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Analysis of groundwater–lake interaction by distributed temperature sensing in Badain Jaran Desert, Northwest China

机译:基于分布温度感测的巴丹吉林沙漠地下水与湖泊相互作用分析

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The Badain Jaran Desert is the second largest desert of China with a total area of 49 200 km2. At least 72 perennial lakes are scattered throughout the desert, sustaining a unique desert–lake ecosystem. Groundwater of various origins was believed to play an essential role in maintaining those desert lakes, but hydrological measurements are lacking due to difficult field conditions. This study applied the distributed temperature sensing technique to continuously measure temperature variations in one of the desert lakes – the Badain Lake – to identify groundwater discharge to the lake based on the temperature differences between groundwater and lake water. Because temperature may be influenced by various unforeseen and temporary factors, it is critical to discern those factors that may affect the temperature such as solar radiation and vertical temperature stratification and to ensure that the temperature variations of the lake water as detected by the distributed temperature sensing are mainly caused by groundwater discharge. A time window was identified during which the groundwater discharge is the dominant factor that determines the temperature pattern of the lake water. The results show that the temperature near the eastern and southeastern lakeshore of the eastern Badain Lake is colder than the average, indicating that this area is the main groundwater discharge zone. Near the northwestern lakeshore adjacent to a sand dune, a weak cold abnormal area was identified, indicating that the sand dune is another recharge source to the lake through channelling the local precipitation toward the lake. The contribution from the sand dune, however, appeared to be less than that from the regional groundwater flow. This study provides the first identification of the temperature abnormal areas, which imply groundwater discharges into desert lakes and contributes to a better understanding of the unique desert–lake ecosystem. Copyright © 2015 John Wiley & Sons, Ltd.
机译:巴丹吉林沙漠是中国第二大沙漠,总面积为49 200 km2。至少72个常年湖泊遍布整个沙漠,维持了独特的沙漠湖生态系统。人们认为,各种来源的地下水在维护这些沙漠湖泊中起着至关重要的作用,但由于田间条件艰苦,缺乏水文测量。这项研究应用了分布式温度传感技术,连续测量了一个沙漠湖泊-巴丹湖的温度变化,从而根据地下水与湖水之间的温差确定了向该湖排放的地下水。由于温度可能会受到各种不可预见和临时性因素的影响,因此辨别那些可能影响温度的因素(例如太阳辐射和垂直温度分层),并确保通过分布式温度感应检测到的湖水温度变化至关重要。主要是由地下水排放引起的。确定了一个时间窗口,在该时间窗口中,地下水流量是决定湖泊水温模式的主要因素。结果表明,巴丹湖东部和东部湖岸附近的温度比平均温度低,表明该地区是主要的地下水排放区。在靠近沙丘的西北湖岸附近,发现了一个弱冷异常区,这表明沙丘是通过将局部降水引向湖面的另一个补给源。然而,沙丘的贡献似乎小于区域地下水流量的贡献。这项研究首次发现了温度异常区域,这暗示着地下水排入沙漠湖泊,并有助于更好地了解独特的沙漠湖生态系统。版权所有©2015 John Wiley&Sons,Ltd.

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