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

Dettagli Bibliografici
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.]
Autore principale: Soldatova E. A. Evgeniya Aleksandrovna
Ente Autore: 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)
Altri autori: Guseva N. V. Natalia Vladimirovna, Wang G.
Riassunto: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
Lingua:inglese
Pubblicazione: 2014
Serie:Hydrogeochemistry and Hydrogeoecology
Soggetti:
Accesso online:http://iopscience.iop.org/1755-1315/21/1/012023
Natura: Elettronico Capitolo di libro
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=638258
Descrizione
Riassunto: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