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    巴丹吉林沙漠盐湖水面蒸发与矿化度协同关系探究

    • 摘要: 【研究目的】巴丹吉林沙漠盐湖蒸发研究对区域水资源管理和生态系统维护意义重大,但现有研究存在难度大、结果差异显著的问题。本研究旨在揭示盐湖水面蒸发与矿化度协同关系,为湖泊蒸发及区域水循环研究提供数据和理论支持。【研究方法】本研究在巴丹西湖西北侧开展原位蒸发试验,以巴丹东、西湖水为基准配制不同矿化度水样,利用 Φ20 小型蒸发皿在 2017 年 9 月 - 2018 年 8 月进行观测,通过特定数据处理方法分析数据。【研究结果】研究结果显示:相同环境和矿化度条件下,从非冻结期到冻结期日蒸发量逐渐减小;月蒸发量4-9月较大,占全年 80% 以上,冬季冻结期(12 - 2 月)显著降低,仅占全年约 5%,且矿化度升高会使水面蒸发量降低。在一定矿化度范围内,水体矿化度与蒸发量呈显著负相关。蒸发量较小的时段(春、冬及相应月份)二者关系符合线性模型,蒸发量大的时段(夏、秋及相应月份)符合指数模型,年蒸发量符合指数模型(y=3436.2e−0.097x),即矿化度达到研究区湖水矿化度的最大值 441.5g/L,水面蒸发仍会发生。此外,引入高矿化度水面蒸发折算系数,发现矿化度对蒸发量影响存在临界值,高于此值时,矿化度越高,蒸发量越小。【结论】巴丹吉林沙漠盐湖蒸发量存在季节变化规律,在一定矿化度范围内,与矿化度呈负相关且在不同时段符合不同模型,矿化度对蒸发量影响存在临界值。本研究成果可为该区域水资源管理和生态保护提供了重要依据。

       

      Abstract: 【Objectives】The study of evaporation in the salt lakes of the Badain Jaran Desert is of great significance for regional water resource management and ecosystem maintenance. However, existing studies face difficulties and show significant differences in results. This research aims to reveal the synergistic relationship between water surface evaporation and salinity in salt lakes, providing data and theoretical support for lake evaporation and regional water cycle research.【Methods】An in-situ evaporation experiment was conducted on the northwest side of Badanxi Lake. Different salinity water samples were prepared based on the water from Badandong and Badanxi Lakes. A Φ20 small evaporation pan was used for observations from September 2017 to August 2018, and the data were analyzed through specific data processing methods.【Results】The research results show that under the same environmental and salinity conditions, the daily evaporation amount gradually decreases from the non-freezing period to the freezing period. The monthly evaporation amount is relatively large from April to September, accounting for more than 80% of the annual total, and significantly decreases during the winter freezing period (December - February), accounting for only about 5% of the annual total. Moreover, an increase in salinity leads to a decrease in the water surface evaporation amount. Within a certain range of salinity, there is a significant negative correlation between water salinity and evaporation. In periods with low evaporation (spring, winter, and corresponding months), the relationship between them conforms to a linear model, while in periods with high evaporation (summer, autumn, and corresponding months), it conforms to an exponential model. The annual evaporation amount conforms to the exponential model (y = 3436.2e−0.097x). Even when the salinity reaches the maximum value of 441.5 g/L in the study area, water surface evaporation still occurs. In addition, by introducing the conversion coefficient of high-salinity water surface evaporation, it was found that there is a critical value for the influence of salinity on evaporation. When the salinity is higher than this critical value, the higher the salinity, the lower the evaporation amount.【Conclusions】There are seasonal variation patterns in the evaporation amount of salt lakes in the Badain Jaran Desert. Within a certain range of salinity, it has a negative correlation with salinity and conforms to different models in different periods. There is a critical value for the influence of salinity on evaporation. The research results can provide an important basis for regional water resource management and ecological protection.

       

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