</strong>rate<br />

the hardened massive calcareous horizon.<br />

Moreover, water is mainly confined in the<br />

zone above the massive horizon, so that the<br />

geom<strong>et</strong>rical model of root growth changes.<br />

Roots, seeking water, tend to grow laterally,<br />

favouring the development of the horizontal<br />

secondary roots (Esteban & Klappa 1983;<br />

Alonso-Zarza <strong>et</strong> al. 1989).<br />

Practically, in oasis, these gypseous formations<br />

of water table constitute a very important<br />

limiting factor, in particular for the<br />

shrubby cultures (date palms and fruit trees).<br />

Som<strong>et</strong>imes, they brutally block root depth<br />

increase which come to be crushed on a true<br />

sandy bank (Durand 1959; Poug<strong>et</strong> 1968).<br />

Gypseous calcareous crusts are compact and<br />

not very porous. Because of mechanical resistance<br />

posed by the crusts, roots of the palm<br />

tree have difficulty pen<strong>et</strong>rating soil. Root<br />

depth decreases in soil and rooting takes a<br />

lateral orientation. The groundwater rise exasperates<br />

the problem, because the root zone is<br />

impoverished in oxygen, which produces<br />

asphyxiation and root rot. According to Callot<br />

<strong>et</strong> al. (1982), root development of plants is<br />

not only related to soil porosity, but also to<br />

moisture and soil resistance to pen<strong>et</strong>ration.<br />

Our study showed that date palm tolerated<br />

high moisture because, according to Went &<br />

Darley (1953), date palm does not have the<br />

capacity to form a fine root mass. In spite of<br />

its tolerance to moisture, <strong>des</strong>cription of roots<br />

of the palm trees in Arizona showed that root<br />

depth in contact with the groundwater does<br />

not exceed 2.2 m, and horizontal lengthening<br />

increases to 8.3 m. Vertical development of<br />

the roots is slowed down by the level of the<br />

water table (Simmons 1926). Bad drainage of<br />

salted water from the water table increases the<br />

concentration of salts in soil solution; soil<br />

becomes toxic and incompatible with normal<br />

date palm veg<strong>et</strong>ation (Monciero 1954). Salinity<br />

of groundwater in the root zone exceeds<br />

the standard limit of the salinity threshold,<br />

estimated at 3 dS.m-1 by Ayers and Westcot<br />

(1976). Contact of the roots with very salted<br />

groundwater, causes fall of the outputs, then<br />

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

Effects of hydro-edaphic environment on the rooting of date palm (Phoenix dactylifera L.) Degl<strong>et</strong> Noor<br />

in the Ouargla Basin (south-east algeria)<br />

Figure 7 <strong>–</strong> Relationship b<strong>et</strong>ween date palm rooting and shallow water table<br />

in areas without crusts.<br />

drainage becomes paramount under these<br />

conditions (Weeks 1957; Furr 1975). To counter<br />

all these difficulties, it is necessary to<br />

maintain the water level at approximately<br />

1.3 m in sandy soils, possibly up to 1.5 m in<br />

silty soils (Dubost 1991).<br />

Conclusion<br />

In light of the results obtained from different<br />

soil classes, we can conclude that the shallow<br />

groundwater in the Ouargla basin constituted<br />

the main obstacle to the root development of<br />

Degl<strong>et</strong> Noor date palms in soil depth. Roots<br />

avoided both water saturated zone and mechanical<br />

resistance in crusts, causing them developping<br />

in a horizontal direction. Salinity of<br />

the groundwaters proved to be less important<br />

to rooting of the date palm compared to level<br />

of the groundwater. Long term, clogging of<br />

the soils by water can cause hypoxia problems,<br />

root rot, salinization, dropping crop<br />

yields, and, d<strong>et</strong>erioration and degradation of<br />

palm plantations in certain extreme situations.<br />

Lastly, to avoid all these problems for date<br />

palm crops, it is necessary to maintain the<br />

level of the water table below root zone of<br />

date palms by using a good drainage n<strong>et</strong>work<br />

in the Ouargla basin.<br />

Taking into account the prevailing situation,<br />

it is advised that groundwater salinity levels<br />

be reduced by implementing suitable hydroagricultural<br />

improvements. However, it is<br />

necessary for groundwater salinity to remain<br />

above the threshold which allows the date<br />

palm to resist the bayoud disease. In crust<br />

zones, it is recommended to break soil before<br />

plantation of young date palms using subsoi-<br />

47

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