Abstract

Abstract. The Jialu River, a secondary tributary of the Huaihe River, has been severely contaminated from major contaminant sources, such as a number of untreated or lightly treated sewage waste in some cities. Groundwater along the river is not an isolated component of the hydrologic system, but is instead connected with the surface water. This study aims to investigate temporal and spatial variations in water chemistry affected by humans and to characterize the relationships between surface water (e.g. reservoirs, lakes and rivers) and groundwater near the river in the shallow Quaternary aquifer. Concentration of Cl− in north Zhengzhou City increased prominently due to the discharge of a large amount of domestic water. Nitrate and potassium show maximum concentrations in groundwater in Fugou County. These high levels can be attributed to the use of a large quantity of fertilizer over this region. Most surface water appeared to be continuously recharged from the surrounding groundwater (regional wells) based on comparison surface water with groundwater levels, stable-isotopes and major ion signatures. However, the groundwater of a transitional well (location SY3) seemed to be recharged by river water via bank infiltration in September 2010. Fractional contributions of river water to the groundwater were calculated based on isotopic and chemical data using a mass-balance approach. Results show that the groundwater was approximately composed of 60–70% river water. These findings should be useful for a better understanding of hydrogeological processes at the river-aquifer interface and ultimately benefit water management in the future.

Highlights

  • The Jialu River (JR), the secondary tributary of the Huaihe River, is severely contaminated by a variety of contaminant sources such as a large number of trade waste and the untreated or lightly treated sewage waste in some cities (Zhang et al, 2009)

  • When the altitude of the river stage is higher than altitudes of groundwater levels in the nearby area, water flows from the river to the aquifer

  • The Jialu River basin is being faced with environmental pressures mainly coming from anthropogenic influences

Read more

Summary

Introduction

The Jialu River (JR), the secondary tributary of the Huaihe River, is severely contaminated by a variety of contaminant sources such as a large number of trade waste and the untreated or lightly treated sewage waste in some cities (Zhang et al, 2009). These wastes have resulted in elevated concentrations of chemical oxygen demand (COD) and ammonia nitrogen (NH3-N) in water within the Zhengzhou region (Lu et al, 2008) and the lower reaches in the Zhoukou region (Zhao et al, 2005; Xie et al, 2008). Groundwater and surface water are not isolated components of the hydrologic system, but instead interact with each other across a variety of physiographic and climatic landscapes

Objectives
Methods
Results
Discussion
Conclusion

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.