000887876 001__ 887876
000887876 005__ 20210130010704.0
000887876 0247_ $$2doi$$a10.1186/s12302-020-0299-5
000887876 0247_ $$2Handle$$a2128/26147
000887876 0247_ $$2altmetric$$aaltmetric:75748558
000887876 0247_ $$2WOS$$aWOS:000520494900002
000887876 037__ $$aFZJ-2020-04498
000887876 082__ $$a610
000887876 1001_ $$0P:(DE-HGF)0$$aLi, Fayong$$b0
000887876 245__ $$aEnhanced soil aggregate stability limits colloidal phosphorus loss potentials in agricultural systems
000887876 260__ $$aHeidelberg$$bSpringer$$c2020
000887876 3367_ $$2DRIVER$$aarticle
000887876 3367_ $$2DataCite$$aOutput Types/Journal article
000887876 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article$$bjournal$$mjournal$$s1605288568_16532
000887876 3367_ $$2BibTeX$$aARTICLE
000887876 3367_ $$2ORCID$$aJOURNAL_ARTICLE
000887876 3367_ $$00$$2EndNote$$aJournal Article
000887876 520__ $$aBackgroundColloid-facilitated phosphorus (P) transport is recognized as an important pathway for the loss of soil P in agricultural systems; however, information regarding soil aggregate-associated colloidal P (Pcoll) is lacking. To elucidate the effects of aggregate size on the potential loss of Pcoll in agricultural systems, soils (0–20 cm depth) from six land-use types were sampled in the Zhejiang Province in the Yangtze River Delta region, China. The aggregate size fractions (2–8 mm, 0.26–2 mm, 0.053–0.26 mm and < 0.053 mm) were separated using the wet sieving method. Colloidal P and other soil parameters in aggregates were analyzed.ResultsOur study demonstrated that 0.26–2 mm small macroaggregates had the highest total P (TP) content. In acidic soils, the highest Pcoll content was observed in the 0.26- to 2-mm-sized aggregates, while the lowest was reported in the < 0.053 mm (silt + clay)-sized particles, the opposite of that revealed in alkaline and neutral soils. Paddy soils contained less Pcoll than other land-use types. The proportion of Pcoll in total dissolved P (TDP) was dominated by < 0.053 mm (silt + clay)-sized particles. Aggregate size strongly influenced the loss potential of Pcoll in paddy soils, where Pcoll contributed up to 83% TDP in the silt + clay-sized particles. The Pcoll content was positively correlated with TP, Al, Fe, and the mean weight diameter. Aggregate-associated total carbon (TC), total nitrogen (TN), C/P, and C/N had significant negative effects on the contribution of Pcoll to potential soil P loss. The Pcoll content of the aggregates was controlled by the aggregate-associated TP and Al content, as well as the soil pH value. The potential loss of Pcoll from aggregates was controlled by its organic matter content.ConclusionWe concluded that management practices that increase soil aggregate stability or its organic carbon content will limit Pcoll loss in agricultural systems.
