C. Kabała, J. Komisarek, M. Świtoniak, M. Kozłowski
{"title":"Correspondence between the legend units of the soil map of Poland (1:300,000), soil-agricultural map, forest soil-habitat map and soil types of Polish Soil Classification (2019) based on analysis of soil profiles","authors":"C. Kabała, J. Komisarek, M. Świtoniak, M. Kozłowski","doi":"10.37501/soilsa/156069","DOIUrl":"https://doi.org/10.37501/soilsa/156069","url":null,"abstract":"","PeriodicalId":44772,"journal":{"name":"Soil Science Annual","volume":"79 1","pages":""},"PeriodicalIF":1.5,"publicationDate":"2022-10-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"82636701","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}
{"title":"In memory of Professor Zbigniew Czerwiński (1932-2022)","authors":"J. Chojnicki","doi":"10.37501/soilsa/156068","DOIUrl":"https://doi.org/10.37501/soilsa/156068","url":null,"abstract":"","PeriodicalId":44772,"journal":{"name":"Soil Science Annual","volume":"59 1","pages":""},"PeriodicalIF":1.5,"publicationDate":"2022-10-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"88390815","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}
{"title":"Soil loss tolerance for agricultural land of the Right-Bank Steppe of Ukraine","authors":"S. Chornyy","doi":"10.37501/soilsa/156066","DOIUrl":"https://doi.org/10.37501/soilsa/156066","url":null,"abstract":"","PeriodicalId":44772,"journal":{"name":"Soil Science Annual","volume":"1 1","pages":""},"PeriodicalIF":1.5,"publicationDate":"2022-10-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"81390341","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}
The inhibitory effects of neem leaf extract on fertilizer nitrogen (N) transformation in soil have not been fully recognized. This study therefore aimed to evaluate the effects of fi ve nitri fi cation inhibitors on the status of soil inorganic N, urea hydrolysis, and nitri fi cation: i) no inhibitor (control); ii) nitrapyrin; and three rates of neem leaf extract based on the dry weight of the raw material: iii) 1 g kg –1 soil; iv) 2 g kg –1 soil; v) 4 g kg –1 soil. Neem leaf extract in all rates increased urea hydrolysis rate on days 5 − 15. In contrast, nitrapyrin decreased urea hydrolysis on days 5 − 10, compared to the control. As for nitri fi cation, neem leaf extract showed both stimulatory and inhibitory effects. The stimulation ap-peared on day 3, whereas inhibition occurred and peaked on days 5 − 15. Nitrapyrin showed inhibitory effects on days 10 − 15, reaching its peak on day 15. Increasing rates of neem leaf extract brought about increases in stimulation and inhibition of urea hydrolysis and nitri fi cation. The results conclusively stated that the neem leaf extract had generally faster, stronger, and longer nitri fi cation inhibition than nitrapyrin. The stimulation in the early phase and the inhibition in the later phase of the incubation of neem leaf extract were more pronounced with higher application rates.
楝叶提取物对土壤氮素转化的抑制作用尚未得到充分认识。因此，本研究旨在评价5种氮化抑制剂对土壤无机氮、尿素水解和氮化状态的影响:1)无抑制剂(对照);(二)nitrapyrin;根据原料的干重，印楝叶提取物的三种配比:iii) 1 g kg -1土壤;Iv) 2 g kg -1土壤;V) 4克公斤-1土壤。在第5 ~ 15天，所有比例的印楝叶提取物都提高了尿素水解率。相比之下，与对照组相比，硝基吡啶在第5 ~ 10天减少了尿素水解。印楝叶提取物对硝态氮具有刺激和抑制作用。刺激在第3天出现，而抑制在第5 ~ 15天出现并达到峰值。Nitrapyrin在第10 ~ 15天表现出抑制作用，在第15天达到峰值。随着印楝叶提取物用量的增加，对尿素水解和硝态化的刺激和抑制作用增强。结果表明，印楝叶提取物对硝基阳离子的抑制作用一般比硝基霉素更快、更强、更持久。印楝叶提取物在培养初期的刺激作用和后期的抑制作用随着施用量的增加而明显。
