A new multi-level model for calculating the carbon footprint of agroecosystem products is proposed. The concept of “final carbon footprint” is introduced, which includes both direct CO₂ emissions from the operation of tractors, combines, oxidation of soil humus, CO₂-eq. during the transformation of nitrogen fertilizers in the soil, and indirect CO₂ emissions – carbon dioxide release into the atmosphere during the production of tractors, combines, tillage equipment, mineral fertilizers etc.
Based on the results of field experiments on gray forest soils in the Southern Moscow region, it is shown that when applying average doses of mineral fertilizers to field crops, the indirect CO₂ emissions are comparable to the CO₂ input from organic fuel oxidation when machinery is operating in the field. At higher doses of fertilizers, the indirect emissions are significantly greater than the CO₂ emissions from machinery operation. In order of increasing CO₂ emissions per 1 ha of sowing, crops on gray forest soils are arranged as follows: corn for silage > barley > winter wheat > clover.
Clover is a carbon-negative crop (−1.7 t/ha CO₂), i.e., CO₂ sequestration in the soil exceeds all CO₂ emissions from hay crop production. The final carbon footprint for grain crops, calculated using the standard method, was as follows: for winter wheat (with a fertilizer dose of N40P40K40) – 116 kg CO₂ per 1 centner of grain, for barley (with a dose of N60P40K40) – 104 kg CO₂ per 1 centner of grain. The final carbon footprint, taking into account the aftereffects of predecessors, was: for winter wheat (predecessor: two-year clover) – 48 kg CO₂ per 1 centner of grain; for barley (predecessor: silage corn) – 113 kg CO₂ per 1 centner of grain.

The article examines the problem of energy efficiency in the chain from the production of fertilizers to their logistics, application, and waste production and disposal based on the huge amount of data accumulated in recent years on greenhouse gas (GHG) emissions (primarily CO₂ and methane). Carbon dioxide emissions are shown to occur primarily from fuel combustion, as well as from the use of methane and CO₂ as precursors for nitrogen fertilizers. GHG emissions can be considered as a measure of energy efficiency when assessing the life cycle of mineral fertilizers. Relevant examples are given.

A new three-stage method for assessing the CO₂ balance in plant communities was formulated. The methodology includes not only taking into account the absorption of C-CO₂ during plantation vegetation, but also the processes occuring when using wood. In managed forests, when calculating the carbon balance, it is necessary to take into account the release of CO₂ not only at direct, but also at indirect consumption of technical energy for laying plantations, caring for them, and felling for final use. As a model, the consumption of technical energy in cultivating natural and genetically modified forms of aspen Populus tremula L. was calculated. The large role of indirect expenditure of technical energy in the C-CO₂ balance in forest plantations is shown. The use of a genetically modified clone of aspen significantly increases the productivity of plantations and CO₂ absorption from the atmosphere compared to its natural form. On a long time scale the final amount of CO₂ runoff from the atmosphere depends not only on the area of forests and their productivity, but also on the way of using wood. There is a highly effective way of using forest plantations to regulate the carbon dioxide content in the atmosphere, which is currently little paid attention, namely, the so-called substitution effect. Replacing energy-intensive materials (reinforced concrete, plastic, metal, and brick) with wood may be one of the main ways for the positive impact of forests on the CO₂ content in the atmosphere. The use of wood biomass from thinning, wood processing wastes, short-rotation forests for heat and power generation is a great reserve for replacing fossil hydrocarbons. The forest area needs to be expanded to increase wood production to replace energy-intensive building materials and generate biofuels.

This article examines the anthropogenic contribution to the planet’s climate system due to thermal pollution. Despite the quantitative predominance of solar and geothermal energy in the Earth’s heat balance, anthropogenic heat impacts the planet’s most sensitive shell – the biosphere. Thermal pollution in various countries has been assessed based on specific (per unit area) energy consumption, as all energy consumed by humanity is ultimately converted into heat and released into the biosphere. Specific carbon dioxide emissions also serve as an indirect indicator (marker) of thermal pollution, as fossil fuels remain the primary energy source. Calculated correlation coefficients between thermal pollution indicators (specific energy consumption and CO2 emissions) and climate warming in various regions have revealed a low positive correlation between these indicators (0.17–0.13, respectively), which indicates thermal pollution’s contribution to global warming to be still insignificant. Thus, the current contribution of anthropogenic heat to the climate system is primarily regional, which is undoubtedly important to consider in environmental policy to prevent the negative impact of this factor on the functioning of natural ecosystems. This is especially important in the context of global warming, primarily caused by natural factors.

At present, it is possible to identify a number of new directions for the development of biogeochemical research, at the junction of fundamental and applied studies. A novel field of research is being formed, namely, engineering biogeochemistry, within the framework of which innovative biogeochemical technologies and technological processes based on modeling and management of ecosystematic biogeochemical cycles are being developed. The application of these innovative technologies for the restoration of disturbed and polluted impact ecosystems, in particular, polar ecosystems in the zones of operation of gas-producing enterprises, is considered. Technological examples of calculations of geoecological risks, as well as microbial contamination risks are given. A pool of the developed biogeochemical technologies and their connection with other innovative technologies within the framework of gas-producing companies is shown.

Due to the large volume of coal mining in the Russian Federation and other countries, there is a serious issue of the formation of waste heaps from coal dumps, which pose a significant threat to the environment of adjacent territories. One of such areas is the Donetsk coal basin, whose area is more than 60 thousand km2. Phytoreclamation is the most common and cost-effective method recommended for the restoration of degraded coal dump soil, which reduces the removal of toxic substances with dust emissions and water runoff. However, plant growth on these soils is hindered by their phytotoxicity and unfavorable physical and physicochemical properties. The aim of this research was to develop a biogeochemical technology for the reclamation of coal dumps in Donbas based on phytoreclamation with various additives. Our experiments involved soil samples taken from the upper layer of the Ayutinskaya mine waste heap in the Donetsk coal basin, as well as zonal ordinary chernozem samples. The experiments were conducted in microfield conditions in bottomless vessels with an area of 0.1 m2 dug into the ground. The additives used were wood biochar and other sorbents, including mineral (diatomite and vermiculite) and organic (acidic and neutralized peat) ones, as well as ordinary chernozem and quarry sand – clean and with biohumus additives. The soil was seeded with a drought-resistant lawn mixture. All additives had a positive effect on the growth of green mass of drought-resistant lawn, measured during 3 cuttings ib the vegetation season of 2024. However, the best results were obtained with the addition of neutralized peat and chernozem at doses of 25 %, as well as quarry sand at doses of 25 and 50 % with the addition of biohumus; at the same time, the additional addition of 5 % biochar to all these samples gave no desired result.

The problem of global climate warming and attempts to solve it, including using low-carbon power engineering, are analyzed. The success of solving this problem depends on the degree of understanding of the processes which cause it. As more and more data speak about natural causes of climate fluctuations, and of anthropogenic factors the greatest contribution to the warming is made by thermal pollution rather than the anthropogenic growth of carbon dioxide in the atmosphere, low-carbon power, with all its positive qualities, is unable to solve the problem of climate warming.