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Factors that control the seasonal dynamics of the shallow lakes in the Pampean region, Buenos Aires, Argentina

机译:控制阿根廷布宜诺斯艾利斯Pampean地区浅湖季节性动态的因素

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Shallow lakes are distinctive aquatic ecosystems of the Pampean region. In this paper, climatic, morphometric and chemical-environmental aspects of six lacustrine bodies of the Salado River basin, Buenos Aires, are analyzed. The climatic variability of the region was estimated and linked to the behavior of each water body during the studied period (2017-2018); precipitations displayed deviations from the mean values, with periods of deficit in spring and summer, and excess in autumn. The analysis of satellite images showed a group of lakes with very low variation of the morphometric parameters because they have gates that keep the water level constant. On the contrary, those without anthropic intervention displayed a greater morphometric variability, since the water levels have been directly linked to local weather fluctuations. From a chemical-environmental perspective, changes were observed both at the regional (p = 0.015) and local (p = 0.0014) levels. Differences among sites cannot be characterized by a single variable but by a set of them. The dominant cation in the Pampean shallow lakes is the Na+ coming from the contact of groundwater with loessic sediments. Lakes showed a particular anionic dominance that not following a seasonal but a particular pattern. These are mainly linked to the characteristics of the substrate (presence of marine sediments or gypsum deposits). The great vulnerability of these environments to global and regional climatic changes, anthropic modifications and a large number of shallow lakes in the area, allow finding different scenarios (geomorphological, ecological, hydrogeological, etc.) to assess their vulnerability and predict their behavior against future climate scenarios in an economically important area for Argentine.
机译:浅湖是庞贝地区独特的水生生态系统。本文分析了布宜诺斯艾利斯萨洛多河流域的六个湖相湖泊的气候,形态和化学环境方面。在研究期间(2017-2018)估算了该区域的气候变化并将其与每个水体的行为联系起来;降水显示出与平均值的偏差,春季和夏季出现赤字时期,秋季则出现过剩时期。卫星图像分析显示,一组湖泊的形态参数变化很小,因为它们的闸门可保持水位恒定。相反,由于水位直接与当地的天气波动有关,因此没有人为干预的人表现出更大的形态变异性。从化学环境的角度来看,在区域(p = 0.015)和局部(p = 0.0014)水平上都观察到了变化。站点之间的差异不能用单个变量来表征,而只能用一组变量来表征。在Pampean浅湖中,主要的阳离子是Na +,它来自地下水与黄土沉积物的接触。湖泊显示出特定的阴离子优势,该趋势不是随季节变化而是特定的模式。这些主要与基质的特性(存在海洋沉积物或石膏沉积物)有关。这些环境极易受全球和区域气候变化,人类活动的改变以及该地区大量浅湖的影响,因此可以找到不同的情景(地貌,生态,水文地质等)来评估其脆弱性并预测其未来的行为阿根廷经济上重要地区的气候情景。

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