{"title":"Effects of neem leaf extract on inorganic nitrogen transformation in sandy soil","authors":"S. Butnan, Janista Duangpukdee, P. Sriraj","doi":"10.37501/soilsa/156072","DOIUrl":"https://doi.org/10.37501/soilsa/156072","url":null,"abstract":"The inhibitory effects of neem leaf extract on fertilizer nitrogen (N) transformation in soil have not been fully recognized. This study therefore aimed to evaluate the effects of fi ve nitri fi cation inhibitors on the status of soil inorganic N, urea hydrolysis, and nitri fi cation: i) no inhibitor (control); ii) nitrapyrin; and three rates of neem leaf extract based on the dry weight of the raw material: iii) 1 g kg –1 soil; iv) 2 g kg –1 soil; v) 4 g kg –1 soil. Neem leaf extract in all rates increased urea hydrolysis rate on days 5 − 15. In contrast, nitrapyrin decreased urea hydrolysis on days 5 − 10, compared to the control. As for nitri fi cation, neem leaf extract showed both stimulatory and inhibitory effects. The stimulation ap-peared on day 3, whereas inhibition occurred and peaked on days 5 − 15. Nitrapyrin showed inhibitory effects on days 10 − 15, reaching its peak on day 15. Increasing rates of neem leaf extract brought about increases in stimulation and inhibition of urea hydrolysis and nitri fi cation. The results conclusively stated that the neem leaf extract had generally faster, stronger, and longer nitri fi cation inhibition than nitrapyrin. The stimulation in the early phase and the inhibition in the later phase of the incubation of neem leaf extract were more pronounced with higher application rates.","PeriodicalId":44772,"journal":{"name":"Soil Science Annual","volume":"87 1","pages":""},"PeriodicalIF":1.5,"publicationDate":"2022-10-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"84045396","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}
The aim of our research was to present the properties of alluvial soils from mountain forest areas. Additionally, the paper presents the vegetation accompanying the studied soils. The detailed characteristics will include the stand and the undergrowth. 10 study plots representing mountain areas were included in the study. Study plots were located in the mountains in the Bielsko, Ustro ń , Szklarska Por ę ba, W ę gierska Górka forest districts as well as the Bieszczadzki, Babiogórski and Tatrza ń ski National Parks. At each sample plot a detailed description of soil pro fi le has been carried out, samples were collected from each genetic horizon in order to perform the basic determinations of the soil properties. On each research plot, a phytosociological relevé using the Braun-Blanquet method and a taxonomic description of the tree stand were performed. The diagnosis of forest site type was determined according to forest management principles and the Trophic Soil Index was calculated. The properties of mountain alluvial soils are related to the properties of the rock complexes within which alluvial terraces are formed. Mountain alluvial soils belong to various groups (Fluvisols, Leptosols, Cambisols, Phaeozems), which depend on the valley location and anthropogenic factors. River regulation and the disappearance of fl oods result in the formation of soils with a cambic horizon and acidi fi cation of the surface horizons devoid of the in fl uence of water. Two main plant communities are associated with mountain alluvial soils: Alnetum incanae and Carici remotae-Fraxinetum . Ecosystems related to mountain alluvial soils are very valuable due to their high biodiversity and ful fi lling various ecosystem functions.
