yeŞilirmak河(土耳其)桤木坝湖温度、溶解氧分层及其gis图

Fatih Polat, Tarık Dal, İ. Karataş, E. Buhan
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引用次数: 1

摘要

对位于托喀省阿尔穆斯区的阿尔穆斯大坝湖泊的温度和溶解氧参数进行了季节性测定。将测量参数的结果与洲际水源水质分类的值进行比较,确定了桤木坝湖的水质等级。采用双因素方差分析分析各物理参数的空间和季节变化。根据洲际水源水质分类,以温度(14.30±7.44C°)、溶解氧(10.15±2.67mg/L)为标准,Almus Dam Lake为一级水质。通过对季节温深剖面的分析,发现冬季停滞和春季和秋季垂直混合分别发生在1月和3月和春季5月和11月。7月和9月气温分层明显。在前10米、10 - 20米之间和20米以下,分别可以清楚地看到表层土、金属土(温跃层)和低表层土。为温度和溶解氧变量创建了具有空间和季节值的GIS地图。
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TEMPERATURE AND DISSOLVED OXYGEN STRATIFICATION IN ALMUS DAM LAKE ON YEŞILIRMAK RIVER (TURKEY) AND ITS GIS MAPS
The temperature and dissolved oxygen parameters of Almus Dam Lake located in the district Almus of province Tokat were seasonally determined at nine stations located along the lake. The water quality class of Almus Dam Lake was determined by comparing the results of our measured parameters with the values of Intercontinental Water Sources Quality Classification. The spatial and seasonal variations in physical parameters were analyzed with the Two-Way ANOVA, the relationships among these parameters. According to Intercontinental Water Sources Quality Classification, Almus Dam Lake has Class I water quality when considering parameters of temperature (14.30±7.44C°), dissolved oxygen (10.15±2.67mg/L. With the examination of seasonal temperature-depth profile, it was observed that winter stagnation and spring and fall vertical mixing occurred during the January and March and spring May and November, respectively. Temperature stratification was clearly observed during the July and September. Epilimnion, metalimnion (thermocline) and hypolimnion were well clearly visible at the first 10 meters, between 10–20 meters, and below 20 meters, respectively . GIS maps with spatial and seasonal values ​​ were created for temperature and dissolved oxygen variables.
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