Pub Date : 2023-12-13DOI: 10.3103/s014768742304004x
A.O. Makeev, A. V. Rusakov
Abstract
Paleopedology is a booming scientific discipline that studies the soils of the past geological epochs in order to assess the paleoenvironmental evolution. The scope of paleosol studies embraces not only soils themselves, but also the products of their involvement in biogeosphere cycles. This ensures the planetary role of pedogenesis, which includes the transformation of the upper layers of the lithosphere leading to the increase in fine earth, formation of new minerals, and residual or accumulative concentration of elements. In the geological history of the Earth, pedogenesis is realized within the framework of exogenesis, which includes weathering, soil formation, sedimentation, diagenesis, and geochemical migration. The pedolithosphere records the critical points in the landscape evolution of the Earth from the very onset of the geological record, including the oxygenation of the atmosphere, the emergence of the higher plants and herbaceous biomes, the dynamics of Interglacial–Glacial cycles, etc. Paleosols are the base for paleogeographic reconstructions and predictive models of the future climate change. Paleopedology expands the horizons of soil science within the system of biogeosphere sciences and determines the development of new scientific disciplines—bacterial paleontology, paleogeochemistry, biogeomorphology, astropedology, geoarchaeology, ecological paleopedology, soil paleocryogenesis and cryobiosphere studies. The historical dimension granted by paleopedology makes pedology a mature historical science.
{"title":"The Skyline of Paleopedology","authors":"A.O. Makeev, A. V. Rusakov","doi":"10.3103/s014768742304004x","DOIUrl":"https://doi.org/10.3103/s014768742304004x","url":null,"abstract":"<h3 data-test=\"abstract-sub-heading\">Abstract</h3><p>Paleopedology is a booming scientific discipline that studies the soils of the past geological epochs in order to assess the paleoenvironmental evolution. The scope of paleosol studies embraces not only soils themselves, but also the products of their involvement in biogeosphere cycles. This ensures the planetary role of pedogenesis, which includes the transformation of the upper layers of the lithosphere leading to the increase in fine earth, formation of new minerals, and residual or accumulative concentration of elements. In the geological history of the Earth, pedogenesis is realized within the framework of exogenesis, which includes weathering, soil formation, sedimentation, diagenesis, and geochemical migration. The pedolithosphere records the critical points in the landscape evolution of the Earth from the very onset of the geological record, including the oxygenation of the atmosphere, the emergence of the higher plants and herbaceous biomes, the dynamics of Interglacial–Glacial cycles, etc. Paleosols are the base for paleogeographic reconstructions and predictive models of the future climate change. Paleopedology expands the horizons of soil science within the system of biogeosphere sciences and determines the development of new scientific disciplines—bacterial paleontology, paleogeochemistry, biogeomorphology, astropedology, geoarchaeology, ecological paleopedology, soil paleocryogenesis and cryobiosphere studies. The historical dimension granted by paleopedology makes pedology a mature historical science.</p>","PeriodicalId":501690,"journal":{"name":"Moscow University Soil Science Bulletin","volume":"4 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2023-12-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"138633241","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 : 2023-12-13DOI: 10.3103/s0147687423040051
A. I. Shcheglov, O. B. Tsvetnova, G. I. Agapkina, D. N. Lipatov, D. V. Manakhov, S. V. Mamikhin, T. A. Paramonova, V. V. Stolbova, E. V. Tsvetnov
Abstract
The article deals with issues related to the development of radioecology as an independent scientific discipline. The achievements of past years and the studies that are currently being carried out, as well as promising areas of development in this area are analyzed. A corrected periodization of the stages of development of radioecology is proposed, taking into account the experience accumulated to date in the field of this discipline. At the initial stage (1895–1929), empirical material was collected; at the first stage (1930–1960), the theoretical foundation was laid and radioecology was formed as an independent discipline; at the second stage (1961–1990), intensive development of radioecology was noted; and, at the third stage (1991–2010), there was progressive development of radioecology; the fourth—modern—stage of the development of radioecology is in the beginning of the 21st century (2011–present). For each stage, the main scientific achievements and evolution of ideas in the field of radioecology are considered. It is postulated that, at present, the development of this discipline is associated with the further improvement of world nuclear technologies, the elimination of the consequences of a number of radiation incidents (the accident at the Fukushima nuclear power plant in 2011), the revision of the concept of radiation protection of the environment and a number of other provisions. Particular attention is paid to forest radioecology, one of the most important main areas of this science.
