Pub Date : 2020-03-27DOI: 10.19047/0136-1694-2020-101-5-18
I. Savin
: The analysis of peculiarities of applied use of soil data has been carried out. It is shown that most of practical tasks require spatial information about soils and their properties. In this regard, a soil map is considered as a kind of interface between theoretical and applied soil science. The disadvantages complete the information of soil maps with information about modern processes occurring in soils, which can be obtained from spatial digital modeling.
{"title":"Spatial aspects of applied Soil Science","authors":"I. Savin","doi":"10.19047/0136-1694-2020-101-5-18","DOIUrl":"https://doi.org/10.19047/0136-1694-2020-101-5-18","url":null,"abstract":": The analysis of peculiarities of applied use of soil data has been carried out. It is shown that most of practical tasks require spatial information about soils and their properties. In this regard, a soil map is considered as a kind of interface between theoretical and applied soil science. The disadvantages complete the information of soil maps with information about modern processes occurring in soils, which can be obtained from spatial digital modeling.","PeriodicalId":52755,"journal":{"name":"Biulleten'' Pochvennogo instituta im VV Dokuchaeva","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2020-03-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"41933339","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2020-01-03DOI: 10.19047/0136-1694-2019-100-159-189
O. Kutovaya, A. Tkhakakhova, M. Semenov, T. Chernov, N. A. Ksenofontova, Alena Zhelezova, R. Gadzhiumarov, R. S. Stukalov, E. Ivanova, D. Nikitin
Using the method of inoculation on elective nutrient media, the abundance and activity of taxonomic (bacteria, actinomycetes, micromycetes) and functional (nitrogen fixers, ammonifiers, denitrifiers of amylolytic, cellulolytic) groups of microorganisms in agrochernozems of the Stavropol region under the influence of various tillage systems – direct seeding (no-till) and moldboard plowing with the turnover of soil horizon (traditional treatment). Analyzes were carried out for such crops as winter wheat, corn, sunflower and soybean with/without application of mineral fertilizers. Traditional tillage for the majority of crops leads to increased activity of aerobic ammonifiers, cellulolytics, denitrifiers, actinomycetes and micromycetes. No-till technology, in its turn, increases the intensity of anaerobic cellulolytics and nitrogen fixers, aerobic diazotrophs and amylolytics activity. The most responsive crop, under which the biological activity of almost all groups of microorganisms increased in the no-till variant, was corn, while winter wheat contributed to the increase in the number of microorganisms in the moldboard plowing variant. The use of mineral fertilizers provoked the growth of soil biological activity under sunflower sown directly in the soil, while conventional tillage resulted in higher soil biological activity without application of mineral fertilizers.
{"title":"Comparative evaluation of the influence of no-till and traditional treatment on the biological activity of agricultural chernozem of the Stavropol region","authors":"O. Kutovaya, A. Tkhakakhova, M. Semenov, T. Chernov, N. A. Ksenofontova, Alena Zhelezova, R. Gadzhiumarov, R. S. Stukalov, E. Ivanova, D. Nikitin","doi":"10.19047/0136-1694-2019-100-159-189","DOIUrl":"https://doi.org/10.19047/0136-1694-2019-100-159-189","url":null,"abstract":"Using the method of inoculation on elective nutrient media, the abundance and activity of taxonomic (bacteria, actinomycetes, micromycetes) and functional (nitrogen fixers, ammonifiers, denitrifiers of amylolytic, cellulolytic) groups of microorganisms in agrochernozems of the Stavropol region under the influence of various tillage systems – direct seeding (no-till) and moldboard plowing with the turnover of soil horizon (traditional treatment). Analyzes were carried out for such crops as winter wheat, corn, sunflower and soybean with/without application of mineral fertilizers. Traditional tillage for the majority of crops leads to increased activity of aerobic ammonifiers, cellulolytics, denitrifiers, actinomycetes and micromycetes. No-till technology, in its turn, increases the intensity of anaerobic cellulolytics and nitrogen fixers, aerobic diazotrophs and amylolytics activity. The most responsive crop, under which the biological activity of almost all groups of microorganisms increased in the no-till variant, was corn, while winter wheat contributed to the increase in the number of microorganisms in the moldboard plowing variant. The use of mineral fertilizers provoked the growth of soil biological activity under sunflower sown directly in the soil, while conventional tillage resulted in higher soil biological activity without application of mineral fertilizers.","PeriodicalId":52755,"journal":{"name":"Biulleten'' Pochvennogo instituta im VV Dokuchaeva","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2020-01-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"47173380","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2020-01-03DOI: 10.19047/0136-1694-2019-100-5-35