{"title":"Forest habitats developed on alluvial soils in the area of mountains","authors":"J. Lasota, E. Błońska","doi":"10.37501/soilsa/156060","DOIUrl":"https://doi.org/10.37501/soilsa/156060","url":null,"abstract":"The aim of our research was to present the properties of alluvial soils from mountain forest areas. Additionally, the paper presents the vegetation accompanying the studied soils. The detailed characteristics will include the stand and the undergrowth. 10 study plots representing mountain areas were included in the study. Study plots were located in the mountains in the Bielsko, Ustro ń , Szklarska Por ę ba, W ę gierska Górka forest districts as well as the Bieszczadzki, Babiogórski and Tatrza ń ski National Parks. At each sample plot a detailed description of soil pro fi le has been carried out, samples were collected from each genetic horizon in order to perform the basic determinations of the soil properties. On each research plot, a phytosociological relevé using the Braun-Blanquet method and a taxonomic description of the tree stand were performed. The diagnosis of forest site type was determined according to forest management principles and the Trophic Soil Index was calculated. The properties of mountain alluvial soils are related to the properties of the rock complexes within which alluvial terraces are formed. Mountain alluvial soils belong to various groups (Fluvisols, Leptosols, Cambisols, Phaeozems), which depend on the valley location and anthropogenic factors. River regulation and the disappearance of fl oods result in the formation of soils with a cambic horizon and acidi fi cation of the surface horizons devoid of the in fl uence of water. Two main plant communities are associated with mountain alluvial soils: Alnetum incanae and Carici remotae-Fraxinetum . Ecosystems related to mountain alluvial soils are very valuable due to their high biodiversity and ful fi lling various ecosystem functions.","PeriodicalId":44772,"journal":{"name":"Soil Science Annual","volume":"84 5 1","pages":""},"PeriodicalIF":1.5,"publicationDate":"2022-10-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"89328413","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}
In terms of the mutual arrangement of individual properties, alluvial soils are unpredictable and do not fi t into the regularities most often found in arable soils. Often, soil density does not increase with the sampling depth
{"title":"Selected physical and water properties of alluvial soils in the context of their susceptibility to drainage degradation","authors":"Z. Kaczmarek, P. Gajewski","doi":"10.37501/soilsa/156063","DOIUrl":"https://doi.org/10.37501/soilsa/156063","url":null,"abstract":"In terms of the mutual arrangement of individual properties, alluvial soils are unpredictable and do not fi t into the regularities most often found in arable soils. Often, soil density does not increase with the sampling depth","PeriodicalId":44772,"journal":{"name":"Soil Science Annual","volume":"22 1","pages":""},"PeriodicalIF":1.5,"publicationDate":"2022-10-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"72898713","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}
The aim of the research carried out in the middle Odra valley, SW Poland, was to demonstrate the diversi fi cation of the morphology and selected properties of alluvial soils used for agricultural purposes and to assess their changes in the conditions of river regulation. The research was carried out in the low valley of the Odra River in its middle course downstream from Wroc ł aw. Four soil pro fi les were exposed on the right bank of the Odra River on the Holocene fl oodplain terrace. Two pro fi les were located in the embanked zone used as grassland
{"title":"Morphology and selected properties of alluvial soils in the Odra River valley, SW Poland","authors":"D. Kawałko, J. Kaszubkiewicz, P. Jezierski","doi":"10.37501/soilsa/156062","DOIUrl":"https://doi.org/10.37501/soilsa/156062","url":null,"abstract":"The aim of the research carried out in the middle Odra valley, SW Poland, was to demonstrate the diversi fi cation of the morphology and selected properties of alluvial soils used for agricultural purposes and to assess their changes in the conditions of river regulation. The research was carried out in the low valley of the Odra River in its middle course downstream from Wroc ł aw. Four soil pro fi les were exposed on the right bank of the Odra River on the Holocene fl oodplain terrace. Two pro fi les were located in the embanked zone used as grassland","PeriodicalId":44772,"journal":{"name":"Soil Science Annual","volume":"55 1","pages":""},"PeriodicalIF":1.5,"publicationDate":"2022-10-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"79863894","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}
This study was aimed at characterizing the soil-forming processes and certain properties of soils that have developed from alluvial sediments in the valley of the Kamienna stream, which represents a headwater stream valley deeply incised into the glacial and fl uvioglacial deposits of Middle Pomerania, north Poland. Seven soil pro fi les distributed, along the stream, were described, sam-pled, and analyzed using standard procedures. The parent materials of the soils showed strati fi cation and were characterized by a sandy texture with considerable admixtures of gravel in some horizons. A textural measures indicated their accumulation in a highly dynamic fl uvial environment. The soils showed broad spatial heterogeneity, highlighting the importance of local-scale factors in their formation. The accumulation of soil organic matter (SOM) and gleying from groundwater were identi fi ed as major soil-forming processes, which was re fl ected in soil reference groups dis-tinguished – Eutric Gleyic Fluvisols, Fluvic Gleyic Mollic Umbrisols, Fluvic Gleyic Phaeozems, and Fluvic Phaeozems. The soils were characterized by deep A horizons and high SOM contents. The strati fi cation of these horizons can indicate the partially allochthonous origin of this component, with the headwater bogs in the upper and middle courses of the stream potentially its source. Additionally, the soils were rich in nitrogen, but poor in total P, K, Ca, Mg, Fe, and Al. The generally low contribution of free Fe oxides to the soils indicated poorly advanced weathering, whereas the predominance of amorphous forms of Fe over crystalline could be the effect of high moisture and the SOM content. The soils were also characterized by a low cation exchange capacity, that varied depending on the SOM and clay contents. The soils were generally acidic, with pH values fl uctuating around 5.0–7.0, in most cases, although the predominance of acidic over basic ions was not appar-ent in the sorption complex.
