Soil Science Annual最新文献_第10页

Soil cover patterns in the forest-steppe and steppe zones of the East European Plain 东欧平原森林草原和草原带的土壤覆盖格局

IF 1.5

Soil Science Annual Pub Date : 2019-09-01 DOI: 10.2478/ssa-2019-0018

N. Khitrov, M. Smirnova, N. Lozbenev, E. Levchenko, V. Gribov, D. Kozlov, D. Rukhovich, N. Kalinina, P. Koroleva

{"title":"Soil cover patterns in the forest-steppe and steppe zones of the East European Plain","authors":"N. Khitrov, M. Smirnova, N. Lozbenev, E. Levchenko, V. Gribov, D. Kozlov, D. Rukhovich, N. Kalinina, P. Koroleva","doi":"10.2478/ssa-2019-0018","DOIUrl":"https://doi.org/10.2478/ssa-2019-0018","url":null,"abstract":"Abstract The soil cover of the forest-steppe and steppe zones of the East European Plain is characterized by diverse soil combinations revealed during large-scale and detailed soil mapping against the background of a traditional zonal sequence of dominant automorphic soils alternating from the north to the south and clearly displayed on small-scale soil maps. The composition, configuration and functioning of particular soil cover patterns are determined by the soil forming factors acting within a given area. The elementary soil areas (detailed scale) and elementary soil cover patterns maps (large scale) of the Central Russian, Kalach, and Volga Uplands are created by both traditional and digital soil mapping methods. Low-contrasting soil combinations with the background Haplic Chernozems (Loamic or Clayic, Pachic) alternating with zooturbated Haplic Chernozems (Loamic or Clayic, Pachic) on convex elements of the microtopography and Luvic Chernozems (Loamic or Clayic, Pachic) on concave elements of the microtopography prevails under conditions of thick clay loamy parent materials and free drainage. Under conditions of shallow embedding by low-permeable clayey sediments, the soil cover includes Chernozems or Chernic Phaeozems with stagnic features in some part of the soil profile or even Mollic Stagnosols. The presence of shrink-swell clays of different ages leads to the formation of Bathyvertic Chernozems, Vertic Chernozems, Vertic Chernic Phaeozems and/or Pellic Vertisols. The presence of soluble salts in the parent material leads to the development of solonetzic soil complexes consisting of Protosodic or Sodic Chernozems and different types of Solonetzes.","PeriodicalId":44772,"journal":{"name":"Soil Science Annual","volume":"39 5 1","pages":"198 - 210"},"PeriodicalIF":1.5,"publicationDate":"2019-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"84700253","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}

引用次数: 11

Forest habitats and forest types on chernozems in south-eastern Poland 波兰东南部黑钙土上的森林生境和森林类型

IF 1.5

Soil Science Annual Pub Date : 2019-09-01 DOI: 10.2478/ssa-2019-0021

J. Lasota, E. Błońska, Stanisław Łyszczarz, Adrian Sadowy

{"title":"Forest habitats and forest types on chernozems in south-eastern Poland","authors":"J. Lasota, E. Błońska, Stanisław Łyszczarz, Adrian Sadowy","doi":"10.2478/ssa-2019-0021","DOIUrl":"https://doi.org/10.2478/ssa-2019-0021","url":null,"abstract":"Abstract The objective of the study is the presentation of the chemical properties of forest chernozems and the features of forest habitats developed on chernozems in south-eastern Poland. The assessment of the trophic status of chernozems was presented based on the Trophic Soil Index (SIG). Moreover, the paper presents the diversity of forest vegetation on chernozems. The research covered 15 plots from the habitat inventory performed for the Mircze and Strzelce Forest Districts (SE Poland). Habitat conditions were characterised on the research plots, with particular consideration of the soil and vegetation. The analysed soils were featured by the presence of thick humus horizons and the occurrence of calcium carbonate. High SIG values confirm the eutrophic status of the analysed soils. In general, fresh and wet habitats of broadleaved forests (Lśw and Lw), as well as fresh habitats of broadleaved upland forest (Lwyżśw) develop on chernozems in Poland. They are associated with multi-species broadleaved tree stands. The conducted research indicates that, in current environmental conditions, the potential plant community is oak-hornbeam forest with predominance of oak, hornbeam, and abundant admixtures of other broadleaved species. High trophic status of the analysed chernozems is confirmed by high bonitation of tree stands and richness of forest floor vegetation.","PeriodicalId":44772,"journal":{"name":"Soil Science Annual","volume":"24 1","pages":"234 - 243"},"PeriodicalIF":1.5,"publicationDate":"2019-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"90375914","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}

