Characteristic features of groundwater pollution in the Poyang Lake catchment; IOP Conference Series: Earth and Environmental Science; Vol. 21: XVIII International Scientific Symposium in Honour of Academician M. A. Usov: Problems of Geology and Subsurface Development 7–11 April 2014, Tomsk, Russia

Detalles Bibliográficos
Parent link:IOP Conference Series: Earth and Environmental Science
Vol. 21: XVIII International Scientific Symposium in Honour of Academician M. A. Usov: Problems of Geology and Subsurface Development 7–11 April 2014, Tomsk, Russia.— 2014.— [012023, 6 p.]
Autor Principal: Soldatova E. A. Evgeniya Aleksandrovna
Autor Corporativo: Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра гидрогеологии, инженерной геологии и гидрогеоэкологии (ГИГЭ) Научно-образовательный центр "Вода" (НОЦ "ВОДА") Проблемная научно-исследовательская лаборатория гидрогеохимии (ПНИЛ ГГХ)
Outros autores: Guseva N. V. Natalia Vladimirovna, Wang G.
Summary:Title screen
Research of shallow groundwater in the Poyang Lake catchment should be considered as one of the priority targets in this region, due to the fact that shallow groundwater is formed under the influence of complex factors, including both natural and anthropogenic, and also the fact that it is related to the Poyang Lake water. Shallow groundwater of the Poyang Lake area is fresh. High concentrations of NO[3] ,Cl-SO[4]{2-}, K{+} and rarely, Na{+} are not typical of the groundwater of subtropical humid climate. Within the investigated territory the groundwater could be divided into two types - relatively pure shallow groundwater, formed primarily under the effect of natural factors and having a high content of NO[3] - but rarely K{+} , Cl{-}, SO[4]{2-} , in some sampling points; and relatively polluted shallow groundwater, characterized by significant changes of chemical composition due to intensive agricultural activity. This type has higher pHvalues, concentration of main components, including NO[3]{-} , K{+}, SO[4]{2-}, Cl{-}, and, accordingly, value of total dissolved solids in comparison with relatively pure shallow groundwater.
Режим доступа: по договору с организацией-держателем ресурса
Idioma:inglés
Publicado: 2014
Series:Hydrogeochemistry and Hydrogeoecology
Subjects:
Acceso en liña:http://iopscience.iop.org/1755-1315/21/1/012023
Formato: Electrónico Capítulo de libro
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=638258

MARC

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330 |a Research of shallow groundwater in the Poyang Lake catchment should be considered as one of the priority targets in this region, due to the fact that shallow groundwater is formed under the influence of complex factors, including both natural and anthropogenic, and also the fact that it is related to the Poyang Lake water. Shallow groundwater of the Poyang Lake area is fresh. High concentrations of NO[3] ,Cl-SO[4]{2-}, K{+} and rarely, Na{+} are not typical of the groundwater of subtropical humid climate. Within the investigated territory the groundwater could be divided into two types - relatively pure shallow groundwater, formed primarily under the effect of natural factors and having a high content of NO[3] - but rarely K{+} , Cl{-}, SO[4]{2-} , in some sampling points; and relatively polluted shallow groundwater, characterized by significant changes of chemical composition due to intensive agricultural activity. This type has higher pHvalues, concentration of main components, including NO[3]{-} , K{+}, SO[4]{2-}, Cl{-}, and, accordingly, value of total dissolved solids in comparison with relatively pure shallow groundwater. 
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