REBAIXAMENTO RESIDUAL DO AQUÍFERO GUARANI NA CIDADE DEMARÍLIA, SP.

E. C. Prandi, Rafael Carrion Montero, Suraya Damas de Oliveira Modaelli, João Carlos Polegato, João Edilson De Oliveira Filho, Pedro Lifter Rodrigues Prandi
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Abstract

There are four wells drilled in Marilia extracting water from Guarani aquifer, confined in the area that was studied. All of these wells have more than a thousand meters deep. After two decades of operation, the piezometric levels of these wells showed high residual drawdown in order of 50 meters. On this paper we present the theoretical foundations that can explain such downgrades. These downgrades are regional and can take the loss of wells operated if these levels continue going down. Maps are presented to show the difference between the original levels and current levels.
在马里亚有四口井从瓜拉尼含水层取水,被限制在研究区域内。所有这些井都有一千多米深。经过20年的运行,这些井的压力水平显示出50米左右的高残余压降。在本文中,我们提出了可以解释这种降级的理论基础。这些降级是区域性的,如果这些水平继续下降,可能会造成作业井的损失。地图显示了原始关卡和当前关卡之间的差异。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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