引用次数: 3

Chernozem (czarnoziem) – soil of the year 2019 in Poland. Origin, classification and use of chernozems in Poland 黑钙土(czarnoziem) -波兰2019年度土壤。黑钙土在波兰的起源、分类和使用

IF 1.5

Soil Science Annual Pub Date : 2019-09-01 DOI: 10.2478/ssa-2019-0016

C. Kabała

引用次数: 11

Suitability of World Reference Base for Soil Resources (WRB) to describe and classify chernozemic soils in Central Europe 世界土壤资源参考基地(WRB)描述和分类中欧黑钙土的适宜性

IF 1.5

Soil Science Annual Pub Date : 2019-09-01 DOI: 10.2478/ssa-2019-0022

C. Kabała, P. Charzyński, S. Czigány, T. Novák, Martin Saksa, M. Świtoniak

{"title":"Suitability of World Reference Base for Soil Resources (WRB) to describe and classify chernozemic soils in Central Europe","authors":"C. Kabała, P. Charzyński, S. Czigány, T. Novák, Martin Saksa, M. Świtoniak","doi":"10.2478/ssa-2019-0022","DOIUrl":"https://doi.org/10.2478/ssa-2019-0022","url":null,"abstract":"Abstract Chernozemic soils are distinguished based on the presence of thick, black or very dark, rich in humus, well-structural and base-saturated topsoil horizon, and the accumulation of secondary carbonates within soil profile. In Central Europe these soils occur in variable forms, respectively to climate gradients, position in the landscape, moisture regime, land use, and erosion/accumulation intensity. “Typical” chernozems, correlated with Calcic or Haplic Chernozems, are similarly positioned at basic classification level in the national soil classifications in Poland, Slovakia and Hungary, and in WRB. Chernozemic soils at various stages of their transformation are placed in Chernozems, Phaeozems or Kastanozems, supplied with respective qualifiers, e.g. Cambic, Luvic, Salic/Protosalic, Sodic/Protosodic etc. Some primeval Chernozems thinned by erosion may still fulfil criteria of Chernozems, but commonly are shifted to Calcisols. Soils upbuilt (aggraded) with colluvial additions may also retain their original placement in Chernozems, getting supplementary qualifier Colluvic. “Hydromorphic” chernozemic soils, in many CE systems are placed as separate soil type (“czarne ziemie” or “čiernice”) at the same level with “typical” chernozems. Classification of these soils in WRB depends on the presence of chernic horizon, depth of secondary carbonate accumulation and depth of gleyic/stagnic properties, and may vary from Gleyic/Stagnic Chernozems/Phaeozems to Mollic Gleysols/Stagnosols. Although WRB classification differs from national classifications in the concepts and priorities of classification, it provides large opportunity to reflect the spatial variability and various stages of transformation/degradation of chernozemic soils in Central Europe.","PeriodicalId":44772,"journal":{"name":"Soil Science Annual","volume":"172 1","pages":"244 - 257"},"PeriodicalIF":1.5,"publicationDate":"2019-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"90434358","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}

引用次数: 4

Morphological diversity of chernozemic soils in south-western Poland 波兰西南部黑钙土的形态多样性