{"title":"Radioecology: Past, Present, Future","authors":"A. I. Shcheglov, O. B. Tsvetnova, G. I. Agapkina, D. N. Lipatov, D. V. Manakhov, S. V. Mamikhin, T. A. Paramonova, V. V. Stolbova, E. V. Tsvetnov","doi":"10.3103/s0147687423040051","DOIUrl":"https://doi.org/10.3103/s0147687423040051","url":null,"abstract":"<h3 data-test=\"abstract-sub-heading\">Abstract</h3><p>The article deals with issues related to the development of radioecology as an independent scientific discipline. The achievements of past years and the studies that are currently being carried out, as well as promising areas of development in this area are analyzed. A corrected periodization of the stages of development of radioecology is proposed, taking into account the experience accumulated to date in the field of this discipline. At the initial stage (1895–1929), empirical material was collected; at the first stage (1930–1960), the theoretical foundation was laid and radioecology was formed as an independent discipline; at the second stage (1961–1990), intensive development of radioecology was noted; and, at the third stage (1991–2010), there was progressive development of radioecology; the fourth—modern—stage of the development of radioecology is in the beginning of the 21st century (2011–present). For each stage, the main scientific achievements and evolution of ideas in the field of radioecology are considered. It is postulated that, at present, the development of this discipline is associated with the further improvement of world nuclear technologies, the elimination of the consequences of a number of radiation incidents (the accident at the Fukushima nuclear power plant in 2011), the revision of the concept of radiation protection of the environment and a number of other provisions. Particular attention is paid to forest radioecology, one of the most important main areas of this science.</p>","PeriodicalId":501690,"journal":{"name":"Moscow University Soil Science Bulletin","volume":"18 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2023-12-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"138633242","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 : 2023-12-01DOI: 10.3103/s0147687423040063
S. Shoba, I. Alyabina, O. Golozubov, P. A. Chekmaryov, S. V. Lukin, O. V. Chernova, V. Kolesnikova
{"title":"Experience in Creating an Information System for Rational Use of Soil Resources","authors":"S. Shoba, I. Alyabina, O. Golozubov, P. A. Chekmaryov, S. V. Lukin, O. V. Chernova, V. Kolesnikova","doi":"10.3103/s0147687423040063","DOIUrl":"https://doi.org/10.3103/s0147687423040063","url":null,"abstract":"","PeriodicalId":501690,"journal":{"name":"Moscow University Soil Science Bulletin","volume":"286 ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2023-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"139016664","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 : 2023-12-01DOI: 10.3103/s0147687423040087
A. L. Stepanov, N. A. Manucharova, D. A. Nikitin, M. V. Semenov
{"title":"Achievements and Prospects for Advancement of Soil Microbiology at Moscow State University","authors":"A. L. Stepanov, N. A. Manucharova, D. A. Nikitin, M. V. Semenov","doi":"10.3103/s0147687423040087","DOIUrl":"https://doi.org/10.3103/s0147687423040087","url":null,"abstract":"","PeriodicalId":501690,"journal":{"name":"Moscow University Soil Science Bulletin","volume":"17 ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2023-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"139015461","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 : 2023-12-01DOI: 10.3103/s0147687423060029
Abstract
In a long-term stationary field experiment on soddy–podzolic soil, the effectiveness of organic and mineral fertilizers and their effect on soil properties, yield, and quality of perennial grasses in feed six-field crop rotation was established. It was determined that the combined use of fertilizers most effectively affected the increase in soil fertility and the productivity of the clover-timothy mixture. The content of humus increased by 0.4–0.6%, mobile phosphorus by 70–150 mg/kg, metabolic and hydrolytic acidity decreased. The complex application of fertilizers, especially in high doses, most significantly increased the yield and quality of perennial grasses.
