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Journal articles on the topic 'Brunic Arenosols'

Author: Grafiati

Published: 2 June 2025

Last updated: 31 July 2025

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1

Błońska, Ewa, Jarosław Lasota, and Kazimierz Januszek. "Variability of enzymatic activity in forest Cambisols and Brunic Arenosols of Polish lowland areas." Soil Science Annual 64, no. 2 (2013): 54–59. http://dx.doi.org/10.2478/ssa-2013-0010.

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Abstract The aim of this study was to determine the enzymatic activity (dehydrogenase and urease) in trophically diverse Brunic Arenosols and Cambisols. Efforts to establish the relationship between enzymatic activity and physico-chemical properties of various subtypes of Brunic Arenosols and Cambisols were attempted. Another aim was to determine the effect of vegetation on the properties of soil surface levels. The study was conducted on 94 plots located in nature reserves and national parks in the Polish lowland area. Dehydrogenase activity and urease showed large variations in the subtypes

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2

Jonczak, Jerzy, Marek Degórski, and Bogusława Kruczkowska. "Comparing quartz silt surface microstructures in two sandy soils in young-glacial landscape of northern Poland." Soil Science Annual 67, no. 3 (2016): 131–39. http://dx.doi.org/10.1515/ssa-2016-0016.

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AbstractThe studies on quartz silt surface microstructures using scanning electron microscopy (SEM) were performed in Brunic Arenosol and Gleyic Ortsteinic Podzol, as major components of soil cover of the lower supra-flood terrace of the Słupia River, N Poland. Brunic Arenosols have developed from coarse- and medium-grained fluvioglacial sands, whereas Podzols from aeolian sands of mid-Holocene age, which in some places were covered with younger aeolian deposits. A group of at least 100 randomly selected grains from each soil horizon have been analyzed. The grains were classified into one of t

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3

Baćmaga, Małgorzata, Jadwiga Wyszkowska, Agata Borowik, Jan Kucharski, and Łukasz Paprocki. "Microbiological and Biochemical Properties in Eutric/Dystric Brunic Arenosols, Eutric/Endocalcaric Cambisols, and Haplic/Albic Luvisols Soils." Journal of Soil Science and Plant Nutrition 21, no. 2 (2021): 1277–92. http://dx.doi.org/10.1007/s42729-021-00439-7.

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AbstractTo understand the role of microorganisms in the functioning of forest ecosystems, the structure of bacterial communities and the enzymatic activity were determined in forest soils representing the following soil subtypes: Eutric/Dystric Brunic Arenosols (A), Eutric/Endocalcaric Cambisols (C), and Haplic/Albic Luvisols (L). Their microbiological and biochemical properties were compared based on bacterial counts and diversity, and activities of seven soil enzymes: dehydrogenases, catalase, urease, acid phosphatase, alkaline phosphatase, arylsulfatase, and β-glucosidase. Organotrophic bac

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4

Jonczak, Jerzy. "Vertical distribution of Cu, Ni and Zn in Brunic Arenosols and Gleyic Podzols of the supra-flood terrace of the Słupia River as affected by litho-pedogenic factors." Forest Research Papers 75, no. 4 (2015): 333–41. http://dx.doi.org/10.2478/frp-2014-0030.

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Abstract The aim of the study was to assess the influence of lithological and pedogenic factors in the shaping of Cu, Ni and Zn distribution patterns in the profiles of Brunic Arenosols and Gleyic Podzols of the lower supra-flood terrace of the Słupia River, which is located outside the range of significant anthropogenic sources of pollution with these metals. The contents of the investigated metals were analysed in aqua regia extracts of samples collected from three profiles of Brunic Arenosols, formed from river sands, and three profiles of Gleyic Podzols, formed from river sands transformed

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5

Jonczak, Jerzy. "Vertical distribution of Cu, Ni and Zn in Brunic Arenosols and Gleyic Podzols of the supra-flood terrace of the Słupia River as affected by litho-pedogenic factors." Forest Research Papers 75 (4) (December 1, 2015): 333–41. https://doi.org/10.2478/frp-2014-0030.

