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resumen

Resumen
Loss on ignition (LOI) is one of the most widely used methods for measuring organic matter content in soils but does not have a universal standard protocol. A large number of factors may influence its accuracy, such as furnace type, sample mass, duration and temperature of ignition and clay content of samples. We conducted a series of experiments to quantify these effects, which enabled us to derive (i) guidelines for ignition conditions (sample mass, [ver mas...]
dc.contributor.authorHoogsteen, Martine J.J.
dc.contributor.authorLantinga, Egbert A.
dc.contributor.authorBakker, Evert Jan
dc.contributor.authorGroot, Jeroen C.J.
dc.contributor.authorTittonell, Pablo Adrian
dc.date.accessioned2019-05-16T11:36:34Z
dc.date.available2019-05-16T11:36:34Z
dc.date.issued2015-03
dc.identifier.issn1365-2389
dc.identifier.otherhttps://doi.org/10.1111/ejss.12224
dc.identifier.urihttp://hdl.handle.net/20.500.12123/5125
dc.identifier.urihttps://onlinelibrary.wiley.com/doi/abs/10.1111/ejss.12224
dc.description.abstractLoss on ignition (LOI) is one of the most widely used methods for measuring organic matter content in soils but does not have a universal standard protocol. A large number of factors may influence its accuracy, such as furnace type, sample mass, duration and temperature of ignition and clay content of samples. We conducted a series of experiments to quantify these effects, which enabled us to derive (i) guidelines for ignition conditions (sample mass, duration and temperature), (ii) temperature-specific soil organic matter (SOM) to soil organic carbon (SOC) conversion factors and (iii) clay content-dependent correction factors for structural water loss (SWL). Bulk samples of a sandy soil (4% clay) and a silt loam soil (25% clay) were used to evaluate the effects of ignition conditions. Samples with a range of clay contents (0–50%) were used to quantify conversion and correction factors. Two furnaces, one without and one with pre-heated air, did not show significant differences in terms of within-batch LOI variability. In both furnaces less combustion occurred close to the door, which necessitated tray turning at half-time as this reduced the standard deviation per batch significantly. Variation in mass loss declined exponentially with sample mass (range, 0.15–20 g). The LOI increased with duration at lower temperatures (≤550∘C) for the sandy soil. At greater temperatures (600 and 650∘C), no effect of duration was found. For the silt loam soil, LOI values increased with duration for each temperature, which was attributed to SWL. The SOM to SOC conversion factor decreased strongly with temperature at an ignition duration of 3 hours from 0.70 (350∘C) to 0.57 (500∘C) and stabilized around 0.55 between 550 and 650∘C, indicating that at temperatures ≥550∘C all SOM had been removed. The clay correction factor for SWL increased from 0.01 to 0.09 as the temperature of ignition increased from 350 to 650∘C. To minimize within-batch LOI variation we recommend a standard ignition duration of 3 hours, tray turning at half-time, a sample mass ≥20 g and temperatures equal to or greater than 550 ∘C. To avoid over-estimates of SOM through structural water loss, the presented SWL correction procedure should always be applied.eng
dc.formatapplication/pdfes_AR
dc.language.isoenges_AR
dc.publisherJohn Wiley & Sons Ltdes_AR
dc.rightsinfo:eu-repo/semantics/restrictedAccesses_AR
dc.sourceEuropean Journal of Soil Science 66 : 320-328 (Marzo 2015)es_AR
dc.subjectMateria Orgánica del Sueloes_AR
dc.subjectSoil Organic Mattereng
dc.subjectSuelo
dc.subjectSoileng
dc.subjectCarbono
dc.subjectCarboneng
dc.subjectEvaporación
dc.subjectEvaporationeng
dc.subject.otherPérdida de Igniciónes_AR
dc.subject.otherPérdida de Agua
dc.titleEstimating soil organic carbon through loss on ignition: effects of ignition conditions and structural water losses_AR
dc.typeinfo:ar-repo/semantics/artículoes_AR
dc.typeinfo:eu-repo/semantics/articlees_AR
dc.typeinfo:eu-repo/semantics/publishedVersiones_AR
dc.description.origenEstación Experimental Agropecuaria Barilochees_AR
dc.description.filFil: Hoogsteen, Martine J.J. Wageningen University and Research Centre. Department of Plant Sciences. Farming Systems Ecology Group; Holandaes_AR
dc.description.filFil: Lantinga, Egbert A.Wageningen University and Research Centre. Department of Plant Sciences. Farming Systems Ecology Group; Holandaes_AR
dc.description.filFil: Bakker, Evert Jan. Wageningen University and Research Centre. Department of Plant Sciences. Mathematical and Statistical Methods; Holandaes_AR
dc.description.filFil: Groot, Jeroen. Wageningen University and Research Centre. Department of Plant Sciences. Farming Systems Ecology Group; Holandaes_AR
dc.description.filFil: Tittonell, Pablo Adrian. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agropecuaria Bariloche; Argentina. Wageningen University and Research Centre. Department of Plant Sciences. Farming Systems Ecology Group; Holandaes_AR
dc.subtypecientifico


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