2013
DOI: 10.1080/19648189.2013.788984
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Numerical modelling on fate and transport of nitrate in an unsaturated system under non-isothermal condition

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Cited by 18 publications
(8 citation statements)
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“…This temperature variation can affect the biological activity (nitrification and denitrification) and further affect the concentration of nitrogen species (Saadi and Maslouhi 2003;Berlin et al 2013). Since, current study focuses more on biological clogging; the authors have assumed that the unsaturated domain can be treated under isothermal conditions.…”
Section: Physical System and Model Formulationmentioning
confidence: 99%
See 1 more Smart Citation
“…This temperature variation can affect the biological activity (nitrification and denitrification) and further affect the concentration of nitrogen species (Saadi and Maslouhi 2003;Berlin et al 2013). Since, current study focuses more on biological clogging; the authors have assumed that the unsaturated domain can be treated under isothermal conditions.…”
Section: Physical System and Model Formulationmentioning
confidence: 99%
“…The reduction and transport of various nitrogen species in unsaturated zone are affected by nitrate input, volumetric water content, depth of water table, pH, temperature, microbial activity (Huang et al 2012). Berlin et al (2013) studied the fate and transport of nitrate in an unsaturated system under non-isothermal condition.…”
Section: Introductionmentioning
confidence: 99%
“…connected to tile drains, for instance, may be most important in terms of the rapid movement of land-surface-derived contaminants to subsurface water flow systems (e.g., tile drains) (Fleming and Bradshaw, 1992;Fox et al, 2004;Akay and Fox, 2007;Frey et al, 2016). A substantial body of literature has been produced regarding N transformations and transport in agricultural soils (i.e., Lee et al, 2006;Berlin et al, 2013Berlin et al, , 2014aLi et al, 2015). And while some studies have characterized or modeled macropore connectivity in soil in the context of flow (Akay et al, 2008;Klaus and Zehe, 2010), there is a need to elucidate dynamic chemical transformations and transport in soil macropores under various degrees of macropore connectivity (Jarvis et al, 2017).…”
mentioning
confidence: 99%
“…Vadose zone thickness can extend several meters and the soil hydraulic parameters are nonlinear [27][28][29][30][31]. Few studies indicated the vadose zone thickness can extend up to 50 m [32].…”
Section: Introductionmentioning
confidence: 99%