Principles, Application and Assessment in Soil Science 2011
DOI: 10.5772/29556
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Phosphorus: Chemism and Interactions

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Cited by 5 publications
(5 citation statements)
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“…Most of the previous studies concentrate on the monitoring of green roof runoff quality [7,[9][10][11]14], not on substrate chemical composition. In some exceptions, e.g., [64], substrate mix components are analyzed for chemical composition but phosphorus, which excess loads have the potential to increase eutrophication risk for lakes and rivers, is not included. For the sustainable use of green roofs it is therefore suggested to test the substrate and its components as a potential source of P in runoff.…”
Section: Discussionmentioning
confidence: 99%
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“…Most of the previous studies concentrate on the monitoring of green roof runoff quality [7,[9][10][11]14], not on substrate chemical composition. In some exceptions, e.g., [64], substrate mix components are analyzed for chemical composition but phosphorus, which excess loads have the potential to increase eutrophication risk for lakes and rivers, is not included. For the sustainable use of green roofs it is therefore suggested to test the substrate and its components as a potential source of P in runoff.…”
Section: Discussionmentioning
confidence: 99%
“…Most of the mineral materials tested in this study contain phosphorus in different amounts that ranged between 5.3-130 mg P-PO 4 /kg in hydrochloric acid extracts. This fraction represents apatite and calcium associated P [64] and is not available for plants, however it can be released from substrate at low pH. The phosphorus found in water extracts was detected for crushed red brick and pollytag, and is available for easily leaching by rain percolation through green roof substrate.…”
Section: Discussionmentioning
confidence: 99%
“…In the slightly acidic soil, H 2 PO $ _4^ - $ is the main water‐soluble phosphate anion ( Henderson , 2011). Labile Fe 3+ /Al 3+ can be hydrolyzed into Fe‐/Al‐OH and then absorb and fix water‐soluble H 2 PO $ _4^ - $ to decrease the availability of P in the soil ( Saljnikov and Cakmak , 2011; Jan et al, 2015). O‐P is almost unavailable for plant uptake when a thin film of Fe 2 O 3 exists as a ‘shield' all around ( Hu et al, 2012), while Fe‐P and Al‐P, occluded in O‐P, are relatively available P sources in slightly acidic conditions ( Henderson , 2011).…”
Section: Discussionmentioning
confidence: 99%
“…The amount of total P in soil varies from 50 to 5000 mg/kg in top 0-30 cm soil (Mengel andKirkby 2001, Saljnikov andCakmak 2012). However, compared with the other major nutrients, the P is the least mobile and less available to plants in most soil conditions.…”
mentioning
confidence: 99%