D. Kozlov, A. Zhidkin, N. I. Lozbenev
: The paper presents original developments on the application of WaTEM/SEDEM erosion model for large-scale mapping of erosion patterns of the soil cover in the Central Russian Upland. The share of eroded soils in the composition of soil combinations on plowed slopes was evaluated; such estimation was carried out on the basis of a statistical comparison of the calculated rates of soil losses with the results of actual soil-morphological diagnostics of the degree of chernozems erosion. The obtained relations between share of eroded soils in soil cover patterns and modelled erosion rates were used for development of the map depicting typified combinations of soils with various degrees of erosion. Comparison with detailed soil survey materials showed that the map is accurate enough for the spatial diversity and configuration of eroded soils combinations description. At the given input parameters of the erosion model qualitative changes in the soil cover structure (share of slightly-eroded soils is more than 10%) start from the threshold value of water erosion of 8 t·ha -1 ·year -1 . With an average annual erosion of 30 t·ha - 1 ·year -1 , the share of denuded soils exceeds 50%. The developed approach seems and for planning the erosion control measures in adaptive-landscape agriculture. в) and modelled
{"title":"Digital mapping of soil cover eroded patterns on the bassis of soil erosion simulation model (northern forest-steppe of the Central Russian Upland)","authors":"D. Kozlov, A. Zhidkin, N. I. Lozbenev","doi":"10.19047/0136-1694-2019-100-5-35","DOIUrl":"https://doi.org/10.19047/0136-1694-2019-100-5-35","url":null,"abstract":": The paper presents original developments on the application of WaTEM/SEDEM erosion model for large-scale mapping of erosion patterns of the soil cover in the Central Russian Upland. The share of eroded soils in the composition of soil combinations on plowed slopes was evaluated; such estimation was carried out on the basis of a statistical comparison of the calculated rates of soil losses with the results of actual soil-morphological diagnostics of the degree of chernozems erosion. The obtained relations between share of eroded soils in soil cover patterns and modelled erosion rates were used for development of the map depicting typified combinations of soils with various degrees of erosion. Comparison with detailed soil survey materials showed that the map is accurate enough for the spatial diversity and configuration of eroded soils combinations description. At the given input parameters of the erosion model qualitative changes in the soil cover structure (share of slightly-eroded soils is more than 10%) start from the threshold value of water erosion of 8 t·ha -1 ·year -1 . With an average annual erosion of 30 t·ha - 1 ·year -1 , the share of denuded soils exceeds 50%. The developed approach seems and for planning the erosion control measures in adaptive-landscape agriculture. в) and modelled","PeriodicalId":52755,"journal":{"name":"Biulleten'' Pochvennogo instituta im VV Dokuchaeva","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2020-01-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"68253642","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2019-12-09DOI: 10.19047/0136-1694-2019-99-47-61
E. I. Kravchenko
The agents that determine the soil salinity of the key plots “Chervlenoe” and “Duboovrazhniy” of the Svetloyarsk irrigation system (Volgograd region) are studied. We carried out a multifactor analysis of the toxic salts amount variance depending on the following agents: relief, vegetation, parent material and irrigation method, the water extract (1 : 5) being used. It was found that the factors determining the degree of soil salinity in terms of the amount of toxic salts in both cases is parent material. Its contribution into the total variance was more than 80 % for both studied plots. On the plot “Duboovrazhniy” relief also turned out to be a significant factor. Anthropogenic factor – the method of irrigation – was insignificant. The graphs of cumulative frequencies of the occurrence of salinity levels were constructed for soil layers of 0–30 cm, 30–100 cm, 100–150 cm, 150–200 cm. The top soil layer of 0–30 cm is almost non-saline in both areas. On the “Chervlenoe” plot there are strong and very strong degrees of soil salinization; in general, this site is characterized by higher toxic salts amount compared to the “Duboovrazhniy” plot.
