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Vegetations- und Standortsveränderungen auf von Hochwasser überschlickten Streuwiesen
LEUTHOLD, Barbara
1994
Changes in vegetation and site conditions in wet meadows after a flood.
Restitution von Hochmooren und nassen Heiden im Hohen Venn (Ost-Belgien): eine bilanz 10-jähriger Feldversuche)
FRANKARD, Philippe
2005
Rehabilitation of raised bogs and wet heaths on the Hautes-Fagnes (East Belgium): an assessment after ten years of management trials.
Bult- und Schlenkenbildung in Hochmoortorf
CASPARIE, W.A.
1969
Formation (évolution) des buttes et gouilles dans les tourbières bombées.
Renaturierung von Hochmooren – Möglichkeiten und Grenzen nach 20-jähriger Erfahrung und wissenschaftlicher Begleitung
JÜRGEN Eigner, Kiel
1995
Réhabilitation naturelle des tourbières bombées. Potentialités et limites à la suite de 20 ans d’expérience et de suivi scientifique.
Hydrologic-hydrochemical monitoring to the effect of re-wetting in a bog in the western upper Erzgebirge
KRUGER, Annett ; NEUMESITER, Hans ; TOLKE, Detlef ; HEINRICH, Jürgen
2011
"The relationship between the distribution of naturally occuring dissolved organic carbon (DOC), other nutrients and catchment characteristics is determined by a monitoring program and concept for an upland catchment system in the western upper Erzgebirge. In the drinking water area of the dam "Carlsfeld" are situated acid bogs witch are in parts destroyed, drained and now in re-wetting. The aim of our investigations insists on the analysing of the impact of the bog drainage and re-wetting for the matter dynamic. The mobilisation of DOC is controlled by the humification in the Katotelm based on moving ground water level in different transformed areas in the bogs (drained areas, no intact bog...
DOC export from rewetted Fens – a case study
ZAUFT, Michael ; ZEITZ, Jutta
2011
"Dissolved organic carbon (DOC) is the largest discharge component in the carbon balance of peat bogs with the exception of carbon dioxide (CO 2) and methane (CH 4). Very little attention has been devoted to the behaviour of DOC after peat bogs have been rewetted. It is already known that DOC discharges from degraded peat bogs can rise when the water level is raised. The size of this discharge and the influencing factors are however still little understood. To measure and determine the influencing factors, this case study looks at three rewetted peat bogs which differ in terms of hydrogenetic peat bog type, the intensity of the former use, and the level of anthropogenic pedogenesis. The resu...
Production and export of DOC on peatlands. A review
SCHWALM, Mayte ; ZEITZ, Jutta
2011
"Dissolved organic carbon (DOC) occurs in high amounts in peatlands. Remarkable export of DOC due to low absorption capacity of organic soils causes concern, because DOC impairs water quality and leads to emission of climate gases after its decomposition. Concentration and export of DOC is influenced by season, abiotic soil characteristics and land use. Production and consumption of DOC is determined by the vitality of soil microbes, which is in turn controlled by temperature, water and pH. Unlike to laboratory experiments, in field experiments correlation of DOC concentration and abiotic soil parameters is often not detectable. Obviously, further parameters have to be taken into account. DO...
Theory of the carrying capacity of peat
SCHWEIKLE, Volker
2011
"The distribution of pressures under load in peat soil depends on the soil structure. Rolling loads produce shear in the middle and in front and behind wheels. The movement of mass of peat soil under load by the responsible forces is presented. Wet peat will be compressed only if the water in the pores will shift. Loads are effective on peat soil volumes and in time. Therefore the use of vectors has to be replaced by balances of the specific energy/power. Impacts transmit similar amounts of power, as loads do. The compression of peat soil has to be valued by the requirements of the prevailing vegetation; that means due to the penetrability of roots in depth and volume of peat soil and the pl...

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