Incidental losses of dissolved reactive phosphorus (DRP) to a surface waterbody originate from direct losses during land application of fertilizer, or where a rainfall event occurs immediately thereafter. Another source is the soil. One way of immobilising DRP in runoff before discharge to a surface waterbody, is to amend soil within the edge of field area with a high phosphorus (P) sequestration material. One such amendment is iron ochre, a by-product of acid mine drainage. Batch experiments utilising two grassland soils at two depths (topsoil and sub-soil), six ochre amendment rates (0, 0.15, 1.5, 7.5, 15 and 30 g kg-1 mass per dry weight (dwt) of soil) and five P concentrations (0, 5, 10, 20 and 40 mg L-1) were carried out. A proportional equation, which incorporated P sources and losses, was developed and used to form a statistical model. Back calculation identified optimal rates of ochre amendment to soil to ameliorate a specific DRP concentration in runoff. Ochre amendment of soils (with no further P inputs) was effective at decreasing DRP concentrations to acceptable levels. A rate of 30 g ochre kg-1 soil was needed to decrease DRP concentrations to acceptable levels for P inputs of ≤ 10 mg L-1, which represents the vast majority of cases in grassland runoff experiments. However, although very quick and sustained metal release above environmental limits occurred, which makes it unfeasible for use as a soil amendment to control P release to a waterbody, the methodology developed within this paper may be used to test the effectiveness and feasibility of other amendments.
1The Effectiveness and Feasibility of using Ochre as a Soil immobilising DRP in runoff before discharge to a surface waterbody, is to amend soil 17 within the edge of field area with a high phosphorus (P) sequestration material. One 18 such amendment is iron ochre, a by-product of acid mine drainage. Batch experiments 19 utilising two grassland soils at two depths (topsoil and sub-soil), six ochre amendment 20 rates (0, 0.15, 1.5, 7.5, 15 and 30 g kg -1 mass per dry weight (dwt) of soil) and five P 21 concentrations (0, 5, 10, 20 and 40 mg L -1 ) were carried out. A proportional equation, 22 which incorporated P sources and losses, was developed and used to form a statistical 23 model. Back calculation identified optimal rates of ochre amendment to soil to 24 ameliorate a specific DRP concentration in runoff. Ochre amendment of soils (with no 25 further P inputs) was effective at decreasing DRP concentrations to acceptable levels. 26A rate of 30 g ochre kg -1 soil was needed to decrease DRP concentrations to 27 acceptable levels for P inputs of ≤ 10 mg L -1 , which represents the vast majority of 28 cases in grassland runoff experiments. However, although very quick and sustained 29 metal release above environmental limits occurred, which makes it unfeasible for use 30 as a soil amendment to control P release to a waterbody, the methodology developed 31 within this paper may be used to test the effectiveness and feasibility of ot...