The Bhagirathi streams are a major source of fresh water in the form of glaciers meltwater streams and monsoonal phenomena. The watersheds of the Bhagirathi basin is trending towards water chemistry as well as changing morphological and land cover features due to the climatic and anthropogenic activity. To understand seasonal hydrochemistry and the impact of watershed morphology a total of 32 stream water samples collected during post and pre-monsoon seasons. The bicarbonate is the most dominant ion in the streams water followed by Na+, Ca+2, SO4-2, Cl-, SiO2, K+, and Mg+2. The results were found that HCO3- is in very good correlation with the base cations Ca+2, Mg+2 and Na+ in both pre and post-monsoon seasons. The higher concentration of HCO3- in Bhagirathi stream water and its positive correlation with Ca+2 and Mg+2 indicates that their main source comes from the dissolution of carbonates. Most of the hydro-chemical parameters (EC, pH) and ions (Ca+2, Mg+2, Na+, K+, HCOf-, SO4-2, Cl-, and F-) indicated a relationship with morphometric and land cover and these parameters vary with the season. It is observed that elevation, relief, basin length, area, and perimeter impact on stream water chemistry. Due to the processes of chemical weathering, mixing of the groundwater, snow/glacier meltwater, and surface water components responsible for the seasonal variation in the hydrochemistry of streams. Impact of agriculture land is more dominant than any land cover followed by barren land and glacier cover that influence the hydrochemistry of streams.
Events of substantial aeolian dust deposition on seasonal snow covers and glaciers are a common phenomenon in mid-latitude, (subtropical) and even high arctic regions. Such events are emerging as important environmental issues in view of their glacio-chemical and glaciometeorological aspects. The atmosphere, an integral and huge component of biosphere, receives inputs from myriad anthropogenic activities including expanding industrial establishments. Varied emissions, inter alia, noxious gases and particulate pollutants have inherent potential to travel long
The present paper deals with variability in snow chemistry of various sites spread in six districts of the Kashmir Himalayan valley, experiencing frequent snow fall during winter ( Dec.-Feb). Chemical composition of fresh snow samples shows wide changes in pH (5.8-7.3), dissolved oxygen content (22-26 mg L -1 ), and total alkalinity (2-3 mg L -1 ). The levels ( mg L -1 ) of calcium (13.3-28 ), magnesium (8-12 ), chloride (15-30), sulphate (2-8), silicate (1-4) and nitrate (1.9-3.9) differed considerably. The study makes a strong plea for in-depth investigations of snow chemistry of littleexplored Himalayan region, useful for assessing the impact of environmental pollution.
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