“…In many irrigated orchard crops, OMA sources have been shown to increase soil C storage (Bittenbender et al, 1998; Canali et al, 2004; Neilsen et al, 2014; Sanchez et al, 2003). Many different OMA sources are also capable of increasing soil extractable P (Neilsen et al, 2014; Preusch & Tworkoski, 2003) and K (Baldi et al, 2010; Bittenbender et al, 1998; Gülser et al, 2015) as well as improving cation exchange capacity (Cayuela et al, 2004; Arvanitoyannis & Kassaveti, 2007; Amiri & Fallahi, 2009; Miller et al, 2013; Villa et al, 2021) without increasing the risk of soil pollution from heavy metals (Baldi et al, 2021). Despite these studies, understanding P and K availability in relation to OMA use is necessary given the potential effects by phosphatase activity (Neilsen et al, 2014), soluble factors of these nutrients (Brandt et al, 2004; Hammermeister et al, 2006) and surface application (Baitilwake et al, 2012; Corbeels et al, 2003; Jin et al, 2008).…”