alexa Effects of Municipal Reclaimed Wastewater Irrigation on Organic and Inorganic Composition of Soil and Groundwater in Souhil Wadi Area (Nabeul, Tunisia)
ISSN: 2157-7587
Hydrology: Current Research

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  • Research Article   
  • Hydrol Current Res 2013, Vol 4(4): 160
  • DOI: 10.4172/2157-7587.1000160

Effects of Municipal Reclaimed Wastewater Irrigation on Organic and Inorganic Composition of Soil and Groundwater in Souhil Wadi Area (Nabeul, Tunisia)

Jemai I1*, Ben Aissa N2, Gallali T1 and Chenini F3
1Faculté des sciences de Tunis (FST), Campus Universitaire - Tunis - 1060, Tunisia
2Institut national d’agronomie de Tunisie (INAT), 43, avenue Charles Nicolle 1082-Tunis Mahrajène, Tunisia
3Institut national de Recherche en Génie Rural Eaux et Forêt (INFGREF), Avenue El Hadi Karray 2049 Ariana, Tunisia
*Corresponding Author: Jemai I, Faculté des sciences de Tunis (FST), Campus Universitaire - Tunis - 1060, Tunisia, Tel: 0021698959954, Email: [email protected]

Received Date: May 28, 2013 / Accepted Date: Nov 28, 2013 / Published Date: Dec 03, 2013


Tunisia has mobilized the important amount of its conventional hydraulic resources (surface water and ground water). It is brought today, for considerations of saving of water but also in environmental ethics, to recycle its noconventional resources like municipal waste water and to applicant it for agriculture. The effect of treated wastewater (TWW), compared to the ordinary irrigation (with ground water (GW)) by means of tow irrigation methods (sprinkler (S) and integrated Gouttor (IG)) on the chemical properties of the sandy soil, and its organic composition, were investigated in 2004 at the experimental station of Oued-Souhil in Nabeul Governorate, NE Tunisia. Soil samples were collected from five depths (0–20, 20–40, 40–60, 60–80 and 80–100 cm) and were analyzed for electric conductivity (EC), pH, total nitrogen (TN), organic carbon (OC), potassium (K), phosphorus (P205) and nitrate (NO3 -). The results observed after a partner of irrigation show that the electric conductivity (EC) and pH of experimental soil decreased compared to his initial state. The irrigation has reduced the OC content in surface layer and has increased it in the deeper layer. The TN content varied in opposite direction. The P205, K and NO3 - concentrations decreased in the upper 40 cm at the end of the study for both TWW and GW irrigated soil; however the effect of TWW irrigation was significant only with potassium (K). The evolution of these elements in the soil during the study proves their important concentration in the GW.

Keywords: Sandy soil; Treated waste water; Nitrate; Phosphorus; Irrigation; Groundwater


In recent years, many Mediterranean countries have experienced severe water supply and demand imbalances, with more frequent and longer periods of drought. In Tunisia, several regions have suffered successive droughts over the last 10 years [1]. Due to water scarcity and population growth, the demand on freshwater increases and agricultural activities (using more than 80% of the total water resource extracted) are in competition with other demands (domestic and industrial). A national wastewater reuse policy was launched at the beginning of the eighties in Tunisia. The first wastewater reuse regulation was issued in 1989. The reclaimed water has been used mainly for irrigation (9000 ha in 2005), the reuse of TWW is currently an integral part of national water resources strategy [2-4]. 29% of treated sewages are reused for the cultivation of fruit trees, cereals, fodder crops and industrial crops (7900 ha of agricultural lands in 2005) as well as for golf courses (760 ha in 2005) and green spaces (340 ha in 2005). TWW is also reuse in recharges purposes and conservation of wetlands. It is actually considered as an additional water resource and as a potential source of fertilizing elements [5].

The reuse of treated domestic wastewater in agricultural purposes has been increasingly considered to be beneficial for crop production, and due to its significant source of nutrients for the plants [6,7] it can help to reduce the requirements for commercial fertilizers [8]. First and foremost, it is promoted in order to save fresh water for water supply and to protect receiving waters.