{"title":"Agents of soil salinization in “Chervlenoe” and “Duboovrazhniy” plots of the Svetloyarsk irrigation system","authors":"E. I. Kravchenko","doi":"10.19047/0136-1694-2019-99-47-61","DOIUrl":"https://doi.org/10.19047/0136-1694-2019-99-47-61","url":null,"abstract":"The agents that determine the soil salinity of the key plots “Chervlenoe” and “Duboovrazhniy” of the Svetloyarsk irrigation system (Volgograd region) are studied. We carried out a multifactor analysis of the toxic salts amount variance depending on the following agents: relief, vegetation, parent material and irrigation method, the water extract (1 : 5) being used. It was found that the factors determining the degree of soil salinity in terms of the amount of toxic salts in both cases is parent material. Its contribution into the total variance was more than 80 % for both studied plots. On the plot “Duboovrazhniy” relief also turned out to be a significant factor. Anthropogenic factor – the method of irrigation – was insignificant. The graphs of cumulative frequencies of the occurrence of salinity levels were constructed for soil layers of 0–30 cm, 30–100 cm, 100–150 cm, 150–200 cm. The top soil layer of 0–30 cm is almost non-saline in both areas. On the “Chervlenoe” plot there are strong and very strong degrees of soil salinization; in general, this site is characterized by higher toxic salts amount compared to the “Duboovrazhniy” plot.","PeriodicalId":52755,"journal":{"name":"Biulleten'' Pochvennogo instituta im VV Dokuchaeva","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2019-12-09","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"47316390","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2019-09-23DOI: 10.19047/0136-1694-2019-98-5-36
P. M. Shilov, D. Kozlov
A methodical approach to the digital mapping of the arable lands area depending on their soil-agroecological and positional conditions is proposed. The approach was tested on a model plot located on the Valdai Upland with an area of 160 thousand ha. Small-scale agricultural development of the poorly dissected moraine plains is limited by the wide distribution of overmoistened soils. Using the traditional discriminant analysis, a measure of the topographically determined duration of soil overmoistening was calculated based on a comparison of the morphological diagnostics of water regime and topography runoff properties according to the grid elements of 30 × 30 m. The drainability range was determined for the arable lands of XVIII century, reconstructed according to the materials of the General Survey. This allowed us to determine the potential area of the arable lands for this period. The area of arable lands, which is characterized by favorable conditions of transport accessibility and soil drainability, was 12 %. At the same time, reconstructed area contained 5 %. In the subsistence economy of the XVIII century more than a half of the potential arable lands of the model region turned out to be undeveloped.
{"title":"SOIL-AGRO-ECOLOGICAL ASSESSMENT OF THE ARABLE LAND OF THE VALDAI UPLAND BASED ON THE GENERAL SURVEY","authors":"P. M. Shilov, D. Kozlov","doi":"10.19047/0136-1694-2019-98-5-36","DOIUrl":"https://doi.org/10.19047/0136-1694-2019-98-5-36","url":null,"abstract":"A methodical approach to the digital mapping of the arable lands area depending on their soil-agroecological and positional conditions is proposed. The approach was tested on a model plot located on the Valdai Upland with an area of 160 thousand ha. Small-scale agricultural development of the poorly dissected moraine plains is limited by the wide distribution of overmoistened soils. Using the traditional discriminant analysis, a measure of the topographically determined duration of soil overmoistening was calculated based on a comparison of the morphological diagnostics of water regime and topography runoff properties according to the grid elements of 30 × 30 m. The drainability range was determined for the arable lands of XVIII century, reconstructed according to the materials of the General Survey. This allowed us to determine the potential area of the arable lands for this period. The area of arable lands, which is characterized by favorable conditions of transport accessibility and soil drainability, was 12 %. At the same time, reconstructed area contained 5 %. In the subsistence economy of the XVIII century more than a half of the potential arable lands of the model region turned out to be undeveloped.","PeriodicalId":52755,"journal":{"name":"Biulleten'' Pochvennogo instituta im VV Dokuchaeva","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2019-09-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"68254182","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2019-09-23DOI: 10.19047/0136-1694-2019-98-77-104
E. Taller, Z. Artemyeva, N. Kirillova, N. Danchenko
{"title":"DYNAMICS OF ORGANIC MATTER UNDER THE AFFORESTATION OF THE FORMER AGRICULTURAL SOD-PODZOLIC SOILS","authors":"E. Taller, Z. Artemyeva, N. Kirillova, N. Danchenko","doi":"10.19047/0136-1694-2019-98-77-104","DOIUrl":"https://doi.org/10.19047/0136-1694-2019-98-77-104","url":null,"abstract":"","PeriodicalId":52755,"journal":{"name":"Biulleten'' Pochvennogo instituta im VV Dokuchaeva","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2019-09-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"47919699","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2019-09-23DOI: 10.19047/0136-1694-2019-98-132-152
S. Yudin, V. Belobrov, V. K. Drediger, A. M. Grebenikov, A. J. Aydiev, B. Ilyin, N. Ermolaev
{"title":"TO THE QUESTION OF THE METHODOLOGY OF CONDUCTING LONG-TERM EXPERIMENTS ON THE NO-TILL TECHNOLOGY INFLUENCE ON SOIL PROPERTIES","authors":"S. Yudin, V. Belobrov, V. K. Drediger, A. M. Grebenikov, A. J. Aydiev, B. Ilyin, N. Ermolaev","doi":"10.19047/0136-1694-2019-98-132-152","DOIUrl":"https://doi.org/10.19047/0136-1694-2019-98-132-152","url":null,"abstract":"","PeriodicalId":52755,"journal":{"name":"Biulleten'' Pochvennogo instituta im VV Dokuchaeva","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2019-09-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"45494510","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2019-09-23DOI: 10.19047/0136-1694-2019-98-153-184
