Investigations in to the intensity of soil erosion have been conducted by measurements of rill capacities on selected hillslopes in agricultural areas of North-Eastern Poland. The intensity of interrill erosion has been measured by using sediment traps. Owing to the interrill erosion, it is the convex parts of the slopes which have been eroded the most intensively. On gentle slopes (<9 degrees), the most intensive erosion has been observed in the upper convex part (0,3-7 t/ha/ yr.) and a zone of temporary deposition has been identified just below the zone of erosion i.e. in the middle and the lower parts of a convex-concave slope. On steeper slopes (those steeper than 9-10°) the upper and middle part of the slope are also part of the zone o...
Krajobraz wyżyn lessowych Polski SE ulega intensywnym przekształceniom antropogenicznym od około 5 t...
The investigations aimed to: 1) evaluate water erosion rates on undulating slopes in Lithuania under...
The study on water erosion in young-glacial catchment of the Chwalimski Potok (upper Parsęta tributa...
The paper shows results of soil erosion research undertaken in November 2006 on 7 experimental plots...
Sheet and rill erosion plays an important role in the transformation of agricultural slopes in the C...
The research area is located in the Bytów District (NW Poland). The following analysis were performe...
The study aimed at evaluating the changes occurred in loess soils of Opatówka river catchment (Sando...
FAO and OECD data point at erosion as a main soil degradation factor in the global scale. Although t...
Autorzy opisują jakie procesy erozyjne gleb występują w górskich terenach Karpat i czym są powodowan...
This paper presents the results of the quantification of water erosion rate in the rolling old-glaci...
The paper presents the results studies on the intensity of water erosion processes in the road gully...
The research was carried out in the years 2008-2011 in the loess catchment area in Wielkopole in the...
Research on soil erosion undertaken on selected slopes of the Suwałki Lakeland (NE Poland) in years ...
This paper presents the results of the quantification of water erosion rate in the rolling old-glaci...
Systematic decrease of agricultural surface and continuous degradation of soil environment, among ot...
Krajobraz wyżyn lessowych Polski SE ulega intensywnym przekształceniom antropogenicznym od około 5 t...
The investigations aimed to: 1) evaluate water erosion rates on undulating slopes in Lithuania under...
The study on water erosion in young-glacial catchment of the Chwalimski Potok (upper Parsęta tributa...
The paper shows results of soil erosion research undertaken in November 2006 on 7 experimental plots...
Sheet and rill erosion plays an important role in the transformation of agricultural slopes in the C...
The research area is located in the Bytów District (NW Poland). The following analysis were performe...
The study aimed at evaluating the changes occurred in loess soils of Opatówka river catchment (Sando...
FAO and OECD data point at erosion as a main soil degradation factor in the global scale. Although t...
Autorzy opisują jakie procesy erozyjne gleb występują w górskich terenach Karpat i czym są powodowan...
This paper presents the results of the quantification of water erosion rate in the rolling old-glaci...
The paper presents the results studies on the intensity of water erosion processes in the road gully...
The research was carried out in the years 2008-2011 in the loess catchment area in Wielkopole in the...
Research on soil erosion undertaken on selected slopes of the Suwałki Lakeland (NE Poland) in years ...
This paper presents the results of the quantification of water erosion rate in the rolling old-glaci...
Systematic decrease of agricultural surface and continuous degradation of soil environment, among ot...
Krajobraz wyżyn lessowych Polski SE ulega intensywnym przekształceniom antropogenicznym od około 5 t...
The investigations aimed to: 1) evaluate water erosion rates on undulating slopes in Lithuania under...
The study on water erosion in young-glacial catchment of the Chwalimski Potok (upper Parsęta tributa...