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ГИДРОХИМИЧЕСКИЕ ОСОБЕННОСТИ АТМОСФЕРНЫХ ОСАДКОВ НА ПОЛИГОНЕ КРЫМСКОЙ ГЕОЛОГИЧЕСКОЙ ПРАКТИКИ СПБГУ. / Kayukova, E. P.

In: ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ, Vol. 2011, No. 3, 14.12.2011, p. 26-42.

Research output: Contribution to journal › Article › peer-review

Harvard

Kayukova, EP 2011, 'ГИДРОХИМИЧЕСКИЕ ОСОБЕННОСТИ АТМОСФЕРНЫХ ОСАДКОВ НА ПОЛИГОНЕ КРЫМСКОЙ ГЕОЛОГИЧЕСКОЙ ПРАКТИКИ СПБГУ', ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ, vol. 2011, no. 3, pp. 26-42.

APA

Kayukova, E. P. (2011). ГИДРОХИМИЧЕСКИЕ ОСОБЕННОСТИ АТМОСФЕРНЫХ ОСАДКОВ НА ПОЛИГОНЕ КРЫМСКОЙ ГЕОЛОГИЧЕСКОЙ ПРАКТИКИ СПБГУ. ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ, 2011(3), 26-42.

Vancouver

Kayukova EP. ГИДРОХИМИЧЕСКИЕ ОСОБЕННОСТИ АТМОСФЕРНЫХ ОСАДКОВ НА ПОЛИГОНЕ КРЫМСКОЙ ГЕОЛОГИЧЕСКОЙ ПРАКТИКИ СПБГУ. ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ. 2011 Dec 14;2011(3):26-42.

Author

Kayukova, E. P. / ГИДРОХИМИЧЕСКИЕ ОСОБЕННОСТИ АТМОСФЕРНЫХ ОСАДКОВ НА ПОЛИГОНЕ КРЫМСКОЙ ГЕОЛОГИЧЕСКОЙ ПРАКТИКИ СПБГУ. In: ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ. 2011 ; Vol. 2011, No. 3. pp. 26-42.

BibTeX

@article{a5f0e34b585e41f3aa5affab4e2c7e89,
title = "ГИДРОХИМИЧЕСКИЕ ОСОБЕННОСТИ АТМОСФЕРНЫХ ОСАДКОВ НА ПОЛИГОНЕ КРЫМСКОЙ ГЕОЛОГИЧЕСКОЙ ПРАКТИКИ СПБГУ",
abstract = "The site of Crimean geological field training of St.Petersburg University is situated within the Second ridge of the Crimean Mountains. Chemical characteristics of wet precipitation were measured here from 1999 to 2010 (in summer). All samples were analyzed for major ions (Cl -, HCO 3 -, CO 3 2-, SO 4 2-, NC 3 -, Ca 2+, Na +, K +, Mg 2+) and pH. The predominant ions of precipitation are mostly HCO 3 - (or sometimes SO 4 2-), Ca 2+ and Mg 2+. The average pH value was 7,0 and varied from 5.9 to 8.9. Enrichment factors, sea salt factor, non sea salt factor have been calculated. The saturation indices minerals species in precipitation (SI) were calculated by the PHREEQC program. Chemical composition of rains with minimal anthropogenic influence can be considered as representative of background values for the region. Bibliogr.",
keywords = "Crimean Mountains, Enrichment factors (EF), Non sea salt factor (NSSF), Precipitation, Predominant ions, Rainwater chemistry, Saturation index (SI), Sea salt factor (SSF), Trace elements",
author = "Kayukova, {E. P.}",
year = "2011",
month = dec,
day = "14",
language = "русский",
volume = "2011",
pages = "26--42",
journal = "Вестник Санкт-Петербургского университета. Науки о Земле",
issn = "2541-9668",
publisher = "Издательство Санкт-Петербургского университета",
number = "3",

}

RIS

TY - JOUR

T1 - ГИДРОХИМИЧЕСКИЕ ОСОБЕННОСТИ АТМОСФЕРНЫХ ОСАДКОВ НА ПОЛИГОНЕ КРЫМСКОЙ ГЕОЛОГИЧЕСКОЙ ПРАКТИКИ СПБГУ

AU - Kayukova, E. P.

PY - 2011/12/14

Y1 - 2011/12/14

N2 - The site of Crimean geological field training of St.Petersburg University is situated within the Second ridge of the Crimean Mountains. Chemical characteristics of wet precipitation were measured here from 1999 to 2010 (in summer). All samples were analyzed for major ions (Cl -, HCO 3 -, CO 3 2-, SO 4 2-, NC 3 -, Ca 2+, Na +, K +, Mg 2+) and pH. The predominant ions of precipitation are mostly HCO 3 - (or sometimes SO 4 2-), Ca 2+ and Mg 2+. The average pH value was 7,0 and varied from 5.9 to 8.9. Enrichment factors, sea salt factor, non sea salt factor have been calculated. The saturation indices minerals species in precipitation (SI) were calculated by the PHREEQC program. Chemical composition of rains with minimal anthropogenic influence can be considered as representative of background values for the region. Bibliogr.

AB - The site of Crimean geological field training of St.Petersburg University is situated within the Second ridge of the Crimean Mountains. Chemical characteristics of wet precipitation were measured here from 1999 to 2010 (in summer). All samples were analyzed for major ions (Cl -, HCO 3 -, CO 3 2-, SO 4 2-, NC 3 -, Ca 2+, Na +, K +, Mg 2+) and pH. The predominant ions of precipitation are mostly HCO 3 - (or sometimes SO 4 2-), Ca 2+ and Mg 2+. The average pH value was 7,0 and varied from 5.9 to 8.9. Enrichment factors, sea salt factor, non sea salt factor have been calculated. The saturation indices minerals species in precipitation (SI) were calculated by the PHREEQC program. Chemical composition of rains with minimal anthropogenic influence can be considered as representative of background values for the region. Bibliogr.

KW - Crimean Mountains

KW - Enrichment factors (EF)

KW - Non sea salt factor (NSSF)

KW - Precipitation

KW - Predominant ions

KW - Rainwater chemistry

KW - Saturation index (SI)

KW - Sea salt factor (SSF)

KW - Trace elements

UR - http://www.scopus.com/inward/record.url?scp=83155183304&partnerID=8YFLogxK

M3 - статья

AN - SCOPUS:83155183304

VL - 2011

SP - 26

EP - 42

JO - Вестник Санкт-Петербургского университета. Науки о Земле

JF - Вестник Санкт-Петербургского университета. Науки о Земле

SN - 2541-9668

IS - 3

ER -

ID: 52135714