{"title":"The Effect of Long-Term Use of Organic and Mineral Fertilizers on the Agrochemical Properties of Soddy–Podzolic Soil and the Productivity of Perennial Grasses in Forage Culture in the European North","authors":"","doi":"10.3103/s0147687423060029","DOIUrl":"https://doi.org/10.3103/s0147687423060029","url":null,"abstract":"<span> <h3>Abstract</h3> <p>In a long-term stationary field experiment on soddy–podzolic soil, the effectiveness of organic and mineral fertilizers and their effect on soil properties, yield, and quality of perennial grasses in feed six-field crop rotation was established. It was determined that the combined use of fertilizers most effectively affected the increase in soil fertility and the productivity of the clover-timothy mixture. The content of humus increased by 0.4–0.6%, mobile phosphorus by 70–150 mg/kg, metabolic and hydrolytic acidity decreased. The complex application of fertilizers, especially in high doses, most significantly increased the yield and quality of perennial grasses.</p> </span>","PeriodicalId":501690,"journal":{"name":"Moscow University Soil Science Bulletin","volume":"5 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2023-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"139763461","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 : 2023-12-01DOI: 10.3103/s0147687423050046
Abstract
The banana sector contributes to 3% of the Colombia total exports, becoming the most important crop in the north of the country, benefiting more than 2.5 million families. Banana production is concentrated on the Colombian Caribbean coast where most of 90% of the soils are affected to some degree of salt affection in soils. This study was carried out in the municipality of Zona Bananera, Department of Magdalena (Colombia) elsewhere eleven geomorphological units were delimited through geomorphological surveying with geopedological methods. Given the high costs of implementing salt monitoring and management programs in the field, the implementation of Near Infrared spectroscopy (NIR) and image analysis are proposed as an alternative for mapping soils salt affectation. Geostatistical methods, traditional soil laboratory methods and multispectral analysis of 697 soil samples were analyzing using machine learning and spectral models. The Orthogonal Partial Linear Square- Discriminant Analyses (OPLS-DA), Principal Component Regression (PCR), Partial Linear Square (PLS–PLSR), Least Absolute Shrinkage and Selection Operator (LASSO) were implemented. Soil cartographies for SAS were designed in areas under banana cultivation, determining the affectation degree. The results obtained showed that 45.1% of the soils are affected by salts, with R2 0.76 and RMS 0.15 for the applied of supervised models. OPLS-DA had a better performance being the high above sea level was the principal covariable to improve the model accuracy. LASSO and PLS were useful to Mg+2 and K+ with RMSE 0.92 and 0.34 and R2 of 0.37 and 0.44, while Saitsky&Golay filter improved the predictions model for pH and Ca+2. The use of combined techniques of geopedology, geostatistics and spectroscopy were efficient, practical and cheap methodologies for evaluate soil properties associate to SAS in the stablished banana crops.
{"title":"Use of NIRS in Soil Properties Evaluation Related to Soil Salinity and Sodicity in Colombian Caribbean Coast","authors":"","doi":"10.3103/s0147687423050046","DOIUrl":"https://doi.org/10.3103/s0147687423050046","url":null,"abstract":"<span> <h3>Abstract</h3> <p>The banana sector contributes to 3% of the Colombia total exports, becoming the most important crop in the north of the country, benefiting more than 2.5 million families. Banana production is concentrated on the Colombian Caribbean coast where most of 90% of the soils are affected to some degree of salt affection in soils. This study was carried out in the municipality of Zona Bananera, Department of Magdalena (Colombia) elsewhere eleven geomorphological units were delimited through geomorphological surveying with geopedological methods. Given the high costs of implementing salt monitoring and management programs in the field, the implementation of Near Infrared spectroscopy (NIR) and image analysis are proposed as an alternative for mapping soils salt affectation. Geostatistical methods, traditional soil laboratory methods and multispectral analysis of 697 soil samples were analyzing using machine learning and spectral models. The Orthogonal Partial Linear Square- Discriminant Analyses (OPLS-DA), Principal Component Regression (PCR), Partial Linear Square (PLS–PLSR), Least Absolute Shrinkage and Selection Operator (LASSO) were implemented. Soil cartographies for SAS were designed in areas under banana cultivation, determining the affectation degree. The results obtained showed that 45.1% of the soils are affected by salts, with R<sup>2</sup> 0.76 and RMS 0.15 for the applied of supervised models. OPLS-DA had a better performance being the high above sea level was the principal covariable to improve the model accuracy. LASSO and PLS were useful to Mg<sup>+2</sup> and K<sup>+</sup> with RMSE 0.92 and 0.34 and R<sup>2</sup> of 0.37 and 0.44, while Saitsky&Golay filter improved the predictions model for pH and Ca<sup>+2</sup>. The use of combined techniques of geopedology, geostatistics and spectroscopy were efficient, practical and cheap methodologies for evaluate soil properties associate to SAS in the stablished banana crops.