Cs-137 is considered to be the most significant anthropogenic contributor to human dose and presents a particularly difficult remediation challenge after a dispersal following nuclear incident. The Chernobyl Nuclear Power Plant meltdown in April 1986 represents the largest nuclear accident in history and released over 80 PBq of 137Cs into the environment. As a result, much of the land in close proximity to Chernobyl, which includes the Polessie State Radioecology Reserve in Belarus, remains highly contaminated with 137Cs to such an extent they remain uninhabitable. Whilst there is a broad scale understanding of the depositional patterns within and beyond the exclusion zone, detailed mapping of the distribution is often limited. New developments in mobile gamma spectrometry provide the opportunity to map the fallout of 137Cs and begin to reconstruct the depositional environment and the long-term behaviour of 137Cs in the environment. Here, full gamma spectrum analysis using algorithms based on the peak-valley ratio derived from Monte Carlo simulations are used to estimate the total 137Cs deposition and its depth distribution in the soil. The results revealed a pattern of 137Cs distribution consistent with the deposition occurring at a time of flooding, which is validated by review of satellite imagery acquired at similar times of the year. The results were also consistent with systematic burial of the fallout 137Cs by annual flooding events. These results were validated by sediment cores collected along a transect across the flood plain. The true merit of the approach was confirmed by exposing new insights into the spatial distribution and long term fate of 137Cs across the floodplain. Such systematic patterns of behaviour are likely to be fundamental to the understanding of the radioecological behaviour of 137Cs whilst also providing a tracer for quantifying the ecological controls on sediment movement and deposition at a landscape scale.

There are some peculiarities in instrumental observation over snow cover characteristics in Belarus and those of neighboring countries. Maximum snow water equivalent varies around Belarus from 107 mm in Brest to 207 mm in Novogrudok. It differs significantly in terms of years, which is proved by high values of variation coefficients (Cᵥ). Maximums are observed in the south and south-west of Belarus. Minimum values are typical for central and north-eastern parts of Belarus with a stable snow cover. There is a distinct correlation between snow water equivalent and the stations’ altitude. We observe a space-time variability of SWE in Belarus’ river catchments. Changes in SWE are of cyclic nature. They correlate with current climate fluctuations. In certain parts of Belarus, there is a trend in reduction of SWE up to 8–10 mm in 10 years. This research determines the amount of water that forms spring flood runoff in the catchments of Belarus’ big rivers. Possible daily snow melting is calculated in the research as well. It reaches 26 mm in its maximum and 5–6 mm on average. The amount of river runoff water, which is formed within Belarus, is 58 km³. The amount of melt water is 11 km³, which accounts for 19%. In particularly extreme years, melt water reaches 29 km³, which is over a half of all annual river runoff.

This article investigates the long-run and causal linkages between economic growth, CO₂ emissions, renewable and non-renewable (fossil fuels) energy consumption, the Composite Trade Intensity (CTI) as a proxy for trade openness, and the Chinn-Ito index as a proxy for financial openness for a panel of the Commonwealth of Independent States (CIS) region including Armenia, Azerbaijan, Belarus, Georgia, Kazakhstan, Kyrgyzstan, Moldova, Russia, Tajikistan, Turkmenistan, Ukraine, and Uzbekistan over the period of 1992–2015. It is the first time that CTI and the Chinn-Ito indexes are used in an economic-pollution model. Employing three panel unit root tests, panel cointegration estimation methods (DOLS and FMOLS), and two panel causality tests, the main empirical results provided evidence for the bidirectional long-run relationship between all the variables in all 12 sampled countries except for economic growth-renewable energy use linkage. The findings of causality tests indicated that there is a unidirectional short-run panel causality running from economic growth, financial openness, and trade openness to CO₂ emissions and from fossil fuel energy consumption to renewable energy use.

Presented in this paper is result of the study of the bioconcentration potential of mercury (Hg) by Suillus luteus mushroom collected from regions within Central, Eastern, and Northern regions of Europe. As determined by cold-vapor atomic absorption spectroscopy, the Hg content varied from 0.13 ± 0.05 to 0.33 ± 0.13 mg kg⁻¹ dry matter for caps and from 0.038 ± 0.014 to 0.095 ± 0.038 mg kg⁻¹ dry matter in stems. The Hg content of the soil substratum (0–10 cm layer) underneath the fruiting bodies showed generally low Hg concentrations that varied widely ranging from 0.0030 to 0.15 mg kg⁻¹ dry matter with mean values varying from 0.0078 ± 0.0035 to 0.053 ± 0.025 mg kg⁻¹ dry matter, which is below typical content in the Earth crust. The caps were observed to be on the richer in Hg than the stems at ratio between 1.8 ± 0.4 and 5.3 ± 2.6. The S. luteus mushroom showed moderate ability to accumulate Hg with bioconcentration factor (BCF) values ranging from 3.6 ± 1.3 to 42 ± 18. The consumption of fresh S. luteus mushroom in quantities up to 300 g week⁻¹ (assuming no Hg ingestion from other foods) from background areas in the Central, Eastern, and Northern part of Europe will not result in the intake of Hg exceeds the provisional weekly tolerance limit (PTWI) of 0.004 mg kg⁻¹ body mass.

The environmental radiation pollution resulting from the Chernobyl nuclear disaster in 1986 is one of the main factors limiting agriculture in the eastern regions of Belarus. In the first decade after the accident, the need to mitigate the effects of radiation had a key role in the implementation of countermeasures. As a result, there are widespread areas of high soil fertility potential in the contaminated zone. Today there is a possibility to include new crops (e.g. sugar beet [Beta vulgaris L.]) into regular crop rotation to increase the effectiveness of agriculture and to use the accumulated soil fertility potential. The article discusses a possible agronomic approach to estimating specific fields (working plots) at the scale of agricultural enterprises for placement of sugar beet. The territory of the Mahilyow region of the Republic of Belarus was examined from the perspective of soil suitability to the cultivation of sugar beet. Along with estimating radionuclide accumulation by sugar beet roots, the areas of soils suitable for sugar beet within agricultural enterprises were calculated for selected districts. It was revealed that sugar beet has low ability to absorb radiocaesium and radiostrontium from soils. The contamination density does not restrict the possibility for placement of sugar beet. Instead, soil fertility, specifically content of plant-available phosphorus and boron, was the limiting factor in that. Based on data from field experiments and soil fertility data, a number of enterprises were selected where sugar beet could be included into crop rotations to high economic effect.