E. Migunova
The main results of studying the effect of artificial woody vegetation on chernozem are briefly described in the article, as well as the influence of soil and soil condition on composition and productivity of forest plantations. The effect of soil salinity on plant growth is characterized. The toxicity of different groups of readily soluble salts, especially chlorides and soda, has been evaluated. The decisive role of the depth of toxic amounts of chlorides and the level of water availability in the soil usability has been established. The ecological series of water availability for plants in different soil types have been developed and the degree of suitability of groundwater of different salinity has been evaluated. The power of the root zone as a limiting factor has been estimated, as far as the level of mineral elements supply for plant nutrition (trophicity) in the soil is determined by the greatest total amounts of phosphorus and potassium in the root zone (excluding potassium enclosed in feldspar lattices). All the intrazonal diversity of nature is due to the nutrient status and moisture content in the soil. Along with the warmth level these limiting resources develop one or another level of soil fertility. The role of subsurface runoff in the formation of forest-steppe landscapes is characterized. The stages and phases of the primary soil-forming process are highlighted. It is argued that soil zonality results from bioinert nature of the soil. The article substantiates the statement that soil fertility is a factor ensuring the stability of life on Earth; and the ways of promoting Soil Science at the level of the theoretical basis for agriculture have been proposed.
{"title":"RESULTS OF THE 70-YEAR RESEARCH AT THE INTERFACE OF FORESTRY AND SOIL SCIENCE","authors":"E. Migunova","doi":"10.19047/0136-1694-2019-98-153-184","DOIUrl":"https://doi.org/10.19047/0136-1694-2019-98-153-184","url":null,"abstract":"The main results of studying the effect of artificial woody vegetation on chernozem are briefly described in the article, as well as the influence of soil and soil condition on composition and productivity of forest plantations. The effect of soil salinity on plant growth is characterized. The toxicity of different groups of readily soluble salts, especially chlorides and soda, has been evaluated. The decisive role of the depth of toxic amounts of chlorides and the level of water availability in the soil usability has been established. The ecological series of water availability for plants in different soil types have been developed and the degree of suitability of groundwater of different salinity has been evaluated. The power of the root zone as a limiting factor has been estimated, as far as the level of mineral elements supply for plant nutrition (trophicity) in the soil is determined by the greatest total amounts of phosphorus and potassium in the root zone (excluding potassium enclosed in feldspar lattices). All the intrazonal diversity of nature is due to the nutrient status and moisture content in the soil. Along with the warmth level these limiting resources develop one or another level of soil fertility. The role of subsurface runoff in the formation of forest-steppe landscapes is characterized. The stages and phases of the primary soil-forming process are highlighted. It is argued that soil zonality results from bioinert nature of the soil. The article substantiates the statement that soil fertility is a factor ensuring the stability of life on Earth; and the ways of promoting Soil Science at the level of the theoretical basis for agriculture have been proposed.","PeriodicalId":52755,"journal":{"name":"Biulleten'' Pochvennogo instituta im VV Dokuchaeva","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2019-09-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"41251235","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2019-09-23DOI: 10.19047/0136-1694-2019-98-105-131
E. Prudnikova, E. Varlamov, N. Churilin, A. E. Churilina
During the model experiment the changes in the mineralogical composition of the open surface of arable soil (leached chernozem, gray forest soil, sod-podzolic soil) under the impact of raindrops under fallow conditions were studied. At the end of the experiment a mineralogical analysis of individual particle size fractions 10 μm from microcrusts formed on open surfaces and a soil substrate not exposed to the effects of precipitation was conducted. The study found that during the exposure there was redistribution and changes in the proportional ratios of the contents of different particle size fractions and associated clay and clastogenic minerals. During the experiment the most significant changes due to their composition occurred in the sample of sod-podzolic soil and leached chernozem. The content of clay minerals in exposed samples decreased the most. The redistribution of clastogenic minerals from the upper open layer, mostly from fine silt and to a lesser extent from the middle silty fraction, was accompanied by a relative accumulation of the fraction > 10 μm. The redistribution of granulometric fractions was accompanied by a relative accumulation of quartz, orthoclases and a decrease in the content of chlorite and biotide in them. Such a distribution is determined by their resistance to weathering. Balance calculations allowed establishing that the total losses of clay and clastogenic minerals from the upper open surface of the monoliths in comparison with the initial soil substrate were more than 4 kg / 100 kg of monolith for gray forest soil, 16 kg / 100 kg of monolith for leached chernozem and 46 kg / 100 kg of monolith for sod-podzolic soil.
