Department of Chemistry, University of Lagos, Akoka, Yaba, Lagos, PMB. 1005, Nigeria.
Environ Sci Pollut Res Int. 2017 Mar;24(9):8645-8657. doi: 10.1007/s11356-017-8479-6. Epub 2017 Feb 15.
Air pollution is influenced by wind-aided particulate suspension, open-air waste burning, and fossil fuel combustion. The pollutants from these sources eventually deposit on ambient surfaces. Atmospheric wet deposition into Lagos Lagoon may be significant additions to the nutrient levels of the eutrophic lagoon. Precipitation was monitored at three stations in the Lagos Lagoon basin from May to November, 2012, in order to estimate the contribution of wet deposition to the nutrient cycles of the lagoon. Water samples were digested with potassium persulfate, and the species of phosphorus (P) and nitrogen (N) were analyzed by colorimetric methods. The mean [NO+NO]-N level was 0.39 ± 0.51 kg ha month. The average total N was 3.16 ± 6.39 kg ha month. The mean soluble reactive P was lower than the [NO+NO]-N averaging 0.06 ± 0.09 (at control site S2) to 0.24 ± 0.10 kg ha month (at site S1). Average total P was 1.25 ± 0.82 kg ha month. The annual total N (May-September) was 4.55 (at S2) to 32.4 kg ha year (at S3). The annual total P (May-November) over Lagos Lagoon basin was 5.06 kg ha year (at S2). This study demonstrated that wet deposition of anthropogenically derived nutrients to the Lagos Lagoon is ongoing and may represent a considerable proportion of the total nutrient loading to it. The increased P availability in the wet deposition is likely responsible for the water hyacinths, which usually blossom on Lagos Lagoon during the late rainy season, and the reported harmattan-season bottom water hypoxia.
空气污染受到风力助长的颗粒物悬浮、露天废物燃烧和化石燃料燃烧的影响。这些来源的污染物最终会沉积在环境表面。大气湿沉降可能是拉各斯泻湖富营养化水平的重要补充。为了估计湿沉降对泻湖营养循环的贡献,于 2012 年 5 月至 11 月在拉各斯泻湖流域的三个站监测降水。水样用过硫酸钾消解,用比色法分析磷(P)和氮(N)的形态。[NO+NO]-N 的平均水平为 0.39±0.51 kg ha month。平均总氮为 3.16±6.39 kg ha month。平均可溶性活性磷低于[NO+NO]-N,平均为 0.06±0.09(在对照点 S2)至 0.24±0.10 kg ha month(在 S1)。平均总磷为 1.25±0.82 kg ha month。5 月至 9 月(S2)的年总氮(S2)为 4.55(S3)至 32.4 kg ha year(S3)。拉各斯泻湖流域年总磷(5 月至 11 月)为 5.06 kg ha year(S2)。本研究表明,人为来源营养物质的湿沉降仍在继续,并可能代表其总营养负荷的相当大一部分。湿沉降中磷的可用性增加可能是水葫芦的原因,水葫芦通常在拉各斯泻湖的雨季后期开花,以及报道的哈马坦季节底层缺氧。