Zhang et al. (2026) Irrigation reshaping groundwater dynamics to regulate salinity threshold and transport
Identification
- Journal: Journal of Hydrology
- Year: 2026
- Date: 2026-01-22
- Authors: Yuting Zhang, Hui Qian, Kai Hou, Yuan Fang
- DOI: 10.1016/j.jhydrol.2026.134999
Research Groups
- School of Water Conservancy, North China University of Water Resources and Electric Power, Zhengzhou, China
- School of Water and Environment, Chang’an University, Xi’an, Shaanxi, China
- Key Laboratory of Subsurface Hydrology and Ecological Effect in Arid Region of Ministry of Education, Chang’an University, Xi’an, Shaanxi, China
- Yellow River Engineering Consulting Co.Ltd, Zhengzhou, Henan, China
- Key Laboratory of Water Management and Water Security for Yellow River Basin, Ministry of Water Resources, Zhengzhou, Henan, China
- Ningxia Survey and Monitor Institute of Land and Resources, China
Short Summary
This study investigates how irrigation-induced groundwater table fluctuations (GWTF) influence solute transport and accumulation in arid regions, proposing dynamic safety thresholds for groundwater total dissolved solids (TDS) that adapt to changing hydrodynamic conditions.
Objective
- To clarify the mechanisms of solute transport and accumulation under groundwater table fluctuations (GWTF) triggered by water diversion irrigation, and to propose a dynamic safety threshold for groundwater total dissolved solids (TDS).
Study Configuration
- Spatial Scale: Arid irrigated regions (mechanistic study applicable to such environments).
- Temporal Scale: Dynamic, seasonal, and long-term periodic changes in groundwater table and salinity.
Methodology and Data
- Models used: Greenberg logarithmic model.
- Data sources: Analysis of groundwater table fluctuations (GWTF) driven by pumping, water diversion, and irrigation; hydrodynamic field data; groundwater total dissolved solids (TDS) data; soil salinity data; and consideration of anthropogenic inputs (e.g., fertilizers) and evaporite.
Main Results
- Pumping, water diversion, and irrigation contribute 25.61%, 26.33%, and 21.37% respectively to changes in the groundwater table.
- The amplitude of groundwater table fluctuation follows the order: natural fluctuation < irrigation fluctuation < diversion fluctuation < pumping fluctuation.
- A negative correlation exists between groundwater table fluctuation (GWTF) and groundwater total dissolved solids (TDS), while a positive correlation exists between groundwater TDS and soil salinity.
- In high-evaporation environments, groundwater salinization is primarily driven by external salts from anthropogenic inputs and evaporite, rather than direct evaporation.
- Groundwater table fluctuations (GWTF) govern the cyclic processes of salt accumulation and re-dissolution.
- The Greenberg logarithmic model was used to quantify dynamic groundwater TDS safety thresholds, demonstrating that these thresholds are not static but vary significantly with hydrodynamic conditions.
Contributions
- Elucidates the comprehensive mechanisms linking groundwater table fluctuation generation to salt transport and accumulation in arid irrigated regions.
- Quantifies the relative contributions of pumping, water diversion, and irrigation to groundwater table changes.
- Proposes and quantifies a dynamic safety threshold for groundwater total dissolved solids (TDS), highlighting its environmental dependence and variability with hydrodynamic conditions, which challenges the concept of static, universal thresholds.
Funding
- Not specified in the provided text.
Citation
@article{Zhang2026Irrigation,
author = {Zhang, Yuting and Qian, Hui and Hou, Kai and Fang, Yuan},
title = {Irrigation reshaping groundwater dynamics to regulate salinity threshold and transport},
journal = {Journal of Hydrology},
year = {2026},
doi = {10.1016/j.jhydrol.2026.134999},
url = {https://doi.org/10.1016/j.jhydrol.2026.134999}
}
Original Source: https://doi.org/10.1016/j.jhydrol.2026.134999