Self-purification ability of natural waters in the arid zones
The paper presents the analysis of literature data and research results on self-purification and self-purification ability of natural waters at arid zones (on example of closed Lake Balkhash). The self-purification processes are a combination of all natural (hydrodynamic, chemical, microbiological a...
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al-Farabi Kazakh National University
2018-06-01
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doaj-4f8f4a257bfb448bbfff0a13cd11efed2020-11-25T04:00:46Zengal-Farabi Kazakh National UniversityChemical Bulletin of Kazakh National University1563-03312312-75542018-06-012364210.15328/cb971Self-purification ability of natural waters in the arid zonesSofiya M. Romanova0Roza G. Ryskaliyeva1Oksana I. Ponomarenko2al-Farabi Kazakh National University, Almaty, Kazakhstanal-Farabi Kazakh National University, Almaty, Kazakhstanal-Farabi Kazakh National University, Almaty, KazakhstanThe paper presents the analysis of literature data and research results on self-purification and self-purification ability of natural waters at arid zones (on example of closed Lake Balkhash). The self-purification processes are a combination of all natural (hydrodynamic, chemical, microbiological and hydrobiological) processes in contaminated natural waters. A large number of pollutants and specific (physical and geographical) conditions of reservoirs causes the complexity and variety of cleaning processes of natural waters. Large amounts of pollutants discharged into water reservoirs and drains impede the self-purification processes. It has been established that the sediments and clay of Lake Balkhash absorb the metal ions. Thus, the process of absorption of Mn2+ ions by clay minerals mainly occurs within the first three hours of contact, whereas sorption by slits continues until 10-15 days. The sediments are good absorbents for cadmium (90%), zinc (86%) and copper (78%). The sorption properties in the dynamic mode decreases in the row of zeolite (SEC = 1.02·10-3), then Fe (OH)3 (SEC = 0.28·10-3) and Al (OH)3 (SEC = 0.10·10-3 mmol-eq/g) with respect to Mn+2 ion with concentrations from 5.0 to 100 μg/L.https://bulletin.chemistry.kz/index.php/kaznu/article/view/971self-purificationself-purification abilitynatural waterssorptionmetals |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Sofiya M. Romanova Roza G. Ryskaliyeva Oksana I. Ponomarenko |
spellingShingle |
Sofiya M. Romanova Roza G. Ryskaliyeva Oksana I. Ponomarenko Self-purification ability of natural waters in the arid zones Chemical Bulletin of Kazakh National University self-purification self-purification ability natural waters sorption metals |
author_facet |
Sofiya M. Romanova Roza G. Ryskaliyeva Oksana I. Ponomarenko |
author_sort |
Sofiya M. Romanova |
title |
Self-purification ability of natural waters in the arid zones |
title_short |
Self-purification ability of natural waters in the arid zones |
title_full |
Self-purification ability of natural waters in the arid zones |
title_fullStr |
Self-purification ability of natural waters in the arid zones |
title_full_unstemmed |
Self-purification ability of natural waters in the arid zones |
title_sort |
self-purification ability of natural waters in the arid zones |
publisher |
al-Farabi Kazakh National University |
series |
Chemical Bulletin of Kazakh National University |
issn |
1563-0331 2312-7554 |
publishDate |
2018-06-01 |
description |
The paper presents the analysis of literature data and research results on self-purification and self-purification ability of natural waters at arid zones (on example of closed Lake Balkhash). The self-purification processes are a combination of all natural (hydrodynamic, chemical, microbiological and hydrobiological) processes in contaminated natural waters. A large number of pollutants and specific (physical and geographical) conditions of reservoirs causes the complexity and variety of cleaning processes of natural waters. Large amounts of pollutants discharged into water reservoirs and drains impede the self-purification processes. It has been established that the sediments and clay of Lake Balkhash absorb the metal ions. Thus, the process of absorption of Mn2+ ions by clay minerals mainly occurs within the first three hours of contact, whereas sorption by slits continues until 10-15 days. The sediments are good absorbents for cadmium (90%), zinc (86%) and copper (78%). The sorption properties in the dynamic mode decreases in the row of zeolite (SEC = 1.02·10-3), then Fe (OH)3 (SEC = 0.28·10-3) and Al (OH)3 (SEC = 0.10·10-3 mmol-eq/g) with respect to Mn+2 ion with concentrations from 5.0 to 100 μg/L. |
topic |
self-purification self-purification ability natural waters sorption metals |
url |
https://bulletin.chemistry.kz/index.php/kaznu/article/view/971 |
work_keys_str_mv |
AT sofiyamromanova selfpurificationabilityofnaturalwatersinthearidzones AT rozagryskaliyeva selfpurificationabilityofnaturalwatersinthearidzones AT oksanaiponomarenko selfpurificationabilityofnaturalwatersinthearidzones |
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1724449339439316992 |