Phosphorus desorption from calcareous soils with different initial Olsen-P levels and relation to phosphate fractions

2019 ◽  
Vol 19 (7) ◽  
pp. 2997-3007 ◽  
Author(s):  
Yan Shen ◽  
Yinghua Duan ◽  
Neil McLaughlin ◽  
Shaomin Huang ◽  
Doudou Guo ◽  
...  
Soil Research ◽  
2018 ◽  
Vol 56 (2) ◽  
pp. 136 ◽  
Author(s):  
Arzhang Fathi Gerdelidani ◽  
Hossein Mirseyed Hosseini

In the present study we investigated the effects of using sugar cane bagasse biochar and spent mushroom compost (SMC) on different fractions of phosphorus and plant availability in three calcareous soils with a loam, clay loam and sandy loam texture. The incubation experiment was performed using a completely randomised design, with five treatments (B1 and B2 (15 and 30 t biochar ha–1 respectively), SMC1 and SMC2 (20 and 40 t SMC ha–1 respectively) and C (control)) and three incubation periods (14, 60 and 120 days) over three replicates. The different P fractions evaluated in the soil were Olsen P, dicalcium phosphate (Ca2-P), octacalcium phosphate (Ca8-P), aluminium phosphate (Al-P), iron phosphate, occluded phosphate and apatite. Application of SMC at both levels increased Olsen P, whereas biochar application was less effective. SMC2 increased Olsen P by 473%, 227% and 89% in clay loam, loam and sandy loam soils respectively. In addition, for all soils and all incubation times, SMC1 and SMC2 significantly increased Ca2-P compared with C, which had an increasing trend with time, but biochar only increased Ca2-P significantly in sandy loam soil. SMC2 also increased Ca8-P and Al-P at 120 days. In conclusion, application of SMC can enhance plant-available P and affect P fractions and distribution, with the degree of the increase being soil specific. In contrast, the effects of biochar on P availability, fractions and distribution need more time to become apparent.


2011 ◽  
Vol 42 (2) ◽  
pp. 208-219 ◽  
Author(s):  
Ali Reza Hosseinpur ◽  
Farzaneh Sadate Biabanaki ◽  
Hossein Ali Alikhani

Agronomy ◽  
2020 ◽  
Vol 10 (9) ◽  
pp. 1344 ◽  
Author(s):  
Muhammad Zahir Aziz ◽  
Muhammad Yaseen ◽  
Muhammad Naveed ◽  
Xiukang Wang ◽  
Kaniz Fatima ◽  
...  

Low bioavailability of phosphorus (P) in alkaline/calcareous soils leads to low yields due to its precipitation/fixation with calcium (Ca). An effective method to enhance phosphorus use efficiency (PUE) and its availability to plants is the application of alginate bioaugmented coated di-ammonium phosphate (DAP). In this study, the pre-isolated P solubilizing Paraburkholderia phytofirmans (PsJN) coated with different concentrations of polymer (alginate) on DAP with and without carbon source was tested in incubation, pot, and field experiments to investigate microbial survival, Olsen P release, and its availability to plants. Results indicated that the maximum recovery of PsJN loaded on alginate at 30 days incubation with and without carbon source was 199 × 1010 and 82 × 106 CFU mL−1 respectively. Application of alginate bioaugmented DAP released 962 mg kg−1 Olsen P after 60 days of incubation compared to 280 and 370 mg kg−1 Olsen P released by uncoated and simple alginate coated DAP, respectively. Results from pot trial revealed that application of 100% alginate bioaugmented DAP increased 26% plant height, 31% photosynthetic rate, 55% grain yield, and 6 × 105 CFU g−1 root bacterial population, compared to uncoated DAP. Field trial results indicated that 22% grain yield, 14% straw yield, and 44% agronomy P efficiency were increased by applying 100% alginate bioaugmented DAP compared to uncoated DAP. This new approach resulted in controlled release of P from coated DAP that not only reduced phosphorus fixation but also enhanced the bioavailability of P to plants.


Geoderma ◽  
2017 ◽  
Vol 305 ◽  
pp. 275-280 ◽  
Author(s):  
Saber Heidari ◽  
Adel Reyhanitabar ◽  
Shahin Oustan

1988 ◽  
Vol 110 (3) ◽  
pp. 505-513 ◽  
Author(s):  
B. S. Brar ◽  
A. C. Vig

SummaryLaboratory and glasshouse experiments were conducted to study P release kinetics and uptake of P by wheat (Trilicum, aestivum L.) in ten benchmark soils of Punjab (India). Phosphorus desorption, determined by successive extraction with 0·01 m-CaCl2 solution, was lower in calcareous soils (group I) than in non-calcareous soils (group II). Desorption of surface P in soils followed pseudo-first-order kinetics. The values of the kinetic constant of desorption and the radial diffusion coefficient of P increased with the amount of added P in soils.A significant linear relationship between cumulative desorbed P and both dry-matter yield and P uptake indicated that the rate of release of P from the solid matrix is important in determining P uptake by wheat crop. Phosphate uptake was less dependent on the initial solution P concentration than on the rate of phosphate release.


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