Experimental Investigation of Water Migration Characteristics for Saline Soil

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Editorial policies Publication Policy Overview Peer Review Policy Research Ethics and Malpractice Policy Plagiarism Policy Conflict of Interest Policy Open Access Policy Instructions for Reviewers Generative AI and AI-Assisted Technologies Policy Advertising Policy Direct Marketing & Manuscript Solicitation Digital Archiving and Preservation Policy CrossMark, Correction, and Retraction Policy

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ORIGINAL RESEARCH

Experimental Investigation of Water Migration Characteristics for Saline Soil

Xudong Zhang ¹

,

Shouwei Liu ²

,

Qing Wang ¹

,

Gang Wang ³

,

Yufeng Liu ¹

,

Wei Peng ¹

,

Xinchuan Xu ²

,

Yaowu Liu ¹

1

College of Construction Engineering, Jilin University

2

Water Conservancy and Hydropower Survey and Design Institute of Jilin Province, Changchun

3

School of Geomatics& Prospecting Engineering, Jilin Jianzhu University

Submission date: 2017-09-25

Final revision date: 2018-02-25

Acceptance date: 2018-02-28

Online publication date: 2018-11-09

Publication date: 2019-01-28

Corresponding author

Qing Wang

College of Construction Engineering, Jilin University, 938 Ximinzhu Street, Changchun, Jilin, China, 130026 Changchun, China

Pol. J. Environ. Stud. 2019;28(3):1495-1505

DOI: https://doi.org/10.15244/pjoes/85952

KEYWORDS

carbonate-saline soil

soil water potential

water migration

TOPICS

ABSTRACT

Soil in western Jilin, China has the properties of a saline soil, seasonal frozen soil, and a dispersive soil, in which the freezing process can induce many engineering and environmental problems, including soil secondary salinization and frost heave. During the freezing process, water, heat, stress, and even solute interact with each other. Water migration plays an important role in this process. In this paper, a sampling point in Nong’an, western Jilin was selected for soil collection and experimental tests. The experiment included two tests: the capillary water test and a water migration test subjected to freezing. The results showed that the height of capillary water is low, while the water migrates obviously after the process of freezing in different conditions. The results indicate that the bound water film hinders the capillary pores, which can impair the matric potential. During the freezing process, the temperature potential and gravitational potential can drive the water to migrate through the bound water film. For the soil in western Jilin, temperature potential plays a decisive role in water migration, but gravitational potential and matric potential have a minor effects.

CONFLICT OF INTEREST

The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.

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