2017
DOI: 10.2134/agronj2016.07.0409
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Long‐Term Agronomic Drawdown of Soil Phosphorus in Mid‐Atlantic Coastal Plain Soils

Abstract: Core Ideas Rate of soil P drawdown is a slow process having economic impacts to producers. Cropping system affected drawdown of soil P concentrations at all locations. Forage cropping systems exhibited faster soil P drawdown. Lower initial soil P status resulted in faster soil P drawdown at one location. Soils could take 18 to 44 yr to return to agronomic optimum P concentrations. Phytoremediation remains the only management option to lower soil P concentrations. Elevated soil P concentrations exist where manu… Show more

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Cited by 38 publications
(54 citation statements)
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“…However, this process of soil P "draw-down" can require decades. For example, Fiorellino et al [9] conducted a long term P draw-down study on soils that had initial Mehlich-3 P concentrations ranging from 200 to nearly 400 mg kg −1 . The authors ceased P applications and removed soil P via grain and forage crop rotations; they estimated 20 to 25 years until soil P levels return to 100 mg kg −1 .…”
Section: Purpose and Justification For Phosphorus Removal Structuresmentioning
confidence: 99%
“…However, this process of soil P "draw-down" can require decades. For example, Fiorellino et al [9] conducted a long term P draw-down study on soils that had initial Mehlich-3 P concentrations ranging from 200 to nearly 400 mg kg −1 . The authors ceased P applications and removed soil P via grain and forage crop rotations; they estimated 20 to 25 years until soil P levels return to 100 mg kg −1 .…”
Section: Purpose and Justification For Phosphorus Removal Structuresmentioning
confidence: 99%
“…Second, typical rates of annual crop P removal (∼20 to 40 kg ha −1 ) are often orders of magnitude less than total soil P in high P soils (∼3000 to 4000 kg ha −1 in a 0‐ to 30‐cm depth). Therefore, once soil P has become high, it can remain in excess of agronomic needs for years to decades and lose P to the environment at rates that impair water quality (Fiorellino et al, 2017). It is important from both management and policy perspectives to have realistic expectations about the pace of water quality improvement in watersheds with widespread legacy soil P. It is therefore necessary to reliably estimate rates of soil P drawdown and associated rates of P loss in runoff and erosion for a variety of soil and management conditions.…”
mentioning
confidence: 99%
“…Fiorellino et al (2017) and Kamprath (1999) demonstrated that at very high STP (>100 mg kg −1 ; as Mehlich‐3 P), crop yields were not affected for over 15 yr when P applications ceased. Extrapolating STP drawdown, these researchers suggested it would take more than 30 yr to decrease STP below the agronomic critical level depending on the soil texture and initial soil test level.…”
Section: Implementing Conservation Practices That Reduce Agriculturalmentioning
confidence: 99%
“…The STP of Lynchburg soil (fine‐loamy, siliceous, semiactive, thermic Aeric Paleaquult) was three times greater than the agronomic critical level (50 mg kg −1 ), the level at which a yield response would be expected (Kamprath, 1999). Elevated STP was more than seven times greater than the agronomic critical level (also 50 mg kg −1 for Maryland) in Mattapex silt loam (fine‐silty, mixed active, mesic Aquic Hapludult) (Fiorellino et al, 2017). …”
Section: Implementing Conservation Practices That Reduce Agriculturalmentioning
confidence: 99%