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Sambhar salt lake: a hydrochemical approach

机译:桑巴尔盐湖:一种水化学方法

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Sambhar salt lake, is an Athalassic and endorheic lake and is always changing. Water spread Area, depth, temperature and hydro-chemical conditions vary with season and year to year. Shoreline of the lake shifts dramatically as it lies in a broad and relatively flat basin. The present work focuses on the hydro-chemical study carried out during 2013. Total rainfall during the period was 348 mm. Average Temperature variations were from 7 to 37°C, pH 6.54 to 8.87, water Density 3-25 Be, Alkalinity Nil-2670 mg/L, Hardness from 28-115 mg/L, Salinity 0.53-162.21% and Dissolved oxygen from Nil-3.6mg/L. Total anoxic condition prevailed during most of the months while Free Carbon di-oxide was recorded only once during July-13 value being 25 ppm. Nutrient were in low concentration as Nitrate and Phosphate fluctuated between 1.16 -7.21 mug/L and 1.9-8.94 mug/L. NaCl content in lake brine was 98.67% in Jan-13 while post monsoon the values lowered to 88.56%. A steady increase in NaCl concentration was recordedagain reaching 98.27% in Dec-13.
机译:桑巴哈尔盐湖是无生气和内吸性湖,并且一直在变化。水传播面积,深度,温度和水化学条件随季节和年份而变化。由于湖位于宽阔而相对平坦的盆地中,其海岸线发生了巨大变化。目前的工作重点是在2013年进行的水化学研究。该期间的总降雨量为348 mm。平均温度变化为7至37°C,pH为6.54至8.87,水密度为3-25 Be,碱度为Nil-2670 mg / L,硬度为28-115 mg / L,盐度为0.53-162.21%,Nil为溶解氧-3.6毫克/升。在大多数月份中,总缺氧情况普遍存在,而在7月13日期间仅记录一次游离二氧化碳值为25 ppm。由于硝酸盐和磷酸盐在1.16 -7.21马克杯/升和1.9-8.94马克杯/升之间波动,因此营养素浓度较低。 1月13日,湖盐水中的NaCl含量为98.67%,而在季风后,该值降至88.56%。在12月13日,NaCl浓度再次稳定增长,达到98.27%。

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