However, under certain conditions, this type of water if not well managed, can have negative impacts on cultivated crops and soils, particularly on soil salinity and sodicity, so that the effluent for reuse must comply with reuse standards to minimize environmental and health risks [9]. Among the potential risks associated with TWW irrigation are degradation of soil structure, decrease in soil hydraulic conductivity [10,11], surface sealing, runoff and soil erosion problems, soil compaction, soil contamination with faecal coliform [12,13] and pollution of groundwater, as a result of high nitrogen concentration [14]. Generally, as stated in the 2002 Hyderabad Declaration, on Wastewater Use in Agriculture, ‘without proper management, wastewater use poses serious risks to human health and the environment’, [15]. However, environmental risks to the soil compartment have been much less studied, with the exception of heavy metals [8,16-21].

The choice of irrigation method can also influence the soil chemical response to TWW irrigation. Studies about changes in the chemical properties of soils irrigated with TWW have mainly shown an increase of Na+ and a fast oxidation of NH4 + into NO3 - using subsurface dripping [22] or sprinkling aspersion [23,24].

The experimental station of Oued-Souhil in Nabeul constitutes since the eighties a pilot site for the management and the control of the reuse of the treated municipal waste water. Most studies focus on yield crop under irrigation and nitrogen fertilization or on health risks [25]. However, impact of the irrigation by TWW, especially in an experiment field, on evolution of chemical elements in the soil is not well studied yet. The goal of this study is to evaluate, on short period, the effects of the TWW irrigation, in comparison to that of the GW, on the inorganic and organic composition of a soil cultivated with potato and never irrigated by TWW.

Materials and Methods

Site description

This study was conducted during October-March 2004, at the experimental station of Souhil Wadi (36°27'22"N 10°42'02"E, Figure 1) near Nabeul city which is located at ‘Cap Bon’ peninsula at the North Eastern part of Tunisia. The altitude is 25 m above mean sea level. The site is characterized by a Mediterranean semi-arid climate (rainy and fresh winter without frosts) with a mean annual precipitation of 391 mm concentrated during the months of September to December and a mean annual temperature of 18, 3°C.


Figure 1: Location map of the experimental site.

The station comprises a reclaimed water irrigated plots and an artificial recharge site. The effluents of two sewage treatment plants, SE3 (oxidation ditches) and SE4 (activated sludge) are stored in a 4500 m3 capacity storage basin.

During the summer season, effluents are carried in a network to provide irrigated subunits where mainly citrus trees and fodder are grown. During the fall season the effluents are used for artificial aquifer recharge by spreading on infiltration basins.

As for the groundwater, the Hammamet–Nabeul aquifer is the main water resource in the station. The vadose zone of the aquifer has been described by Rekaya [26] and Plata Bedmar and Rekaya [27] and more recently by Kallali and Yoshida [28] as varying between 10 and 13 m thick from the river bed to the infiltration basins. The aquifer is about 2-3 m thick; the substratum is formed of Pliocene clay with 12 m thickness at the level of the recharge site.

At the level of the irrigated area, the groundwater table is estimated to be about 10 m deep [29]. This was confirmed by measures done between June 2004 and April 2006 in the monitoring wells in the recharge site. The permeability of the aquifer is estimated between 10-5 and 6.10-3 m/s.

The soil of experimental field is composed of alluvia of coarse material belonging to the Quaternary marine formation and is classified as Vertic Xero Fluvent according to American classification. The texture is sandy with low contents of silts and clays, and the surface infiltration rate at saturation level is 4.3 10-3 ms-1.The physical characteristics of this soil at the beginning of the study are listed in Table 1.

