Maksimović, Srboljub

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  • Maksimović, Srboljub (2)
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Author's Bibliography

Soil Properties and Trace Elements Contents Following 40 Years of Phosphate Fertilization

Cakmak, Dragan; Saljnikov, Elmira; Mrvić, Vesna; Jakovljević, Miodrag D; Marjanović, Žaklina; Sikiric, Biljana; Maksimović, Srboljub

(Wiley, Hoboken, 2010)

TY  - JOUR
AU  - Cakmak, Dragan
AU  - Saljnikov, Elmira
AU  - Mrvić, Vesna
AU  - Jakovljević, Miodrag D
AU  - Marjanović, Žaklina
AU  - Sikiric, Biljana
AU  - Maksimović, Srboljub
PY  - 2010
UR  - http://rimsi.imsi.bg.ac.rs/handle/123456789/387
AB  - Long-term application of P fertilizers may eventually result: in excess and/or toxic accumulations of trace elements and microelements in soil. The effect of monoammonium-phosphate (MAP) on basic soil properties (pH, CEC, texture), the total content of C N, and F, hot acid-extractable Cu, Zn, Ni, Cr, Pb, Cd, Co, As, Hg, and F, and the content of extractable macro- and trace elements (P, K, Ca, Mg, Al, Fe, Zn, Cu, Ni, Pb, Cd, F) were Studied on a Stagnosol soil. Phosphate fertilizer had been applied (26, 39, and 52 kg P ha(-1)) over a 40-yr period. Phosphorus fertilization significantly decreased pH and increased clay content of the soil. Increases were detected in available P, exchangeable Al, Ca, cation exchange capacity (CEC), and clay content. The content of hot acid-ex tractable Pb increased, whereas the content of diethylenetriaminepentaacetic acid-extractable Pb decreased in accordance with applied rates of MAP. The status of some hot acid-extractable trace elements (Cu, Zn, Ni, and Co) did not change after 40 yr of MAP application, whereas Hg and Cd increased. However, despite the statistically significant increases in the amounts of some potentially toxic elements, they did riot accumulate to concentrations considered toxic as overall concentrations are far below the maximum allowed concentrations for natural unpolluted soils.
PB  - Wiley, Hoboken
T2  - Journal of Environmental Quality
T1  - Soil Properties and Trace Elements Contents Following 40 Years of Phosphate Fertilization
EP  - 547
IS  - 2
SP  - 541
VL  - 39
DO  - 10.2134/jeq2009.0216
ER  - 
@article{
author = "Cakmak, Dragan and Saljnikov, Elmira and Mrvić, Vesna and Jakovljević, Miodrag D and Marjanović, Žaklina and Sikiric, Biljana and Maksimović, Srboljub",
year = "2010",
abstract = "Long-term application of P fertilizers may eventually result: in excess and/or toxic accumulations of trace elements and microelements in soil. The effect of monoammonium-phosphate (MAP) on basic soil properties (pH, CEC, texture), the total content of C N, and F, hot acid-extractable Cu, Zn, Ni, Cr, Pb, Cd, Co, As, Hg, and F, and the content of extractable macro- and trace elements (P, K, Ca, Mg, Al, Fe, Zn, Cu, Ni, Pb, Cd, F) were Studied on a Stagnosol soil. Phosphate fertilizer had been applied (26, 39, and 52 kg P ha(-1)) over a 40-yr period. Phosphorus fertilization significantly decreased pH and increased clay content of the soil. Increases were detected in available P, exchangeable Al, Ca, cation exchange capacity (CEC), and clay content. The content of hot acid-ex tractable Pb increased, whereas the content of diethylenetriaminepentaacetic acid-extractable Pb decreased in accordance with applied rates of MAP. The status of some hot acid-extractable trace elements (Cu, Zn, Ni, and Co) did not change after 40 yr of MAP application, whereas Hg and Cd increased. However, despite the statistically significant increases in the amounts of some potentially toxic elements, they did riot accumulate to concentrations considered toxic as overall concentrations are far below the maximum allowed concentrations for natural unpolluted soils.",
publisher = "Wiley, Hoboken",
journal = "Journal of Environmental Quality",
title = "Soil Properties and Trace Elements Contents Following 40 Years of Phosphate Fertilization",
pages = "547-541",
number = "2",
volume = "39",
doi = "10.2134/jeq2009.0216"
}
Cakmak, D., Saljnikov, E., Mrvić, V., Jakovljević, M. D., Marjanović, Ž., Sikiric, B.,& Maksimović, S.. (2010). Soil Properties and Trace Elements Contents Following 40 Years of Phosphate Fertilization. in Journal of Environmental Quality
Wiley, Hoboken., 39(2), 541-547.
https://doi.org/10.2134/jeq2009.0216
Cakmak D, Saljnikov E, Mrvić V, Jakovljević MD, Marjanović Ž, Sikiric B, Maksimović S. Soil Properties and Trace Elements Contents Following 40 Years of Phosphate Fertilization. in Journal of Environmental Quality. 2010;39(2):541-547.
doi:10.2134/jeq2009.0216 .
Cakmak, Dragan, Saljnikov, Elmira, Mrvić, Vesna, Jakovljević, Miodrag D, Marjanović, Žaklina, Sikiric, Biljana, Maksimović, Srboljub, "Soil Properties and Trace Elements Contents Following 40 Years of Phosphate Fertilization" in Journal of Environmental Quality, 39, no. 2 (2010):541-547,
https://doi.org/10.2134/jeq2009.0216 . .
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34

