Publications related to Carbon balance of a European mountain bog at contrasting stages of regeneration

Adsorption and strain: The CO2-induced swelling of coal

Enhanced coal bed methane recovery (ECBM) consists in injecting carbon dioxide in coal bed methane reservoirs in order to facilitate the recovery of the methane. The injected carbon dioxide gets adsorbed at the surface of the coal pores, which causes the c ...

2010

Gradual Introduction of Coercive Instruments in Climate Policy

Philippe Thalmann, Andrea Baranzini

Acceptance is the key problem of carbon taxes. This chapter is about acceptance building, ie devising a mechanism for the gradual preparation of the population and the economy in order to implement a carbon tax. It draws on experiences in Switzerland, wher ...

2008

Modeling study of the interannual variability in global tropospheric hydroxyl radical and methane concentrations over the last two decades

Jérôme Drevet

Methane (CH4) is a major greenhouse gas whose global warming potential is 23 times more important than carbon dioxide (CO2). CH4 concentrations have steadily increased since the beginning of the industrial era, reaching an unprecedent level (almost 1800 pp ...

EPFL2008

Growth of carbon nanotubes and microfibers over stainless steel mesh by cracking of methane

Albert Renken, Lioubov Kiwi

The

{La}_{2}{NiO}_{4}

film was synthesized on the 304 stainless steel (SS) mesh. The hydrogen reduction of La2NiO4 generated homogeneous nanocatalyst particles (probably

{Ni}/{La}_2{O}_{3}

) over which methane was cracked, producing carbon notubes/micro ...

2008

Reducing carbon dioxide emissions by gas turbine processes | [CO2-Reduktion bei gasturbinen-prozessen]

François Maréchal

Selective process modifications were considered among the possible process variations for carbon dioxide separation in natural gas fired combined gas and steam turbine power plants that differ greatly among themselves in terms of additional expense (effici ...

2007

Carbon storage on exposed continental shelves during the glacial-interglacial transition

Jed Oliver Kaplan

We present analyses of new and previously published estimates of total (vegetation plus soil) carbon storage on exposed continental shelves during the LGM. Carbon stock estimates from environmental reconstructions vary from 113 to 202 Pg C. Estimates from ...

2006

Assessing Model Complexity from Anaerobic Digestion Data: When is Model AM1 Required?

Benoît Chachuat, Olivier Bernard

The anaerobic digestion ecosystem is complex, involving a broad variety of substrates and up to 140 bacterial species. This paper applies a methodology that determines the least number of macroscopic bioreactions to be taken into account in order to explai ...

2005

Continuous and simultaneous multigas monitoring using a highly sensitive and selective photoacoustic sensor

Luc Thévenaz, Jean-Philippe Besson, Marcel Gyger

A multi-gas photoacoustic sensor is reported. Simultaneous measurement of ammonia, carbon dioxide and water vapor is demonstrated at ppm level using semiconductor lasers. In-situ measurements to control the housing conditions of laboratory animals are pres ...

IEEE2005

Spatio-temporal pattern of bog pine (Pinus uncinata var. rotundata) at the interface with the Norway spruce (Picea abies) belt on the edge of a raised bog in the Jura Mountains, Switzerland

Alexandre Buttler, Jean-Michel Gobat, François Frelechoux

In a bog site in way of paludification, a pine stand is declining, which presently is an infrequent phenomenon on the Swiss Jura scale. A transect was positioned in the bog, from the external and driest part (pine-spruce stand) towards the central and wett ...

2004

Marine isotope stage (MIS) 11 in the vostok ice core: CO2 forcing and stability of East Antarctica

Jérôme Chappellaz

Changes in temperature and carbon dioxide during glacial cycles recorded in Antarctic ice cores are tightly coupled. However, this relationship does not hold for interglacials. While climate cooled towards the end of both the last (Eemian) and present (Hol ...

Elsevier BV2003

Carbon balance of a European mountain bog at contrasting stages of regeneration

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Adsorption and strain: The CO2-induced swelling of coal

Gradual Introduction of Coercive Instruments in Climate Policy

Modeling study of the interannual variability in global tropospheric hydroxyl radical and methane concentrations over the last two decades

Growth of carbon nanotubes and microfibers over stainless steel mesh by cracking of methane

Reducing carbon dioxide emissions by gas turbine processes | [CO2-Reduktion bei gasturbinen-prozessen]

Carbon storage on exposed continental shelves during the glacial-interglacial transition

Assessing Model Complexity from Anaerobic Digestion Data: When is Model AM1 Required?

Continuous and simultaneous multigas monitoring using a highly sensitive and selective photoacoustic sensor

Spatio-temporal pattern of bog pine (Pinus uncinata var. rotundata) at the interface with the Norway spruce (Picea abies) belt on the edge of a raised bog in the Jura Mountains, Switzerland

Marine isotope stage (MIS) 11 in the vostok ice core: CO2 forcing and stability of East Antarctica

Modeling study of the interannual variability in global tropospheric hydroxyl radical and methane concentrations over the last two decades

Carbon storage on exposed continental shelves during the glacial-interglacial transition

Spatio-temporal pattern of bog pine (Pinus uncinata var. rotundata) at the interface with the Norway spruce (Picea abies) belt on the edge of a raised bog in the Jura Mountains, Switzerland

Continuous and simultaneous multigas monitoring using a highly sensitive and selective photoacoustic sensor

Gradual Introduction of Coercive Instruments in Climate Policy

Adsorption and strain: The CO2-induced swelling of coal

Growth of carbon nanotubes and microfibers over stainless steel mesh by cracking of methane

Reducing carbon dioxide emissions by gas turbine processes | [CO2-Reduktion bei gasturbinen-prozessen]

Assessing Model Complexity from Anaerobic Digestion Data: When is Model AM1 Required?

Marine isotope stage (MIS) 11 in the vostok ice core: CO2 forcing and stability of East Antarctica