The Migration Law of Iron during the Process of Water Icing
In this study, we utilized simulated icing experiments to investigate the effect of icing thickness, freezing temperature and initial concentration on the migration of iron in the ice−water system during water icing. The distribution coefficient “K” (the ratio of the av...
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doaj-03c92a5a6a7246efa3de6d7b0b2706462020-11-25T01:12:58ZengMDPI AGWater2073-44412020-02-0112244110.3390/w12020441w12020441The Migration Law of Iron during the Process of Water IcingYuanqing Tang0Yan Zhang1Wanli Zhao2Tongshuai Liu3Yucan 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, ChinaIn this study, we utilized simulated icing experiments to investigate the effect of icing thickness, freezing temperature and initial concentration on the migration of iron in the ice−water system during water icing. The distribution coefficient “K” (the ratio of the average concentration of iron in the ice to that in the under-ice water) was used to describe the effect. The results indicated that iron partitioned stronger to under-ice water than to ice during the process of water icing, resulting in the concentration of iron in ice−water system before and after freezing being expressed as: ice < pre-freezing water < under-ice water. K decreased with the increase in icing thickness, freezing temperature and initial concentration. The temperature change in the solution will change the solubility of the solvent, so we explained the migration of iron during the process of water icing from the perspective of solid−liquid equilibrium theory. Too high or too low iron concentration may inhibit the growth of algae, thus affecting the underwater ecological environment. We expect that our study will arouse researcher’s attention to the change in iron concentration in shallow lakes and ponds at high latitudes during the icebound period.https://www.mdpi.com/2073-4441/12/2/441simulated icingmigration lawdistribution coefficient “k”solid–liquid equilibrium theoryiron |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Yuanqing Tang Yan Zhang Wanli Zhao Tongshuai Liu Yucan Liu |
spellingShingle |
Yuanqing Tang Yan Zhang Wanli Zhao Tongshuai Liu Yucan Liu The Migration Law of Iron during the Process of Water Icing Water simulated icing migration law distribution coefficient “k” solid–liquid equilibrium theory iron |
author_facet |
Yuanqing Tang Yan Zhang Wanli Zhao Tongshuai Liu Yucan Liu |
author_sort |
Yuanqing Tang |
title |
The Migration Law of Iron during the Process of Water Icing |
title_short |
The Migration Law of Iron during the Process of Water Icing |
title_full |
The Migration Law of Iron during the Process of Water Icing |
title_fullStr |
The Migration Law of Iron during the Process of Water Icing |
title_full_unstemmed |
The Migration Law of Iron during the Process of Water Icing |
title_sort |
migration law of iron during the process of water icing |
publisher |
MDPI AG |
series |
Water |
issn |
2073-4441 |
publishDate |
2020-02-01 |
description |
In this study, we utilized simulated icing experiments to investigate the effect of icing thickness, freezing temperature and initial concentration on the migration of iron in the ice−water system during water icing. The distribution coefficient “K” (the ratio of the average concentration of iron in the ice to that in the under-ice water) was used to describe the effect. The results indicated that iron partitioned stronger to under-ice water than to ice during the process of water icing, resulting in the concentration of iron in ice−water system before and after freezing being expressed as: ice < pre-freezing water < under-ice water. K decreased with the increase in icing thickness, freezing temperature and initial concentration. The temperature change in the solution will change the solubility of the solvent, so we explained the migration of iron during the process of water icing from the perspective of solid−liquid equilibrium theory. Too high or too low iron concentration may inhibit the growth of algae, thus affecting the underwater ecological environment. We expect that our study will arouse researcher’s attention to the change in iron concentration in shallow lakes and ponds at high latitudes during the icebound period. |
topic |
simulated icing migration law distribution coefficient “k” solid–liquid equilibrium theory iron |
url |
https://www.mdpi.com/2073-4441/12/2/441 |
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