نتایج جستجو برای: dissolved ch4

تعداد نتایج: 38430  

2016
R. M. Wilson A. M. Hopple M. M. Tfaily S. D. Sebestyen C. W. Schadt L. Pfeifer-Meister C. Medvedeff K. J. McFarlane J. E. Kostka M. Kolton R.K. Kolka L. A. Kluber J. K. Keller T. P. Guilderson N. A. Griffiths J. P. Chanton S. D. Bridgham P. J. Hanson

Peatlands contain one-third of soil carbon (C), mostly buried in deep, saturated anoxic zones (catotelm). The response of catotelm C to climate forcing is uncertain, because prior experiments have focused on surface warming. We show that deep peat heating of a 2 m-thick peat column results in an exponential increase in CH4 emissions. However, this response is due solely to surface processes and...

2003

This paper investigates how vascular plants affect carbon flow and the formation and emission of the greenhouse gas methane (CH4) in an arctic wet tundra ecosystem in NE Greenland. We present a field experiment where we studied, in particular, how speciesspecific root exudation patterns affect the availability of acetate, a hypothesized precursor of CH4 formation. We found significantly higher ...

2004
M. Strack J. M. Waddington

[1] As natural sources of methane (CH4), peatlands play an important role in the global carbon cycle. Climate models predict that evapotranspiration will increase under a 2 CO2 scenario due to increased temperatures leading to lowered water tables at many northern latitudes. Given that the position of the water table within a peatland can have a large effect on CH4 emissions, climate change may...

2007

A comprehensive biogeochemistry model, DNDC, was revised to simulate crop growth and soil processes more explicitly and improve its ability to estimate methane (CH4) emission from rice paddy fields under a wide range of climatic and agronomic conditions. The revised model simulates rice growth by tracking photosynthesis, respiration, C allocation, tillering, and release of organic C and O2 from...

2017
Jessie Guyader Emilio M. Ungerfeld Karen A. Beauchemin

A decrease in methanogenesis is expected to improve ruminant performance by allocating rumen metabolic hydrogen ([2H]) to more energy-rendering fermentation pathways for the animal. However, decreases in methane (CH4) emissions of up to 30% are not always linked with greater performance. Therefore, the aim of this study was to understand the fate of [2H] when CH4 production in the rumen is inhi...

2017
Henk J. van Lingen Joan E. Edwards Jueeli D. Vaidya Sanne van Gastelen Edoardo Saccenti Bartholomeus van den Bogert André Bannink Hauke Smidt Caroline M. Plugge Jan Dijkstra

Diurnal patterns of ruminal fermentation metabolites and microbial communities are not commonly assessed when investigating variation in ruminal CH4 production. The aims of this study were to monitor diurnal patterns of: (i) gaseous and dissolved metabolite concentrations in the bovine rumen, (ii) H2 and CH4 emitted, and (iii) the rumen microbiota. Furthermore, the effect of dietary inclusion o...

2015
Dawn Cardace D'Arcy R. Meyer-Dombard Kristin M. Woycheese Carlo A. Arcilla

A field campaign targeting high pH, H2-, and CH4-emitting serpentinite-associated springs in the Zambales and Palawan Ophiolites of the Philippines was conducted in 2012-2013, and enabled description of several springs sourced in altered pillow basalts, gabbros, and peridotites. We combine field observations of pH, temperature, conductivity, dissolved oxygen, and oxidation-reduction potential w...

2018
José R Paranaíba Nathan Barros Raquel Mendonça Annika Linkhorst Anastasija Isidorova Fábio Roland Rafael M Almeida Sebastian Sobek

The magnitude of diffusive carbon dioxide (CO2) and methane (CH4) emission from man-made reservoirs is uncertain because the spatial variability generally is not well-represented. Here, we examine the spatial variability and its drivers for partial pressure, gas-exchange velocity (k), and diffusive flux of CO2 and CH4 in three tropical reservoirs using spatially resolved measurements of both ga...

2018
Franco Tassi Stefano Fazi Simona Rossetti Paolo Pratesi Marco Ceccotti Jacopo Cabassi Francesco Capecchiacci Stefania Venturi Orlando Vaselli

Volcanic lakes are characterized by physicochemical favorable conditions for the development of reservoirs of C-bearing greenhouse gases that can be dispersed to air during occasional rollover events. By combining a microbiological and geochemical approach, we showed that the chemistry of the CO2- and CH4-rich gas reservoir hosted within the meromictic Lake Averno (Campi Flegrei, southern Italy...

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