2015
DOI: 10.1007/s12665-015-4586-1
|View full text |Cite
|
Sign up to set email alerts
|

Evaluation of contaminant transport parameters for hexavalent chromium migration through saturated soil media

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

0
6
0

Year Published

2017
2017
2024
2024

Publication Types

Select...
6
1

Relationship

0
7

Authors

Journals

citations
Cited by 11 publications
(6 citation statements)
references
References 18 publications
0
6
0
Order By: Relevance
“…A negative correlation between Cd and Pb was discovered with soil saturation, while a positive correlation was found with Cr. The Cr with its oxidation states may affect greater downward mobility in the presence of high soil saturation [58]. Generally Cr is highly mobile in soil, however, Cr(VI), due to its anionic nature, can be adsorbed by clays, iron and manganese oxides and hydroxides in acidic soil because of an increase in positively charged sites at mineral surfaces [59].…”
Section: The Exploratory Analysis Of Soil Variablesmentioning
confidence: 99%
“…A negative correlation between Cd and Pb was discovered with soil saturation, while a positive correlation was found with Cr. The Cr with its oxidation states may affect greater downward mobility in the presence of high soil saturation [58]. Generally Cr is highly mobile in soil, however, Cr(VI), due to its anionic nature, can be adsorbed by clays, iron and manganese oxides and hydroxides in acidic soil because of an increase in positively charged sites at mineral surfaces [59].…”
Section: The Exploratory Analysis Of Soil Variablesmentioning
confidence: 99%
“…Gupta and Bahu () successfully simulated breakthrough curves of Cr(VI) by combining the Langmuir model with a mathematical transport model. Chakraborty, Ghosh, Ghosh, and Mukherjee () embedded the Langmuir and linear isotherms, respectively, in a one‐dimensional advection–dispersion–reaction equation to estimate Cr(VI) transport parameters. Such isotherms have also been integrated in well‐known numerical codes (e.g., Hydrus‐1D [Šimůnek, Šejna, Saito, Sakai, & van Genuchten, ] and MT3DMS [Zheng & Wang, ]) to simulate reactive solute migration.…”
Section: Introductionmentioning
confidence: 99%
“…Mathematical model of copper ion transport in sediment is derived by applying the conservation law of mass [ 64–66 ] and mass flux [ 67 ] and has the form: θCtbadbreak=D2Cx2goodbreak+λCgoodbreak+K,$$\begin{equation}\theta \frac{{\partial C}}{{\partial t}} = D\frac{{{\partial ^2}C}}{{\partial {x^2}}} + \lambda C + K,\end{equation}$$where C = C ( x , t ) is the concentration which depends on the position x and time t , D is the effective diffusion term of copper, λ is the constant with the concentration C , which includes electric and hydraulic properties of the system and K is a constant which represents the flow rate of aquifer and its concentration. Mass conservation Equation (1) is a second‐order differential equation whose solution is assumed in the form: Cbadbreak=bgoodbreak−aexp()ptsx,$$\begin{equation}C = b - a\exp{\left(pt - sx\right)},\end{equation}$$where a , b , p , and s are unknown constants.…”
Section: Resultsmentioning
confidence: 99%
“…The suggested procedure has been already applied for simulation of Ni transport in sediment. [19] Mathematical model of copper ion transport in sediment is derived by applying the conservation law of mass [64][65][66] and mass flux [67] and has the form:…”
Section: Mathematical Model-numerical Simulation Of the Transport Phe...mentioning
confidence: 99%