scholarly journals Wastewater‐recovered struvite effects on total extractable phosphorus compared with other phosphorus sources

age ◽  
2021 ◽  
Vol 4 (2) ◽  
Author(s):  
Ryder Anderson ◽  
Kristofor R. Brye ◽  
Lauren Greenlee ◽  
Trent L. Roberts ◽  
Edward Gbur
Keyword(s):  
Phosphorus Sources ◽  
Extractable Phosphorus

INFLUENCE OF PHOSPHORUS SOURCES AND RATES ON SOIL pH, EXTRACTABLE PHOSPHORUS, AND DTPA-EXTRACTABLE MICRONUTRIENTS1

Soil Science ◽  
1987 ◽  
Vol 144 (1) ◽  
pp. 36-42 ◽  
Author(s):  
A. M. AL-SHOWK ◽  
R. L. WESTERMAN ◽  
D. L. WEEKS
Keyword(s):  
Soil Ph ◽  
Phosphorus Sources ◽  
Extractable Phosphorus

scholarly journals Electrochemically precipitated struvite effects on extractable nutrients compared with other fertilizer‐phosphorus sources

age ◽  
2021 ◽  
Vol 4 (2) ◽  
Author(s):  
Ryder Anderson ◽  
Kristofor Brye ◽  
Laszlo Kekedy‐Nagy ◽  
Lauren Greenlee ◽  
Edward Gbur ◽  
...  
Keyword(s):  
Phosphorus Sources ◽  
Extractable Nutrients

scholarly journals Estimation of Phosphorus and Nitrogen Waste in Rainbow Trout (Oncorhynchus mykiss, Walbaum, 1792) Diets Including Different Inorganic Phosphorus Sources

Animals ◽  
2021 ◽  
Vol 11 (6) ◽  
pp. 1700
Author(s):  
Maria Consolación Milián-Sorribes ◽  
Ana Tomás-Vidal ◽  
David S. Peñaranda ◽  
Laura Carpintero ◽  
Juan S. Mesa ◽  
...  
Keyword(s):  
Rainbow Trout ◽  
Oncorhynchus Mykiss ◽  
Inorganic Phosphorus ◽  
Point Of View ◽  
Inorganic P ◽  
Monocalcium Phosphate ◽  
Rainbow Trout Oncorhynchus Mykiss ◽  
Phosphorus Sources ◽  
Total P ◽  
P Sources

This study was conducted to evaluate the apparent availability and P and N excretion in rainbow trout (Oncorhynchus mykiss) using different inorganic phosphorus sources. With this goal, fish (153 ± 14.1 g) fed four inorganic P sources were assayed: monoammonium phosphate (MAP, NH4H2PO4), monosodium/monocalcium phosphate (SCP-2%, AQphos+, NaH2PO4/Ca(H2PO4)2·H2O in proportion 12/88), monosodium/monocalcium phosphate (SCP-5%, NaH2PO4/Ca(H2PO4)2·H2O in proportion 30/70) and monocalcium phosphate (MCP, Ca(H2PO4)2·H2O). Phosphorus (P) digestibility, in diets that included MAP and SCP-2% as inorganic phosphorus sources, were significantly higher than for SCP-5% and MCP sources. In relation to the P excretion pattern, independent of the diet, a peak at 6 h after feeding was registered, but at different levels depending on inorganic P sources. Fish fed an MAP diet excreted a higher amount of dissolved P in comparison with the rest of the inorganic P sources, although the total P losses were lower in MAP and SCP-2% (33.02% and 28.13, respectively) than in SCP-5% and MCP sources (43.35% and 47.83, respectively). Nitrogen (N) excretion was also studied, and the fish fed an SCP-5% diet provided lower values (15.8%) than MAP (28.0%). When N total wastes were calculated, SCP-2% and SCP-5% showed the lowest values (31.54 and 28.25%, respectively). In conclusion, based on P and N digestibility and excretion, the SCP-2% diet showed the best results from a nutritional and environmental point of view.

Causes and prediction of changes in extractable phosphorus during flooding

Soil Research ◽  
1989 ◽  
Vol 27 (1) ◽  
pp. 45 ◽  
Author(s):  
IR Willett
Keyword(s):  
Organic Matter ◽  
Soil Ph ◽  
Sodium Acetate ◽  
Chemical Properties ◽  
Sodium Acetate Buffer ◽  
P Release ◽  
Reduction Of Iron ◽  
No Release ◽  
Extractable Phosphorus ◽  
A Minor

In a laboratory experiment, samples of 18 soils, which are known to be flooded in the field, were flooded for up to 32 days. Both untreated and phosphate-treated (50 mg P kg-1) soils were studied. It was attempted to identify which chemical properties measured on the dry untreated soils, and the changes in pH, Eh and extractable Fe and Mn over the flooding periods, controlled the changes in sodium acetate buffer (pH 3.0) extractable phosphorus during flooding. It was shown that the reduction of iron(III) oxides was the dominant source of the P released during flooding. However, the amount of P released was strongly inhibited by re-sorption. Direct measurement of the amount of iron(III) reduced during flooding and measurement of phosphate sorption were required to predict the amount of P released during flooding. Organic matter contributed toward the P released during flooding. Its contribution appeared to be by mineralization, rather than by accelerating FeIII reduction. The reduction of MnIII and MnIII was a minor source of P in the untreated soils. Changes in soil pH during flooding were responsible for desorption of freshly applied P, but did not appear to affect P release in the untreated soils. The Vertisols and some of the Alfisols showed very little, or no release of P during flooding.

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