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首页> 外文期刊>Pollution research >HYDROCHEMICAL STATUS OF SAMBHAR SALT LAKE: A RAMSAR SITE
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HYDROCHEMICAL STATUS OF SAMBHAR SALT LAKE: A RAMSAR SITE

机译:桑巴尔盐湖的水化学状态:RAMSAR站点

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Sambhar lake, a Ramsar site; wetland of international importance, has a surface area of 190 Sq km and lies in 27° 58 N, 75° 55 E. It is a shallow Athalassic and Polymictic lake with depth varying between 9.3 cm to 3m. It can be categorized as a playa as it inundates during rainy season and dries up during summers. The lake exhibits considerable temporal changes in volume and surface area. The hydro-chemical study was carried out for a period of one year; Feb 2012 to Jan 2013 and covered all seasons and one complete hydrological cycle. The total rainfall received during the study period was 603 mm. Average Ambient and Water temperature fluctuated between 18℃ to 42.7℃ and 10.5 to 34℃ and has prominent influence on salinity and water density of the lake. Results show that the lake is halo-alkaline with pH and Salinity ranging between 8.13 to 8.93 and 0.34% to 158% respectively. Salinity in the lake results from evaporative concentration of ions leached from its drainage basin. Alkalinity of the lake water was high with Carbonate and Bicarbonate values falling between 249 to 910 and 849 to 2191 mg/L respectively. Density of lake water varied between 1.5 to 8 Be (Baume). Density is the prime factor controlling salt crystallization. Hardness was recorded between 79 to 660 mg/L. Dissolved Oxygen content fell between 0-8.6 mg/L and were inversely correlated to salinity. Free CO_2 was always absent owing to carbonate dominance. Nitrate and Phosphate appeared in all the samples during the course of study and showed values between 1.3 to 9.6 ug/L and 3.9 to 15.1 ug/L respectively. NaCl Content of lake brine was 98.31%, 98.56% and 98.80% in the months of Oct, Nov and Dec-12 respectively. Dominating cation is Na~+ and dominating anion is Cl: The total annual yield of Salt was 2.2 lac tons.
机译:Sambhar湖,Ramsar遗址;具有国际重要性的湿地,表面积为190 Sq km,位于27°58 N,75°55E。这是一个浅层的Athalassic和Polymictic湖,深度在9.3 cm至3m之间变化。它可以归类为普拉亚(Playa),因为它在雨季泛滥而在夏天变干。该湖在体积和表面积方面表现出相当大的时间变化。水化学研究进行了一年; 2012年2月至2013年1月,涵盖所有季节和一个完整的水文循环。在研究期间,总降雨量为603毫米。平均环境温度和水温在18℃至42.7℃和10.5至34℃之间波动,对湖泊的盐度和水密度具有显着影响。结果表明,该湖为碱性盐湖,pH和盐度分别为8.13至8.93和0.34%至158%。湖泊中的盐度是从流域沥出的离子蒸发浓缩而产生的。湖泊水的碱度很高,碳酸盐和碳酸氢盐值分别介于249至910和849至2191 mg / L之间。湖泊水的密度在1.5至8 Be(波美)之间变化。密度是控制盐结晶的主要因素。记录的硬度在79至660 mg / L之间。溶解氧含量在0-8.6 mg / L之间,与盐度成反比。由于碳酸盐占主导地位,始终不存在游离的CO_2。在研究过程中,所有样品中均出现硝酸盐和磷酸盐,其值分别在1.3至9.6 ug / L和3.9至15.1 ug / L之间。 10月,11月和12月12日的湖盐水中的NaCl含量分别为98.31%,98.56%和98.80%。主要的阳离子为Na〜+,主要的阴离子为Cl:盐的年总产量为2.2 lac吨。

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