Munyangane Portia, Mouri Hassina, Kramers Jan
Limpopo Unit, Council for Geoscience, 30A Schoeman Street, Polokwane, 0700, South Africa.
Department of Geology, University of Johannesburg, Johannesburg, 2006, South Africa.
Environ Geochem Health. 2017 Oct;39(5):1201-1219. doi: 10.1007/s10653-016-9887-0. Epub 2016 Oct 15.
The present investigation was conducted in order to evaluate the occurrence and distribution patterns of some potentially harmful trace elements in the borehole water of the Greater Giyani area, Limpopo, South Africa, and their possible implications on human health. Twenty-nine borehole water samples were collected in the dry season (July/August 2012) and another 27 samples from the same localities in the wet season (March 2013) from the study area. The samples were analysed for trace elements arsenic (As), cadmium (Cd), chromium (Cr), selenium (Se), and lead (Pb) using the inductively coupled plasma mass spectrometry technique. The average concentrations of As, Cd, Cr, Se, and Pb were 11.3, 0.3, 33.1, 7.1, and 6.0 µg/L in the dry season and 11.0, 0.3, 28.3, 4.2, and 6.6 µg/L in the wet season, respectively. There was evidence of seasonal fluctuations in concentrations of all analysed elements except for As, though Cd and Pb displayed low concentrations (<0.2 and <6.0 µg/L, respectively) in almost all sampled boreholes. Se and Cr concentrations slightly exceed the South African National Standard permissible limits for safe drinking water in few boreholes. A total of four boreholes exceeded the water quality guideline for As with two of these boreholes containing five times more As than the prescribed limit. The spatial distribution patterns of elevated As closely correlate with the underlying geology. The findings of this investigation have important implications for human health of the communities drinking from the affected boreholes.
本次调查旨在评估南非林波波省大吉亚尼地区钻孔水中一些潜在有害微量元素的存在情况和分布模式,以及它们对人类健康可能产生的影响。在旱季(2012年7月/8月)采集了29份钻孔水样,2013年3月雨季又从研究区域内相同地点采集了另外27份水样。采用电感耦合等离子体质谱技术对水样中的微量元素砷(As)、镉(Cd)、铬(Cr)、硒(Se)和铅(Pb)进行了分析。旱季As、Cd、Cr、Se和Pb的平均浓度分别为11.3、0.3、33.1、7.1和6.0μg/L,雨季分别为11.0、0.3、28.3、4.2和6.6μg/L。除As外,所有分析元素的浓度均有季节性波动的迹象,不过Cd和Pb在几乎所有采样钻孔中的浓度都较低(分别<0.2和<6.0μg/L)。少数钻孔中Se和Cr的浓度略超过南非国家饮用水安全标准允许的限值。共有4个钻孔的As含量超过了水质准则,其中2个钻孔的As含量是规定限值的5倍多。As含量升高的空间分布模式与底层地质密切相关。本次调查结果对从受影响钻孔取水的社区居民的健康具有重要意义。