海水入侵条件下埃及北尼罗河三角洲部分水源和土壤质量评价

M. El-Ghannam, Mona K. M. Abdel-Razek, Hesham Abo El-Soud
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引用次数: 3

摘要

水质差的主要原因是人口增加和横向扩张,这与卫生和作物生产力的恶化有关。本研究旨在对伊勒谢赫省北三角洲3个方向海水入侵下不同水源和土壤的质量进行评价。在3条线路的15个地点共采集了45个水样。结果表明:灌溉水的盐度、碱度和硝酸盐浓度向北升高;各排水沟中Mn、Pb、Cd、Fe和Zn的浓度分别为0.20 ~ 1.36、0.15 ~ 0.97、0.0 ~ 0.2、0.29 ~ 2.70和0.0 ~ 0.1 mg / l。土壤盐分和碱度在远离海洋的地方最低,而在靠近海洋的地方最高。这可以解释为近海咸化地下水自流压力的影响,其中线1的值最高,达到20.25 dS/m,线3的值最低。对所研究的地下水样品进行了海水入侵计算,其大小由大到小依次为:第3线→第2线→第1线。另一方面,灌溉、排水和地下水的显著残留量碳酸钠(RSC)分别为-1.51、-7.99和-34.1。具有高RSC的水样可能具有明显的碱化危害。
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Quality assessment of some water sources and soil under sea water intrusion conditions in North Nile Delta, Egypt
Poor water quality mainly exists because of the increasing population and horizontal expansion which are associated with deterioration in sanitation and crop productivity. The present study is aiming to assess the quality of different water sources and soil under sea water intrusion along 3 directions in North Delta, kafr Elsheikh Governorate. A total of 45 water samples were collected from 15 loctions along 3 lines. The results showed that the salinity, sodicity and nitrate concentrations of irrrigarion water were increased toward the north due to the use of blended water for irrigation.The concentrations of Mn, Pb, Cd, Fe and Zn for all drains were varied from 0.20 to 1.36, 0.15 to 0.97, 0.0 to 0.2, 0.29 to 2.70 and 0.0 to 0.1 mgL-1, respectively. The lowest values of soil salinity and sodicity were recorded far from the sea, while the highest values were recorded near the sea. It could be rendered to the effect of artesian pressure of saline ground water near the sea, where the highest value reached 20.25 dS/m in line 1 and the lowest value was observed in line 3. Sea water intrusion were calculated for the studied groundwater samples and followed the decending order of: line 3˃ line 2˃ line 1. On the other hand, appreciable quantities of residual sodium carbonate (RSC) were -1.51, -7.99 and -34.1 for irrigation, drainage and groundwater, respectively. The water samples having high RSC can have an appreciable sodicity hazard.
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