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The aim of the study was to assess the influence of lithological and pedogenic factors in the shaping of Cu, Ni and Zn distribution patterns in the profiles of Brunic Arenosols and Gleyic Podzols of the lower supra-flood terrace of the Słupia River, which is located outside the range of significant anthropogenic sources of pollution with these metals. The contents of the investigated metals were analysed in aqua regia extracts of samples collected from three profiles of Brunic Arenosols, formed from river sands, and three profiles of Gleyic Podzols, formed from river sands transformed by eolia

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6

Kondratowicz-Maciejewska, Krystyna, Mirosław Kobierski, and Anna Murawska. "Effect of Brunic Arenosols Use on Selected Physicochemical Properties in Organic Matter." Soil Science Annual 63, no. 2 (2012): 19–24. http://dx.doi.org/10.2478/v10239-012-0019-y.

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7

Lasota, Jarosław, Ewa Błońska, and Wojciech Piaszczyk. "State of soil enzymatic activity in relationship to some chemical properties of Brunic Arenosols." Soil Science Annual 72, no. 4 (2021): 1–8. http://dx.doi.org/10.37501/soilsa/140641.

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8

Siwik-Ziomek, Anetta, Monika Skowrońska, Atilgan Atilgan, and Burak Sayin. "Enzyme Activities Transforming Sulphur in Brunic Arenosols in Forest Exposure to the Nitrogen Plants." Sustainability 17, no. 5 (2025): 1776. https://doi.org/10.3390/su17051776.

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This study has been conducted to assess the anthropogenic impact of the ANWIL S.A. nitrogen plants, one of the largest producers of nitrogen fertilizers in Poland, on the activity of arylsulphatase (AR), rhodanese (RDN) and catalase (CAT) related to sulphur transformation in forest soils. Samples of rusty brown soils were collected in the area adjacent to the ANWIL S.A. nitrogen plants in Włocławek. The profiles were located in the vicinity of the following production plants: No. W1—approximately 2.5 km away, No. W2—approximately 2 km away, and No. W3—approximately 0.8 km away. The control pro

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9

Kabała, Cezary, Marek Ksepko, and Przemysław Musiał. "Typological and physicochemical variability of rusty soils (Brunic Arenosols) in the Bialowieża Forests, eastern Poland." Soil Science Annual 72, no. 4 (2021): 1–14. http://dx.doi.org/10.37501/soilsa/143900.

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10

Gus-Stolarczyk, Magdalena, Marek Drewnik, and Wojciech Szymański. "Origin, properties and transformation of soil lamellae in rusty soils (Brunic Arenosols) in southeastern Poland." Soil Science Annual 72, no. 4 (2021): 1–15. http://dx.doi.org/10.37501/soilsa/143881.

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11

Sztabkowski, Krzysztof, and Jerzy Jonczak. "Parent material origin as a factor influencing the development and properties of Brunic Arenosols in a young glacial landscape." CATENA 258 (October 2025): 109320. https://doi.org/10.1016/j.catena.2025.109320.

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12

Świtoniak, Marcin, Marcin Sykuła, Maciej Markiewicz, Julia Dziczek, and Paweł Radomski. "Genetic map of the Wielka Żuława soil cover: blanks to be filled using existing cartographic materials and remote-sensing data." Bulletin of Geography. Physical Geography Series, no. 27 (December 20, 2024): 71–85. https://doi.org/10.12775/bgeo-2024-0011.

