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Impact of the shift from groundwater to surface water irrigation on aquifer dynamics and hydrochemistry in a semi-arid region in the south of Portugal.

机译:葡萄牙南部半干旱地区从地下水灌溉到地表水灌溉对含水层动力学和水化学的影响。

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In semi-arid regions, the shift from locally extracted groundwater to regionally supplied surface water for irrigation can have a large impact on the aquifer dynamics and hydrochemistry, as is shown for an area of intensive citrus culture in the south of Portugal. Studying the changes that occur is important, particularly in the light of European and national policies that seek to preserve the quality of groundwater and the involved ecosystems. In September 2005, the application of Nitrates Directive 91/676/CEE to the study area led to its designation as a vulnerable zone and the obligation of implementing measures that reduce the risk of nitrate leaching to groundwater. In addition, the area is bordered to the south by the internationally recognized ecosystem of the Ria Formosa lagoon, which requires a careful management of water quantity and quality. This article shows that the substitution of the irrigation source indirectly caused the reduction of the nitrogen load on soil and groundwater. The study is based on a large number of groundwater head and quality data gathered over the past decade. It is observed that irrigation with surface water triggered freshening of the upper aquifer, inverting a long-existing trend of increasing groundwater salinities caused by irrigation with local groundwater. The occurrence of both phenomena in the same aquifer is rather unique and is simulated with the hydrogeochemical software PHREEQC. In terms of aquifer dynamics, a sharp rise of the water table is observed, together with an almost complete attenuation of its interseasonal oscillations. A further rise, which is to be expected in years with average or higher rainfall, could cause the water table to enter the root zone of the citrus trees in some areas, with potentially negative consequences. Therefore, an integrated mixed-source irrigation system using both surface and groundwater is highly recommended..
机译:在半干旱地区,从局部提取的地下水向区域供应的地表灌溉用水的转移可能会对含水层的动力学和水化学产生重大影响,如葡萄牙南部密集柑橘种植区所示。研究发生的变化非常重要,尤其是考虑到欧洲和国家旨在维护地下水和相关生态系统质量的政策。 2005年9月,《硝酸盐指令91/676 / CEE》在研究区域中的应用导致其被指定为脆弱地区,并有义务采取措施降低硝酸盐向地下水中的淋溶风险。此外,该地区与国际公认的Ria Formosa泻湖生态系统接壤,需要对水的数量和水质进行精心管理。本文表明,灌溉源的替代间接减少了土壤和地下水的氮负荷。该研究基于过去十年中收集的大量地下水水头和质量数据。可以看出,用地表水灌溉触发了上层含水层的新鲜化,扭转了长期以来由局部地下水灌溉引起的盐度增加的趋势。两种现象在同一含水层中的发生是非常独特的,并使用水文地球化学软件PHREEQC进行了模拟。在含水层动力学方面,观察到地下水位急剧上升,同时其季节间振荡几乎完全减弱。在降雨水平更高或更高的年份中,预计还会有进一步的上升,这可能导致地下水位进入某些地区的柑橘树的根部区域,并可能带来负面影响。因此,强烈建议同时使用地表水和地下水的混合源灌溉系统。

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