Comparison of loss on ignition and thermal analysis stepwise methods for determination of sedimentary organic matter
Autor: | Emanuela Molinaroli, Gretel Frangipane, Mario Pistolato, Stefano Guerzoni, Davide Tagliapietra |
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Rok vydání: | 2009 |
Předmět: |
chemistry.chemical_classification
Ecology sediments organic matter thermogravimetric differential thermal analysis loss on ignition Extraction (chemistry) Mineralogy Sediment Aquatic Science Grain size chemistry Sedimentary organic matter Organic matter Particle size Loss on ignition Thermal analysis Nature and Landscape Conservation |
Zdroj: | Aquatic conservation 19 (2009): 24–33. doi:10.1002/aqc.970 info:cnr-pdr/source/autori:Frangipane G, Pistolato M, Molinaroli E, Guerzoni S, Tagliapietra D/titolo:Comparison of loss on ignition and thermal analysis stepwise methods for determination of sedimentary organic matter/doi:10.1002%2Faqc.970/rivista:Aquatic conservation (Print)/anno:2009/pagina_da:24/pagina_a:33/intervallo_pagine:24–33/volume:19 |
ISSN: | 1099-0755 1052-7613 |
Popis: | 1. Loss on ignition (LOI) is a widely used method to estimate organic matter (OM) in the sediment of marine and freshwater ecosystems. Thermogravimetric-differential thermal analysis (TG-DTA) of organic species provides information on thermal reactions, the amount and properties of clay structural water, organic species and carbonates. 2. The accuracy of LOI compared with that of TG-DTA was evaluated in 33 sediment samples from the Lagoon of Venice (Italy). 3. In all tests conducted with TG-DTA the mass loss of OM and the loss of clay structural water (LCSW) from oxidized samples were measured. The mass loss of OM at 350 degrees C (TG-DTA 350 OM) and the total extraction of organic matter at 567 degrees C (TEOM) calculated from the difference between natural state samples and oxidized samples highlight the presence of both thermally labile and thermally stable substances. 4. The grain size data of sediment samples from the Lagoon shows a variable distribution between slightly muddy sand and mud. Loss of clay structural water at 350 degrees C (LCSW 350) and total extraction of clay structural water at 567 degrees C (TECSW) both estimated by TG-DTA on oxidized samples, were found to correspond approximately to 6% and 10%, respectively of the clay fraction ( |
Databáze: | OpenAIRE |
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