</p> </span>","PeriodicalId":501690,"journal":{"name":"Moscow University Soil Science Bulletin","volume":"11 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2023-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"139580073","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 : 2023-12-01DOI: 10.3103/s0147687423050058
Abstract
We present a review of the life and scientific legacy of the founder of soil colloid chemistry Konstantin Gedroiz. The phenomenon of absorption was first studied in the mid-1800s, and Gedroiz started working on base exchange and absorption in soils in 1906. Based on the general pattern of cation exchange reactions, he proposed the concept of “absorption capacity” and “soil absorption complex”, developed ideas about exchange acidity and the rate of exchange reactions, revealed the unique role of absorbed sodium and potassium in soil processes, and proposed the theory of the accumulation of sodium due to exchange reactions. He was one of the first to classify soil on the basis of the absorbing complexes and cations, which was a new approach in pedology. He used the climate classification of soils, and described Podzols, Laterites, and Chernozems in terms of their absorbing complexes and cations. The system of classification worked for mature soils in which pedogenic processes had proceeded to such an extent that the profile characteristics reflected a climatic region, but was less effective in alluvial soils and eroded soils. His studies established the connections between chemical and physical processes and the morphology of soils. He studied the evolution of saline soils from a chemical point of view, which led to the practical recommendations for chemical reclamation of Solonetz and liming of acidic soils. Gedroiz’s work was groundbreaking but insufficiently known outside Russia until his books have been translated into English and German in the late 1920s. The soil microbiologist Selman Waksman in the 1925 translated 11 of his papers into English, and the United State Department of Agriculture distributed copies of these translations. In 1927 a textbook on chemical analysis, “Die chemische Bodenanalyse”, was published; in 1930 the books “Der adsorbierende Bodenkomplex und die adsorbierten Bodenkationen als Grundlage der genetischen Bodenklassification” and “On the Problem of exchangeable Hydrogen and exchangeable Aluminium in acid soils”, a 1931 – “Die Lehre vom Adsorptionsvermögen der Böden”.
摘要 我们对土壤胶体化学创始人康斯坦丁-格德罗伊茨的生平和科学遗产进行了回顾。19 世纪中期，人们开始研究吸收现象，格德罗伊茨于 1906 年开始研究土壤中的碱基交换和吸收。他根据阳离子交换反应的一般规律，提出了 "吸收能力 "和 "土壤吸收复合体 "的概念，发展了关于交换酸度和交换反应速率的观点，揭示了吸收的钠和钾在土壤过程中的独特作用，并提出了交换反应导致钠积累的理论。他是最早根据吸收络合物和阳离子对土壤进行分类的人之一，这是土壤学的一种新方法。他采用了土壤的气候分类法，并根据土壤的吸收复合体和阳离子对 Podzols、Laterites 和 Chernozems 进行了描述。该分类系统适用于成土，因为成土过程已经发展到一定程度，其剖面特征反映了一个气候区域，但对冲积土和侵蚀土的效果较差。他的研究建立了化学和物理过程与土壤形态之间的联系。他从化学角度研究了盐碱土的演变，从而提出了对索洛涅茨进行化学开垦和对酸性土壤进行石灰化处理的实用建议。格德罗伊茨的工作具有开创性，但在俄罗斯之外却鲜为人知，直到 20 世纪 20 年代末，他的著作才被翻译成英文和德文。1925 年，土壤微生物学家塞尔曼-瓦克斯曼（Selman Waksman）将他的 11 篇论文翻译成英文，美国农业部分发了这些译本。1927 年出版了化学分析教科书《Die chemische Bodenanalyse》；1930 年出版了《Der adsorbierende Bodenkomplex und die adsorbierten Bodenkationen als Grundlage der genetischen Bodenklassification》和《On the Problem of exchangeable Hydrogen and exchangeable Aluminium in acid soils》，1931 年出版了《Die Lehre vom Adsorptionsvermögen der Böden》。
{"title":"Konstantin Gedroiz (1872–1932)—the Initial Studies of Soil Colloid Chemistry and Soil Salinity","authors":"","doi":"10.3103/s0147687423050058","DOIUrl":"https://doi.org/10.3103/s0147687423050058","url":null,"abstract":"<span> <h3>Abstract</h3> <p>We present a review of the life and scientific legacy of the founder of soil colloid chemistry Konstantin Gedroiz. The phenomenon of absorption was first studied in the mid-1800s, and Gedroiz started working on base exchange and absorption in soils in 1906. Based on the general pattern of cation exchange reactions, he proposed the concept of “absorption capacity” and “soil absorption complex”, developed ideas about exchange acidity and the rate of exchange reactions, revealed the unique role of absorbed sodium and potassium in soil processes, and proposed the theory of the accumulation of sodium due to exchange reactions. He was one of the first to classify soil on the basis of