2020
DOI: 10.1016/j.rsma.2020.101083
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Influence of hypoxia on phosphorus cycling in Alappuzha mud banks, southwest coast of India

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Cited by 6 publications
(4 citation statements)
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“…P i concentrations also decrease as a function of soil development, ranging from an average of 684 µg /g soil in Entisols, to between 200 and 430 µg/g soil in Ultisols and Oxisols [29]. P i exists in different forms and proportions in soil, which may leach into streams to deposit P in ocean sediments, or be taken up by plants or soil microorganisms in the secondary P o cycle [41]. After mineralization by plant structures (e.g., roots, stems, leaves), dead soil animals, and microorganisms, a large share of the assimilated P o returns to soils [42].…”
Section: Basic P Forms and P Cycling In The Soilmentioning
confidence: 99%
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“…P i concentrations also decrease as a function of soil development, ranging from an average of 684 µg /g soil in Entisols, to between 200 and 430 µg/g soil in Ultisols and Oxisols [29]. P i exists in different forms and proportions in soil, which may leach into streams to deposit P in ocean sediments, or be taken up by plants or soil microorganisms in the secondary P o cycle [41]. After mineralization by plant structures (e.g., roots, stems, leaves), dead soil animals, and microorganisms, a large share of the assimilated P o returns to soils [42].…”
Section: Basic P Forms and P Cycling In The Soilmentioning
confidence: 99%
“…P i exists in different forms and proportions in soil, which may leach into streams to deposit P in ocean sediments, or be taken up by plants or soil microorganisms in the secondary P o cycle [ 41 ]. After mineralization by plant structures (e.g., roots, stems, leaves), dead soil animals, and microorganisms, a large share of the assimilated P o returns to soils [ 42 ].…”
Section: Basic P Forms and P Cycling In The Soilmentioning
confidence: 99%
“…The upwelling induced hypoxic conditions in mudbank regions were studied by many, and these hypoxic conditions induced significant changes in the presence of the elements as carbon, phosphorus, iron, and manganese [49][50][51]. Fig 5 shows the seasonal variations in temperature, salinity and dissolved oxygen in madbank region of Alappuzha [52]. Results show the variations of the above parameters based on observations at three locations -(1) mudbank region (M2), (2) alongshore non-mudbank region (M1) and (3) offshore non-mudbank region (M3).…”
Section: Biogeochemical Processes In Mudbanksmentioning
confidence: 99%
“…Inorganic P is present in soil in a variety of forms and proportions (Mathew et al, 2020). It may leach into rivers to store P in marine sediments, or absorbed by plants or soil microbes to participate in the secondary organic phosphorus cycle.…”
mentioning
confidence: 99%