Приказ основних података о документу
The chemical characteristics of soil which determine phosphorus partitioning in highly calcareous soils
Hemijske karakteristike visoko-krečnjačkih zemljišta koje određuju raspodelu fosfora
dc.creator | Topalović, Ana | |
dc.creator | Pfendt, Lidija B. | |
dc.creator | Perovic, Natalija | |
dc.creator | Đorđević, Dragana S. | |
dc.creator | Trifunović, Snežana S. | |
dc.creator | Pfendt, Petar A. | |
dc.date.accessioned | 2018-11-22T00:10:21Z | |
dc.date.available | 2018-11-22T00:10:21Z | |
dc.date.issued | 2006 | |
dc.identifier.issn | 0352-5139 | |
dc.identifier.uri | https://cherry.chem.bg.ac.rs/handle/123456789/819 | |
dc.description.abstract | Phosphorus fractions from three highly calcareous soils (average, 24.9 +/- 4.8 %CO32-) from sampling sites with a Mediterranean climate were isolated by sequential extraction. In order to provide a more reliable basis for the definition of the obtained P-fractions, principal component analysis was applied and from the chemical characteristics of the 14 investigated soils, those characteristics which define at he content and association features of the P-fractions were assessed. The soils are characterized by a relatively high pH (8.0-8.2) and by significantly differing contents of organic mater, acid-soluble Mg and total P. These differences affected the various association features of the P-fraction with the soil constituents. The NH4F-P fraction (isolated with 0.5 M NH4F, pH 8.2) is defined by the contents of the main metals of the oxide-hydroxide-clay associations (Al, Fe, Mn) or by the the redox potential (Eh) of Mn. The accumulation of NaOH-phosphorus (extractable with 0.1 M NaOH) depended on the constituents of the oxide hydroxide-clay association, the humic substances and Eh-related factors. In those soils in which NaOH-P is defined by the oxide-hydroxide-clay association, the participation of Fe as a bridge-forming metal is proposed. The main part of total P, i.e., Delta P = TP - (NH4F-P + NaOH-P) is defined by the status of Mn- and Fe-humic complexes or by the concentration of hydroxyl-ions. | en |
dc.description.abstract | Iz tri visoko-krečnjačka zemljišta (prosečni sadržaj CO 3 2- 24.9 ± 4.8%, pH 8.0 - 8.2), sa lokacija sa sredozemnom klimom, izolovane su frakcije fosfora sekvencijalnom ekstrakcijom. U cilju obezbeđivanja pouzdanije osnove za definisanje dobijenih frakcijafosfora (P-frakcija), primenjena je analiza principalne komponente (PC-analiza). Među 14 hemijskih karakteristika zemljišta, izdvojene su one koje definišu sadržaj pojedinih P-frakcija i prirodu njihove asocijacije sa sastojcima zemljišta. Frakcija NH 4-P (izolovana sa 0,5M NH 4F, pH = 8,2) definisana je sadržajem glavnih metala oksidne-hidroksidne-glinene asocijacije (Al, Fe, Mn) ili Eh-statusom izraženim sadržajem Mn. Akumulacija NaOH-P (ekstrahovanog sa 0,1 M NaOH) zavisila je od sastojaka oksidne-hidroksidne-glinene asocijacije, od huminskih supstanci i od faktora koji stoje u vezi sa Eh. U onim zemljištima u kojima je NaOH-P definisana sastojcima oksidne-hidroksidne-glinene asocijacije, pretpostavljeno je vezivanje fosfora preko Fe-mostova. Glavna količina fosfora ∆P = TP - (NH 4F-P + NaOH-P), u pojedinim zemljištima definisana je ili statusom Mn- i Fe-huminskih kompleksa, ili pH-vrednošću. | sr |
dc.publisher | Serbian Chemical Soc, Belgrade | |
dc.rights | openAccess | |
dc.rights.uri | https://creativecommons.org/licenses/by-nc-nd/4.0/ | |
dc.source | Journal of the Serbian Chemical Society | |
dc.subject | NH4F-extractable P | en |
dc.subject | NaOH-extractable P | en |
dc.subject | NaOH-extractable P | en |
dc.subject | phosphorus-associations | en |
dc.subject | phosphorus-associations | en |
dc.subject | principal component analysis | en |
dc.subject | principalcomponent analysis | en |
dc.title | The chemical characteristics of soil which determine phosphorus partitioning in highly calcareous soils | en |
dc.title | Hemijske karakteristike visoko-krečnjačkih zemljišta koje određuju raspodelu fosfora | sr |
dc.type | article | |
dc.rights.license | BY-NC-ND | |
dcterms.abstract | Топаловиц, Aна; Трифуновић, Снежана; Перовиц, Наталија; Пфендт, Петар A.; Пфендт, Лидија Б.; Дордевиц, Драгана; Хемијске карактеристике високо-кречњачких земљишта које одређују расподелу фосфора; Хемијске карактеристике високо-кречњачких земљишта које одређују расподелу фосфора; | |
dc.citation.volume | 71 | |
dc.citation.issue | 11 | |
dc.citation.spage | 1219 | |
dc.citation.epage | 1236 | |
dc.identifier.wos | 000243619400010 | |
dc.identifier.doi | 10.2298/JSC0611219T | |
dc.citation.other | 71(11): 1219-1236 | |
dc.citation.rank | M23 | |
dc.type.version | publishedVersion | |
dc.identifier.scopus | 2-s2.0-33846342971 | |
dc.identifier.fulltext | https://cherry.chem.bg.ac.rs/bitstream/id/10019/817.pdf |