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斯里兰卡北部贾夫纳半岛用于地下水开发的天然水的同位素和化学评估。

Isotope and chemical assessment of natural water in the Jaffna Peninsula in northern Sri Lanka for groundwater development aspects.

作者信息

Edirisinghe E A N V, Karunarathne G R R, Tilakarathna I A N D P, Gunasekara J D C, Priyadarshanee K S G S

机构信息

Isotope Hydrology Section, Sri Lanka Atomic Energy Board (SLAEB), Orugodawatta, Sri Lanka.

Water Resources Board (WRB), Colombo, Sri Lanka.

出版信息

Isotopes Environ Health Stud. 2020 Jun;56(3):205-219. doi: 10.1080/10256016.2020.1766457. Epub 2020 May 26.

Abstract

The demand for fresh groundwater in the Jaffna peninsula in northern Sri Lanka, has been increasing as the only water source for domestic and agricultural needs. Isotopic and hydro-chemical assessment on groundwater recharge and quality was done with the objective of assisting groundwater management plans. Water samples were collected in pre and post monsoon periods for isotope analyses (H, O and H) and major ions. Isotope data provide evidence that the groundwater is predominantly recharged by inter-monsoon (convectional) and North-East monsoon rains. Different residence times of shallow groundwater were found. The study revealed that the groundwater quality is mainly deteriorated due to dissolution of geogenic elements. However, in some instances, seawater intrusion and evaporation have caused lowering of groundwater quality. More saline groundwater is found in deeper levels in the karstic limestone aquifer system. Fresh water is available in coastal sandy aquifers in the eastern part of the peninsula. The impact of rainfall variations and agricultural activities are contributory factors for producing variations in the quality of groundwater. The current study suggests artificial groundwater recharge for the development and utilization of groundwater resources through small scale tanks/reservoirs or ponds in the areas where direct rain recharge occurs.

摘要

作为满足家庭和农业需求的唯一水源,斯里兰卡北部贾夫纳半岛对新鲜地下水的需求一直在增加。为协助制定地下水管理计划,对地下水补给和水质进行了同位素和水化学评估。在季风前后采集水样进行同位素分析(氢、氧和氚)以及主要离子分析。同位素数据表明,地下水主要由季风间期(对流)降雨和东北季风降雨补给。研究发现浅层地下水的停留时间各不相同。该研究表明,地下水质量主要因地质成因元素的溶解而恶化。然而,在某些情况下,海水入侵和蒸发导致了地下水质量下降。在岩溶石灰岩含水层系统的较深处发现了更多的咸水地下水。半岛东部沿海沙质含水层中有淡水。降雨变化和农业活动的影响是导致地下水质量变化的因素。当前的研究建议,在有直接降雨补给的地区,通过小型水箱/蓄水池或池塘进行人工地下水补给,以开发和利用地下水资源。

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