“…shown in Equation 1 and Figure 2. Ra in groundwater can also be derived from external U-and Th-rich sources, such as effluents from uranium mining (Carvalho et al, 2007;De Pree, 2020;Gil-Pacheco et al, 2020;Mangeret et al, 2020;Mathuthu et al, 2020;Matshusa and Makgae, 2017;Ruedig and Johnson, 2015), oil and gas wastewater (Agbalagba et al, 2013;Ahmad et al, 2021;Jaeschke et al, 2020;Knee and Masker, 2019;Lauer et al, 2018;Ni et al, 2018;Tomita et al, 2010;Van Sice et al, 2018;Vengosh et al, 2014;Warner et al, 2013), and deicing using oil-produced water (Lazur et al, 2020;McNaboe et al, 2017). Both Ra and U are enriched in phosphorite rocks, but during extraction and fertilizer production most of the Ra is incorporated in the solid waste product (phosphogysum), while U is enriched in the fertilizers (Al Attar et al, 2011;Barisic et al, 1992;Haridasan et al, 2002;Hassan et al, 2016;Lauria et al, 2004;Pearson et al, 2019;Sandhu et al, 2018).…”