Labile fractions of soil organic carbon in mollisols from different climatic regions

Saljnikov, Elmira; Cakmak, Dragan; Kostić Kravljanac, Ljiljana; Maksimović, Srboljub

(Pisa Univ Press, Pisa, 2009)

TY  - JOUR
AU  - Saljnikov, Elmira
AU  - Cakmak, Dragan
AU  - Kostić Kravljanac, Ljiljana
AU  - Maksimović, Srboljub
PY  - 2009
UR  - http://rimsi.imsi.bg.ac.rs/handle/123456789/326
AB  - Characterization of Labile Fractions of Soil Organic Carbon in Mollisols from different climatic regions. The research studied the potential mineralization and characterization of labile SOM of different types of Mollisols: Hapludolls, Argiudolls, Calciustolls, and Haplustolls. Labile C fractions distributed oppositely than total SOC and were the greatest in Calciustolls and the lowest in Hapludolls. The amount of soil microbial biomass C (MBC) was significantly higher in dry than in wet regions. The highest amount of light fraction C was in dry-thermic followed by dry-frigid, and the least amount was in wet regions. Dry regions were able to retain a higher level of labile C than the moist regions, due to a slower annual decomposition rate.
PB  - Pisa Univ Press, Pisa
T2  - Agrochimica
T1  - Labile fractions of soil organic carbon in mollisols from different climatic regions
EP  - 385
IS  - 6
SP  - 376
VL  - 53
UR  - https://hdl.handle.net/21.15107/rcub_rimsi_326
ER  - 
@article{
author = "Saljnikov, Elmira and Cakmak, Dragan and Kostić Kravljanac, Ljiljana and Maksimović, Srboljub",
year = "2009",
abstract = "Characterization of Labile Fractions of Soil Organic Carbon in Mollisols from different climatic regions. The research studied the potential mineralization and characterization of labile SOM of different types of Mollisols: Hapludolls, Argiudolls, Calciustolls, and Haplustolls. Labile C fractions distributed oppositely than total SOC and were the greatest in Calciustolls and the lowest in Hapludolls. The amount of soil microbial biomass C (MBC) was significantly higher in dry than in wet regions. The highest amount of light fraction C was in dry-thermic followed by dry-frigid, and the least amount was in wet regions. Dry regions were able to retain a higher level of labile C than the moist regions, due to a slower annual decomposition rate.",
publisher = "Pisa Univ Press, Pisa",
journal = "Agrochimica",
title = "Labile fractions of soil organic carbon in mollisols from different climatic regions",
pages = "385-376",
number = "6",
volume = "53",
url = "https://hdl.handle.net/21.15107/rcub_rimsi_326"
}
Saljnikov, E., Cakmak, D., Kostić Kravljanac, L.,& Maksimović, S.. (2009). Labile fractions of soil organic carbon in mollisols from different climatic regions. in Agrochimica
Pisa Univ Press, Pisa., 53(6), 376-385.
https://hdl.handle.net/21.15107/rcub_rimsi_326
Saljnikov E, Cakmak D, Kostić Kravljanac L, Maksimović S. Labile fractions of soil organic carbon in mollisols from different climatic regions. in Agrochimica. 2009;53(6):376-385.
https://hdl.handle.net/21.15107/rcub_rimsi_326 .
Saljnikov, Elmira, Cakmak, Dragan, Kostić Kravljanac, Ljiljana, Maksimović, Srboljub, "Labile fractions of soil organic carbon in mollisols from different climatic regions" in Agrochimica, 53, no. 6 (2009):376-385,
https://hdl.handle.net/21.15107/rcub_rimsi_326 .