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Groundwater characteristics within loessic deposits: the coastal springs of Los Acantilados, Mar del Plata, Argentina

机译:黄土沉积物中的地下水特征:阿根廷马德普拉塔的洛斯阿坎蒂拉多斯沿海温泉

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摘要

The urban growth of the southern neighborhoods of Mar del Plata City provoked significant changes in the groundwater balance of the loessic sequences. These regional loessic levels with a significant portion of volcanic ash layers were reported subject to fluoride and nitrate concentrations. Residential houses pump from sands located 70m depth and withdraw the sewages to depths less than 5m. These effects cause significant local and seasonal (summer) increments of the water table outcropping via springs at certain unconformities of the coastal cliffs. A mathematical model was applied to analyze the water level lowering at the productive levels, while there is a decrease in the quality of the upper levels subject to waste discharges. Much of this groundwater flow is concentrated in unconformities between different types of sediments. Human activities have affected the aquifer dynamics increasing the groundwater pumping rates and the return velocity of the sewages. This should be considered in the management strategies of coastal hydric resources.
机译:马德普拉塔市南部居民区的城市发展引起了黄土层序地下水平衡的重大变化。据报道,这些地区的黄土层中有大量的火山灰层,受氟化物和硝酸盐浓度的影响。住宅从深度为70m的沙子中抽水,并将污水排到深度小于5m的地方。这些影响导致沿沿海悬崖某些不整合面的泉水露头显着的局部和季节性(夏季)增量。应用了一个数学模型来分析生产水平的水位下降,而受废物排放影响的较高水位的质量却下降了。这种地下水流大部分集中在不同类型沉积物之间的不整合面中。人类活动已经影响了含水层的动力学,从而增加了地下水的抽取速度和污水的回流速度。在沿海水文资源的管理策略中应考虑到这一点。

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