Peatlands are wetlands that provide important ecosystem services including carbon
sequestration and water storage that respond to hydrological, biological, and …

Hydro-pedotransfer functions (PTFs) relate easy-to-measure and readily available soil
information to soil hydraulic properties (SHPs) for applications in a wide range of process …

Hydrocarbon fate and transport in various categories of peatlands is complicated by the
botanical origin, and thus variations in the hydraulic structures and surface chemistry of its …

Undisturbed peatlands are effective carbon sinks and provide a variety of ecosystem
services. However, anthropogenic disturbances, especially land drainage, strongly alter …

Due to the non-vascular nature of Sphagnum mosses, the capitula (growing surface) of the
moss must rely solely on capillary action to receive water from beneath. Moss subsides and …

The restoration and subsequent regeneration of Sphagnum moss on harvested peatlands
can result in poor hydrological connectivity between the regenerated Sphagnum moss and …

Sphagnum mosses are a keystone peatland species whose ecohydrology governs carbon
sequestration processes in many peatlands. Globally, there are~ 380 Sphagnum species …

The dual-porosity structure of peat and the extremely high organic matter content give rise to
a complex medium that typically generates prolonged tailing and early 50% concentration …

The underlying processes governing solute transport in peat from an experimentally
constructed fen peatland were analyzed by performing saturated and unsaturated solute …

In ombrotrophic peatlands, the moisture content of the acrotelm (vadoze zone) controls
oxygen diffusion rates, redox state, and the turnover of organic matter. Thus, variably …