Abstract:
The Transylvanian Plain (TP), with an area of 395,616 hectares is an important agricultural production area of
Romania. During the last two hundred years, TP has been undergoing considerable anthropic impact, currently being a
hilly area with serious issues of sustainability of soils, scarce in water resources, with deficient rainfall and an extremely
low degree of afforestation: 6.8%. Monitoring the thermal and hydric regime of the area is essential in order to identify
and implement sets of measures of adjustment to the impact of climatic changes. Soil moisture and temperature regimes
have been evaluated on a basis of a set of 20 data logging stations positioned throughout the plain. Each station stores
electronic data of ground temperature on 3 different levels of depth (10, 30 and 50 cm), of soil humidity at a depth of 10
cm, of the air temperature at 1 meter and of precipitation. The multiannual average air temperature situates between
9.35-12.040C and grow in the soil with increasing depth to 9.89-12.82°C – at 10 cm; 10.05-12.85°C – at 30 cm; 10.03-
12.86°C – at 50 cm. The multiannual average air temperatures during the period 2008-2012 increased with 0.15(north) -
2.84(south) C as compared to the multiannual average temperature of the area (9.2°C). The thermal regime of the
ground is of the mesic type, multiannual average soil temperature at 50 cm depth situating between 10.03-12.86°C and
the differences between the average summer temperatures and average winter temperatures range between 11.35-
17.72°C. Monitoring the hydric regime of the soils in TP demonstrate that the moisture regime is of the ustic type for
the northern and north-western part, whereas for the southern and south-eastern part the hydric regime is of the xeric
type; the soil being dry over 45 consecutive days following the summer solstice. The analysis of recorded data results in
a situation similar to the southern, south-eastern and eastern slopes- lower rainfall with approx. 43.8 mm, higher
temperatures with 0.370C in air, with 1.910C at 10 cm, with 2.220C at 20 cm and with 2.430C at 30 cm in soil, compared
to northern, north-western and western slopes. These issues, supplemented by those of slope require special
agrotechnical measures generated by TP relief.
