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首页> 外文期刊>Fresenius Environmental Bulletin >THE SALINITY PROBLEM AT YELKOMA LAGOON (YUMURTALIK-ADANA) AND ITS RESTORATION BY MIXING WITH FRESHWATER FROM CEYHAN RIVER
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THE SALINITY PROBLEM AT YELKOMA LAGOON (YUMURTALIK-ADANA) AND ITS RESTORATION BY MIXING WITH FRESHWATER FROM CEYHAN RIVER

机译:塞罕河Yelkoma泻湖(YUMURTALIK-ADAA)的盐度问题及其与淡水的混合修复

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摘要

The Yelkoma Lagoon located at Ceyhan River Delta has been significantly deteriorated due to dam construction activities that cause lower freshwater inputs. Compared to the Mediterranean (~40 ppt), high salinity of the Yelkoma Lagoon (up to 116.0 ppt), has adversely affected the ecological life in the lagoon as evidenced by the number of fish deaths. In addition to less freshwater input, high evaporation rates and structure of the inlet channel between the lagoon and the Mediterranean are determined as major causes of high salinities. In this study, we applied End-Member Mixing Analysis to calculate the monthly amount of freshwater that should be contributed from the Ceyhan River to the Yelkoma Lagoon to decrease salinity and ensure sustainability of ecological life and fisheries. As a first stage of the study, a conceptual hydrological model of the Yelkoma Lagoon has been developed based on water volume and its salinity. A bathymetric map of the lagoon was produced allowing measurement of the area and volume of each sector in the lagoon. Monthly salinities were obtained from field surveys for all components of mixing equations. The optimum salinity of the lagoon water has been foreseen to be between the salinity of the Ceyhan River and the Mediterranean. Based on the conceptual model and using a mass balance equation, contributions of saline and freshwater end-members were calculated. As a result of mixing calculations, monthly required flow-rates of freshwater from the Ceyhan River to the Yelkoma Lagoon were determined to be in the range of 0.199 m~3/s to 3.698 m~3/s. The calculated freshwater has been given to the lagoon since March 2009, and positive developments have been observed in terms of ecological life.
机译:由于大坝建设活动导致淡水输入量减少,位于杰伊汉河三角洲的叶尔科马泻湖已经严重恶化。与地中海(约40 ppt)相比,叶尔科马礁湖的高盐度(高达116.0 ppt)对泻湖的生态生活产生了不利影响,这可从鱼类死亡的数量中看出。除了较少的淡水输入外,高盐分的主要原因是高蒸发率和泻湖与地中海之间的进口通道结构。在这项研究中,我们应用了最终成员混合分析来计算从Ceyhan河到Yelkoma泻湖应提供的淡水的每月量,以减少盐度并确保生态生活和渔业的可持续性。作为研究的第一阶段,已经根据水量及其盐度开发了耶尔科马礁湖的概念性水文模型。绘制了泻湖的测深图,可以测量泻湖中每个扇区的面积和体积。从混合方程式所有组成部分的现场调查中获得了每月的盐度。预计泻湖水的最佳盐度介于Ceyhan河和地中海的盐度之间。基于概念模型并使用质量平衡方程,计算了盐水和淡水末端成员的贡献。作为混合计算的结果,从塞汉河到叶尔科马泻湖的淡水每月需求流量确定为0.199 m〜3 / s至3.698 m〜3 / s。自2009年3月以来,已计算出的淡水已被送入泻湖,在生态生活方面已观察到积极的发展。

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