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Forest fields temporary occupied by different industrial activities are restored to the silvicultural circuit after the industrial activity has ended. These fields should be apt for reforestation and should have admissible values regarding their content of dangerous substances. The present article describes and interprets the characteristics of soils from four fields occupied temporary by oil wells in Moine�ti, Bacau County. The content of clay, soluble salts and nutritive elements were analysed, together with the soil�s reaction, the content of hydrocarbons or other soil characteristics. The admissible values for installing, growing and developing forest species were then emphasized. The obtained results have illustrated the fact that the oil extraction activity had negative effects on soils, namely: a strong consolidation (especially on access roads); the truncation and/or derangement/mixture of horizons or soils stratums with the rock; depletion of nutritive substances; salinization, argilisation and pollution with oil residues. In order to render these fields back to the silvicultural circuit, bio remedy technologies must be applied or other measures that can eliminate the pollutant from the soil (decontamination methods), followed by pedoameliorative measures.

State forests are analyzed periodically, once every 10 years. This includes an analysis of forest soils. The present paperdescribes and interprets the chemical properties of forest soils from Bacau County focusing on the period 1983-2015. As such, 823 soil profiles and 2435 pedogenetic horizons were analysed taking into consideration the soil type, pH, humus content, nitrogen content, base saturation degree and the total cation exchange capacity. The most widespread types of soils are: eutriccambisol, luvisol, preluvisoland dystriccambisol. The dystriccambisols from Bacau County are strongly acid soils, while eutriccambisols and preluvisols are moderately acid. All forest soils from this area have a high cationic exchange capacity and are very well (dystriccambisol, eutriccambisol,luvisol) or well supplied (preluvisol, rendzina) with nitrogen. Knowing the chemical properties of soils is important for the analysis of stand variability and for adopting silvicultural methods adequate for the management of long-lasting forests.

This paper aims to describe and interpret the chemical properties of forest soils in the Dobrogea Plateau. Data on soil analyzes are obtained in the laboratories of National Institute of Research and Development in Silviculture `Marin Dracea` after a recognized and accredited national and international methodology. There were analyzed soil reaction, base saturation degree, total cationic exchange capacity, humus content, total nitrogen and compared with results of soil analysis from other geographical regions of Romania. In the case of forest soils in Dobrogea Plateau, a higher pH was found than in other hilly or highland areas in the country to eutric cambisol, luvisol and preluvisol. Thus soil pH ranges from moderately acidic in the case of luvisols to low alkaline in the case of chernozems. Regarding the base saturation degree (V), there are higher values in this part of the country for preluvisol, luvisol and eutric cambisol and slightly lower values for phaeozem than in other regions of Romania. The amount of humus of eutric cambisols from Dobrogea Plateau is smaller than other hilly areas of the country and slightly higher than similar altitude areas.

The present paper characterizes the soils from Romania�s West Plain from a chemical property point of view, based on data from forest management plans. As such, for each forest district, soil samples from characteristic forest areas are gathered once at ten years and then analyzed. In this manner, soil reaction, base saturation degree, total cationic exchange capacity, humus content and total nitrogen where analyzed and compared with results of soil analysis from other Romanian areas.