Depth (cm) Clay (%) Loam (%) Sand (%) pH EC (mS/cm) CaCO3 (%) C % N % C/N
0-20 7.4 3.20 88.20 8.7 0.90 4.6 2.14 0.038 56.3
20-40 10.4 4.80 85.40 9.0 1.14 3.8 1.06 0.027 39.2
40-60 4.6 4.00 93.60 9.2 1.16 2.4 0.26 0.040 6.5
60-80 5.25 10.75 84.75 9.1 1.40 2.6 0.06 0.018 3.3
80-100 7.5 3.70 90.25 9.1 1.50 3.8 0.06 0.014 4.3

Table 1: Initial characteristics of the soil at the experimental field.

Experimental design

The field experiment was carried out on 750 m2 plots which are divided in two blocs adopted as two main treatments: GW treatment corresponding to irrigation with groundwater and TWW treatment corresponding to irrigation with treated waste water. In each treatment, the irrigation by sprinkler (S) and integrated Gouttor (IG) was repeated in three blocs respectively in a manner that GW and TWW blocs are divided in six (3 S and 3 IG). The GW was pumped from the wells of surface of the station. The TWW were from the wastewater treatment plant of Dar Châabane (SE4) with a mainly urban wastewater origin 9585 m3/day [30].

A crop of potato (SPUNTA variety) was sown on October 10, 2003 in all plots. Plant emergence began on October 20 and the crop was removed from the field on February 10, 2003. Before that, the experimental field was sometimes cultivated but never irrigated by TWW. An organic spreading of manure was carried out before the plantation at a rate of 40 t ha-1. At the time potato was planted, inorganic nitrogen fertilizer (NH4 NO3) was applied at a rate of 200 kg ha-1. Potato-growing period, October to February, is characterized by rainy winter. Weather data for the crop-growing period were obtained from the nearby weather station; about 100 m from the experimental plot. The amount of water applied during the experiment, was 84 m3 for each bloc.

Soil sampling and analysis

An initial soil sampling before the irrigation and a final soil sampling after harvest was performed. Soil samples were collected at three points for each treatment at five depths (0-20, 20-40, 40-60, 60-80 and 80- 100 cm). The samples were then dried, sieved at 2 mm and analyzed. The particle size was measured by sedimentation (Robinson pipette). The pH was measured by the electrometric method in distilled water (1:2.5). EC of the soil was determined in an extract of saturated paste. The total calcium carbonate content (CaCO3) was measured by acid digestion using a Bernard calcimeter. The soil OC was determined by Wet digestion method [31]. TN was determined by Kjeldahl digestiondistillation method [32]. Extractable K by NH4OAc [33] and available P by 0.5 M NaHCO3 [34]. NO3 - was measured by steam distillation in presence of MgO to remove NH4 + and in the presence of both MgO and Devarda alloy to reduce NO2 - and NO3 - and to remove the NH4 + obtained.

Water sampling and analysis

Samples of irrigation water, taken at each irrigation (what suits five samples), were placed in plastic bottles, filtered and stored at low temperature (4°C). Analyses were performed after four days of storage. pH and EC were measured directly by pH meter and salinometer respectively. The determination of cations was performed by Flame Photometry. PO4 3- ions are measured, in an acidic solution with ammonium molybdate, by visible spectrophotometry at the wavelength of 720 nm. Mineral nitrogen was determined by distillation.

Statistical analyses

Significance of differences in soil properties in response to the effects of kind of water, system of irrigation, and depth were assessed by computing the Analysis of Variance of two or three factors, by the software STATISTICA, Version 5 and a Newman and Keuls test was used to compare the means, considering a significance level of p < 0.05 throughout the study.

Results and Discussion

TWW and GW characteristics

The irrigation water characteristics at the end and the beginning of the study are shown in Table 2. Both water types were slightly alkaline. The water samples present a variable pH ranging between 7.2 and 8.6 but which remains acceptable according to the standards of World Health Organization [35] and the Tunisian standard (NT 106.03, 1989) [36]. The EC, ranging between 1.9 and 5 ms/cm, remain acceptable according the Tunisian Standards (NT 106.03, 1989). However, by Richards diagram (Riverside) [37], the electrical conductivity indicates a high and a very high risk of salinization for TWW and GW respectively, whereas the estimated sodium adsorption ratio (SAR) indicates a low risk of sodification.

