title: Analysis of the polydispersity of soil-like bodies in glacier environments by the laser light scattering (diffraction) method
metadata.name: dc.contributor.author
metadata.value: Abakumov, Evgeny
metadata.lang: -
metadata.name: dc.contributor.author
metadata.value: Nizamutdinov, Timur
metadata.lang: -
metadata.name: dc.contributor.author
metadata.value: Polyakov, Vyacheslav
metadata.lang: -
metadata.name: dc.date.accessioned
metadata.value: 2021-12-10T12:10:21Z
metadata.lang: -
metadata.name: dc.date.available
metadata.value: 2021-12-10T12:10:21Z
metadata.lang: -
metadata.name: dc.date.issued
metadata.value: 2021-09
metadata.lang: -
metadata.name: dc.identifier.citation
metadata.value: Abakumov, E., Nizamutdinov, T., and Polyakov, V. 2021. Analysis of the polydispersity of soil-like bodies in glacier environments by the laser light scattering (diffraction) method. Bio. Comm. 66(3): 198–209.
metadata.lang: en_GB
metadata.name: dc.identifier.other
metadata.value: https://doi.org/10.21638/spbu03.2021.302
metadata.lang: -
metadata.name: dc.identifier.uri
metadata.value: http://hdl.handle.net/11701/33812
metadata.lang: -
metadata.name: dc.description.abstract
metadata.value: This study presents the results of polydispersity analysis of soil-like bodies from
  two various polar regions using the laser light scattering method. The differences
  in the particle size distribution of cryoconite samples from the Anuchin
  Glacier (Antarctica) and the Mushketov Glacier (Arctic) are described. The samples
  obtained from the Mushketov Glacier are characterized by a finer particle
  size distribution than samples collected on the Anuchin Glacier. While comparing
  our results with previously published studies, it was found that the method
  of laser light scattering shows a lower content of small fractions (<0.05 mm)
  compared to the classical methods of sedimentation, since these methods are
  based on fundamentally different physical principles. The laser method used
  requires low amounts of samples (0.2–0.5 g), while the classical sedimentary
  method uses a higher gravimetric portion of cryoconite (5–10 g), which is critical
  for field sampling.
metadata.lang: en_GB
metadata.name: dc.description.sponsorship
metadata.value: This work was supported by
  Russian Foundation for Basic Research,
  project No 19-05-50107.
metadata.lang: en_GB
metadata.name: dc.language.iso
metadata.value: en
metadata.lang: en_GB
metadata.name: dc.publisher
metadata.value: St Petersburg State University
metadata.lang: en_GB
metadata.name: dc.relation.ispartofseries
metadata.value: Biological Сommunications;Volume 66; Issue 3
metadata.lang: -
metadata.name: dc.subject
metadata.value: soloids
metadata.lang: en_GB
metadata.name: dc.subject
metadata.value: cryoconites
metadata.lang: en_GB
metadata.name: dc.subject
metadata.value: Anuchin Glacier
metadata.lang: en_GB
metadata.name: dc.subject
metadata.value: Mushketov Glacier
metadata.lang: en_GB
metadata.name: dc.title
metadata.value: Analysis of the polydispersity of soil-like bodies in glacier environments by the laser light scattering (diffraction) method
metadata.lang: en_GB
metadata.name: dc.type
metadata.value: Article
metadata.lang: en_GB
resources.filename: 10142-Article Text-38476-1-10-20211112.pdf
resources.url: https://dspace.spbu.ru/bitstream/11701/33812/1/10142-Article%20Text-38476-1-10-20211112.pdf
resources.format: Adobe PDF
resources.size: 8,24 MB