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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Main Authors: Yuanqing Tang, Yan Zhang, Wanli Zhao, Tongshuai Liu, Yucan Liu
Format: Article
Language:English
Published: MDPI AG 2020-02-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/12/2/441
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spelling 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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