Diyabalanage Saranga, Abekoon Sumith, Watanabe Izumi, Watai Chie, Ono Yuko, Wijesekara Saman, Guruge Keerthi S, Chandrajith Rohana
Postgraduate Institute of Science, University of Peradeniya, Peradeniya, Sri Lanka.
Department of Geology, Faculty of Science, University of Peradeniya, Peradeniya, Sri Lanka.
Environ Geochem Health. 2016 Jun;38(3):679-90. doi: 10.1007/s10653-015-9749-1. Epub 2015 Jul 17.
The Mahaweli is the largest river basin in Sri Lanka that provides water to the dry zone region through multipurpose irrigation schemes . Selenium, arsenic, cadmium, and other bioimportant trace elements in surface waters of the upper Mahaweli River were measured using ICP-MS. Trace element levels were then compared with water from two other rivers (Maha Oya, Kalu Ganga) and from six dry zone irrigation reservoirs. Results showed that the trace metal concentrations in the Mahaweli upper catchment were detected in the order of Fe > Cu > Zn > Se > Cr > Mn > As > Ni > Co > Mo. Remarkably high levels of Ca, Cr, Co, Ni, Cu, As, and Se were observed in the Mahaweli Basin compared to other study rivers. Considerably high levels of Cr, Mn, Fe, Co, Ni, Cu, Zn, As, and Se were found in upstream tributaries of the Mahaweli River. Such metals possibly originated from phosphate and organic fertilizers that are heavily applied for tea and vegetable cultivations within the drainage basin. Cadmium that is often attributed to the etiology of unknown chronic kidney diseases in certain parts of the dry zone is much lower than previously reported levels. Decrease in these metals in the lower part of the Mahaweli River could be due to adsorption of trace metals onto sediment and consequent deposition in reservoirs.
马哈韦利河是斯里兰卡最大的流域,通过多用途灌溉计划为干旱地区供水。使用电感耦合等离子体质谱法(ICP-MS)测量了马哈韦利河上游地表水的硒、砷、镉和其他对生物重要的微量元素。然后将微量元素水平与另外两条河流(马哈奥亚河、卡卢甘加河)以及六个干旱地区灌溉水库的水进行了比较。结果表明,马哈韦利河上游集水区的痕量金属浓度检测顺序为铁>铜>锌>硒>铬>锰>砷>镍>钴>钼。与其他研究河流相比,马哈韦利河流域的钙、铬、钴、镍、铜、砷和硒含量显著较高。在马哈韦利河的上游支流中发现了相当高含量的铬、锰、铁、钴、镍、铜、锌、砷和硒。这些金属可能源自流域内大量用于茶叶和蔬菜种植的磷酸盐和有机肥料。在干旱地区某些地方常被认为是不明慢性肾病病因的镉含量远低于先前报告的水平。马哈韦利河下游这些金属含量的降低可能是由于痕量金属吸附到沉积物上并随后沉积在水库中。