Abstract:
The natural conditions in the extra-Carpathian zone of the Moldova
river meadow and hydrographical basin from the Păltinoasa-Timişeşti field,
which also includes the Baia Depression, have favoured water excess in soil.
Subsurface drainage, associated to modeling in ridge strips from the Baia
experimental field was set up in 1978 on a stagnic-glosic albic Luvosol. The
project comprised an area of 3.00 ha, on which six technical solutions of
conducting low depth subsoil drainage were found. Before conducting the
works of subsoil drainage, soil was used only as natural meadow with
perennial hygrophyte vegetation. In the first stage of the years 1978-1995,
the soil from drainage field was first cultivated with annual plants. In the
second stage of the years 1996-2007, soil was used for animal grazing. The
pasture was formed as a result of field sowing with a mixture made of 70%
grasses and 30% legumes. The behaviour in exploitation of soil improvement
works was studied as concerns the sustainability of the projects for subsoil
drainage, associated to the modeling in ridge strips and the evolution in time
of some characteristics of drained and cultivated soil. After the first cycle, we
have determined, according to the accurate measurements of geometric
leveling, an average height of ridges of 18-29 cm, compared to the level of
channels. The average transversal slope of profiles was of 2-3%. The
average initial depth of placing suction drains at 0.942 m has registered after
the first exploitation cycle the value of 0.812 m, as a result of land modeling
in ridge strips and, respectively, the process of settling the drained soil. After
the second cycle, when no works of restoring the field modeling in ridge
strips were done, and soil from the drainage field was used as natural
meadow, the constructive parameters were maintained within the limits
relatively close to the first period.