Parameter GW TWW NTb WHOc
Rangea Mean ± SD Range Mean ± SD
pH 7.4–7.2 7.72 ± 0.37 7.7–6.9 7.82 ± 0.55 6.50-8.50 6.5-9.5
EC mS cm-1 2.6–5 3.08 ± 0.97 1.9–3.9 2.36 ± 0.78 7 -
RS (g L-1 2–2.5 2.20 ± 0.24 1–2 1.50 ± 0.45 - -
SAR 6.5–8.1 6.22 ± 1.38 5–9.9 6.22 ± 1.95 - -
HCO32- (mg L-1) 427–549 402.60 ± 113.14 305–244 317.20 ± 59.77 - -
SO42- (mg L-1) 345–405 377.60 ± 19.97 260–345 305.20 ± 35.20   500
Cl- (mg L-1) 701–445 590.60 ± 114.63 401–319 429.80 ± 64.92 2000 250
Ca2+ (mg L-1) 326–213 321.40 ± 6.56 206–82 192.00 ± 61.06 - -
Mg2+ (mg L-1) 7–8 8.00 ± 1.10 6–5 5.80 ± 0.75 -  
Na+ (mg L-1) 434–442 397.20 ± 71.88 270–341 300.60 ± 34.35 - -
K+ (mg L-1) 39–46 41.80 ± 3.06 38–54 41.80 ± 6.21 - -
NO3- (mg L-1) 183.5–228.6 193.52 ± 25.64 22.3–17.3 22.76 ± 2.89 - 50
NH4+ (mg L-1) 2.8–10.8 6.74±0.05 25.2–45.3 24.36±13.51 - -
P (mg L-1) 1.53–41.89 18.38±20.14 1.53–64.31 31.03±28.42 - -

a Range indicates (value of initial water sampling - value of final water sampling)
b Tunisian standards [33].
c WHO's drinking water standards 2006
RS: dry residue
SAR: sodium adsorption ratio

Table 2: Characteristics of GW and TWW used for irrigation.

The chemical composition of the two kind of irrigation water indicated that Cl-, Na+, Ca2+ and SO42- were the most abundant cations and anions, respectively. These were followed by bicarbonate (HCO3 2- ) and K+ in descending order according to the concentration levels. Concentrations of these ions show that the water irrigation is strongly mineralized.

For both types of water, the levels of dissolved salts increases with time, which shows an increase in the salinity of which is more important with GW where the values range between 2 and 2.5g/l.

TWW characterization revealed that the mean Cl content is 429.8 mg L−1 and is lower than reclaimed water irrigation standards (2000 mg L−1). According to data taken at 2003 from National Office for Sanitation, the suspended solids content is of 20 mg L−1 (Tunisian standards NT 106.03, 1989=30mg L−1). The COD and the BOD concentrations are respectively 91 (NT=90 mg L−1) and 14.5 mg L−1 (NT=30 mg L−1). Thus, the TWW has the characteristics of a relatively high quality effluent.

Soil EC and pH

At the beginning of the experiment, the pH was strongly alkaline, values were between 8.7 and 9.2 (Table 3). Values of EC were important in the deep soil layer which could be explained by the accumulation of salts resulted of evaporation and capillary rise. So, GW moves upward from a shallow water table close to the soil surface. The water carries salts which accumulate in the soil as the water is evaporated from the soil surface or transpired through the plants to the atmosphere. These levels will be then the higher limit reached by subsoil waters.

Depth (cm) (Initial state) (Final state)
0-20 8.70 0.9 8.52 0.77 8.45 0.78
20-40 9.00 1.14 8.44 0.61 8.58 0.67
40-60 9.20 1.16 8.93 0.7 8.56 0.84
60-80 9.14 1.4 9.01 0.67 8.79 0.74
80-100 9.20 1.5 9.06 0.65 8.85 0.82

Table 3: Mean values of pH and Electrical conductivity (ms/cm) for the experimental soil under effect of water irrigation.