IF 1.5

Soil Science Annual Pub Date : 2019-09-01 DOI: 10.2478/ssa-2019-0019

B. Łabaz, C. Kabała, M. Dudek, Jarosław Waroszewski

{"title":"Morphological diversity of chernozemic soils in south-western Poland","authors":"B. Łabaz, C. Kabała, M. Dudek, Jarosław Waroszewski","doi":"10.2478/ssa-2019-0019","DOIUrl":"https://doi.org/10.2478/ssa-2019-0019","url":null,"abstract":"Abstract Diverse chernozemic soils featured by thick mollic horizon, rich in humus, dark-coloured, structural, and saturated with base cations are relatively common in the loess-belt of SW Poland. It is postulated, that most of these soils may have similar initial (chernozemic) history of thick humus horizon, related to climate conditions and vegetation in the Late Pleistocene and the Neolithic periods. However, these soils exist on various bedrocks and under different moisture conditions that led to the development accompanying features and variable classification of soils, both in Polish and international soil classifications. The aim of the paper is to presents the most important variants of loess-derived chernozemic soils of SW Poland, in relation to local conditions, which influenced soil transformation and present spatial diversification. ‘Typical’ chernozems (WRB: Calcic Chernozems), which have a mollic horizon and secondary carbonates, but are free of strong redoximorphic features, are rather uncommon in the region. Whereas, the black earths (WRB: Gleyic/Stagnic Chernozems/Phaeozems), featured by the presence of mollic horizon and strong gleyic or stagnic properties in the middle and bottom parts of the profiles, are predominant loess-derived chernozemic soils in SW Poland. Their most specific forms, developed on the clayey bedrock, are black earths with a vertic horizon (WRB: Vertic Stagnic Phaeozems). The strongly leached chernozemic soils developed over permeable subsoils, lacking carbonates and free of (strongly developed) stagnic/gleyic properties are called grey soils, often featured by the presence of subsurface diagnostic horizons cambic or luvic (WRB: Cambic/Luvic Phaeozems).","PeriodicalId":44772,"journal":{"name":"Soil Science Annual","volume":"45 1","pages":"211 - 224"},"PeriodicalIF":1.5,"publicationDate":"2019-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"86889004","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}

引用次数: 10

Properties and classification of heavily eroded post-chernozem soils in Proszowice Plateau (southern Poland) 波兰南部普罗佐维采高原重度侵蚀黑钙土的性质与分类

IF 1.5

Soil Science Annual Pub Date : 2019-09-01 DOI: 10.2478/ssa-2019-0020

Marek Drewnik, Marcin Żyła

{"title":"Properties and classification of heavily eroded post-chernozem soils in Proszowice Plateau (southern Poland)","authors":"Marek Drewnik, Marcin Żyła","doi":"10.2478/ssa-2019-0020","DOIUrl":"https://doi.org/10.2478/ssa-2019-0020","url":null,"abstract":"Abstract The morphology and properties of heavily eroded soils found in chernozems in the upland landscape of the Proszowice Plateau (southern part of Poland) was presented. The issue of classification of these soils was also discussed. Taking into account the terrain context, it should have been assumed that these soils were formed as a result of strong erosion (truncation) of chernozems. These (post-chernozem) soils were relatively young, in which only the development of humus horizon can be documented. However, the accumulation of humus was hampered by constantly intense erosion processes. Evidence of the occurrence of the illuviation process as well as formation of cambic horizon is not visible macroscopically and microscopically. These soils are often classified as weakly developed soils though despite the poor development of the soil profile, they are characterized by potentially high productivity, which results both from the properties of their parent material (texture, porosity) and from their youthfulness (carbonate content both in fine earths and in nodules, high pH in whole profile). Therefore, the name proposed in Polish Soil Classification, 6th edition (‘pararędzina’) seems to be justified. These soils would be classified as Entisols according to USDA Soil Taxonomy and as Regosols according to WRB.","PeriodicalId":44772,"journal":{"name":"Soil Science Annual","volume":"39 1","pages":"225 - 233"},"PeriodicalIF":1.5,"publicationDate":"2019-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"79727523","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}

引用次数: 12

Chernozems of Lubelszczyzna (eastern Poland) 卢贝尔什日纳的Chernozems(波兰东部)