000887876 536__ $$0G:(DE-HGF)POF3-255$$a255 - Terrestrial Systems: From Observation to Prediction (POF3-255)$$cPOF3-255$$fPOF III$$x0
000887876 588__ $$aDataset connected to CrossRef
000887876 7001_ $$00000-0002-3521-9761$$aLiang, Xinqiang$$b1$$eCorresponding author
000887876 7001_ $$0P:(DE-Juel1)159111$$aLi, Hua$$b2
000887876 7001_ $$0P:(DE-HGF)0$$aJin, Yingbin$$b3
000887876 7001_ $$0P:(DE-HGF)0$$aJin, Junwei$$b4
000887876 7001_ $$0P:(DE-HGF)0$$aHe, Miaomiao$$b5
000887876 7001_ $$0P:(DE-Juel1)129484$$aKlumpp, Erwin$$b6
000887876 7001_ $$0P:(DE-Juel1)145865$$aBol, Roland$$b7
000887876 773__ $$0PERI:(DE-600)2593962-2$$a10.1186/s12302-020-0299-5$$p17$$tEnvironmental sciences Europe$$v32$$x0934-3504$$y2020
000887876 8564_ $$uhttps://juser.fz-juelich.de/record/887876/files/Enhanced%20soil%20aggregate%20stability%20limits%20colloidal%20phosphorus%20loss%20potentials%20in%20agricultural%20systems.pdf$$yOpenAccess
000887876 909CO $$ooai:juser.fz-juelich.de:887876$$pdnbdelivery$$pVDB$$pVDB:Earth_Environment$$pdriver$$popen_access$$popenaire
000887876 9101_ $$0I:(DE-588b)5008462-8$$6P:(DE-Juel1)129484$$aForschungszentrum Jülich$$b6$$kFZJ
000887876 9101_ $$0I:(DE-588b)5008462-8$$6P:(DE-Juel1)145865$$aForschungszentrum Jülich$$b7$$kFZJ
000887876 9131_ $$0G:(DE-HGF)POF3-255$$1G:(DE-HGF)POF3-250$$2G:(DE-HGF)POF3-200$$3G:(DE-HGF)POF3$$4G:(DE-HGF)POF$$aDE-HGF$$bErde und Umwelt$$lTerrestrische Umwelt$$vTerrestrial Systems: From Observation to Prediction$$x0
000887876 9141_ $$y2020
000887876 915__ $$0StatID:(DE-HGF)0200$$2StatID$$aDBCoverage$$bSCOPUS$$d2020-09-10
000887876 915__ $$0StatID:(DE-HGF)0160$$2StatID$$aDBCoverage$$bEssential Science Indicators$$d2020-09-10
000887876 915__ $$0StatID:(DE-HGF)1050$$2StatID$$aDBCoverage$$bBIOSIS Previews$$d2020-09-10
000887876 915__ $$0StatID:(DE-HGF)1190$$2StatID$$aDBCoverage$$bBiological Abstracts$$d2020-09-10
000887876 915__ $$0LIC:(DE-HGF)CCBY4$$2HGFVOC$$aCreative Commons Attribution CC BY 4.0
000887876 915__ $$0StatID:(DE-HGF)0100$$2StatID$$aJCR$$bENVIRON SCI EUR : 2018$$d2020-09-10
000887876 915__ $$0StatID:(DE-HGF)9905$$2StatID$$aIF >= 5$$bENVIRON SCI EUR : 2018$$d2020-09-10
000887876 915__ $$0StatID:(DE-HGF)0501$$2StatID$$aDBCoverage$$bDOAJ Seal$$d2020-09-10
000887876 915__ $$0StatID:(DE-HGF)0500$$2StatID$$aDBCoverage$$bDOAJ$$d2020-09-10
000887876 915__ $$0StatID:(DE-HGF)0113$$2StatID$$aWoS$$bScience Citation Index Expanded$$d2020-09-10
000887876 915__ $$0StatID:(DE-HGF)0700$$2StatID$$aFees$$d2020-09-10
000887876 915__ $$0StatID:(DE-HGF)0150$$2StatID$$aDBCoverage$$bWeb of Science Core Collection$$d2020-09-10
000887876 915__ $$0StatID:(DE-HGF)0510$$2StatID$$aOpenAccess
000887876 915__ $$0StatID:(DE-HGF)0030$$2StatID$$aPeer Review$$bDOAJ : Blind peer review$$d2020-09-10
000887876 915__ $$0StatID:(DE-HGF)0561$$2StatID$$aArticle Processing Charges$$d2020-09-10
000887876 915__ $$0StatID:(DE-HGF)1060$$2StatID$$aDBCoverage$$bCurrent Contents - Agriculture, Biology and Environmental Sciences$$d2020-09-10
000887876 915__ $$0StatID:(DE-HGF)0300$$2StatID$$aDBCoverage$$bMedline$$d2020-09-10
000887876 915__ $$0StatID:(DE-HGF)0199$$2StatID$$aDBCoverage$$bClarivate Analytics Master Journal List$$d2020-09-10
000887876 9201_ $$0I:(DE-Juel1)IBG-3-20101118$$kIBG-3$$lAgrosphäre$$x0
000887876 980__ $$ajournal
000887876 980__ $$aVDB
000887876 980__ $$aUNRESTRICTED
000887876 980__ $$aI:(DE-Juel1)IBG-3-20101118
000887876 9801_ $$aFullTexts