Background to the research project and its implementation

Eero Tikkanen

Prior to the mid-1980s, very little forest damage research related to airborne pollutants had been conducted in Finnish Lapland and what there was was of non-uniform character (Tikkanen 1989, 1991). This state of affairs was partly explained by the general conception of Finnish Lapland as an unpolluted region and of its forests as being healthy and vigorous. As a thought-to-be pollution-free background area, Lapland found use mainly as a source of control material for environmental studies conducted elsewhere. Air quality measurements were attended to at national stations located in Sodankylä and Kevo (Utsjoki) where data was collected on the quality of background air.

It was in connection with the national acidification research project HAPRO (an acronym derived from the programme's name in Finnish meaning The Finnish Acidification Research Programme) in 1985 that the Finnish Forest Research Institute (METLA) launched a project called ILME (an acronym derived from the project's name in Finnish meaning The Effect of Air Pollution on Forest Ecosystems) delving into the impact of airborne pollutants on forests. A network of more than 3 000 permanent sample plots was established during the years 1985 and 1986 in connection with the 8th national forest inventory to enable the vitality and state of health of Finnish forests to be monitored. Based on systematic sampling, this network was made less dense in Lapland (as it was believed to be less polluted than the rest of the country) than in southern and central Finland.

Forest damage in Lapland at the end of the 1980s

Research looking into forest vitality and their state of health in Lapland was stepped up after the mid-1980s. In 1986, around 390 permanent forest-stand sample plots were established in Finnish Lapland to meet the requirements of the ILME project. These sample plots are mainly located in pine stands. Some of them are intended for what may be called extensive research while others are for intensive research. Measurements and observations made on the intensive level sample plots are repeated annually; on the extensive level plots this is done every five years. Assessments done on these sample plots include, for instance, assessment of relative defoliation.

Severest defoliation in Scots pine in northernmost Lapland

The annually repeated assessment of forest vitality during the years 1986-1989 revealed that Lapland's most severely defoliated pines were located in northernmost Lapland, around Inari (Fig. 2) (Jukola-Sulonen et al. 1993). The loss of needles by these trees increased by 10 percent points during the four year monitoring period. Needle loss increased with increasing tree age. In addition to being influenced by tree age and the northern location, needle loss by Scots pine in the Inari region of Finnish Lapland was also believed to be influenced by sulphur and heavy metal deposition originating from the Kola Peninsula.

Severe needle loss phenomenon in southern Lapland in the summer of 1987

Northern Finland's forests provided the setting for an unexpected phenomenon in the early weeks of the summer of 1987. In numerous stands located on peatland sites and sorted, nutrient-poor heathland mineral soil sites, conifers of varying ages began to shed their needles prematurely. The shedding started from the oldest year classes of needles and advanced to the younger shoots. At first the afflicted needles turned yellow, and then, prior to being shed, brown. This damage was at its worst in Scots pine (Fig. 3).

Research into the causes of the premature needle shedding showed that the afflicted pines were suffering from disturbances in their nutrient and water status. Needle analyses showed that the afflicted trees translocated mobile nutrients from their old needles abnormally early to their juvenile, meristematic parts (Tikkanen & Raitio 1990a, 1990b, 1990/91, 1993). However, the afflicted trees' contents of nutrients that plants are unable to translocate were lower in the youngest shoots of the afflicted trees than in healthy trees and in trees in control areas.

The disturbances in the nutrient status of the trees were found to be caused by root injuries, since the results of soil analyses conducted in the study areas showed that the nutrient levels in the soil were equal to the average of equivalent sites. The primary cause of root damage was in the exceptional weather conditions of the years 1986 and 1987. The needle loss situation was at its worst in southern Lapland and Kainuu - regions where the above-average warm and rainy autumn of 1986 was followed by a steep fall in temperature in early December. Severe frosts froze up the almost snowless ground rapidly and to a great depth. Even in January 1987 the cover of snow was 20-30 cm below the average for that time of the year.

