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  • Kumar, RameshDepartment of Environmental Science, SBSR, Sharda University, Greater Noida, India (författare)

Hydro-geochemical analysis of meltwater draining from Bilare Banga glacier, Western Himalaya

  • Artikel/kapitelEngelska2019

Förlag, utgivningsår, omfång ...

  • 2019-02-09
  • Springer,2019
  • printrdacarrier

Nummerbeteckningar

  • LIBRIS-ID:oai:DiVA.org:ltu-72835
  • https://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-72835URI
  • https://doi.org/10.1007/s11600-019-00262-wDOI

Kompletterande språkuppgifter

  • Språk:engelska
  • Sammanfattning på:engelska

Ingår i deldatabas

Klassifikation

  • Ämneskategori:ref swepub-contenttype
  • Ämneskategori:art swepub-publicationtype

Anmärkningar

  • Validerad;2019;Nivå 2;2019-04-12 (johcin)
  • The changing climate is affecting the melting process of glacier ice and snow in Himalaya and may influence the hydro-geochemistry of the glacial meltwater. This paper represents the ionic composition of discharge from Bilare Banga glacier by carrying out hydro-geochemical analysis of water samples of melting season of 2017. The pH and EC were measured on-site in field, and others parameters were examined in the laboratory. The abundance of the ions observed in meltwater has been arranged in decreasing order for cations as Ca2+ > Mg2+ > Na+ > K+ and for anions as HCO3− > SO42− > Cl− > NO3−, respectively. Analysis suggests that the meltwater is mostly dominated by Ca2+ and HCO3−. It has been observed that the ionic concentration HCO3− is dominant and Cl− is the least in the catchment. Piper plot analysis suggests that the chemical composition of the glacier discharge not only has natural origin but also has some anthropogenic input. Hydro-geochemical heterogeneity reflected the carbonate-dominated features (Ca2+–HCO3−) in the catchment. The carbonate weathering was found as the regulatory factor to control the chemistry of the glacial meltwater due to the high enrichment ratio of (Ca2+ + Mg2+) against TZ+ and (Na+ + K+). In statistical approach, PCA analysis suggests that geogenic weathering dynamics in the catchment is associated with carbonate-dominant lithology.

Ämnesord och genrebeteckningar

Biuppslag (personer, institutioner, konferenser, titlar ...)

  • Kumar, RajeshDepartment of Environmental Science, SBSR, Sharda University, Greater Noida, India (författare)
  • Singh, AtarDepartment of Environmental Science, SBSR, Sharda University, Greater Noida, India (författare)
  • Singh, ShaktimanLuleå tekniska universitet,Rymdteknik,Sharda University, Greater Noida, India(Swepub:ltu)shasin (författare)
  • Bhardwaj, AnshumanLuleå tekniska universitet,Rymdteknik(Swepub:ltu)ansbha (författare)
  • Kumari, AnupmaDepartment of Zoology, Patna University, Patna, India (författare)
  • Sinha, Ravindra KumarDepartment of Zoology, Patna University, Patna, India, Nalanda Open University, Biscoman Bhawan, Gandhi Maidan, Patna, India (författare)
  • Gupta, AkhileshDST, Technology Bhavan, New Mehrauli Road, New Delhi, India (författare)
  • Department of Environmental Science, SBSR, Sharda University, Greater Noida, IndiaRymdteknik (creator_code:org_t)

Sammanhörande titlar

  • Ingår i:Acta Geophysica: Springer67:2, s. 651-6601895-65721895-7455

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