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Authordc.contributor.authorAguilera S., S. María 
Authordc.contributor.authorBorie B., Gilda es_CL
Authordc.contributor.authorPeirano V., Pedro es_CL
Authordc.contributor.authorGalindo G., G. es_CL
Admission datedc.date.accessioned2010-03-23T20:07:29Z
Available datedc.date.available2010-03-23T20:07:29Z
Publication datedc.date.issued1997
Cita de ítemdc.identifier.citationCOMMUNICATIONS IN SOIL SCIENCE AND PLANT ANALYSIS 28(11-12): 899-912en_US
Identifierdc.identifier.issn0010-3624
Identifierdc.identifier.urihttps://repositorio.uchile.cl/handle/2250/120887
Abstractdc.description.abstractDeterminations were made of total soil organic matter (SOM), stable and labile organic fractions, biomass carbon (C), and chemical composition of several humus-soil-fractions in chilean volcanic soils, Andosols and Ultisols. Their physico-chemical Properties and humification degree at different stages in edaphic evolution were also assessed. In addition, organic matter models were obtained by chemical and biological syntheses and the structures and properties of natural and synthetic humic materials were compared with SOM. Results indicate that Andosols have higher SOM levels than Ultisols, but the fraction distribution in the latter suggests a shift of the more stable fractions to the more labile ones. Moreover, contents of humines, and humic and fulvic acids suggest that Chilean volcanic soil SOM is highly humified. On the other hand, among the SOM labile fractions, carbohydrate and biomass are about 15% of the SOM which are one of the most important fractions in soil fertilityen_US
Lenguagedc.language.isoenen_US
Publisherdc.publisherMARCEL DEKKER INCen_US
Keywordsdc.subjectOrganic-matteren_US
Títulodc.titleOrganic matter in volcanic soils in Chile: Chemical and biochemical characterizationen_US
Document typedc.typeArtículo de revista


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