The research was conducted in 1990-99 in forest observation sites in the neighbourhoods of industrial enterprises of Kohtla-Jaerve-Johvi and the cement plant of Kunda and in the control area in Lahemaa National Park. Differences between the radial increments of conifers growing under pollution and in a relatively unpolluted area were estimated. The stands selected for investigation were similar as to their edaphic conditions and forest survey indicators. The high sensitivity of conifers to long term emissions of pollutants into the atmosphere from oil shale based power engineering and chemical industry, production of building materials and fertilisers and other industrial enterprises in the investigation area is expressed as changes in the radial increment of trees with the changes depending on the pollution load and alterations in precipitation and soil

In 1985-99 studies were carried out in the area of the Kunda cement plant on North Estonian coastal plain on sample plots stretching 1.5 and 2.5 km east and 2 km and 3 km west, where changes in crown damages and radial increment of pine and spruce were estimated. The selected stands were with 0.7-0.8 density and II quality class, with moderately dense or sprase understorey, 75-85-year-old Myrtillus site type pine or spruce stands. Practically every tree in the area of intensive dust pollution had signs of damage. The relations between the defoliation and radial increment in the region were not linear. Weak defoliation (up to 25 per cent) influences slightly the radial growth. The correlations were more evident on Pinus sylvestris with more than half of the trees in the area having moderate or strong defoliation (at least 30-35 per cent). We suppose that defoliation, which leads to a decrease in the assimilating area of trees, causes essential changes in physiological processes. In the region of intensive pollution stress the radial increment decreased along with the defoliation level on both Pinus sylvestris and Picea abies

The aim of the study was to compare the amount of epicuticular waxes of Norway spruce and Scots pine needles from the area of cement production in Kunda. The amount of Norway spruce waxes decreased under air pollution influences and with ageing. The quantity of waxes of Scots pine needles showed an increasing tendency in the polluted area and in one-year-old needles compared with the current-year ones. A rapid decrease in the amount of waxes was established also in the older needles of Scots pine

To study the impact of air pollution on the growth of conifers sample plots were established at different distances and directions from the Kunda cement plant. The plots included stands of 70-80-year-old Scots pine and Norway spruce. Although emission of alkaline cement dust had decreased in the second half of the 1990s analyses of soil samples collected to characterise the growth substrate of trees showed that the pH value of the humus horizon of weakly podzolised temporarily overmoist sandy soils was within the radius of 3 km from the cement plant 2.0-2.9 times as high as that of the control plots in Lahemaa National Park. To ascertain the effect of alkaline environment on the growth of conifers the length (cm) of the needles and shoots formed in 1996-99, dry and wet mass (g) of 100 needles, dry matter content of needles(per cent) and density of needles on shoots were measured. The results obtained were compared with data from 1992 if possible. Both pine and spruce were found to be sensitive towards cement dust pollution and alkalised environment; however, the impact on different morphological parameters was different. As compared to the control, the strongest inhibition of growth was revealed in the sample plot situated 2.5 km east from the cement plant. Conifers on sample plots 2 km west from the emission source showed more vigorous growth than the control. As compared with data from 1992, some improvement in the growth of pine and spruce was observed

A needle trace method was used to reveal the chronology of needle retention and growth rates on Scots pine in a stand near a power plant operating on oil shale. During the period of 1964-97, the height increment varied between 31 and 64 cm yr (-1), and the radial increment ranged from 1.06 to 3.71 mm yr (-1). The average needle density on the newly sprouted shoots of the main stem was 5.9 needles cm (-1) and the mean needle production on the same shoots was 266. The average number of needle sets along the main stem ranged from 2.2 to 3.1, the mean age of needles varied between 1.3 and 2.3 years. The short-term maximum concentrations of oil shale fly ash and SO2 ranged from 55 to 2510, and from 75 to 270 micro g m (-3), respectively. The annual average concentrations of fly ash varied between 6 and 95 micro g m (-3), and of SO2 between 2.5 and 10 micro g m (-3). Changes in neither the concentrations of fly ash nor SO2 were associated with the variation in needle retention of Scots pine. In the case of height increment, however, the correlation with the annual average concentration of oil shale fly ash was significant (r=0.83; p0.05)

The paper is based on the data of geochemical mapping of the humus horizon of soil and geochemical monitoring of soil carried out in 1986-94. These data have been supplemented with results of later investigations. The authors describe the formation of parent rock of soil in NE Estonia and its major geochemical features. The main plant nutrient elements and those having a negative influence of plant growth and the development of animate nature in the case of their elevated concentration in soil are observed. Components are areal distribution of technogenous atmospheric pollution falling on the ground surface in NE Estonia are also dealt with. The chemical composition of the humus horizon of soil in NE Estonia is variable, the variation coefficient of several elements exceeding 100 per cent. The trends of lateral changes in the concentration of elements are accidental. Such heterogeneity is mainly due to great variability of parent rocks of soil. Glacial deposits formed from Proterozoic crystalline rocks of Fennoscandian origin, as well as the Vendian and Paleozoic sedimentary rocks, among the latter mineralised or ore-bearing varieties, Dictyonema shale and phosphorite. Mean concentrations of elements in the humus horizon of NE Estonian soils are close to the respective concentrations of the whole Estonian territory, but differ considerably from the mean concentrations of all continents