{"title":"Soil-forming processes and properties of soils developed from fluvic materials in the headwater river valleys of Middle Pomerania, north Poland: A case study of the Kamienna stream","authors":"J. Jonczak, A. Parzych, Krzysztof Sztabkowski","doi":"10.37501/soilsa/156044","DOIUrl":"https://doi.org/10.37501/soilsa/156044","url":null,"abstract":"This study was aimed at characterizing the soil-forming processes and certain properties of soils that have developed from alluvial sediments in the valley of the Kamienna stream, which represents a headwater stream valley deeply incised into the glacial and fl uvioglacial deposits of Middle Pomerania, north Poland. Seven soil pro fi les distributed, along the stream, were described, sam-pled, and analyzed using standard procedures. The parent materials of the soils showed strati fi cation and were characterized by a sandy texture with considerable admixtures of gravel in some horizons. A textural measures indicated their accumulation in a highly dynamic fl uvial environment. The soils showed broad spatial heterogeneity, highlighting the importance of local-scale factors in their formation. The accumulation of soil organic matter (SOM) and gleying from groundwater were identi fi ed as major soil-forming processes, which was re fl ected in soil reference groups dis-tinguished – Eutric Gleyic Fluvisols, Fluvic Gleyic Mollic Umbrisols, Fluvic Gleyic Phaeozems, and Fluvic Phaeozems. The soils were characterized by deep A horizons and high SOM contents. The strati fi cation of these horizons can indicate the partially allochthonous origin of this component, with the headwater bogs in the upper and middle courses of the stream potentially its source. Additionally, the soils were rich in nitrogen, but poor in total P, K, Ca, Mg, Fe, and Al. The generally low contribution of free Fe oxides to the soils indicated poorly advanced weathering, whereas the predominance of amorphous forms of Fe over crystalline could be the effect of high moisture and the SOM content. The soils were also characterized by a low cation exchange capacity, that varied depending on the SOM and clay contents. The soils were generally acidic, with pH values fl uctuating around 5.0–7.0, in most cases, although the predominance of acidic over basic ions was not appar-ent in the sorption complex.","PeriodicalId":44772,"journal":{"name":"Soil Science Annual","volume":"24 1","pages":""},"PeriodicalIF":1.5,"publicationDate":"2022-10-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"83239261","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}
The Soil Science Society of Poland has elected alluvial soils (Polish: mady) to be the Soils of the Year 2022. Although alluvial soils cover less than 5% of Poland, they have high importance for agriculture and forestry due to their speci fi c location in river valleys, moisture status and high potential productivity. Moreover, alluvial soils play crucial role for functioning of many protected natural and semi-natural ecosystems in river valleys. Strati fi ed alluvial soils, commonly involving buried topsoil horizons, are also important for the reconstruction of natural environmental changes (in particular climatic and hydrological ones) and human impact on the landscape. This paper presents: (a) a concept of alluvial soils in Poland; (b) a review of the development and transformation of alluvial soils in relation to river valley dynamics and human in fl uences, (c) historical and present classi fi cation schemes for alluvial soils in Poland and their correlation with international classi fi cation systems (WRB and Soil Taxonomy); and (d) utility of alluvial soils for agriculture and forestry based on their physicochemical properties and water regime.