At the end of the study the values of the EC and pH decreased significantly in the soil compared to the initial state (Table 3). The reduction of EC value is due to the leaching of salts which is directly related to water movement [38] because crops only remove small amounts of salt. Irrigation water is the main source of adding salts to the soil [39]. In this research the EC values of groundwater and wastewater were significantly similar (Table 2). Therefore, the application of groundwater has caused soil EC statistically equivalent to soil EC caused by wastewater (Table 4). However, mean EC values of wastewater irrigated soil were slightly greater than those of groundwater irrigated soil for the whole layer (Table 3). This result is likely due to the effect of plant uptake on the soil solution. Because wastewater generated higher yield (286 Kg) than groundwater (260 Kg), there was more water uptake and transpiration of Potato due to wastewater irrigation which corroborate the finding of Heidarpour et al. [40].

Depth (cm) (Initial state) Final state (GW) Final state (TWW)
OC % TN ‰ C/N OC % TN ‰ C/N OC % TN ‰ C/N
0-20 2.14 0.38 56.3 1.87 0.67 27.9 2.02 0.63 32.06
20-40 1.06 0.27 39.2 0.8 0.38 21.0 0.52 0.23 22.6
40-60 0.26 0.4 6.5 0.5 0.26 19.2 0.32 0.2 16
60-80 0.06 0.18 3.3 0.37 0.2 18.5 0.32 0.2 16
80-100 0.06 0.14 4.3 0.2 0.15 13.3 0.2 0.14 14.3

Table 4: Organic characteristic of the soil at the beginning and the end of the study.

Whereas, pH decrease in soil could be due to ammonium nitrification which release free hydrogen ions in the soil, thus lowering the soil pH. This reduction of pH is slightly important with application of treated wastewater which corroborates the findings of [41-44]. Higher concentrations of ammonium ions in TWW than GW (Table 2) may lead to a higher rate of nitrification releasing free hydrogen ions in the soil, thus lowering more the soil pH. A reduction in soil pH due to TWW irrigation compared to irrigation by GW has been reported [45-47].

Some investigations showed that the soil irrigation with wastewater increased soil pH [48,49]. Most these investigations described the long term impact of irrigation with sewage and wastewater effluents on soil properties while our study was short term. Soil irrigation with wastewater may cause at first a decrease of soil pH, but after a while it may cause an increase of soil pH.

Soil OC and TN

Before the irrigation, the content of OC and TN in the soil was most important in surface layers, this is due to the organic amendments (manure) added to the soil before plantation.

After the harvest, results showed that irrigation has significantly reduced OC and increased TN of the soil for the first and second soil layer (Table 4), which could be attributed to the mineralization of the organic matter. This mineralization resulted in a reduction of C/N ratio and would be supported by the nitrogen added by irrigation. This is in line with findings of Rusan et al. [48] and Khai et al. [50]. Magesan et al. [51] and Ramirez-Fuentes et al. [52] have reported that nutrients supplied by irrigation water stimulate microbial activity in the soil which promotes mineralization of organic matter.

At the end of the study, below 40 cm depth, the enrichment of the soil by OC might be due to a drive in suspension of the non humified organic particles towards the deeper layer which resulted in an significant increase in the percentages of OC and a significant rise in C/N ratio (Table 4).


The initial and final soil P2O5 concentration decreased significantly from the top of the soil to the deeper layers. Below 20 cm, there was no significant difference in P2O5 concentration in the soil (Table 5). The accumulation of P2O5 in the first soil layer could be due to application of NPK fertilizer and the irrigation effect. Furthermore, the reduction of P205 contents in the surface layer at the end of the study could be due to the plant uptake and especially to the leaching of this element which resulted in the enrichment of the groundwater by the phosphor (Table 2). In 20 cm soil depth, the concentration of P2O5 was significantly higher with GW irrigated soil (Table 5).This result is similar to those of other researchers [40,53-55]. The soil P205 concentration was unaffected by irrigation method (Table 6).

