Hydrochemical Characteristics of the Aral Sea in 2012–2013

全文:

开放存取 开放存取
受限制的访问 ##reader.subscriptionAccessGranted##
受限制的访问 订阅存取

详细

The decrease in Aral Sea area, which started in the 1960s, caused considerable changes in the hydrological, chemical, and biological structure of sea water. Regular observations of Aral water chemistry ceased in the early 1990s. There were no observations of the concentrations of biogenic element compounds in water (the so-called “first-day analyses”). During expeditions of the Institute of Oceanology, RAS, in September 2012 and October 2013, integrated hydrochemical observations were carried out, including measuring the concentrations of biogenic element compounds, dissolved oxygen, hydrogen sulfide, and carbonate equilibrium components. An objective of this study was to develop methods of hydrochemical studies under high water salinity (mineralization). In addition to the standard hydrochemical complex, water samples were taken to determine total water mineralization and the concentration of dissolved and suspended metal forms. The results of these studies are given.

作者简介

P. Makkaveev

Shirshov Institute of Oceanology

编辑信件的主要联系方式.
Email: makkaveev55@mail.ru
俄罗斯联邦, Moscow, 117997

V. Gordeev

Shirshov Institute of Oceanology

Email: makkaveev55@mail.ru
俄罗斯联邦, Moscow, 117997

P. Zav’yalov

Shirshov Institute of Oceanology

Email: makkaveev55@mail.ru
俄罗斯联邦, Moscow, 117997

A. Polukhin

Shirshov Institute of Oceanology

Email: makkaveev55@mail.ru
俄罗斯联邦, Moscow, 117997

P. Khlebopashev

Shirshov Institute of Oceanology

Email: makkaveev55@mail.ru
俄罗斯联邦, Moscow, 117997

A. Kochenkova

Shirshov Institute of Oceanology

Email: makkaveev55@mail.ru
俄罗斯联邦, Moscow, 117997

补充文件

附件文件
动作
1. JATS XML

版权所有 © Pleiades Publishing, Ltd., 2018