“…Since in many cases DOC and nitrogen species concentrations are of the greatest interest, SAT modeling often focuses on processes such as organic carbon consumption by bacteria and bacteria‐mediated nitrogen processes (i.e., mineralization, nitrification, and denitrification). These processes, as mentioned above, are widely discussed in many subareas of soil sciences, and models containing a combination of these processes with various water flow conditions are readily available in the literature (Berlin, Kumar, & Nambi, 2014; Liu et al., 2018; Yang, Wang, Lu, & Jayawardane, 2008). Most of the models that combine unsaturated water flow with carbon and nitrogen dynamics in the soil are solved numerically, often using the finite elements or finite differences methods (Berlin et al., 2014).…”