Technology of drinking water preparation using the reactor - clarifier
Siberian surface water and groundwater are characterized by low temperatures for a long year period. Many groundwater sources’ organic composition are formed of soil and peat humus, marsh feeding of rivers, decomposition of plankton, higher water, and soil grass in reservoirs and lakes. Organic coll...
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Online Access: | https://doi.org/10.1051/e3sconf/20199104006 https://www.e3s-conferences.org/articles/e3sconf/pdf/2019/17/e3sconf_tpacee2019_04006.pdf https://doaj.org/article/60b325f79883484f9b24a52ef4450b73 |
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fttriple:oai:gotriple.eu:oai:doaj.org/article:60b325f79883484f9b24a52ef4450b73 2023-05-15T18:45:06+02:00 Technology of drinking water preparation using the reactor - clarifier Skolubovich Yuriy Skolubovich Aleksander Voitov Evgeniy Makarikhina Inna 2019-01-01 https://doi.org/10.1051/e3sconf/20199104006 https://www.e3s-conferences.org/articles/e3sconf/pdf/2019/17/e3sconf_tpacee2019_04006.pdf https://doaj.org/article/60b325f79883484f9b24a52ef4450b73 en fr eng fre EDP Sciences 2267-1242 doi:10.1051/e3sconf/20199104006 https://www.e3s-conferences.org/articles/e3sconf/pdf/2019/17/e3sconf_tpacee2019_04006.pdf https://doaj.org/article/60b325f79883484f9b24a52ef4450b73 undefined E3S Web of Conferences, Vol 91, p 04006 (2019) geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2019 fttriple https://doi.org/10.1051/e3sconf/20199104006 2023-01-22T17:53:05Z Siberian surface water and groundwater are characterized by low temperatures for a long year period. Many groundwater sources’ organic composition are formed of soil and peat humus, marsh feeding of rivers, decomposition of plankton, higher water, and soil grass in reservoirs and lakes. Organic colloids in natural waters and in humic substances give the color of water. It’s yellowish coloration of varying intensity. Thus, the Om River’s water color in the city of Kuibyshev in the Novosibirsk Region is 500 degrees with feculence of less than 3 mg/l. A number of underground water sources also have an increased content of organic contaminants caused by peat bogs at great depths and high water colority with low turbidity. For example, the water color is up to 1500 degrees in the Namtsy village of the SAHA-Yakutia Republic. In addition, underground water and, to a greater extent, surface water are often characterized by a high content of iron (up to 20 mg/l), manganese (up to 4 mg/l), and other impurities of natural and anthropogenic origin. Iron and manganese are in natural waters in the form of mineral or organic complex compounds of humic or some fatty acids. In the second case, these waters are with increased oxidizability and rather aggressive nature. In particular, the iron content is 3 mg/l, manganese is 1 mg/l, the permanganate oxidizability is 50 mg/l in the water of the Om River. Article in Journal/Newspaper Yakutia Yakutia Republic Unknown Namtsy ENVELOPE(129.667,129.667,62.720,62.720) E3S Web of Conferences 91 04006 |
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English French |
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geo envir Skolubovich Yuriy Skolubovich Aleksander Voitov Evgeniy Makarikhina Inna Technology of drinking water preparation using the reactor - clarifier |
topic_facet |
geo envir |
description |
Siberian surface water and groundwater are characterized by low temperatures for a long year period. Many groundwater sources’ organic composition are formed of soil and peat humus, marsh feeding of rivers, decomposition of plankton, higher water, and soil grass in reservoirs and lakes. Organic colloids in natural waters and in humic substances give the color of water. It’s yellowish coloration of varying intensity. Thus, the Om River’s water color in the city of Kuibyshev in the Novosibirsk Region is 500 degrees with feculence of less than 3 mg/l. A number of underground water sources also have an increased content of organic contaminants caused by peat bogs at great depths and high water colority with low turbidity. For example, the water color is up to 1500 degrees in the Namtsy village of the SAHA-Yakutia Republic. In addition, underground water and, to a greater extent, surface water are often characterized by a high content of iron (up to 20 mg/l), manganese (up to 4 mg/l), and other impurities of natural and anthropogenic origin. Iron and manganese are in natural waters in the form of mineral or organic complex compounds of humic or some fatty acids. In the second case, these waters are with increased oxidizability and rather aggressive nature. In particular, the iron content is 3 mg/l, manganese is 1 mg/l, the permanganate oxidizability is 50 mg/l in the water of the Om River. |
format |
Article in Journal/Newspaper |
author |
Skolubovich Yuriy Skolubovich Aleksander Voitov Evgeniy Makarikhina Inna |
author_facet |
Skolubovich Yuriy Skolubovich Aleksander Voitov Evgeniy Makarikhina Inna |
author_sort |
Skolubovich Yuriy |
title |
Technology of drinking water preparation using the reactor - clarifier |
title_short |
Technology of drinking water preparation using the reactor - clarifier |
title_full |
Technology of drinking water preparation using the reactor - clarifier |
title_fullStr |
Technology of drinking water preparation using the reactor - clarifier |
title_full_unstemmed |
Technology of drinking water preparation using the reactor - clarifier |
title_sort |
technology of drinking water preparation using the reactor - clarifier |
publisher |
EDP Sciences |
publishDate |
2019 |
url |
https://doi.org/10.1051/e3sconf/20199104006 https://www.e3s-conferences.org/articles/e3sconf/pdf/2019/17/e3sconf_tpacee2019_04006.pdf https://doaj.org/article/60b325f79883484f9b24a52ef4450b73 |
long_lat |
ENVELOPE(129.667,129.667,62.720,62.720) |
geographic |
Namtsy |
geographic_facet |
Namtsy |
genre |
Yakutia Yakutia Republic |
genre_facet |
Yakutia Yakutia Republic |
op_source |
E3S Web of Conferences, Vol 91, p 04006 (2019) |
op_relation |
2267-1242 doi:10.1051/e3sconf/20199104006 https://www.e3s-conferences.org/articles/e3sconf/pdf/2019/17/e3sconf_tpacee2019_04006.pdf https://doaj.org/article/60b325f79883484f9b24a52ef4450b73 |
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undefined |
op_doi |
https://doi.org/10.1051/e3sconf/20199104006 |
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E3S Web of Conferences |
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91 |
container_start_page |
04006 |
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1766236060937879552 |