2022
DOI: 10.1002/agg2.20229
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Phosphorus and potassium mineralization as affected by phosphorus levels and soil types under laboratory condition

Abstract: Nutrients’ mineralization‐immobilization in soil is crucial for their management in crop production. An incubation experiment was conducted to study the effects of phosphorus levels on mineralization of phosphorus (P) and potassium (K) under three soil types in laboratory conditions at the National Soil Science Research Center in Nepal with 3 × 4 factorial completely randomized design. Two factors were three soil types (silty clay loam, loam, and sandy loam) and four P levels: 0, 25, 50, and 75 kg P2O5 ha–1. F… Show more

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Cited by 14 publications
(11 citation statements)
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“…Phosphorus is usually more abundant in the upper soil layers, as P is generally considered an immobile element in the soil; hence, as soil pH changes, the activities of P and the other elements with which P can react in the soil will also change. In the soil, P is most readily available between pH 6 and 7.5 (Hinsinger, 2001; Penn & Camberato, 2019; Prasad & Chakraborty, 2019; Rawal et al., 2022), a range in which all the soils in this study fell. If P is rendered more mobile through pH‐induced dissolution, P will then be able to leach downward into the soil profile and potentially beyond the plant root zone where P saturation may eventually occur, posing a threat to leachate/subsurface water quality (Wang et al., 2019) in soils that have shallow or perched water tables.…”
Section: Resultsmentioning
confidence: 86%
See 1 more Smart Citation
“…Phosphorus is usually more abundant in the upper soil layers, as P is generally considered an immobile element in the soil; hence, as soil pH changes, the activities of P and the other elements with which P can react in the soil will also change. In the soil, P is most readily available between pH 6 and 7.5 (Hinsinger, 2001; Penn & Camberato, 2019; Prasad & Chakraborty, 2019; Rawal et al., 2022), a range in which all the soils in this study fell. If P is rendered more mobile through pH‐induced dissolution, P will then be able to leach downward into the soil profile and potentially beyond the plant root zone where P saturation may eventually occur, posing a threat to leachate/subsurface water quality (Wang et al., 2019) in soils that have shallow or perched water tables.…”
Section: Resultsmentioning
confidence: 86%
“…Post‐leaching WS K differences could also have been a factor of soil pH changes, where soil pH increased with the addition of water, which may have facilitated the dissolution of other cations and displaced OH − and basic cations from exchange sites and into solution. The increased pH above 6.0 may have caused K release, as K is commonly released from the soil's nonexchangeable pools above pH 6.0 (Kibreselassie et al., 2017; Rawal et al., 2022).…”
Section: Resultsmentioning
confidence: 99%
“…For example, the positive correlation between Variovorax and Aspergillus with pH, Conversely, Arthrobacter was negatively correlated with EC, dehydrogenase, and nitrate reductase, Burkholderia with P, Variovorax and Aspergillus with K, Trichoderma with moisture, EC, SOC, Cu, dehydrogenase, protease, acid phosphatase, and urease, and Chaetomium with EC and nitrate reductase. Aspergillus was found to adapt well to stress and higher pH conditions, while in winter, soil pH decreased, impacting available K and soil microbial processes (Lladó et al, 2017b;Markina-Iñarrairaegui et al, 2020;Rawal et al, 2022). Soil C, N, and P cycling involve multiple microbial processes such as mineral acquisition, transportation, and availability to plants (Yang et al, 2010;Brockett et al, 2012;Koyama et al, 2018;Liu et al, 2019;Świątek and Pietrzykowski, 2022).…”
Section: Discussionmentioning
confidence: 99%
“…More research is needed to investigate the effects of DCAP on P-Al and P-Fe concentrations in acidic soils, which are factors that significantly influence the availability of P in the soil. Moreover, the study of K availablity content in ASSs is necessary because available K may be affected by key reasons, including soil texture, mineralogy, temperature, and soil acidity ( Rawal et al, 2022 ). In addition, the relationship between K and P availability in acidic soils need to be clarified in the next studies.…”
Section: Discussionmentioning
confidence: 99%