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- W2238476054 abstract "Abstract The dependence of runoff dissolved reactive phosphorus ( DRP ) loss on soil test P or rapid estimations of degree of P saturation ( DPS ) often varies with soil types. It is not clear whether the soil‐specific nature of runoff DRP versus DPS is due to the different sorption characteristics of individual soils or the inability of these rapid DPS estimates to accurately reflect the actual soil P saturation status. This study aimed to assess environmental measures of soil P that could serve as reliable predictors of runoff DRP concentration by using soils collected from Ontario, Canada, that cover a range of chemical and physical properties. A P sorption study was conducted using the Langmuir equation to describe amount of P sorbed or desorbed by the soil ( Q s , mg/kg) versus equilibrium P concentration ( C , mg/L) in solution, where Q max is P sorption maximum (mg/kg), k represents P sorption strength (L/mg), and Q 0 (mg/kg) is the P sorbed to soil prior to analysis. Runoff DRP concentration increased linearly with increasing DPS sorp (i.e. the ratio of ( Q 0 + Q D )/ Q max ) following a common slope value amongst soil types, while the P buffering capacity ( PBC 0 ) at C = C 0 yielded a common change point, below which runoff DRP concentration decreased greatly with increasing PBC 0 compared to that above the change point, where C 0 and Q D represent the equilibrium P concentration and amount of P desorbed, respectively. Both DPS sorp and PBC 0 showed great promises as indicators of runoff DRP concentration." @default.
- W2238476054 created "2016-06-24" @default.
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- W2238476054 date "2015-12-22" @default.
- W2238476054 modified "2023-10-17" @default.
- W2238476054 title "Predicting environmental soil phosphorus limits for dissolved reactive phosphorus loss" @default.
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- W2238476054 doi "https://doi.org/10.1111/sum.12238" @default.
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