Stable isotope evidence for the atmospheric origin of CO2 involved in carbonation of MSWI bottom ash
- 31 December 2006
- journal article
- Published by Elsevier BV in Applied Geochemistry
- Vol. 21 (12), 2037-2048
- https://doi.org/10.1016/j.apgeochem.2006.07.011
Abstract
No abstract availableKeywords
This publication has 38 references indexed in Scilit:
- δ13C variations in tree rings as an indication of severe changes in the urban air qualityAtmospheric Environment, 2002
- Petrogenesis of municipal solid waste combustion bottom ashApplied Geochemistry, 1999
- Municipal Solid Waste Incineration Bottom Ash: Characterization and Kinetic Studies of Organic MatterEnvironmental Science & Technology, 1999
- Determination of the abundance and carbon isotope composition of elemental carbon in sedimentsGeochimica et Cosmochimica Acta, 1997
- δ18O and δ13C values of modern brachiopod shellsGeochimica et Cosmochimica Acta, 1995
- Recarbonation of metamorphosed marls, JordanApplied Geochemistry, 1993
- Stable isotope disequilibria in travertine from high pH waters: Laboratory investigations and field observations from OmanGeochimica et Cosmochimica Acta, 1992
- Chemical and 13C/12C- and 18O/16O-isotope evolution of alkaline drainage waters and the precipitation of calciteApplied Geochemistry, 1992
- Chemical Behaviour of Municipal Solid Waste Incinerator Bottom Ash in MonofillsWaste Management & Research: The Journal for a Sustainable Circular Economy, 1992
- Calcium-magnesium carbonate solid solutions from Holocene conglomerate cements and travertines in the Coast Range of CaliforniaGeochimica et Cosmochimica Acta, 1971