{"title":"Origin, transformation and classification of alluvial soils (mady) in Poland – soils of the year 2022","authors":"C. Kabała","doi":"10.37501/soilsa/156043","DOIUrl":"https://doi.org/10.37501/soilsa/156043","url":null,"abstract":"The Soil Science Society of Poland has elected alluvial soils (Polish: mady) to be the Soils of the Year 2022. Although alluvial soils cover less than 5% of Poland, they have high importance for agriculture and forestry due to their speci fi c location in river valleys, moisture status and high potential productivity. Moreover, alluvial soils play crucial role for functioning of many protected natural and semi-natural ecosystems in river valleys. Strati fi ed alluvial soils, commonly involving buried topsoil horizons, are also important for the reconstruction of natural environmental changes (in particular climatic and hydrological ones) and human impact on the landscape. This paper presents: (a) a concept of alluvial soils in Poland; (b) a review of the development and transformation of alluvial soils in relation to river valley dynamics and human in fl uences, (c) historical and present classi fi cation schemes for alluvial soils in Poland and their correlation with international classi fi cation systems (WRB and Soil Taxonomy); and (d) utility of alluvial soils for agriculture and forestry based on their physicochemical properties and water regime.","PeriodicalId":44772,"journal":{"name":"Soil Science Annual","volume":"140 2","pages":""},"PeriodicalIF":1.5,"publicationDate":"2022-10-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"72393660","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}
B. Malcheva, M. Nustorova, M. Zhiyanski, R. Yaneva, E. Abakumov
Polar soils under different vegetation cover from Livingston Island (Antarctica) were studied ana-lyzing indicators of carbohydrates decomposition in soils: organic carbon, biomass carbon, total nitrogen, C:N ratio, cellulase, amylase, and invertase activity. The highest values of microbial biomass in soils were indicated for sites with vegetation cover while the lowest values in soils without vegetation, which correlate with the content of total organic carbon and the C:N ratio. The highest percentage of biomass carbon compared to the total organic biomass carbon is obtained for two sites with mosses, and the lowest in sites without vegetation, followed by the sites with lichens. Cellulase activity is highest in polar soils with moss cover. Amylase activity depends more strongly on the type of vegetation. The highest amylase activity is detected in soils under algae cover and the lowest in soils without vegetation. Invertase activity is limited by the extreme soil and climatic conditions of Antarctica. A very strong, positive correlation is found between total carbon and total nitrogen. The relationship between total carbon and the C:N ratio, as well as between biomass carbon and amylase activity, is moderate, and positive. The higher dependence of amylase activity from organic carbon with microbial origin correlates with higher values of the enzyme amylase compared to the enzyme cellulase. There is a strong (cellulase) and very strong (amylase) positive relationship between the activity of enzymes and the combination of factors: total carbon, total nitrogen, C: N ratio and biomass carbon.
{"title":"Microbial biomass carbon and enzymes-degraders of carbohydrates in polar soils from the area of Livingston Island, Antarctica","authors":"B. Malcheva, M. Nustorova, M. Zhiyanski, R. Yaneva, E. Abakumov","doi":"10.37501/soilsa/156042","DOIUrl":"https://doi.org/10.37501/soilsa/156042","url":null,"abstract":"Polar soils under different vegetation cover from Livingston Island (Antarctica) were studied ana-lyzing indicators of carbohydrates decomposition in soils: organic carbon, biomass carbon, total nitrogen, C:N ratio, cellulase, amylase, and invertase activity. The highest values of microbial biomass in soils were indicated for sites with vegetation cover while the lowest values in soils without vegetation, which correlate with the content of total organic carbon and the C:N ratio. The highest percentage of biomass carbon compared to the total organic biomass carbon is obtained for two sites with mosses, and the lowest in sites without vegetation, followed by the sites with lichens. Cellulase activity is highest in polar soils with moss cover. Amylase activity depends more strongly on the type of vegetation. The highest amylase activity is detected in soils under algae cover and the lowest in soils without vegetation. Invertase activity is limited by the extreme soil and climatic conditions of Antarctica. A very strong, positive correlation is found between total carbon and total nitrogen. The relationship between total carbon and the C:N ratio, as well as between biomass carbon and amylase activity, is moderate, and positive. The higher dependence of amylase activity from organic carbon with microbial origin correlates with higher values of the enzyme amylase compared to the enzyme cellulase. There is a strong (cellulase) and very strong (amylase) positive relationship between the activity of enzymes and the combination of factors: total carbon, total nitrogen, C: N ratio and biomass carbon.","PeriodicalId":44772,"journal":{"name":"Soil Science Annual","volume":"46 1","pages":""},"PeriodicalIF":1.5,"publicationDate":"2022-10-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"85462986","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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