Managed phreatic zone recharge for irrigation and wastewater treatment

IF 5.9 1区 地球科学 Q1 ENGINEERING, CIVIL
Darrell W.S. Tang , Sjoerd E.A.T.M. Van der Zee , Dominique M. Narain-Ford , Gé A.P.H. van den Eertwegh , Ruud P. Bartholomeus
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Abstract

Managed phreatic zone recharge with marginal water, using (existing) drainage systems, raises the water table and increases water availability for crops. This is a newly developed method of freshwater conservation and marginal water treatment and disposal, but risks crop and environmental contamination. The fate of contaminants of emerging concern (CECs) within the irrigated water is addressed. We introduce numerical and analytical models, inspired loosely by a field site where treated domestic wastewater is used for subsurface irrigation. The treated wastewater would otherwise have been discharged into rivers, thereby spreading downstream. Model results show that minimal amounts of CECs are transported to deeper aquifers. Crops are not contaminated, except during dry years where small amounts of mobile CECs rise to the root zone, but then only directly above each irrigation drain. Under an annual precipitation surplus, less-mobile solutes are thus unlikely to ever enter the root zone. The primary mechanism of solute transport is lateral advection within the phreatic aquifer. Despite spatio-temporal heterogeneity in water flux magnitudes and directions, contaminant retardation does not significantly alter mass balance outcomes, only how fast it gets there. Therefore, persistent CECs pose the greatest risks, though overall environmental and crop contamination risks appear low. To maximize complementarity with subsurface irrigation systems, future advances in water treatment technologies should focus on removing persistent CECs. However, the system may be unsuitable for climates with annual precipitation shortages, as CECs may accumulate in the root zone and crops.

Abstract Image

管理潜水区补给用于灌溉和废水处理
利用(现有的)排水系统,用边际水补给有管理的潜水区,提高了地下水位,增加了作物的可用水性。这是一种新开发的淡水保护和边际水处理和处置方法,但有可能污染作物和环境。解决了灌溉水中出现的污染物(CECs)的命运。我们引入了数值和分析模型,灵感来自于一个使用处理过的生活废水进行地下灌溉的现场。否则,处理过的废水就会排入河流,从而向下游扩散。模型结果显示,极少量的cec被输送到较深的含水层。作物不受污染,除非在干旱年份,少量流动的cec上升到根区,但只在每个灌溉排水沟的正上方。在年降水过剩的情况下,流动性较差的溶质因此不太可能进入根区。溶质运移的主要机制是潜水含水层内的横向平流。尽管水通量的大小和方向在时空上存在异质性,但污染物阻滞不会显著改变质量平衡的结果,只会改变它到达那里的速度。因此,尽管总体环境和作物污染风险似乎较低,但持续存在的ces构成的风险最大。为了最大限度地与地下灌溉系统互补,水处理技术的未来发展应侧重于去除持久的CECs。然而,该系统可能不适合年降水短缺的气候,因为cec可能在根区和作物中积累。
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来源期刊
Journal of Hydrology
Journal of Hydrology 地学-地球科学综合
CiteScore
11.00
自引率
12.50%
发文量
1309
审稿时长
7.5 months
期刊介绍: The Journal of Hydrology publishes original research papers and comprehensive reviews in all the subfields of the hydrological sciences including water based management and policy issues that impact on economics and society. These comprise, but are not limited to the physical, chemical, biogeochemical, stochastic and systems aspects of surface and groundwater hydrology, hydrometeorology and hydrogeology. Relevant topics incorporating the insights and methodologies of disciplines such as climatology, water resource systems, hydraulics, agrohydrology, geomorphology, soil science, instrumentation and remote sensing, civil and environmental engineering are included. Social science perspectives on hydrological problems such as resource and ecological economics, environmental sociology, psychology and behavioural science, management and policy analysis are also invited. Multi-and interdisciplinary analyses of hydrological problems are within scope. The science published in the Journal of Hydrology is relevant to catchment scales rather than exclusively to a local scale or site.
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