The role of weather in the occurrence of the damage was further supported by the observation that roots are more susceptible to injury due to low temperatures than shoots and that the hardening of roots in preparation for winter begins later. Snow is important for roots in that it provides an insulating layer against low temperatures. This is especially so on nutrient-poor, lichen-dominated heathland forest sites, where the humus layer and the lichen layer are thin (the thinness of the latter being due to grazing by reindeer). In addition to being influenced by weather factors, the ability of trees to withstand external stresses may have been affected by airborne pollutants. Among other effects, these are known to cause discoloration of needles and their premature shedding.

Scleroderris canker (Gremmeniella abietina) damage in Salla

In 1988, damaged stands of Scots pine were found in Salla, eastern Lapland, and along the Finno-Russian border. This damage was at its severest along the border zone and in the localities Rikkilehto and Lautakotaoja (both in Salla). The pines were discovered to be damaged by the Scleroderris canker (Gremmeniella abietina) (Fig. 4). The stands afflicted by this fungus pest were concentrated alongside watercourses and other low-lying places on the plateau bearing Scots pine (Kaitera & Jalkanen 1992).

Damage to the environment in the Kola Peninsula

Due to military policy reasons, the Kola Peninsula in north-western Russia was an out-of-bounds region to foreigners for decades. The immense scale of the damage to the environment around the industrial centres of Nikel and Zapolyarnyy in the north-west and Monchegorsk in the central part of the Kola Peninsula was revealed to Finns as recently as in the late 1980s. The nickel and copper smelters established over fifty years ago in these industrial centres (Pechenganikel in Nikel and Zapolyarnyy and Severonikel in Monchegorsk) have caused marked loading of the environment and unparalleled damage to the forest ecosystems of the region (Fig. 5).

Immense emissions of sulphur dioxide and heavy metals have completely destroyed the vegetation over vast areas and erosion has removed the soil overlying the bedrock (Fig. 6). Russian scientists estimate that industrial deserts, entirely or almost entirely void of vegetation, surrounding the smelter towns cover several hundreds of square kilometres (Kryuchkov 1991, 1993).

The northern location of the afflicted areas has increased the susceptibility of the local ecosystems to the detrimental effects of airborne pollutants. A report published in 1989 on the state of the environment in the then Soviet Union mentions the Kola Peninsula among the eight most seriously polluted eco-catastrophe areas (Report on...1988). Some idea as to the amount of emissions of pollutants from the Kola Peninsula was obtained by Western scientists in connection with a joint-Nordic monitoring study conducted in the mid-1980s on heavy metals in mosses (Rühling et al. 1987). Similar observations were made in the late 1980s in the course of the aforementioned HAPRO project and in studies conducted by the Lapland Water and Environment District focusing on the acidification of watercourses in Finnish Lapland and in the Kola Peninsula (Kauppi et al. 1990, Kenttämies 1991, Kinnunen 1990, 1992).

The signs of forest damage observed in Finnish Lapland in the late 1980s, and the information made available on the emissions of pollutants from the Kola Peninsula and the damage to that region's environment, gave rise to suspect some link between them. The conception of an unpolluted Lapland and of its healthy, vigorous forests began to crumble. Forest owners in eastern Finnish Lapland fearing increment losses and other concerned citizens commenced to express demands for stepping up of forest damage studies and air quality measurements in Lapland. The news media were also increasingly vociferous as they joined in these demands.

Launching of the Lapland Forest Damage Project

In May, 1989, the Finnish Forest Research Institute (METLA) invited representatives of Finnish universities and research institutes to the METLA's Vantaa Research Centre to contribute ideas as to the stepping up of air-pollution-related forest damage research in Finnish Lapland. In addition to the METLA's own representatives, this meeting was attended by researchers from the Universities of Helsinki and Oulu, the Finnish Meteorological Institute, the Geological Survey of Finland, and the Lapland Water and Environment District. This meeting founded the five- year (1990-1994) Lapland Forest Damage Project and appointed the project a planning group and a project manager. Planning work for the project was commenced following the granting of a planning appropriation sum of 100 000 Finnish markkas by the Ministry of Agriculture and Forestry.

