Influence of agricultural managed aquifer recharge on nitrate transport: The role of soil texture and flooding frequency

Agricultural managed aquifer recharge (Ag‐MAR) is a concept in which farmland is flooded during the winter using excess surface water to recharge the underlying groundwater. In this study, we show how different recharge practices affect NO 3 − leaching and mineralization–denitrification processes in different soil systems. Two contrasting soil textures (sand and fine sandy loam) from the Central Valley, California, were repeatedly flooded with 15 cm of water at varying time intervals in field and soil column experiments. Nitrogen species (NO 3 – , NH 4 + , total N), total C, dissolved O 2 , and moisture content were measured throughout the experiments. Results show that when flooding occurs at longer intervals (every 1–2 wk), N mineralization increases, leading to an increase of mobile NO 3 − in the upper root zone and leaching of significant quantities of NO 3 − from both soil textures (137.3 ± 6.6% [sand] and 145.7 ± 5.8% [fine sandy loam] of initial residual soil NO 3 − ) during subsequent flooding events. Laboratory mineralization incubations show that long flooding intervals promote mineralization and production of excess NO 3 − at rates of 0.11–3.93 mg N kg –1 wk –1 (sand) and 0.08–3.41 mg N kg –1 wk –1 (fine sandy loam). Decreasing the flooding frequency to 72 h reduces potential mineralization, decreasing the amount of NO 3 − leached during flooding events (31.7 ± 3.8% [sand] and 64.7 ± 10.4% [fine sandy loam] of initial residual soil NO 3 – ). The results indicate that implementing recharge as repeated events over a long (multiple‐week) time horizon might increase the total amount of NO 3 − potentially available for leaching to groundwater.