Accumulation of Subcolloidal Fraction Elements of Bottom Sediments in Amur Bay (Sea of Japan)
- Авторы: Polyakov D.M.1, Utkin I.V.1
- 
							Учреждения: 
							- Il’ichev Pacific Oceanological Institute, Far Eastern Division, Russian Academy of Sciences
 
- Выпуск: Том 58, № 6 (2018)
- Страницы: 900-908
- Раздел: Marine Geology
- URL: https://journals.rcsi.science/0001-4370/article/view/149793
- DOI: https://doi.org/10.1134/S0001437018070044
- ID: 149793
Цитировать
Аннотация
The mean contents of elements (Fe, Mn, Zn, Pb, Cu, Cr, V, Co, Cd, Ni, As, Sc, Ga, Zr, Hf, Nb, Ta, W, Th, Mo) in the subcolloidal fraction of bottom sediments in the northern part of Amur Bay have been determined. A 5–17% increase is observed in the heavy metal content (Pb, Co, Ni, Zn, Cr, V, As) compared to the mean values for sediments directly subjected to the influence of the Razdolnaya River, which is related to flocculation and sorption on Fe and Mn oxyhydroxides. A linear dependence of heavy metal accumulation on the Fe and Mn content is established. An increase in the Cu and Mo content is revealed (by 49 and 44%, respectively), related to vital accumulation by plankton, as well as in increase in V, Cr, Co, Ni, Zn, Cd, and As (by 2–20%) in sediments subjected to anthropogenic impact.
Об авторах
D. Polyakov
Il’ichev Pacific Oceanological Institute, Far Eastern Division, Russian Academy of Sciences
							Автор, ответственный за переписку.
							Email: dmpol@poi.dvo.ru
				                					                																			                												                	Россия, 							Vladivostok, 690041						
I. Utkin
Il’ichev Pacific Oceanological Institute, Far Eastern Division, Russian Academy of Sciences
														Email: dmpol@poi.dvo.ru
				                					                																			                												                	Россия, 							Vladivostok, 690041						
Дополнительные файлы
 
				
			 
						 
					 
						 
						 
						 
									 
  
  
  
  
  Отправить статью по E-mail
			Отправить статью по E-mail  Открытый доступ
		                                Открытый доступ Доступ предоставлен
						Доступ предоставлен Только для подписчиков
		                                		                                        Только для подписчиков
		                                					