Depth (cm) Beginning of the study End of the study
0-20 170.00a 127.00a 93.50a* 80.25a*
20-40 42.00b* 55.67b* 34.00b* 39.00b*
40-60 28.67b* 25.67b* 23.00b* 30.75b*
60-80 24.33b 62.00b 29.75b* 25.75b*
80-100 23.67b* 26.33b* 31.50b* 24.25b*

Data in the same column followed by the same letter (a, c) were not significantly different at the P < 0.05 level (Test of Newman-Keuls) and (*) indicates that there is no significant difference (P < 0.05) between GW and TWW soils.

Table 5: Means of P2O5 (mg kg-1) for each soil layer at the beginning and the end of the study.

Depth (cm) S IG
0-20 176.40 a 139.80 a 111.20 a 149.00 a
20-40 51.40 a 56.40 a 38.00 a 45.40 a
40-60 28.40 a 29.80 a 57.80 a 26.00 a
60-80 39.40 a 31.20 a 30.40 a 39.20 a
80-100 45.00 a 40.96 a 26.40 a 40.46 a

Values in any column followed by the same letter do not differ at the 0.05 significance level (Test of Newman-Keuls).

Table 6: Means of P2O5 (mg kg-1) for the experimental soil under effect of irrigation system.


Based on analysis of variance, the high content of K in the surface layer (Table 7) at the beginning of study is due to the application of NPK fertilizers.

Depth (cm) Begining of the study End of the study
0-20 270a* 260a* 170a* 170a*
20-40 220ab* 230ab* 200a 160a
40-60 160b* 160b* 190a 150a
60-80 90c* 90c* 160a 120a
80-100 70c* 70c* 130a 60b

Data in the same column followed by the same letter (a, c) were not significantly different at the P < 0.05 level (Test of Newman-Keuls), and (*) indicates that there is no significant difference (P < 0.05) between GW soil and TWW soil.

Table 7: Means of K (mg kg-1) for each soil layer at the beginning and the end of the study.

At the end of the study, the soil K content decreased significantly in the 0-40 cm layer and increased significantly below 40 cm depth (Table 7). This result showed the importance of this nutrient leaching in the studied soil.

In the plot irrigated by the GW, irrigation system effect is observed in 0-20, 20-40 and 60-80 cm soil depth (Table 8). Indeed, the accumulation of K in the soil is less large with the IG which probably attests the efficiency of absorption of K with this system of irrigation. In another manner absorption of K is larger by using the IG.

Depth (cm) S IG
0-20 260a 220ab 150b 290b
20-40 210bc 210a 160c 240a
40-60 160a 150a 170a 160a
60-80 190b 110a 080a 120a
80-100 110a 120a 110a 110a

Data in the same column followed by the same letter (a, c) were not significantly different at the P < 0.05 level (Test of Newman-Keuls)

Table 8: Mean value of K (mg kg-1) in the experimental soil under effect of the irrigation system.

In the plot irrigated by the TWW, irrigation system effect is observed only in 0-20 cm soil depth (Table 8). Contrary to the case of the GW, it is with the IG that the accumulation of the K in the soil is the most important. This can be related to the difference in movement of this nutriment with the tow techniques of irrigation.


At the beginning of the study, soil NO3 - content was significantly greater in surface layers, which corroborate the finding of Feng et al. [56]. The higher NO3 - content in the upper layer might be attributed to the application of NPK fertilizers.

After the irrigation, the NO3 - distribution pattern throughout the soil profile was significantly changed (Table 9). The lowest NO3 - content was found in 20-40 cm depth in all plot types. NO3 - content then increased with depth, reaching maximum levels at 40-60 cm.