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Poland is considered to have a very well mapped soil cover and detailed soil cartographic materials. Despite this, some areas have “blank spots” on soil-agricultural or soil-habitat maps. These include the Wielka Żuława island on Jeziorak Lake (on the Iława Plain). This island is almost deserted and inaccessible, making detailed field research there very difficult. The aim of the work was to check the possibility of using existing cartographic materials and remote-sensing data to develop a genetic map of the soils of this area. In order to interpret the existing materials, preliminary field wo

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13

Jonczak, Jerzy, and Krzysztof Sztabkowski. "Spatial variability of Brunic Arenosols and associated soils along the slope of the Słupia River valley (middle Pomerania, northern Poland)." Soil Science Annual 72, no. 4 (2021): 1–15. http://dx.doi.org/10.37501/soilsa/143892.

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14

Gałka, Bernard, Cezary Kabała, Anna Karczewska, Józef Sowiński, and Justyna Jakubiec. "Variability of soil properties in an intensively cultivated experimental field." Soil Science Annual 67, no. 1 (2016): 10–16. http://dx.doi.org/10.1515/ssa-2016-0002.

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AbstractThe aim of the study was to determine whether long-term intensive cultivation that used variable ploughing and fertilisation technologies and schemes influences the differentiation of soil properties which may impact the results of growing experiments in a relatively small experimental field (0.1 ha). The field under study is located in Wrocław, in an agricultural experimental station that has been operating for more than 60 years. A transformation of rusty gleyic soils (Brunic Gleyic Arenosols) into anthropogenic black earths (Gleyic Phaeozems (Arenic)) was noticed. The content of org

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15

Błońska, Ewa, Jarosław Lasota, Maciej Zwydak, and Wojciech Piaszczyk. "Stand mixing effect on enzyme activity and other soil properties." Soil Science Annual 67, no. 4 (2016): 173–78. http://dx.doi.org/10.1515/ssa-2016-0021.

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Abstract In this research study, enzyme activity was used to assess differences occurring in soils as a result of the different tree species influence. The aim of the study was to assess the effects of Scots pine (Pinus sylvestris), sessile oak (Quercus petraea) and mixed-species stands on the enzymatic activity and chemical characteristics of soil. Sample plots were located in central Poland, in the Przedbórz forest district (51.09.59.50°N, 20.00.24.25°E). The test area was dominated by Brunic Arenosols. 15 research plots were established (5 plots under pine, 5 plots under oak and 5 plots und

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16

Dębska, Bożena. "Content and changes in dissolved organic matter in meadow and arable soils over time." Polish Journal of Soil Science 52, no. 2 (2019): 183. http://dx.doi.org/10.17951/pjss.2019.52.2.183.

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<p>Considering the discrepancies in the reports on seasonal changes in the content of dissolved organic carbon, this paper concerns the research which aimed at defining the content and seasonal changes in dissolved organic matter (DOM) in arable and meadow soils in moderate climate conditions. The research has involved the soils sampled in the kujawsko-pomorskie province (Poland). Gleic Phaeozems (meadow soils), Brunic Arenosols and Eutric Cambisols were sampled from the depth of 0-30 cm, 30-60 cm and 60-100 cm, November 2011 through September 2013. The soil samples were analyzed for dry

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17

Lasota, Jarosław, Małgorzata Wiecheć, Ewa Błońska, and Stanisław Brożek. "Biodiversity indexes in relation to soil properties in upland fir forests (Abietetum albae)." Forest Research Papers 78, no. 2 (2017): 120–28. http://dx.doi.org/10.1515/frp-2017-0013.

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Abstract The aim of this study was to present the relationship between soil properties and biodiversity indexes in upland fir (Abies alba) forest associations (Abietetum albae). Our study was conducted in six areas representing the growth conditions of upland fir forests and the research plots were located in the Roztoczański and Świętokrzyski National Parks as well as Przedbórz, Radomsko, Piotrków and Janów lubelski Forest District. on every plot, the topography was described, soil cores were examined and samples for laboratory analysis were taken. the following characteristics were determine

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18

Jarosław, Lasota, Wiecheć Małgorzata, Błońska Ewa, and Brożek Stanisław. "Biodiversity indexes in relation to soil properties in upland fir forests (Abietetum albae)." Lesne Prace Badawcze / Forest Research Papers 78, no. 2 (2017): 120–28. https://doi.org/10.1515/frp-2017-0013.

