2013
DOI: 10.1155/2013/597824
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Nitrate Sorption in an Agricultural Soil Profile

Abstract: Increasing concentrations of NO 3 − in surface water and groundwater can cause ecological and public health effects and has come under increased scrutiny by both environmental scientists and regulatory agencies. For many regions though, including the Sahel of Tunisia, little is known about the NO 3 − sorption capacity of soils. In this project we measured NO 3 − sorption by a profile of an isohumic soil from Chott Meriem, Tunisia. Soil samples were collected from four soil depths (0-25, 25-60, 60-90, and 90-12… Show more

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Cited by 25 publications
(20 citation statements)
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“…A number of researchers [7,8,[29][30][31] reported that two nonlinear adsorption isotherms, namely, Langmuir and Freundlich, are the best models to explain the trend of adsorption based on the essence of absorbents saturated with adsorbate after enough contact time.…”
Section: Estimation Of Adsorptionmentioning
confidence: 99%
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“…A number of researchers [7,8,[29][30][31] reported that two nonlinear adsorption isotherms, namely, Langmuir and Freundlich, are the best models to explain the trend of adsorption based on the essence of absorbents saturated with adsorbate after enough contact time.…”
Section: Estimation Of Adsorptionmentioning
confidence: 99%
“…However, the increasing rate of nitrate adsorption decelerated with further increase in nitrate concentration. This behavior is due to the increase in the driving force of the concentration gradient, as further increase in the initial nitrate concentration overcomes the limitations of low adsorption by absorbent [7]. Such phenomenon is common in a batch test with either constant adsorbent dose or varying initial adsorbate concentration or vice versa [34].…”
Section: Effect Of Initial Concentrationmentioning
confidence: 99%
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“…The transport of nitrate in groundwater under oxic redox conditions can be assumed to be conservative since nitrate shows no or only little sorption effects on the aquifer matrix and does not precipitate as mineral phase (Hamdi et al, ; Harper, ; Singh & Kanehiro, ). In such oxic aquifers, the residence time of nitrate in groundwater may vary from less than 1 year to several decades or even centuries depending on the apparent mean transit times (MTT) of groundwater (Koh et al, ; Sebilo et al, ; Wassenaar et al, ).…”
Section: Introductionmentioning
confidence: 99%
“…Langmuir and Freundlich are the best models to explain the trend of adsorption based on the essence of absorbents saturated with adsorbate after enough contact time. (33), (34), (35), (36 279 absorbance by spectrophotometer (using kits).And the data was fitted into the following isotherms: Langmuir, Freundlich, which are shown in Fig (9a, b).…”
Section: Adsorption Isotherm Of So 4 -2 Ion By (Amberlyst A21)mentioning
confidence: 99%