UNESCO Chair on Groundwater Arsenic within the 2030 Agenda for Sustainable Development, University of Southern Queensland, West Street, Toowoomba, Queensland 4350, Australia; Centro para la Investigación en Recursos Acuáticos de Nicaragua (CIRA/UNAN-Managua). Universidad Nacional Autónoma de Nicaragua. Del Hospital Monte España 300 metros al Norte, Managua, Nicaragua.
Centro para la Investigación en Recursos Acuáticos de Nicaragua (CIRA/UNAN-Managua). Universidad Nacional Autónoma de Nicaragua. Del Hospital Monte España 300 metros al Norte, Managua, Nicaragua.
Sci Total Environ. 2020 May 10;716:136527. doi: 10.1016/j.scitotenv.2020.136527. Epub 2020 Jan 15.
In contrast to other Latin American countries, where the presence of arsenic (As) in drinking water sources and related adverse human health impacts are well-known, little is internationally known from Nicaragua. However, the As problem is of high relevance as numerous assessments by national research, governmental and non-governmental institutions have proven. To assess for the first time and globally disseminate this predominantly nationally originated information is the aim of this review. In Nicaragua, >1000 water samples have been analyzed for total As from 1991 to 2017. By today, 144 communities distributed within 12 departments and one autonomous region (RACCS) are impacted with As. At least 55,700 people are exposed to drinking water with As (n = 173; range: 10-1320 μg/L, mean: 48.30 μg/L; 21.95%). Arsenic in surface water ranged from 0.99 to 2650 μg/L (n = 124, mean: 65.62 μg/L, 62.9% < 10 μg/L); and in groundwater from 0.10 to 1320 μg/L [n = 624, mean: 20.86 μg/L (70.7% < 10 μg/L)]. The highest As concentration was recorded from a well of the El Zapote community in 1996 (1320 μg/L), alerting national authorities and academic's to research As in water sources and health risks. Since then, 10 μg As/L has been the national regulatory limit for drinking water supplies. Occurrence of high As levels is linked to three geoenvironments: (i) Paleocene-Mesozoic metamorphic rocks (Northern Highlands) where As is present in epithermal veins, (ii) Tertiary volcanic rocks (Central Plateau) where As is related to fossil hydrothermal/volcanic systems, (iii) Quaternary rocks (Nicaragua Depression) where As is caused by active geothermal/volcanic activities. No mitigation measures have been implemented. Incipient water treatment efforts (Kanchan filters activated carbon) have failed because they were not socially accepted. More integrated, cross-sectorial research on genesis, health impacts and problem mitigation is needed. Provision of water treatment units for As removal on a single-household and community scale is needed, calling for the cooperation of national entities with communities in problem detection and solving.
与其他拉丁美洲国家不同,在这些国家,饮用水源中的砷(As)及其相关的人类健康影响是众所周知的,而在尼加拉瓜,国际上对此知之甚少。然而,由于国家研究、政府和非政府机构的多次评估已经证明,砷问题具有高度的相关性。本综述的目的是首次评估并在全球范围内传播这一主要源于国内的信息。自 1991 年至 2017 年,尼加拉瓜已对 1000 多个水样进行了总砷分析。迄今为止,分布在 12 个省和一个自治区(RACCS)的 144 个社区受到砷的影响。至少有 55700 人接触到含砷的饮用水(n = 173;范围:10-1320μg/L,平均值:48.30μg/L;21.95%)。地表水砷含量范围为 0.99 至 2650μg/L(n = 124,平均值:65.62μg/L,62.9%<10μg/L);地下水砷含量范围为 0.10 至 1320μg/L[n = 624,平均值:20.86μg/L(70.7%<10μg/L)]。1996 年,来自 El Zapote 社区的一口井中记录到的砷浓度最高(1320μg/L),这引起了国家当局和学术界对水源和健康风险中砷的研究。此后,10μg As/L 一直是国家饮用水供应的监管限值。高砷水平的出现与三个地质环境有关:(i)古近纪-中生代变质岩(北部高地),其中砷存在于浅成热液脉中,(ii)第三纪火山岩(中央高原),其中砷与化石热液/火山系统有关,(iii)第四纪岩石(尼加拉瓜低地),其中砷是由活跃的地热/火山活动引起的。没有采取缓解措施。初步的水处理工作(活性碳 Kanchan 过滤器)已经失败,因为它们没有被社会所接受。需要开展更多关于成因、健康影响和问题缓解的跨部门综合研究。需要在单户和社区层面提供去除砷的水处理设备,这需要国家实体与社区合作,共同发现和解决问题。