Finnish research institutes and universities involved in wide-ranging co-operation

Following the founding meeting, the Universities of Kuopio and Turku (Åbo) and University of Lapland (the Arctic Centre) also joined in the project. All in all, the Lapland Forest Damage Project has been participated in by ca. 50 researchers from four universities and five research institutes. The METLA had personnel from its Helsinki and Vantaa Research Centres and the institute's research stations in Parkano, Suonenjoki, Muhos and Rovaniemi taking part in the project (Fig. 7). In addition to the contribution of researchers, the project has benefited from the involvement of field, laboratory and data processing personnel.

At the time the Lapland Forest Damage Project was launched, the HAPRO project had already come to its conclusion and the work of another research project SILMU (an acronym derived from the Finnish name of the research programme meaning The Finnish Research Programme on Climate Change) had not yet begun. This being the case, the Forest Damage Project had at its disposal some of the best Finnish resources in the field of environmental research.

Co-operation with Russian environmental researchers commences

Up until the late 1980s, the information available on the environmental research conducted in the Kola Peninsula was far from comprehensive. Among the earliest pieces of first-hand knowledge of this work was that provided by the Russian scientists who participated in an environmental seminar in Rovaniemi in 1988 (Kinnunen & Varmola 1990). It was not until the Lapland Forest Damage Project was launched that tangible research co-operation between Finnish and Russian scientists - forest researchers employed in the Kola Peninsula - began.

The first researcher visits from Finland to the problem areas in the Kola Peninsula took place in 1989. This was followed by the forming of contacts with the Kola Science Centre based in Apatity and research co- operation was commenced with the recently founded Institute of North Industrial Ecology Problems and researchers employed at this institute's Laboratory of Terrestial Ecosystems. Subsequently, the sphere of co- operation has been joined in by researchers from the Archangel Forest Research Institute's Monchegorsk Research Station and the Laplandia Nature Reserve (Fig. 7). These forms of co-operation have made it possible for Finnish researchers to work and collect material in Russian territory. Likewise, Russian researchers have made excursions into Finnish Lapland to collect material for their studies. In addition, they have worked at Finnish research institutes and participated in relevant environmental meetings and congresses held in Finland. Finns have also promoted the practice of joint publications with Russian researchers (Tikkanen & Varmola 1991, Tikkanen et al. 1992, Derome 1993).

Sixteen subprojects

Initially, the Lapland Forest Damage Project comprised thirteen subprojects distributed among the universities and research institutes involved in the project in Finland. The overall co-ordination of the project was embodied in the co-ordinating subproject based at the METLA's Rovaniemi research station. Using the project's results, the co-ordinating group has, for instance, compiled a database, which will continue to be updated at the Rovaniemi research station.

Assessment of the damaged areas in the Kola Peninsula began with the interpretation of satellite imagery. The impact of pollutant emissions on the region's forests commenced with studies looking into stress and damage symptoms in conifer needles, their chemical composition and frost-hardiness, the biochemistry and occurrence of the Scleroderris canker, the occurrence, functioning and structure of lichens on the stems and branches of trees, the litter on the forest floor, the chemical composition of bark and mosses, the soil and percolating water, soil microbiology, and the roots and growth of Scots pine. Three new subprojects were established during the years 1990-1992. These addressed the issues of air quality and deposition, and the influence that the lichen layer has on the soil and the frost-hardiness of Scots pine roots. All sixteen subprojects were appointed a responsible researcher.

Challenging goals

The principal goal of the Lapland Forest Damage Project was to study the impact that pollutant emissions from the Kola Peninsula were believed to have on the forests of Finnish Lapland. Alongside this endeavour, there was the aim of producing basic scientific knowledge about Lapland's forest ecosystems and the changes taking place in them. Further goals included the pinpointing and delimiting of damaged areas in Russian territory; at the time when the project was launched, the information available on these damaged areas was of conflicting nature. The research data produced by the project is necessary when taking decisions on restrictions to be imposed on emissions. In the early 1990s, demands were expressed in favour of restricting emissions from the Kola Peninsula; some went as far as to demand their total elimination. The two basic solutions were either to refurbish the smelters or close them down.

Material and methods

The Lapland Forest Damage Project's planning group, which commenced its work in June 1989, decided to employ the gradient research method in the project. This method examines the impact that airborne pollutants have on the environment by taking into consideration the distance from the pollution source.

