Department of Bioenvironmental Systems Engineering, National Taiwan University, Taipei.
Environ Geochem Health. 2011 Oct;33(5):503-14. doi: 10.1007/s10653-010-9367-x. Epub 2010 Nov 25.
Kinmen is located in the southwest of Mainland China. Groundwater supplies 50% of the domestic water use on the island. Residents of Kinmen drink groundwater over the long term because surface water resources are limited. Nitrate-N pollution is found and distributed primarily in the western part of groundwater aquifer whereas saline groundwater is distributed to the northeastern Kinmen. This work applied the DRASTIC model to construct the vulnerability map of Kinmen groundwater. MT3D was then used to evaluate the contamination potential of nitrate-N. The health risk associated with the ingestion of nitrate-N contaminated groundwater is also assessed. The results from DRASTIC model showed that the upland crop and grass land have high contamination potential, whereas the forest, reservoir and housing land have low contamination potential. The calibrated MT3D model inversely determined the high strength sources (0.09-2.74 kg/m(2)/year) of nitrate contaminant located in the west to the north west area and required 2-5 years travel time to reach the monitoring wells. Simulated results of MT3D also showed that both the continuous and instantaneous contaminant sources of nitrate-N release may cause serious to moderate nitrate contamination in the western Kinmen and jeopardize the domestic use of groundwater. The chronic health hazard quotient (HQ) associated with the potential non-carcinogenic risk of drinking nitrate-N contaminated groundwater showed that the assessed 95th percentile of HQ is 2.74, indicating that exposure to waterborne nitrate poses a potential non-cancer risk to the residents of the island. Corrective measures, including protecting groundwater recharge zones and reducing the number of agricultural and non-agricultural nitrogen sources that enters the aquifer, should be implemented especially in the western part of Kinmen to assure a sustainable use of groundwater resources.
金门位于中国大陆的西南部。该岛 50%的家庭用水来自地下水。由于地表水有限,金门居民长期以来一直饮用地下水。硝酸盐氮污染主要分布在西部地下水含水层,而咸地下水则分布在金门东北部。本研究应用 DRASTIC 模型构建了金门地下水脆弱性图。然后使用 MT3D 评估硝酸盐氮的污染潜力。还评估了摄入受硝酸盐氮污染的地下水的健康风险。DRASTIC 模型的结果表明,旱地作物和草地具有较高的污染潜力,而森林、水库和住宅用地具有较低的污染潜力。校准后的 MT3D 模型反演确定了位于西部到西北部的高强度硝酸盐污染源(0.09-2.74kg/m(2)/year),到达监测井需要 2-5 年的传输时间。MT3D 的模拟结果还表明,硝酸盐-N 的连续和瞬时污染源的释放可能导致金门西部严重到中度硝酸盐污染,并危及地下水的家庭使用。与饮用受硝酸盐污染的地下水有关的潜在非致癌风险的慢性健康危害商(HQ)表明,评估的 95%百分位 HQ 为 2.74,这表明饮用水中的硝酸盐对岛上居民构成了潜在的非癌症风险。应采取纠正措施,包括保护地下水补给区和减少进入含水层的农业和非农业氮源数量,特别是在金门西部,以确保地下水资源的可持续利用。