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The aim of this study was to present the relationship between soil properties and biodiversity indexes in upland fir (<em>Abies alba</em>) forest associations (<em>Abietetum albae</em>). Our study was conducted in six areas representing the growth conditions of upland fir forests and the research plots were located in the Roztoczański and Świętokrzyski National Parks as well as Przedbórz, Radomsko, Piotrków and Janów lubelski Forest District. on every plot, the topography was described, soil cores were examined and samples for laboratory analysis were taken. the following

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19

Dłużewski, Paweł, Katarzyna Wiatrowska, and Michał Kozłowski. "Seasonal changes in organic carbon content in post-arable forest soils." Soil Science Annual 70, no. 1 (2019): 3–12. http://dx.doi.org/10.2478/ssa-2019-0001.

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Abstract The purpose of this work is to determine seasonal changes in the organic carbon content in the mineral topsoil horizon of the Dystric Brunic Arenosols currently used as forest. In addition, the influence of forest age on the soil organic carbon (SOC) content in the A horizon was analyzed. The paper presents the results of studies on temporal changes in the SOC content in the mineral surface horizon of 55-year-old (Sk2) and 13-year-old forest (Sk5) in 2013 and 2014. Soil samples were collected from A horizon once a month between April 2013 and March 2015. Based on the conducted studies

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20

Wiśniewski, Paweł, and Mariusz Kistowski. "Structure and importance of soil-protecting forests in the areas administered by the RDSF Toruń." Bulletin of Geography. Physical Geography Series 8, no. 1 (2015): 123–32. http://dx.doi.org/10.1515/bgeo-2015-0010.

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Abstract The paper presents the state and importance of soil-protecting forests in the areas managed by the RDSF in Toruń, as well as changes in their structure over 29 years. The management of the RDSF in Toruń is characterized by a systematic increase in the area, thickness and rich abundance of soil-protecting forests, particularly intense since the mid-nineteen-nineties. They cover mainly rusty soils and podzols on outwash areas, sandy terraces in sloped areas of postglacial valleys and gullies as well. Soil-protecting forests, which are managed by the RDSF in Toruń, vary a great deal cons

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21

Szydlarski, Marcin, Jerzy Modrzyński, Mateusz Stopiński, Michał Majewski, and Krzysztof Maras. "Comparing natural regeneration of Norway spruce Picea abies (L.) Karst. in the Kaszuby Lake District and in the other regions of northern Poland." Forest Research Papers 78, no. 4 (2017): 303–14. http://dx.doi.org/10.1515/frp-2017-0034.

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Abstract The paper investigates the biometric characteristics natural Norway spruce (Picea abies (L.) Karst.) regeneration in the Kaszuby Lake District, which is beyond the acknowledged Norway spruce range, with the natural regeneration in the Augustów Forest situated deep within the natural range, Warmia, at the edge of the natural range and in the West-Pomerania Lake District far beyond the natural range. For each region, four tree stands with similar light conditions on the forest floor were selected, including two cambisols and two brunic arenosols. All sites contained naturally regenerati

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Marcin, Szydlarski, Modrzyński Jerzy, Stopiński Mateusz, Majewski Michał, and Maras Krzysztof. "Comparing natural regeneration of Norway spruce Picea abies (L.) Karst. in the Kaszuby Lake District and in the other regions of northern Poland." Lesne Prace Badawcze / Forest Research Papers 78, no. 4 (2017): 303–14. https://doi.org/10.1515/frp-2017-0034.