The gradient method is generally employed in studies where the study area is fairly small: i.e. when monitoring individual pollution sources or the surroundings of population centres. When dealing with large areas, problems are caused by natural, geographical variation (e.g. climate- related) which is independent of the pollution load. The use of the gradient method over the vast territory involved when examining Finnish and Russian Lapland was made possible by non-complex boreal ecosystems with their dearth of species and the fact that the pollution sources consisted of three smelter towns in the Kola Peninsula. A further aid when making observations of the situation was that there were no other equivalent pollution sources in latitudes above the Arctic Circle in Norway, Sweden, Finland or north-western Russia.

Sample plots established in forests on heathland soils

During the years 1989-1990, the METLA established sample plots in forests growing on dry and dryish heathland sites assumed to be sensitive to acidification. The forest stands thus sampled are pine- dominated with tree age varying between 80 and 200 years and an even or eastwards sloping topography. The sample plot interval along the south-west-, west-, and north-west-oriented gradient lines traversing Finnish Lapland is 4 km at the border, and then progressively increases to 8, 16 and 32 km as the distance from the pollution sources increases (Fig. 9).

The establishing of sample plots in the Kola Peninsula in 1990 secured the continuation of the sampling lines from the border all the way to the pollution sources. Intensive sample plots were also established in Svanvik, north-eastern Norway, in the same year. A total of 133 sample plots were placed along the sampling lines. Of these, fourteen in Finnish Lapland, seven in the Kola Peninsula and two in Norway were subjected to more detailed study - i.e. they were what may be called intensive sample plots. In actual fact, the number of sample plots is several times greater because each sampling point consists of a cluster of 3-4 sample plots. Additionally, data collecting is concentrated to separate "sampling" sample plots as a means of reducing the human impact on the permanent sample plots (Fig. 10). The field measurements and collecting of material serving the needs of all subprojects were concentrated on the same sample plots - occasionally even the same trees.

In 1990 and 1991, a further sixteen "lichen sample plots" were established within the Lapland Forest Damage Project. The decision to do so was influenced by observations made in conjunction with the establishing of the intensive sample plots of the abundance of reindeer lichen communities in the Kola Peninsula. The lichen sample plots are located in western Finnish Lapland, in Angeli (Inari) and Muonio, and in eastern Finnish Lapland, in Inari's Raja-Jooseppi and Salla's Naruska (Fig. 9). These sample plots have enabled studies focusing on the influence of the lichen layer on the soil and the frost-hardiness of Scots pine roots.

Material ranging from satellite imagery to the subsoil

The range of material used in the Lapland Forest Damage Project comprised tree roots, mycorrhizae, fungi, lichens from the stems and branches of trees, ground lichens, mosses, needles, soil, percolating water, rain water and snow, and bark, litter and seeds of trees. Other research data were obtained in the form of increment borings, assessments of tree vitality, air and soil temperature measurements, and satellite imagery, the latter being used in locating and delimiting damaged areas. In addition to these, the project personnel made use of the data collected at the various air-quality monitoring stations in Lapland.

Financing of the project

The funding of the project by Finland's Ministry of Agriculture and Forestry varied within the range of 3.0-3.7 million Finnish marks during the years 1990-1994. Over the five years of the project's activities, the Ministry granted a total of ca. 17.5 million Finnish marks. In addition to the funds from the Ministry, financing was directed to the project via the various participating research organisations. The METLA, for instance, invested nearly 10 million Finnish marks.

Final report in English

The Lapland Forest Damage Projects Interim Report was published in June 1992 (Kauhanen & Varmola 1992). The present document is the 5-year-long project's Final Report hypertext version in English, and it is based on the more comprehensive Final Report in Finnish published in March 1995 (Tikkanen 1995).

Following on from the chapter titled Background to the research project and its implementation, this document contains an article of general interest on The forests and forest research in Finnish Lapland. The subsequent eight chapters then proceed to set out the centrally significant results obtained in the course of the project. The book ends with the chapter Conclusions reflecting upon the results achieved and the degree to which the Lapland Forest Damage Project's goals were fulfilled.