FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3043137432> ?p ?o ?g. }

• W3043137432 abstract "&lt;p&gt;Soil organic matter (SOM) is in the focus of research as it plays crucial role in soil fertility, carbon sequestration, and all adsorption related processes in the soil. Nevertheless, its compound and the methods to investigate it are rather diverse. Some approach prefers to define different theoretical carbon pools in the soil based on input and mineralization dynamics using mean residence times. Other studies apply physical and/or chemical fractionations of the soil to separate the various eg. mineral phase associated or aggregate occluded carbon pools to gain less heterogeneous material. However, in practice, these two approaches are hardly met each other. As a considerable part of SOM is strongly associated with the mineral colloid fraction or even cations its investigation reveals the question of extractions. Traditional methods aimed to extract pure SOM fractions such as fulvic and humic acids (FA; HA)&amp;#160; and characterized the whole SOM based on them, even though these pure fractions represented only a small part of the total SOM and were not present under natural conditions. Recent methods try to characterize the SOM using in situ samples where the role of organic mineral complexes is still not fully understood. As a result, findings based on several approaches are hardly comparable with each other. The present study aims to characterize SOM based on parallel in situ solid-phase investigation FA separation, and water dissolved organic matter extraction. The study site is a haplic Luvisol under plowing and conservation tillage. Fourier transform infrared spectroscopy on the solid phase fractions resulted in an inverse proportion between organic carbon content and aromaticity independently from tillage. The aggregate occluded SOM was characterized by the lack of aliphatic components, whereas the fine fraction, and the bulk soil associated SOM seemed to be rich in them. The water-soluble SOM revealed molecular size increase in both the fine fraction related and the aggregate occluded organic matter owing to plowing, nonetheless, aggregates occluded the same sized OM molecules as those attached to the fine fraction. In general, FA fractions provided more humified organic matter, whereas water dissolved SOM showed a more intensive microbiome origin. The photometric properties of the FA fractions did not differ between the tillage systems, except for the SUVA254, which provided higher aromaticity under conservation tillage due to the lack of plowing. Also, the water-soluble part of SOM showed more humified composition and increased aromaticity under conservation tillage compared to plowing tillage. As a consequence, beneath the fingerprint of recent microbial activity, DOM reflects soil organic matter composition as well, therefore it seems to be suitable as a direct SOM proxy. The present research was supported by the Hungarian National Research and Innovation Office (NKFIH) K-123953, which is kindly acknowledged.&lt;/p&gt;" @default.
• W3043137432 created "2020-07-23" @default.
• W3043137432 creator A5008224325 @default.
• W3043137432 creator A5014817378 @default.
• W3043137432 creator A5024662040 @default.
• W3043137432 creator A5025240717 @default.
• W3043137432 creator A5025977876 @default.
• W3043137432 creator A5041275785 @default.
• W3043137432 creator A5047881053 @default.
• W3043137432 creator A5051563202 @default.
• W3043137432 creator A5071176052 @default.
• W3043137432 date "2020-03-23" @default.
• W3043137432 modified "2023-09-25" @default.
• W3043137432 title "Characterizing soil organic matter differences among extracts and the solid phase &#8211; the role of conservation tillage" @default.
• W3043137432 doi "https://doi.org/10.5194/egusphere-egu2020-6997" @default.
• W3043137432 hasPublicationYear "2020" @default.
• W3043137432 type Work @default.
• W3043137432 sameAs 3043137432 @default.
• W3043137432 citedByCount "0" @default.
• W3043137432 crossrefType "posted-content" @default.
• W3043137432 hasAuthorship W3043137432A5008224325 @default.
• W3043137432 hasAuthorship W3043137432A5014817378 @default.
• W3043137432 hasAuthorship W3043137432A5024662040 @default.
• W3043137432 hasAuthorship W3043137432A5025240717 @default.
• W3043137432 hasAuthorship W3043137432A5025977876 @default.
• W3043137432 hasAuthorship W3043137432A5041275785 @default.
• W3043137432 hasAuthorship W3043137432A5047881053 @default.
• W3043137432 hasAuthorship W3043137432A5051563202 @default.
• W3043137432 hasAuthorship W3043137432A5071176052 @default.
• W3043137432 hasConcept C107872376 @default.
• W3043137432 hasConcept C111696902 @default.
• W3043137432 hasConcept C158787203 @default.
• W3043137432 hasConcept C159390177 @default.
• W3043137432 hasConcept C159750122 @default.
• W3043137432 hasConcept C16397148 @default.
• W3043137432 hasConcept C178790620 @default.
• W3043137432 hasConcept C182124840 @default.
• W3043137432 hasConcept C185592680 @default.
• W3043137432 hasConcept C38774213 @default.
• W3043137432 hasConcept C39432304 @default.
• W3043137432 hasConcept C39464130 @default.
• W3043137432 hasConcept C4725764 @default.
• W3043137432 hasConcept C48743137 @default.
• W3043137432 hasConcept C6557445 @default.
• W3043137432 hasConcept C86803240 @default.
• W3043137432 hasConceptScore W3043137432C107872376 @default.
• W3043137432 hasConceptScore W3043137432C111696902 @default.
• W3043137432 hasConceptScore W3043137432C158787203 @default.
• W3043137432 hasConceptScore W3043137432C159390177 @default.
• W3043137432 hasConceptScore W3043137432C159750122 @default.
• W3043137432 hasConceptScore W3043137432C16397148 @default.
• W3043137432 hasConceptScore W3043137432C178790620 @default.
• W3043137432 hasConceptScore W3043137432C182124840 @default.
• W3043137432 hasConceptScore W3043137432C185592680 @default.
• W3043137432 hasConceptScore W3043137432C38774213 @default.
• W3043137432 hasConceptScore W3043137432C39432304 @default.
• W3043137432 hasConceptScore W3043137432C39464130 @default.
• W3043137432 hasConceptScore W3043137432C4725764 @default.
• W3043137432 hasConceptScore W3043137432C48743137 @default.
• W3043137432 hasConceptScore W3043137432C6557445 @default.
• W3043137432 hasConceptScore W3043137432C86803240 @default.
• W3043137432 hasLocation W30431374321 @default.
• W3043137432 hasOpenAccess W3043137432 @default.
• W3043137432 hasPrimaryLocation W30431374321 @default.
• W3043137432 hasRelatedWork W11199886 @default.
• W3043137432 hasRelatedWork W19644120 @default.
• W3043137432 hasRelatedWork W26626826 @default.
• W3043137432 hasRelatedWork W27225215 @default.
• W3043137432 hasRelatedWork W27385630 @default.
• W3043137432 hasRelatedWork W28604942 @default.
• W3043137432 hasRelatedWork W31367050 @default.
• W3043137432 hasRelatedWork W46600559 @default.
• W3043137432 hasRelatedWork W4716234 @default.
• W3043137432 hasRelatedWork W49969160 @default.
• W3043137432 isParatext "false" @default.
• W3043137432 isRetracted "false" @default.
• W3043137432 magId "3043137432" @default.
• W3043137432 workType "article" @default.