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干湿交替期对两个浅层地中海湖泊长期季节性磷氮收支的影响。

Impact of alternating wet and dry periods on long-term seasonal phosphorus and nitrogen budgets of two shallow Mediterranean lakes.

机构信息

Middle East Technical University, Limnology Laboratory, Department of Biology, Universiteler Mahallesi, Dumlupinar Bulvarı, No. 1, 06800 Ankara, Turkey.

Çankırı Karatekin Üniversitesi, Department of Forest Engineering, Yeni Mah. Bademlik Cd., Çankırı, Turkey.

出版信息

Sci Total Environ. 2016 Sep 1;563-564:456-67. doi: 10.1016/j.scitotenv.2016.04.028. Epub 2016 May 3.

Abstract

The water balance, with large seasonal and annual water level fluctuations, has a critical influence on the nitrogen and phosphorus dynamics of shallow lakes in the semi-arid climate zone. We constructed seasonal water and nutrient budgets for two connected shallow lakes, Lakes Mogan and Eymir, located in Central Anatolia, Turkey. The study period covered 20years with alternations between dry and wet years as well as restoration efforts including sewage effluent diversion and biomanipulations in Lake Eymir. Both lakes experienced a 1-2m water level drop during a drought period and a subsequent increase during the wet period, with seasonal water level fluctuations of 0.60 to 0.70m. During wet years with high water levels, small seasonal differences were observed with a nutrient peak in spring caused by external loading and nutrient loss via retention during summer. During years with low water levels, nutrient concentrations increased due to internal and external loading, exacerbated by evaporative water loss. In Lake Eymir, a shift to eutrophic conditions with turbid water occurred under low water level conditions and consequent internal loading of P from the sediment, causing high nutrient concentrations in summer. Our results indicate a threat of lakes drying out in the semi-arid climate zone if evaporation increases and precipitation decreases as anticipated from the global climate change predictions. In addition, our results show the influence of the water balance on the eutrophication of shallow lakes in the Mediterranean climate zone and highlight the ultimate consequences for lake management.

摘要

水量平衡对半干旱气候区浅水湖泊的氮磷动态具有重要影响,其具有大的季节性和年际水位波动。我们为位于土耳其中安纳托利亚的两个相连的浅水湖莫干湖和埃米尔湖构建了季节性水量和养分收支。研究期间包括 20 年,经历了干湿年交替以及包括污水排放改道和埃米尔湖生物操纵在内的恢复工作。两个湖泊在干旱期间水位下降 1-2m,随后在湿润期间增加,季节性水位波动为 0.60-0.70m。在高水位的湿润年份,观察到春季由于外部负荷和夏季通过滞留导致的营养物峰值引起的小的季节性差异。在低水位年份,由于内部和外部负荷增加,再加上蒸发导致的水分损失,营养物浓度增加。在埃米尔湖,在低水位条件下,水变得浑浊,发生富营养化,随之而来的是来自沉积物的 P 的内部负荷,导致夏季营养物浓度升高。我们的结果表明,如果蒸发增加,降水减少,如全球气候变化预测的那样,半干旱气候区的湖泊有干涸的威胁。此外,我们的结果还表明水量平衡对地中海气候区浅水湖泊富营养化的影响,并突出了对湖泊管理的最终影响。

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