We performed surface and borehole ground penetrating radar (GPR) tests, together with moisture probe measurements and direct gas sampling to detect areas of biogenic gas accumulation in a northern peatland. The main findings are: (1) shadow zones (signal scattering) observed in surface GPR correlate with areas of elevated CH4 and CO2 concentration; (2) high velocities in zero offset profiles and lower water content inferred from moisture probes correlate with surface GPR shadow zones; (3) zero offset profiles depict depth variable gas accumulation from 0-10% by volume; (4) strong reflectors may represent confining layers restricting upward gas migration. Our results have implications for defining the spatial distribution, volume and movemen...
Hydrology has been suggested as the mechanism controlling vegetation and related surficial pore-wate...
Northern Peatlands cover more than 350 million ha (~3 percent of Earth’s surface) and are an importa...
Peatlands deform elastically during precipitation cycles by small (+/- 3 cm) oscillations in surface...
We tested a set of surface common mid-point (CMP) ground penetrating radar (GPR) surveys combined wi...
Ground penetrating radar (GPR) was used to determine peat basin geometry and the spatial distributio...
A set of high resolution surface ground penetrating radar (GPR) surveys, combined with elevation rod...
Emissions of methane and carbon dioxide gases from organic soils contribute to the global carbon cyc...
Biogenic gas emission from northern peatlands, by wicking from vascular plants and by episodic ebull...
The ability of peatlands to produce, sequester, and release large volumes of greenhouse gases (parti...
Northern peatlands are a large source of atmospheric methane (CH4) and both a source and a sink of a...
The study was conducted as part of the NASA Biospherics Research on Emissions from Wetlands (BREW) p...
In this work, we surveyed the internal structure of peat deposit with ground penetrating radar with ...
Physical properties, such as depth, bulk density and humification are closely linked to many of the ...
The spatial and temporal distribution of biogenic gas accumulation and release within peatland soils...
The surface pattern of vegetation influences the composition and humification of peat laid down duri...
Hydrology has been suggested as the mechanism controlling vegetation and related surficial pore-wate...
Northern Peatlands cover more than 350 million ha (~3 percent of Earth’s surface) and are an importa...
Peatlands deform elastically during precipitation cycles by small (+/- 3 cm) oscillations in surface...
We tested a set of surface common mid-point (CMP) ground penetrating radar (GPR) surveys combined wi...
Ground penetrating radar (GPR) was used to determine peat basin geometry and the spatial distributio...
A set of high resolution surface ground penetrating radar (GPR) surveys, combined with elevation rod...
Emissions of methane and carbon dioxide gases from organic soils contribute to the global carbon cyc...
Biogenic gas emission from northern peatlands, by wicking from vascular plants and by episodic ebull...
The ability of peatlands to produce, sequester, and release large volumes of greenhouse gases (parti...
Northern peatlands are a large source of atmospheric methane (CH4) and both a source and a sink of a...
The study was conducted as part of the NASA Biospherics Research on Emissions from Wetlands (BREW) p...
In this work, we surveyed the internal structure of peat deposit with ground penetrating radar with ...
Physical properties, such as depth, bulk density and humification are closely linked to many of the ...
The spatial and temporal distribution of biogenic gas accumulation and release within peatland soils...
The surface pattern of vegetation influences the composition and humification of peat laid down duri...
Hydrology has been suggested as the mechanism controlling vegetation and related surficial pore-wate...
Northern Peatlands cover more than 350 million ha (~3 percent of Earth’s surface) and are an importa...
Peatlands deform elastically during precipitation cycles by small (+/- 3 cm) oscillations in surface...