Research on the Migration of the Total Manganese during the Process of Water Icing
Our research focused on the migration law of the total manganese (TMn) during the process of water icing. We utilized two experimental methods: (1) natural icing and (2) simulated icing. While using laboratory simulation, we explored the effects of ice thickness, freezing temperature, and initial co...
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doaj-c6747c90a1314fe8a3af09e5917d51da2020-11-25T01:57:01ZengMDPI AGWater2073-44412019-08-01118162610.3390/w11081626w11081626Research on the Migration of the Total Manganese during the Process of Water IcingYan Zhang0Yuanqing Tang1Aixin Yu2Wanli Zhao3Yucan Liu4College of Civil Engineering, Yantai University, Yantai 264000, ChinaCollege of Civil Engineering, Yantai University, Yantai 264000, ChinaCollege of Civil Engineering, Yantai University, Yantai 264000, ChinaCollege of Civil Engineering, Yantai University, Yantai 264000, ChinaCollege of Civil Engineering, Yantai University, Yantai 264000, ChinaOur research focused on the migration law of the total manganese (TMn) during the process of water icing. We utilized two experimental methods: (1) natural icing and (2) simulated icing. While using laboratory simulation, we explored the effects of ice thickness, freezing temperature, and initial concentrations on the migration of TMn in the ice-water system. The distribution coefficient “K” (the ratio of the average concentration of TMn in the ice body to the average concentration of TMn in the under-ice water body) was used to characterize it. The results indicated that TMn continuously migrated from ice to under-ice water during the process of water icing. The concentration of TMn in the ice was the upper layer < middle layer < lower layer, and K decreases as the ice thickness, freezing temperature, and initial concentration increased. We explained the migration of TMn during the process of water icing from the perspective of crystallography. Our research can arouse other researcher’s attention towards the change of TMn concentration in lakes in high latitudes during the icebound period.https://www.mdpi.com/2073-4441/11/8/1626natural icingsimulated icingmigration lawdistribution coefficient “K”TMn |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Yan Zhang Yuanqing Tang Aixin Yu Wanli Zhao Yucan Liu |
spellingShingle |
Yan Zhang Yuanqing Tang Aixin Yu Wanli Zhao Yucan Liu Research on the Migration of the Total Manganese during the Process of Water Icing Water natural icing simulated icing migration law distribution coefficient “K” TMn |
author_facet |
Yan Zhang Yuanqing Tang Aixin Yu Wanli Zhao Yucan Liu |
author_sort |
Yan Zhang |
title |
Research on the Migration of the Total Manganese during the Process of Water Icing |
title_short |
Research on the Migration of the Total Manganese during the Process of Water Icing |
title_full |
Research on the Migration of the Total Manganese during the Process of Water Icing |
title_fullStr |
Research on the Migration of the Total Manganese during the Process of Water Icing |
title_full_unstemmed |
Research on the Migration of the Total Manganese during the Process of Water Icing |
title_sort |
research on the migration of the total manganese during the process of water icing |
publisher |
MDPI AG |
series |
Water |
issn |
2073-4441 |
publishDate |
2019-08-01 |
description |
Our research focused on the migration law of the total manganese (TMn) during the process of water icing. We utilized two experimental methods: (1) natural icing and (2) simulated icing. While using laboratory simulation, we explored the effects of ice thickness, freezing temperature, and initial concentrations on the migration of TMn in the ice-water system. The distribution coefficient “K” (the ratio of the average concentration of TMn in the ice body to the average concentration of TMn in the under-ice water body) was used to characterize it. The results indicated that TMn continuously migrated from ice to under-ice water during the process of water icing. The concentration of TMn in the ice was the upper layer < middle layer < lower layer, and K decreases as the ice thickness, freezing temperature, and initial concentration increased. We explained the migration of TMn during the process of water icing from the perspective of crystallography. Our research can arouse other researcher’s attention towards the change of TMn concentration in lakes in high latitudes during the icebound period. |
topic |
natural icing simulated icing migration law distribution coefficient “K” TMn |
url |
https://www.mdpi.com/2073-4441/11/8/1626 |
work_keys_str_mv |
AT yanzhang researchonthemigrationofthetotalmanganeseduringtheprocessofwatericing AT yuanqingtang researchonthemigrationofthetotalmanganeseduringtheprocessofwatericing AT aixinyu researchonthemigrationofthetotalmanganeseduringtheprocessofwatericing AT wanlizhao researchonthemigrationofthetotalmanganeseduringtheprocessofwatericing AT yucanliu researchonthemigrationofthetotalmanganeseduringtheprocessofwatericing |
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1724976908608733184 |