| Lake of Fetzara | |
| Location: | North east of Algeria, South-east of the city of Annaba |
| Basin Countries: | Algeria |
| Length: | 18km (11miles) |
| Width: | 13km (08miles) |
| Pushpin Map: | Algeria |
| Area: | 206.8km2 |
The Lake of Fetzara is located in northeastern Algeria, 18km (11miles) southeast of the city of Annaba. It measures 17km (11miles) from east to west and 13km (08miles) from north to south, with an area of about 18600ha. It was officially classified as an area "Ramsar", which involves protection of this location. Several studies have been conducted on water and soil of the region Fetzara [1-7]. These studies were carried out to monitor the salinity and to highlight its origins and factors governing it. The main objective of this study was to evaluate soil properties of Fetzara Lake that are affected by the phenomenon of salinization and to study their variation with depth. The samples were taken on the first two layers (0–20 cm and 20–40 cm) at eight points around the Fetzara Lake, for a total of 16 samples. The analytical results indicate that soil salinity has reached its maximum in the northeast (region of Wadi Zied) and south of Lake (region of Cheurfa) with a dominance of sodium chloride-chemical facies.
Fetzara Lake is located 18 km southeast of the city of Annaba in the extreme east of Algeria. It is from east to west and from north to south with a surface of about . This area is subject to a Mediterranean climate with two distinct seasons: one humid and another dry. The lake water is temporary depending on the intensity of the rainy season on which it depends almost exclusively, it is generally an area of over 13000 ha of land flooded in winter and forming large meadows. The presence of a main channel across the lake from west to east provides the drainage, but it is insufficient to evacuate the water in the winter.
The geologist Henri Fournel discovered deposits of magnetite near the port of Bône in 1843. The mine is about from Bone in the Mokta hill beside the Lake of Fetzara at the foot of a mountain chain that runs from south to north, then turns east of the port of Bone. The name "Mokta-el-Hadid" (the iron pass) indicates that the deposit of iron has long been known, but there is no sign that it was worked before the first small-scale attempts in 1840. At this time the lake's surface elevation would have reached in winter, with an area of . The lake was bordered with reeds and rushes, used for nesting by migratory birds, and was rich in fish.
The lake was considered a source of fever, and a drainage channel flowing into the Oued Meboudja was proposed, but although the Société Générale Algérienne (SGA) had rights to the northern and eastern shores of the lake it did nothing. In the 1870s the mining company planted many eucalyptus trees around the Lake of Fetzara, but they were all killed by salt water seeping from the lake. In 1877 the Mokta El Hadid company gained permission to drain the lake in exchange for free transfer of the reclaimed land. A channel led from the center of the lake, crossed the western flank and led to the Meboudja. The surface elevation had dropped to by 1880, but the lake remained swampy in summer. After 1903 the company ceded its rights to the Lake of Fetzara to the SGA colony, which took over the work and completed it in 1935.
The soil quality has been defined as the result of its physical, chemical and biological properties, which allows growth and crop development, regulation and the score of water flow through the environment and acting as filter pump towards the pollutants. The soil quality reflects its ability to retain and to release water and nutrients to maintain its biodiversity and resisting to effects of practices that can lead to its degradation. It is obvious that soil quality towards a given use depends on the intrinsic properties of the geochemical environment and climate and its use by humans.
The soils of Fetzara Lake have been the subject of several studies for agricultural development, all of which revealed any significant constraints on their use such as salinization and hydromorphy [1, 2, 3, and 7]. These studies have helped to classify the soils into four classes: the less evolved soils of non-climate origin resulting from erosion, colluvial and alluvial deposits, the vertisols; alluvial deposits with high clay content as the drought comes easy to cracking; hydromorphic soils and halomorphic soils with high salinity.
The sampling was performed on the first two layers (0 – 20 cm and 20 – 40 cm) because, at this level, takes place the most important ions exchange. They were made at eight points around of Fetzara Lake or a total of 16 samples.
The soil samples were dried to fresh air ground and sieved to 2 mm to obtain the fine particles that will be used for all chemical and physicochemical analysis. The soil analysis carried out concerning the density, porosity, carbon and organic matter, pH, electrical conductivity and soluble salts. These characteristics are obtained with the current methods of analysis in soil science.
The soil physical properties affected by soluble salts are reflected by the notable modifications. Soil structure of Fetzara Lake is of prismatic type to columnar tendency, these characteristics are those of the soil affected by salinity. The soil of the Fetzara Lake are characterized by a real density of about 2.31 g/cm3, an average porosity of about 33%, permeability in most cases less than 2 cm / h, the pH is slightly acidic to alkaline (5.65 to 7.93), and an organic matter content highly variable (0.26 to 7.67%) [10]. Their evolution is closely related to the water cycle, by flooding of winter and summer dewatering.
The previous studies show that the salinity is particularly important in the north, in the east and in the southeast of Fetzara Lake. The West and the center of the lake seems to be the areas slightly affected by salts due to movement of salts towards the periphery with desalination of the center Lake [7]. The Average of electrical conductivity of soil solution in the lake is about 1534 μs/cm for the layer 0–20 cm, and 2577 μs/cm for the other layer 20–40 cm, indicating a very large variation between the two layers with a high concentration of soluble salts in depth.
The Soil can be affected by the problem of salinity due to presence of excessive concentrations of soluble salts, sodium or both at once. The soluble salts concerned are essentially, Ca++, Mg++, K+, Na+, Cl-, SO4—and HCO3- (Table 2).
The second axis F2, which represents 12.29% of the variance, opposes the soluble salts to the alkalinity, pH and K+. It may reflect the processes of salinization and alkalinization. But also the phenomenon of fixation of K+ by some clay minerals is not being ruled out. The distribution of individuals allows us to visualize three groups of associations; the first group G1 (S3, S4, S8, S11, S12 and S16) is characterized by mineralized solutions, it is opposed to the second group G2 (S6, S7, S14 and S15) representing the less mineralized solutions. The third group G3 (S1, S2, S9 and S10) includes the solutions loaded with bicarbonate.