the absorbing complexes and cations, which was a new approach in pedology. He used the climate classification of soils, and described Podzols, Laterites, and Chernozems in terms of their absorbing complexes and cations. The system of classification worked for mature soils in which pedogenic processes had proceeded to such an extent that the profile characteristics reflected a climatic region, but was less effective in alluvial soils and eroded soils. His studies established the connections between chemical and physical processes and the morphology of soils. He studied the evolution of saline soils from a chemical point of view, which led to the practical recommendations for chemical reclamation of Solonetz and liming of acidic soils. Gedroiz’s work was groundbreaking but insufficiently known outside Russia until his books have been translated into English and German in the late 1920s. The soil microbiologist Selman Waksman in the 1925 translated 11 of his papers into English, and the United State Department of Agriculture distributed copies of these translations. In 1927 a textbook on chemical analysis, “Die chemische Bodenanalyse”, was published; in 1930 the books “Der adsorbierende Bodenkomplex und die adsorbierten Bodenkationen als Grundlage der genetischen Bodenklassification” and “On the Problem of exchangeable Hydrogen and exchangeable Aluminium in acid soils”, a 1931 – “Die Lehre vom Adsorptionsvermögen der Böden”.</p> </span>","PeriodicalId":501690,"journal":{"name":"Moscow University Soil Science Bulletin","volume":"105 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2023-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"139580133","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 : 2023-12-01DOI: 10.3103/s0147687423060017
Abstract
The organic matter of water-stable macro- (2–1 mm) and free microaggregates (<0.25 mm) isolated from the 2–1 mm air-dry macroaggregates of Haplic Chernozem in the contrasting land use variants was studied by granulo-desitometric fractionation. It was revealed that water-stable free microaggregates are only parts of disintegrated macroaggregates. The composition of microaggregates unstable under the sonication (mWSA) within structural units of different sizes (macro- (WSAma) and microaggregates (WSAmi)) has been studied in detail. The composition of mWSA within WSA of different size is completely identical; they differ only in size, quantity, and packing density. Within WSAmi, the size and quantity of mWSA are by 1.7- and 1130-fold smaller than those within WSAma. The packing density of mWSAma is 1.5-fold less than that of mWSAmi.
{"title":"Organic Matter of the Water-stable Structural Unites of Haplic Chernozem in Contrasting Variants of Land Use (Steppe vs. bare Fallow)","authors":"","doi":"10.3103/s0147687423060017","DOIUrl":"https://doi.org/10.3103/s0147687423060017","url":null,"abstract":"<span> <h3>Abstract</h3> <p>The organic matter of water-stable macro- (2–1 mm) and free microaggregates (<0.25 mm) isolated from the 2–1 mm air-dry macroaggregates of Haplic Chernozem in the contrasting land use variants was studied by granulo-desitometric fractionation. It was revealed that water-stable free microaggregates are only parts of disintegrated macroaggregates. The composition of microaggregates unstable under the sonication (mWSA) within structural units of different sizes (macro- (WSA<sub>ma</sub>) and microaggregates (WSA<sub>mi</sub>)) has been studied in detail. The composition of mWSA within WSA of different size is completely identical; they differ only in size, quantity, and packing density. Within WSA<sub>mi</sub>, the size and quantity of mWSA are by 1.7- and 1130-fold smaller than those within WSA<sub>ma</sub>. The packing density of mWSA<sub>ma</sub> is 1.5-fold less than that of mWSA<sub>mi</sub>.</p> </span>","PeriodicalId":501690,"journal":{"name":"Moscow University Soil Science Bulletin","volume":"22 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2023-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"139763007","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 : 2023-09-01DOI: 10.3103/S0147687423330013
I. Bagdasarov, M. Tseits, Yu.A. Kryukova, K. Taskina, M. V. Konyushkova
{"title":"Erratum to: A Comparative Characterization of the Soils and Plant Cover of Tombolos on the Coasts of the White and Baltic Seas","authors":"I. Bagdasarov, M. Tseits, Yu.A. Kryukova, K. Taskina, M. V. Konyushkova","doi":"10.3103/S0147687423330013","DOIUrl":"https://doi.org/10.3103/S0147687423330013","url":null,"abstract":"","PeriodicalId":501690,"journal":{"name":"Moscow University Soil Science Bulletin","volume":"72 1","pages":"318"},"PeriodicalIF":0.0,"publicationDate":"2023-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"139345732","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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