Temperature effect on the transport of nitrate and ammonium ions in a loose-pore geothermal reservoir

The concentration of NO3−―N in some of the geothermal water samples collected from Kaifeng City, Henan Province, China has exceeded the World Health Organization's guideline value for drinking water (10mg/L). The NH4+―N concentration cannot also meet the demand for quality standard for groundwa...

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Published inJournal of geochemical exploration Vol. 124; pp. 59 - 66
Main Authors Wang, Xinyi, Zhao, Li, Liu, Xiaoman, A, Lili, Zhang, Yanxin
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.01.2013
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Abstract The concentration of NO3−―N in some of the geothermal water samples collected from Kaifeng City, Henan Province, China has exceeded the World Health Organization's guideline value for drinking water (10mg/L). The NH4+―N concentration cannot also meet the demand for quality standard for groundwater (0.2mg/L) in China. There is a need to predict the mobility of these two ions in a geothermal reservoir. Column experiments were performed at temperatures from 15°C to 60°C and the computer code CXTFIT was used to fit the experimental data and to determine the transport parameters and ammonium adsorption parameters. Effects of both the flow rate and temperature on nitrate transport parameters were evaluated. The convection–dispersion equation (CDE) was used to describe the nitrate transport process at temperatures from 15°C to 60°C, where the tracer transport was dominated by advection under experimental conditions. The solute hydrodynamic dispersion and dispersivity in the simulated sandy column were enhanced with the increase of temperature. The asymmetrical shape and tailing of the ammonium breakthrough curve showed that ammonium was subject to nonequilibrium transport. The amounts of adsorbed ammonium increased significantly, while the first-order kinetic rate decreased along with the drop of temperature. ► The loose-pore low-temperature geothermal reservoir environment was simulated. ► The effect of temperature on the transport of ammonium was studied. ► The effect of temperature on nitrate transport parameters was evaluated. ► The transport mechanisms and models of nitrate and ammonium ions were discussed.
AbstractList The concentration of NO3-aN in some of the geothermal water samples collected from Kaifeng City, Henan Province, China has exceeded the World Health Organization's guideline value for drinking water (10 mg/L). The NH4+aN concentration cannot also meet the demand for quality standard for groundwater (0.2 mg/L) in China. There is a need to predict the mobility of these two ions in a geothermal reservoir. Column experiments were performed at temperatures from 15 degree C to 60 degree C and the computer code CXTFIT was used to fit the experimental data and to determine the transport parameters and ammonium adsorption parameters. Effects of both the flow rate and temperature on nitrate transport parameters were evaluated. The convectionadispersion equation (CDE) was used to describe the nitrate transport process at temperatures from 15 degree C to 60 degree C, where the tracer transport was dominated by advection under experimental conditions. The solute hydrodynamic dispersion and dispersivity in the simulated sandy column were enhanced with the increase of temperature. The asymmetrical shape and tailing of the ammonium breakthrough curve showed that ammonium was subject to nonequilibrium transport. The amounts of adsorbed ammonium increased significantly, while the first-order kinetic rate decreased along with the drop of temperature.
The concentration of NO3−―N in some of the geothermal water samples collected from Kaifeng City, Henan Province, China has exceeded the World Health Organization's guideline value for drinking water (10mg/L). The NH4+―N concentration cannot also meet the demand for quality standard for groundwater (0.2mg/L) in China. There is a need to predict the mobility of these two ions in a geothermal reservoir. Column experiments were performed at temperatures from 15°C to 60°C and the computer code CXTFIT was used to fit the experimental data and to determine the transport parameters and ammonium adsorption parameters. Effects of both the flow rate and temperature on nitrate transport parameters were evaluated. The convection–dispersion equation (CDE) was used to describe the nitrate transport process at temperatures from 15°C to 60°C, where the tracer transport was dominated by advection under experimental conditions. The solute hydrodynamic dispersion and dispersivity in the simulated sandy column were enhanced with the increase of temperature. The asymmetrical shape and tailing of the ammonium breakthrough curve showed that ammonium was subject to nonequilibrium transport. The amounts of adsorbed ammonium increased significantly, while the first-order kinetic rate decreased along with the drop of temperature. ► The loose-pore low-temperature geothermal reservoir environment was simulated. ► The effect of temperature on the transport of ammonium was studied. ► The effect of temperature on nitrate transport parameters was evaluated. ► The transport mechanisms and models of nitrate and ammonium ions were discussed.
Author Zhang, Yanxin
Wang, Xinyi
Zhao, Li
A, Lili
Liu, Xiaoman
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  givenname: Li
  surname: Zhao
  fullname: Zhao, Li
  organization: Institute of Resources and Environment, Henan Polytechnic University, Jiaozuo 454000, China
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  givenname: Xiaoman
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  fullname: Liu, Xiaoman
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  givenname: Yanxin
  surname: Zhang
  fullname: Zhang, Yanxin
  organization: Institute of Resources and Environment, Henan Polytechnic University, Jiaozuo 454000, China
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Keywords Ammonium
Loose-pore geothermal reservoir
Nitrate
Fine sand
Breakthrough curve
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Snippet The concentration of NO3−―N in some of the geothermal water samples collected from Kaifeng City, Henan Province, China has exceeded the World Health...
The concentration of NO3-aN in some of the geothermal water samples collected from Kaifeng City, Henan Province, China has exceeded the World Health...
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SubjectTerms Ammonium
Breakthrough curve
C (programming language)
China
Drinking water
Fine sand
Geothermal
Loose-pore geothermal reservoir
Mathematical analysis
Nitrate
Nitrates
Reservoirs
Transport
Title Temperature effect on the transport of nitrate and ammonium ions in a loose-pore geothermal reservoir
URI https://dx.doi.org/10.1016/j.gexplo.2012.08.008
https://www.proquest.com/docview/1429905055
https://www.proquest.com/docview/1753501762
Volume 124
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