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首页> 外文期刊>Environment and Ecology >Comparative Limnological Studies of Barali Lake Hurda and Anasagar Lake Ajmer with Reference to Planktonic Population Dynamics
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Comparative Limnological Studies of Barali Lake Hurda and Anasagar Lake Ajmer with Reference to Planktonic Population Dynamics

机译:比较植物湖泊赫达和Anasagar Lake Ajmer参考浮游人口动力学研究

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Physico-chemical study are summarized. Air temperature varied between 28°C in winter to 35°C in summer 2015-16 and between 26°C in winter to 38°C in summer 2016-17. Water temperature was observed to be highest during summer 2016-17 (27° C) and lowest during winter 2015-16 (170Q;_The overall average value of air and water temperature was 36°C and 27.3 °C respectively. A good synchronization between temperature and dissolved oxygen was seen. Temperature showed a significant inverse relationshipwith dissolved oxygen. Such an inverse relationship has also been observed in monsoon 2015-16 and 2016-17; pH fluctuated between 6.9 to 8.5. The minimum pH was recorded in monsoon 2015-16 and 2016-17 which was mainly attributed to rain water after a longdry period and maximum pH was recorded during summer 2015-16 and 2016-17. According to the study, Anasagar Lake was characterized by low levels of dissolved oxygen with average value of 7.1 mg/1. The highest oxygen valuealso observed. Dissolved oxygen shows a significant negative relation with temperature, alkalinity, total hardness, electrical conductance, nitrate, phosphate, chloride, silicate and respiration. The observed high value of dissolved oxygen in winter dueto the high-solubility at low temperature and less degradation of organic matter. During the study, the highest value of total alkalinity was in summer 2015-16 and 2016-17 (590 mg/1) and lowest value was observed in winter 2005-06 (410 mg/1). Total alkalinity shows a positive relationship with temperature, pH, total hardness, TDS, conductivity, chloride and nitrate. The average value of total hardness during the study was lowest value of 315 mg/1 in 2015-16 and 2016-17 and highest value of 375 mg/1 in 2006-07.
机译:总结了物理化学研究。 2015-16夏季夏季冬季至35°C在冬季达到35°C,冬季26°C至38°C至38°C。观察到水温在2016-17夏季(27°C)和2015-16冬季最低(170Q;空气和水温的总平均值分别为36°C和27.3°C时,最低的水温最高。看到温度和溶解的氧气。温度显示出明显的溶解氧的反向关系。在季风2015-16和2016-17中也观察到这种反比关系; pH波动波动在6.9至8.5之间。在2015年季风记录最低pH- 16和2016-17主要归因于漫长的时期和2016-16〜2016-17夏季延长的雨水和最大pH值。根据该研究,anasagar湖的特点是低水平的溶解氧,平均值7.1毫克/ 1.观察到最高氧气值。溶解氧显示出与温度,碱度,总硬度,电导,硝酸盐,磷酸盐,氯化物,硅酸盐和呼吸有显着的阴性关系。在冬季冬季溶解氧的高值观察到的高溶解度低温下的有机物质降低。在研究期间,总碱度的最高值是2015-16和2016-17夏季(590mg / 1),2005-06冬季观察到最低值(410毫克/ 1)。总碱度显示与温度,pH,总硬度,TDS,导电性,氯和硝酸盐的阳性关系。在该研究期间总硬度的平均值在2015-16和2016-17期间的最低值为315 mg / 1,2006 - 07年的最高值为375 mg / 1。

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