{"title":"DIFFERENTIATION AND BALANCE OF MINERALS DURING TRANSFORMATION OF THE OPEN SURFACE OF ARABLE SOILS UNDER THE IMPACT OF RAIN","authors":"E. Prudnikova, E. Varlamov, N. Churilin, A. E. Churilina","doi":"10.19047/0136-1694-2019-98-105-131","DOIUrl":"https://doi.org/10.19047/0136-1694-2019-98-105-131","url":null,"abstract":"During the model experiment the changes in the mineralogical composition of the open surface of arable soil (leached chernozem, gray forest soil, sod-podzolic soil) under the impact of raindrops under fallow conditions were studied. At the end of the experiment a mineralogical analysis of individual particle size fractions 10 μm from microcrusts formed on open surfaces and a soil substrate not exposed to the effects of precipitation was conducted. The study found that during the exposure there was redistribution and changes in the proportional ratios of the contents of different particle size fractions and associated clay and clastogenic minerals. During the experiment the most significant changes due to their composition occurred in the sample of sod-podzolic soil and leached chernozem. The content of clay minerals in exposed samples decreased the most. The redistribution of clastogenic minerals from the upper open layer, mostly from fine silt and to a lesser extent from the middle silty fraction, was accompanied by a relative accumulation of the fraction > 10 μm. The redistribution of granulometric fractions was accompanied by a relative accumulation of quartz, orthoclases and a decrease in the content of chlorite and biotide in them. Such a distribution is determined by their resistance to weathering. Balance calculations allowed establishing that the total losses of clay and clastogenic minerals from the upper open surface of the monoliths in comparison with the initial soil substrate were more than 4 kg / 100 kg of monolith for gray forest soil, 16 kg / 100 kg of monolith for leached chernozem and 46 kg / 100 kg of monolith for sod-podzolic soil.","PeriodicalId":52755,"journal":{"name":"Biulleten'' Pochvennogo instituta im VV Dokuchaeva","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2019-09-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"68253996","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2019-09-15DOI: 10.19047/0136-1694-2019-98-185-202
А. Л. Иванов, Владимир Степанович Столбовой
The implementation of the “4 per mille” or “4 per 1000” Initiative in Russia can be one of the instruments mitigating concentration of the greenhouse gases in the atmosphere. It is estimated that the total annual absorption of carbon dioxide (CO 2 ), including natural dynamics and application of carbon saving technologies in agriculture, can be as much as 23–28 % of annual emission of the gas into the atmosphere. The “4 per 1000” Initiative mechanism will operate successfully for 12–15 years, which corresponds to the time of saturation of arable soil with carbon. The implementation of the “4 per mille” Initiative is not only Russia's positioning among the countries that support sustainable, energy-efficient and environmentally friendly development, but also demonstrates the ability of the country to realize its competitive advantages in demand in the low-carbon world.
{"title":"ИНИЦИАТИВА “4 ПРОМИЛЛЕ” – НОВЫЙ ГЛОБАЛЬНЫЙ ВЫЗОВ ДЛЯ ПОЧВ РОССИИ","authors":"А. Л. Иванов, Владимир Степанович Столбовой","doi":"10.19047/0136-1694-2019-98-185-202","DOIUrl":"https://doi.org/10.19047/0136-1694-2019-98-185-202","url":null,"abstract":"The implementation of the “4 per mille” or “4 per 1000” Initiative in Russia can be one of the instruments mitigating concentration of the greenhouse gases in the atmosphere. It is estimated that the total annual absorption of carbon dioxide (CO 2 ), including natural dynamics and application of carbon saving technologies in agriculture, can be as much as 23–28 % of annual emission of the gas into the atmosphere. The “4 per 1000” Initiative mechanism will operate successfully for 12–15 years, which corresponds to the time of saturation of arable soil with carbon. The implementation of the “4 per mille” Initiative is not only Russia's positioning among the countries that support sustainable, energy-efficient and environmentally friendly development, but also demonstrates the ability of the country to realize its competitive advantages in demand in the low-carbon world.","PeriodicalId":52755,"journal":{"name":"Biulleten'' Pochvennogo instituta im VV Dokuchaeva","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2019-09-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"68254068","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
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