Depth (cm) Begining of the study End of the study
0-20 70.14a* 81.67a* 48.05a* 36.75a*
20-40 85.35a* 67.75a* 40.15a* 32.42a*
40-60 51.05a* 54.57a* 59.57a* 41.79a*
60-80 64.87a* 81.78a* 55.05a* 36.12a*
80-100 56.04a* 63.27a* 53.89a* 35.65a*

Data in the same column followed by the same letter (a, c) were not significantly different at the P < 0.05 level, and (*) indicates that there is no significant difference (P < 0.05) between GW soil and TWW soil.

Table 9: Means of NO3- (mg kg-1) for each soil layer at the beginning and the end of the study.

Even though the NO3 - content in the upper layers (40 cm deep) was generally found to be lower after the irrigation than before, there were differences in the distribution pattern throughout the soil profile in the different plot types. In TWW irrigated soil, the NO3 - content in all layers was generally lower after the irrigation, whereas in GW irrigated soil, the NO3 - content in the 40-60 cm layers was slightly higher than before irrigation, suggesting that NO3 - had accumulated in deeper soil layers due to the irrigation.

Like the case of P205, the soil NO3 - concentration was unaffected by irrigation method (Table 10).

Depth (cm) S IG
0-20 37.69a 45.10a 42.20a 39.59a
20-40 46.92a 37.34a 51.29a 36.18a
40-60 49.18a 48.59a 38.43a 41.38a
60-80 44.92a 43.92a 43.53a 35.16a
80-100 48.58a 40.90a 42.99a 40.46a

Values in any column followed by the same letter do not differ at the 0.05 significance level (Test of Newman-Keuls).

Table 10: Mean value of NO3 - (mg kg-1) in the experimental soil under effect of the irrigation system.

Impact on groundwater

The NO3 - content of the GW increased from 183.5 before to 228.6 mg/l after the irrigation (Table 2), thereby exceeding the drinking water standard of the World Health Organization of 50 mg L-1 [9].

The leaching of soil NO3 - from the plant root zone to the groundwater is mainly determined by the high amount of NO3 - (large amounts of water and N fertilizer) accumulated in the soil profile exceeding the requirements of the cultivated plants [57] in conjunction with or followed by the high drainage volume [58,59] accentuated by the sandy textured soil and the high amount of rainfall and irrigation (Figure 2).


Figure 2: Monthly distribution of rainfall and irrigation depth during the simulation period for the period of September to March.

According to the international drinking water standards the phosphorus content reaching 41.85 mg L-1 after irrigation exceed the limit of potability (0,5 mg L-1) which can contribute to Algal growth and eutrophication [60].

The pH of the groundwater was decreased by the irrigation from 7.4 to 7.2, and the EC was increased from 2.6 to 5 mS cm-1 (Table 2), indicating a higher concentration of dissolved salts in the groundwater which join the results of Feng et al. [56] and Kallel and Bouzid [61]. In Sokra perimeter of the side of Tunis, Zekri et al. [62] have observed an increase in GW salinity from 2.3 to 4 ms cm-1 after 20 years of irrigation with TWW.


These results show that after a partner of irrigation, the evolution of chemical constituents in soil layers was not influenced by the kind of irrigation water. However, it was influenced by water movement patterns, chemical concentrations in irrigation water and plant uptake. The most important concern was the leaching of salts, phosphorus and nitrate to the GW leading to the degradation of its geochemical quality. Therefore, the impact of TWW irrigation on soil composition was not apparent in this experiment but it was strongly significant on GW quality.


The authors are grateful to the INRGREF institute for providing financial support for this work. El Haddi El Hamrouni and Leila Ben Dhiaa are also thanked for their great help and assistance with laboratory work.


Citation: Jemai I, Ben Aissa N, Gallali T, Chenini F (2013) Effects of Municipal Reclaimed Wastewater Irrigation on Organic and Inorganic Composition of Soil and Groundwater in Souhil Wadi Area (Nabeul, Tunisia). Hydrol Current Res 4: 160. Doi: 10.4172/2157-7587.1000160

Copyright: © 2013 Jemai I, et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.

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