Biological P cycling is influenced by the form of P fertilizer in an Oxisol

Phosphate rock (PR) is an alternative fertilizer to increase the P content of P-deficient weathered soils. We evaluated the effects of fertilizer form on indicators of biological cycling of P using an on-farm trial on a Rhodic Kandiudox in western Kenya. Treatment plots were sampled after 13 croppin...

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Main Authors: Margenot, Andrew J., Sommer, Rolf, Mukalama, John, Parikh, Sanjai J.
Format: Journal Article
Language:Inglés
Published: Springer 2017
Subjects:
Online Access:https://hdl.handle.net/10568/83158
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author Margenot, Andrew J.
Sommer, Rolf
Mukalama, John
Parikh, Sanjai J.
author_browse Margenot, Andrew J.
Mukalama, John
Parikh, Sanjai J.
Sommer, Rolf
author_facet Margenot, Andrew J.
Sommer, Rolf
Mukalama, John
Parikh, Sanjai J.
author_sort Margenot, Andrew J.
collection Repository of Agricultural Research Outputs (CGSpace)
description Phosphate rock (PR) is an alternative fertilizer to increase the P content of P-deficient weathered soils. We evaluated the effects of fertilizer form on indicators of biological cycling of P using an on-farm trial on a Rhodic Kandiudox in western Kenya. Treatment plots were sampled after 13 cropping seasons of P applications as Minjingu phosphate rock (PR) or as triple super phosphate (TSP) (50 kg P ha−1 season−1), as well as a P-unfertilized control (0 kg P ha−1 season−1). Soils (0–15 and 15–30 cm) were analyzed for microbial biomass P (Pmic), activities of acid phosphomonoesterase, alkaline phosphomonoesterase, and phosphodiesterase, and sequentially extractable P fractions. P additions as Minjingu PR yielded 299% greater Pmic than TSP at 0–15-cm depth despite similar labile P concentrations in the two P fertilization treatments and stimulated activities of acid phosphomonoesterase (+39%). When added in the soluble form of TSP, a greater percentage of total soil P was present in mineral-bound forms (+33% Fe- and Al-associated P). Higher soil pH under Minjingu PR (pH 5.35) versus TSP (pH 5.02) and the P-unfertilized treatment (pH 4.69) at 0–15-cm depth reflected a liming effect of Minjingu PR. The form of P fertilizer can influence biological P cycling in weathered soils, potentially improving P availability under Minjingu PR relative to TSP via enhanced microbial biomass P and enzymatic drivers of P cycling.
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spelling CGSpace831582025-03-13T09:44:04Z Biological P cycling is influenced by the form of P fertilizer in an Oxisol Margenot, Andrew J. Sommer, Rolf Mukalama, John Parikh, Sanjai J. phosphorus phosphatase oxisol soil soil properties soil fertility fósforo ferralsoles microbiology Phosphate rock (PR) is an alternative fertilizer to increase the P content of P-deficient weathered soils. We evaluated the effects of fertilizer form on indicators of biological cycling of P using an on-farm trial on a Rhodic Kandiudox in western Kenya. Treatment plots were sampled after 13 cropping seasons of P applications as Minjingu phosphate rock (PR) or as triple super phosphate (TSP) (50 kg P ha−1 season−1), as well as a P-unfertilized control (0 kg P ha−1 season−1). Soils (0–15 and 15–30 cm) were analyzed for microbial biomass P (Pmic), activities of acid phosphomonoesterase, alkaline phosphomonoesterase, and phosphodiesterase, and sequentially extractable P fractions. P additions as Minjingu PR yielded 299% greater Pmic than TSP at 0–15-cm depth despite similar labile P concentrations in the two P fertilization treatments and stimulated activities of acid phosphomonoesterase (+39%). When added in the soluble form of TSP, a greater percentage of total soil P was present in mineral-bound forms (+33% Fe- and Al-associated P). Higher soil pH under Minjingu PR (pH 5.35) versus TSP (pH 5.02) and the P-unfertilized treatment (pH 4.69) at 0–15-cm depth reflected a liming effect of Minjingu PR. The form of P fertilizer can influence biological P cycling in weathered soils, potentially improving P availability under Minjingu PR relative to TSP via enhanced microbial biomass P and enzymatic drivers of P cycling. 2017-11 2017-08-16T16:03:35Z 2017-08-16T16:03:35Z Journal Article https://hdl.handle.net/10568/83158 en Open Access Springer Margenot, Andrew J.; Sommer, Rolf; Mukalama, John; Parikh, Sanjai J.. 2017. Biological P cycling is influenced by the form of P fertilizer in an Oxisol . Biology and Fertility of Soils 53(8): 899-909.
spellingShingle phosphorus
phosphatase
oxisol
soil
soil properties
soil fertility
fósforo
ferralsoles
microbiology
Margenot, Andrew J.
Sommer, Rolf
Mukalama, John
Parikh, Sanjai J.
Biological P cycling is influenced by the form of P fertilizer in an Oxisol
title Biological P cycling is influenced by the form of P fertilizer in an Oxisol
title_full Biological P cycling is influenced by the form of P fertilizer in an Oxisol
title_fullStr Biological P cycling is influenced by the form of P fertilizer in an Oxisol
title_full_unstemmed Biological P cycling is influenced by the form of P fertilizer in an Oxisol
title_short Biological P cycling is influenced by the form of P fertilizer in an Oxisol
title_sort biological p cycling is influenced by the form of p fertilizer in an oxisol
topic phosphorus
phosphatase
oxisol
soil
soil properties
soil fertility
fósforo
ferralsoles
microbiology
url https://hdl.handle.net/10568/83158
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