IF 1.5

Soil Science Annual Pub Date : 2019-09-01 DOI: 10.2478/ssa-2019-0023

J. Chodorowski, P. Bartmiński, A. Plak, R. Dębicki

{"title":"Chernozems of Lubelszczyzna (eastern Poland)","authors":"J. Chodorowski, P. Bartmiński, A. Plak, R. Dębicki","doi":"10.2478/ssa-2019-0023","DOIUrl":"https://doi.org/10.2478/ssa-2019-0023","url":null,"abstract":"Abstract The purpose of the work was to characterize the variously used humus in the south-eastern part of the Lublin region. The basic research material were data taken from the literature on the subject. Standard soil science methods were used in the study. The humus level of humus varieties ranged from 30 to 80 cm. The researched molds were formed from loess deposits, which most often showed graining of clay dust. Organic carbon content in humus levels did not exceed 2.9%. The surface levels of the analyzed molds showed clear decalcification. The CaCO3 content in the loess mother rock was a maximum of 15.5%. These are soils with high saturation of the sorption complex with basic cations. The content of available phosphorus and potassium in humus levels was low and medium. According to Systematics of Poland’s soils (2019), the analyzed molds mainly represented leached molds and typical molds, while according to the international soil classification WRB (IUSS Working Group WRB 2015) they are primarily Phaeozems. All the analyzed humus plants belong to soils with the highest utility value. Phenomena lowering the quality of molds in the Lublin region related to human activity are the use of improper agrotechnics, and above all water surface erosion. The unfavorable processes are favored by the undulating terrain and the grain size of the soils studied, characteristic for this area.","PeriodicalId":44772,"journal":{"name":"Soil Science Annual","volume":"80 1","pages":"258 - 269"},"PeriodicalIF":1.5,"publicationDate":"2019-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"81226449","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}

引用次数: 3

Agricultural suitability and land use of chernozems in Poland 波兰黑钙土的农业适宜性和土地利用

IF 1.5

Soil Science Annual Pub Date : 2019-09-01 DOI: 10.2478/ssa-2019-0024

B. Smreczak, J. Jadczyszyn, P. Sklodowski

引用次数: 2

Chernozems of Ukraine: past, present and future perspectives 乌克兰的Chernozems:过去，现在和未来的观点

IF 1.5

Soil Science Annual Pub Date : 2019-09-01 DOI: 10.2478/ssa-2019-0017

S. Pozniak

引用次数: 6

Classification of mountain soils in a subalpine zone – a case study from the Bieszczady Mountains (SE Poland) 亚高山地区山地土壤的分类——以波兰东南部比耶什恰迪山脉为例

IF 1.5

Soil Science Annual Pub Date : 2019-06-01 DOI: 10.2478/ssa-2019-0015

Łukasz Musielok, Marek Drewnik, W. Szymański, Mateusz Stolarczyk

{"title":"Classification of mountain soils in a subalpine zone – a case study from the Bieszczady Mountains (SE Poland)","authors":"Łukasz Musielok, Marek Drewnik, W. Szymański, Mateusz Stolarczyk","doi":"10.2478/ssa-2019-0015","DOIUrl":"https://doi.org/10.2478/ssa-2019-0015","url":null,"abstract":"Abstract The aim of the study was to test the suitability of the 6th edition of Polish Soil Classification (SGP6) in reflecting the typical features of subalpine Bieszczady Mts. soils in comparison with the 5th edition of Polish Soil Classification (SGP5) and the newest version of World Reference Base for Soil Resources (WRB). Five soil profiles located in differentiated in terms of the parent material, topography and vegetation conditions of the natural environment were investigated. On the basis of described morphology and determined properties soils were classified according to different soil classifications. All soils under study were featured by presence of thick A horizons and high content of soil organic carbon accumulated even very deep in the profiles. Some of the mineral topsoil layers were classified as umbric/umbrik horizons. Moreover cambic/kambik horizons were present and in some cases also weak redoximorphic features occurred. The SGP6 enabled to distinguish soils with a thick, organic carbon-rich A horizons as umbrisols, a newly created subtype of grey soils. Furthermore, the soil taxonomic position according to SGP6 was more detailed in relation to the soil trophic status (in case of brown soils) and occurrence of weak redoximorphic features. That was reflected in number of subtypes to which analyzed soils were classified – 4 in SGP6 vs 2 in SGP5.","PeriodicalId":44772,"journal":{"name":"Soil Science Annual","volume":"1 1","pages":"170 - 177"},"PeriodicalIF":1.5,"publicationDate":"2019-06-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"76842752","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}

引用次数: 2