Groundwater resources around the world are becoming stressed from continued extraction. Advances in pumping technology, growth of irrigated agriculture, and increased population have rapidly increased groundwater use over the past 60 years (Dillon et al., 2018; OECD, 2015). At the same time, many rivers are fully appropriated, and surface water is becoming increasingly variable under climate change (Scanlon et al., 2016). Water managers have responded with increased use of managed aquifer recharge (MAR), the "intentional storing and treatment of water in aquifers" (see also Dillon, 2005; National Research Council et al., 2008; Scanlon et al., 2016). Equation 1 (Scanlon et al., 2016) relates total groundwater storage (GWS) to natural and anthropogenic sources of aquifer inflow and outflow. Inflow is the sum of natural recharge (R NAT) and human recharge, including irrigation (R IRR) and MAR (R MAR); outflow is the sum of natural discharge (Q NAT), including baseflow to streams and riparian evapotranspiration, and anthropogenic pumping (Q PU). To stabilize or increase groundwater levels, water managers can reduce outputs, increase inputs, or both. MAR (R MAR) aims to directly influence recharge by moving water into the aquifer; it is generally contrasted with nonmanaged recharge that occurs as a side effect of irrigation, reservoir storage, and other practices (R IRR) (Dillon et al., 2018; Scanlon et al., 2016). There are numerous physical aquifer recharge technologies, such as slowing down instream flows with check dams, letting water infiltrate through spreading basins, and injecting water through a well or borehole (