In this paper, there were shown the physico-chemical properties of post-boggy soil in the result of conducted melioration in the meadow object of Suraśl Górna. The researches were done in the period of 1987-2001 in two habitats: moist soil-moisture complex (PSMC-B) and drying moist soil-moisture complex (PSMC-C). In the moist habitat, the level of ground water was in the depth of 30-98 cm from the land surface and fed the root layer of soil. In the drying moist habitat, the ground water was below the depth of 100 cm in the vegetation season and was periodically inaccessible for the meadow plants. Unfavourable water conditions in drying moist habitat have caused the condensation of peat mass and the decrease of water capacity of soil. In tim...
For the proper functioning of endangered biodiverse rich fens, base-rich and nutrient-poor (mesotrop...
Soil desiccation of the deep soil layer is considered one of the main limiting factors to achieving ...
The retention potential of landscapes, along with the water regime of spring areas, are important hy...
The changes of the properties of physical-water post-bog soils on the drainage object meadow Upper S...
This work aims to clarify and describe the necessary conditions of the peat soil horizon formation. ...
The aim of this thesis is to summarise the current knowledge of the effects of amelioration enterven...
Lithuania has lost about two thirds of its total peatland area during the 20th century. Due to the d...
The main purpose of the work was to determine the scope and degree of the influence of exploitation ...
On peatlands annually in sunny weather there is a drying and self-ignition of the upper layer due to...
Abstract: Mires as well as meadows resulted in the drainage of mires are ecosystems very sensitive...
Abstract: Considerable changes in plant sociological, pedologic and hydrologic conditions has been...
The vast peatlands of the European North of Russia were drained in the 20th century. Some of the dra...
The paper analyzes changes in the hydro-physical properties of peat micro- and macrosystems in the p...
Wet grasslands represent endangered ecosystems which since the 1950ies have severely decreased in ar...
This study concerns in a three peatland sites: the epilitorals of Pilská reservoir and Hořejší Padrť...
For the proper functioning of endangered biodiverse rich fens, base-rich and nutrient-poor (mesotrop...
Soil desiccation of the deep soil layer is considered one of the main limiting factors to achieving ...
The retention potential of landscapes, along with the water regime of spring areas, are important hy...
The changes of the properties of physical-water post-bog soils on the drainage object meadow Upper S...
This work aims to clarify and describe the necessary conditions of the peat soil horizon formation. ...
The aim of this thesis is to summarise the current knowledge of the effects of amelioration enterven...
Lithuania has lost about two thirds of its total peatland area during the 20th century. Due to the d...
The main purpose of the work was to determine the scope and degree of the influence of exploitation ...
On peatlands annually in sunny weather there is a drying and self-ignition of the upper layer due to...
Abstract: Mires as well as meadows resulted in the drainage of mires are ecosystems very sensitive...
Abstract: Considerable changes in plant sociological, pedologic and hydrologic conditions has been...
The vast peatlands of the European North of Russia were drained in the 20th century. Some of the dra...
The paper analyzes changes in the hydro-physical properties of peat micro- and macrosystems in the p...
Wet grasslands represent endangered ecosystems which since the 1950ies have severely decreased in ar...
This study concerns in a three peatland sites: the epilitorals of Pilská reservoir and Hořejší Padrť...
For the proper functioning of endangered biodiverse rich fens, base-rich and nutrient-poor (mesotrop...
Soil desiccation of the deep soil layer is considered one of the main limiting factors to achieving ...
The retention potential of landscapes, along with the water regime of spring areas, are important hy...