首页> 外文会议>International Conference on Environmental Science and Technology >COMPARATIVE STUDY OF WATER LEVEL FOR GROUNDWATER RESOURCES MANAGEMENT AT URBAN AREA IN THE SOUTHEASTERN PART OF THE ARABIAN PENINSULA REGION
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COMPARATIVE STUDY OF WATER LEVEL FOR GROUNDWATER RESOURCES MANAGEMENT AT URBAN AREA IN THE SOUTHEASTERN PART OF THE ARABIAN PENINSULA REGION

机译:阿拉伯半岛地区城区地区地区水位对比较研究

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Groundwater resources are playing a vital role in the sustainability and development of the natural resources of the United Arab Emirates (UAE). In previous decades, the studied area in the southeastern part of the Arabian Peninsula region and the UAE has witnessed intensive developments and urban constructions, which have led to water demand increasing for farming, landscaping, as well as for domestic uses. The study area belongs to quaternary and limestone aquifer. The quaternary aquifer is composed of sand, gravel, silt as well as intercalated clay and shale layers. However, the limestone aquifer is represented by carbonate rocks as well as interbedded shale, clay and evaporate deposits. The main objectives of this study are to investigate groundwater condition represented by water level fluctuation and to analyze the setting of water level and its possible environmental risk. The objectives of this study were achieved by comparing water levels in 2010 and 2014.The water levels within the study area have risen to be between 2.3 m to 15 m from the ground surface. The results showed that the water levels are not uniform, rather than vary from one zone to another depending on the nature of the soil, sources of recharge and the population growth. The groundwater rising phenomenon in some zones is due to the inability of the aquifer to store and transmit more water due to weak hydrological properties as well as the occurrence of perched layers at the shallowest depths. By contrast, the deepest groundwater levels may reflect the impact of excessive pumping from the aquifer and improper well design. Additionally, the water level fluctuations in the study area resulted from seasonal rainfall and the stream runoff, which takes place in winter, and increase in temperature associated with semi-arid conditions in summer season. The outcomes of this study may be regarded as an early warning for the stockholders and decision makers in the municipality for consideration ahead of licensing of new buildings.
机译:地下水资源在阿拉伯联合酋长国(阿联酋)的自然资源的可持续发展和发展中发挥着重要作用。在过去的几十年中,阿拉伯半岛地区东南部的研究区和阿拉伯联合酋长国都目睹了密集的发展和城市建筑,导致农业,景观以及国内使用的水需求增加。研究区域属于四季和石灰岩含水层。第四纪含水层由沙子,砾石,淤泥以及插入粘土和页岩层组成。然而,石灰石含水层由碳酸盐岩和粘土,粘土和蒸发沉积物代表。本研究的主要目标是调查水位波动所代表的地下水条件,并分析水位的设定及其环境风险。通过比较2010年和2014年的水平来实现这项研究的目标。研究区域内的水位距离地面的水位升高至2.3米至15米。结果表明,根据土壤的性质,充电来源和人口生长,水平不均匀,而不是从一个区域变化。某些区域的地下水上升现象是由于含水层的无法储存和传递更多的水,因此水文特性以及在最浅的深度处的栖息层的发生。相比之下,最深的地下水位可能反映过度泵送从含水层和不正确的设计的影响。此外,研究领域的水位波动由季节性降雨和冬季发生的河流径流,以及夏季半干旱条件的温度增加。本研究的成果可能被视为市政府和决策者在新建筑物许可前审议的股东和决策者的预警。

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