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

I. Jemai, N. Benaissa, T. Gallali, F. Chenini
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引用次数: 9

Abstract

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.
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城市再生废水灌溉对Souhil Wadi地区土壤和地下水有机无机组成的影响
突尼斯调动了大量的常规水力资源(地表水和地下水)。今天,出于节水的考虑,也出于环境伦理的考虑,将其非常规资源如城市废水回收利用,并将其应用于农业。2004年,在突尼斯东北部纳布勒省的Oued-Souhil试验站,研究了处理后的废水(TWW)与普通灌溉(用地下水灌溉(GW))(喷灌(S)和综合喷灌(IG))对沙土化学性质及其有机成分的影响。在0-20、20-40、40-60、60-80和80-100 cm 5个深度采集土壤样品,分析电导率(EC)、pH、总氮(TN)、有机碳(OC)、钾(K)、磷(P205)和硝酸盐(NO3 -)。一次灌溉后的观察结果表明,试验土壤的电导率和pH值较初始状态有所下降。灌溉降低了表层有机碳含量,增加了深层有机碳含量。全氮含量呈相反方向变化。TWW灌水土壤和GW灌水土壤在研究结束时上部40 cm的P205、K和NO3 -浓度均呈下降趋势;然而,TWW灌溉仅对钾(K)有显著影响。研究期间这些元素在土壤中的演变证明了它们在TWW中的重要浓度。
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