首页> 外文期刊>Journal of South American earth sciences >Analysis of groundwater and river stage fluctuations and their relationship with water use and climate variation effects on Alto Grande watershed, Northeastern Brazil
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Analysis of groundwater and river stage fluctuations and their relationship with water use and climate variation effects on Alto Grande watershed, Northeastern Brazil

机译:地下水和河流波动及其与水利用和气候变化影响的地下水和气候变化影响,巴西东北部

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Sustainable use of water resources on the behavior of groundwater table and surface water level variations, especially in phreatic sedimentary aquifers, where a strong interaction between stream flow and groundwater normally takes place. In the present study, precipitation, water level fluctuation, river flow and pivot installation data from an important agricultural frontier with an increasing water use for irrigated agriculture and a downward precipitation trend were compared with surface and water level fluctuation monitoring data. The main purpose was to assess possible impacts on the aquifers and to analyze the variation in groundwater table and surface water levels due to long-term downward precipitation trend (climate variation effects) and increasing water demand (irrigation). A growing number of central pivots installed for irrigation are withdrawing water from the Urucuia Aquifer System (UAS) in western Bahia State, Northeastern Brazil, one of the leading agricultural frontiers of the world. Field surveys provided hydrogeological aspects that led to the construction of a hydrogeological conceptual model. Monitoring groundwater and surface water through Brazilian Geological Survey's Integrated Groundwater Monitoring Network (RIMAS-CPRM), satellite images and Hydrological Information System (HidroWeb-ANA) network formed the databases for the study. This data was compared with rainfall data and evolution of irrigated areas captured by satellite image analysis. Results indicate that reduction of rainfall volumes from 1990 to 2018 in the headwaters of Alto Grande basin, due to cyclic droughts, and an increase in surface and groundwater exploitation due to flourishing agribusiness activity has caused a considerable groundwater level drawdown. The drawdown of up to 6.63 m points to the need of strong management actions, which should provide a long-term sustainable use of water resources (superficial and underground) within Alto Grande watershed. This study is part of the actions undertaken to provide the scientific and technical basis to secure the availability of water and a sustainable agricultural activity, since an important part of the Cerrado, the Brazilian savanna ecosystem, and considerable proportion of Sao Francisco river flow, lies in the study area.
机译:可持续利用水资源对地下水位和地表水位变化的行为,尤其是潜水沉积含水层,其中流流程与地下水之间的强烈相互作用通常发生。在目前的研究中,与灌溉农业的不断增长的水平和向下降水趋势增加了来自重要农业前沿的降水,水位波动,河流流量和枢轴安装数据,以及表面和水位波动监测数据。主要目的是评估由于长期向下降水趋势(气候变化效应)和水需求(灌溉)增加导致地下水位和地表水位的可能影响。越来越多地安装用于灌溉的中央枢轴是从巴西东北北部的巴西西部的乌斯苏西含水层(UAS)的水中取水,是世界领先的农业领先者之一。现场调查提供了水文地质方面,导致了水文地质概念模型的构建。通过巴西地质调查的集成地下水监测网络(RIMAS-CPRM),卫星图像和水文信息系统(HIDROWEB-ANA)网络来监测地下水和地表水,形成了该研究的数据库。将该数据与卫星图像分析捕获的灌溉区域的降雨数据和演变进行了比较。结果表明,由于循环干旱,1990年至2018年降雨量减少了1990年至2018年,由于循环干旱,由于繁荣的农业综合性活动导致的地表和地下水开采的增加导致了相当大的地下水位净化。高达6.63米的降价指出需要强大的管理行动,这应该在阿尔托格兰德水域内提供长期可持续利用水资源(肤浅地下)。本研究是为确保水和可持续农业活动提供科学和技术基础的行动的一部分,以获得水平和可持续的农业活动,自哥拉多队的重要组成部分,巴西大草原生态系统和大部分圣弗朗西斯科河流,谎言在研究区。

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