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Zarrabi, M., Bagvand, F., Mahdavi, S., Kolahchi, Z. (2017). Phosphorus Sorption and Desorption Characteristics of Some Surface and Subsurface Vineyard Soils of Malayer Area in Hamedan Province. , 31(2), 247-262. doi: 10.22092/ijsr.2017.113109
M. Zarrabi; F. Bagvand; S. Mahdavi; Z. Kolahchi. "Phosphorus Sorption and Desorption Characteristics of Some Surface and Subsurface Vineyard Soils of Malayer Area in Hamedan Province". , 31, 2, 2017, 247-262. doi: 10.22092/ijsr.2017.113109
Zarrabi, M., Bagvand, F., Mahdavi, S., Kolahchi, Z. (2017). 'Phosphorus Sorption and Desorption Characteristics of Some Surface and Subsurface Vineyard Soils of Malayer Area in Hamedan Province', , 31(2), pp. 247-262. doi: 10.22092/ijsr.2017.113109
Zarrabi, M., Bagvand, F., Mahdavi, S., Kolahchi, Z. Phosphorus Sorption and Desorption Characteristics of Some Surface and Subsurface Vineyard Soils of Malayer Area in Hamedan Province. , 2017; 31(2): 247-262. doi: 10.22092/ijsr.2017.113109

Phosphorus Sorption and Desorption Characteristics of Some Surface and Subsurface Vineyard Soils of Malayer Area in Hamedan Province

پژوهش های خاک
Article 8, Volume 31, Issue 2, August 2017, Pages 247-262    PDF (409.4 K)
Document Type: Research Paper
DOI: 10.22092/ijsr.2017.113109
Authors
M. Zarrabi* 1; F. Bagvand2; S. Mahdavi1; Z. Kolahchi3
1Assistant Professor., Malayer University
2Former MS student, Malayer University
3Assistant Professor., Bu-Ali Sina University
Abstract
Phosphorus (P) sorption characteristics of soils influence P availability. This study was conducted to investigate P sorption isotherm, standard P requirement (SPR), P buffering capacity (PBC), desorption, and P hysteresis index (PHI) by 10 surface (0-30 cm) and 10 subsurface (30-60 cm) soils in vineyard soils of Malayer area in Hamadan province. Isotherm experiment was carried out by concentrations of P ranging from 0 to 200 mg l-1 of KH2PO4 salt in the presence of 0.01 M CaCl2. Desorption experiments were conducted with 0.01 M CaCl2. Phosphorus sorption characteristics in soil were calculated from isotherm equations. The average values of Olsen’s extractable P (Olsen P) in surface and subsurface soils were 24.3 and 19.4 mg kg–1, respectively. In surface and subsurface soils, Olsen P was higher than the optimum concentration of P for most crops (7-10 mg P kg–1). Phosphorus sorption curves were well fitted to the Freundlich, Van-Hay and Temkin equations. The SPR average of surface and subsurface soils, defined as the amount of P sorbed at an equilibrium concentration of 0.3 mgP l–1 was 18.7 mg kg-1 and 19.7 mg kg-1, respectively. The PBC average of surface and subsurface soils, account from Van-Hay equation was 89.2  l kg-1 and 103.5  l kg-1, respectively. The average value of PHI in surface soils (1.7) was greater than subsurface soils (1.6). There was significant negative correlation between SPR with Olsen-P in surface (p 15≤"> 0.01) and subsurface (p 15≤"> 0.05) soils. We found significant positive correlation between PBC with clay (p 15≤"> 0.01) and ECC (p 15≤"> 0.05) of soils. Our finding showed that high level of Olsen P concentration in surface and subsurface soils may decrease the availability of other nutrients.Appropriate P fertilizer management according to isotherm finding is needed. 
Keywords
Phosphorous sorption isotherm; buffering capacity; Standard requirement; Hysteresis
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