“…The physicochemical reactions of P between overlying water and sediment in natural systems include adsorption/desorption and precipitation/dissolution reactions, which together, regulate soluble P concentrations in natural rivers, streams and estuaries (Wauchope and McDowell, 1984;Price et al, 2010). This phenomenon is known as the "phosphate buffer mechanism" (Richardson, 1985), which assumes that sediment, whether benthic or suspended, maintain dissolved reactive phosphate concentrations at some near-constant value regardless of biological removal and exogenic inputs (Froelich, 1988).…”