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