Hydrological landscape settings of base‐rich fen mires and fen meadows: an overview

AP Grootjans, EB Adema, W Bleuten… - Applied Vegetation …, 2006 - Wiley Online Library
Question: Why do similar fen meadow communities occur in different landscapes? How
does the hydrological system sustain base‐rich fen mires and fen meadows? Location: …

Release of CO2 and CH4 from small wetland lakes in western Siberia

E Repo, JT Huttunen, AV Naumov… - Tellus B: Chemical …, 2007 - Taylor & Francis
CO 2 and CH 4 fluxes were measured from three small wetland lakes located in the middle
taiga and forest tundra zones onWest Siberian Lowlands (WSL), the world’s largest wetland …

Contribution of point sources and diffuse sources to nitrogen and phosphorus loads in lowland river tributaries

NM Pieterse, W Bleuten, SE Jørgensen - Journal of Hydrology, 2003 - Elsevier
Human activities may cause enhanced loads of total N (TN) and total P (TP) in running waters,
which may have a serious impact on their ecological quality. Likely sources for N and P …

[HTML][HTML] Regular surface patterning of peatlands: confronting theory with field data

MB Eppinga, M Rietkerk, W Borren, ED Lapshina… - Ecosystems, 2008 - Springer
Regular spatial patterns of sharply bounded ridges and hollows are frequently observed in
peatlands and ask for an explanation in terms of underlying structuring processes. Simulation …

Holocene peat and carbon accumulation rates in the southern taiga of western Siberia

W Borren, W Bleuten, ED Lapshina - Quaternary research, 2004 - cambridge.org
Although recent studies have recognized peatlands as a sink for atmospheric CO2, little is
known about the role of Siberian peatlands in the global carbon cycle. We have estimated the …

Atmospheric deposition in forest edges measured by monitoring canopy throughfall

GPJ Draaijers, W Ivens, W Bleuten - Water, Air, and Soil Pollution, 1988 - Springer
Atmospheric dry deposition in two forest edges was studied by means of monitoring canopy
throughfall in Douglas Fir stands. Throughfall fluxes in the first 50 to 100 m of forest edges …

PEAT‐CLSM: A specific treatment of peatland hydrology in the NASA Catchment Land Surface Model

M Bechtold, GJM De Lannoy, RD Koster… - Journal of advances …, 2019 - Wiley Online Library
Peatlands are poorly represented in global Earth system modeling frameworks. Here we add
a peatland‐specific land surface hydrology module (PEAT‐CLSM) to the Catchment Land …

Eco-hydrological functioning of the Biebrza wetlands: lessons for the conservation and restoration of deteriorated wetlands

MJ Wassen, T Okruszko, I Kardel, J Chormanski… - Wetlands: Functioning …, 2006 - Springer
Human activities have led to the loss of a large proportion of biodiversity in riverine wetlands
in western Europe (Van Urk 1984; Cirujano et al. 1996). In the second half of the twentieth …

[HTML][HTML] Vegetation characteristics and eco-hydrological processes in a pristine mire in the Ob River valley (Western Siberia)

AM Schipper, R Zeefat, F Tanneberger, JP van Zuidam… - Plant Ecology, 2007 - Springer
Relations between vegetation characteristics and eco-hydrological processes were assessed
in a pristine mire in the valley of the Ob River (Western Siberia). Along a transect from the …

The contribution of ammonia emissions from agriculture to the deposition of acidifying and eutrophying compounds onto forests

GPJ Draaijers, W Ivens, MM Bos, W Bleuten - Environmental Pollution, 1989 - Elsevier
In the vicinity of a large ammonia emission area, dry and wet deposition of acidifying and
eutrophying compounds onto Douglas Fir forests was studied by sampling throughfall, …