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The paper investigates the biometric characteristics natural Norway spruce ( <em>Picea abies</em> (L.) Karst.) regeneration in the Kaszuby Lake District, which is beyond the acknowledged Norway spruce range, with the natural regeneration in the Augustów Forest situated deep within the natural range, Warmia, at the edge of the natural range and in the West-Pomerania Lake District far beyond the natural range. For each region, four tree stands with similar light conditions on the forest floor were selected, including two cambisols and two brunic arenosols. All sites contained naturally re

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23

Chodorowski, Jacek, Piotr Bartmiński, Andrzej Plak, and Ryszard Dębicki. "Soil Cover of the City of Lublin (Eastern Poland)." Annales Universitatis Mariae Curie-Sklodowska, sectio B – Geographia, Geologia, Mineralogia et Petrographia 79 (October 4, 2024): 69–85. http://dx.doi.org/10.17951/b.2024.79.0.69-85.

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Lublin is a voivodeship city located in the Lublin Upland (Eastern Poland). The study aimed to present the spatial differentiation of soils of the city of Lublin and some of their properties. The knowledge of soil cover is very important for spatial planning and for protection and proper use of soil resources of each city. The environmental-genetic map of Lublin’s soils included in this work was made on the basis of soil-agricultural map in the scale 1:25 000 of Lublin and the soil-habitat map of the Świdnik Forest District. The soil units distinguished on the map were classified according to

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Gałązka, Anna, Jacek Niedźwiecki, Jarosław Grządziel, and Karolina Gawryjołek. "Evaluation of Changes in Glomalin-Related Soil Proteins (GRSP) Content, Microbial Diversity and Physical Properties Depending on the Type of Soil as the Important Biotic Determinants of Soil Quality." Agronomy 10, no. 9 (2020): 1279. http://dx.doi.org/10.3390/agronomy10091279.

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The aim of the study was to evaluate the changes in glomalin-related soil proteins (GRSP) content, microbial diversity and soil physical quality depending on the type of soil measures of soil improvement and changes in soil health. The study was based on a 100-year stationary field microplot experiment where the soil profiles were collected with preserving the natural soil horizons. The microplot experiment was carried out on eight different soil types: Brunic Arenosol (Dystric I), Rendzic Leptosol, Fluvic Cambisol, Haplic Cambisol (Eutric), Gleyic Phaeozem, Brunic Arenosol (Dystric II), Hapli

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Majgier, Leszek, and Oimahmad Rahmonov. "Selected Chemical Properties of Necrosols from the Abandoned Cemeteries Słabowo and Szymonka (Great Mazurian Lakes District)." Bulletin of Geography. Physical Geography Series 5, no. 1 (2012): 43–55. http://dx.doi.org/10.2478/v10250-012-0003-8.

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Abstract The paper shows the occurrences of cemetery soils and the physico-chemical features of soils in the cemeteries Słabowo and Szymonka (Great Mazurian Lakes District). Necrosols are anthropogenic soils and belong to Urbanosols. They form only in the area of cemeteries. Four soil profiles (Necrosols) were investigated in terms of morphological description and chemical properties especially phosphorus (Pt), organic carbon (OC) and nitrogen (Nt). These profiles were compared with the reference profile (Rusty soil, according to WRB 2007 Brunic Arenosol) made outside the cemetery. On the basi

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26

Walkiewicz, Anna, Małgorzata Brzezińska, Andrzej Bieganowski, Lidia Sas-Paszt, and Magdalena Frąc. "Early Response of Soil Microbial Biomass and Activity to Biofertilizer Application in Degraded Brunic Arenosol and Abruptic Luvisol of Contrasting Textures." Agronomy 10, no. 9 (2020): 1347. http://dx.doi.org/10.3390/agronomy10091347.

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We tested agriculturally and chemically degraded Brunic Arenosol and Abruptic Luvisol of contrasting textures to establish the early response of soil quality to two different mineral fertilizers (Polifoska and urea) amended with microbes applied in optimal and reduced doses. The soil samples were collected from two fields under maize: one week (Ist sampling time) and six months (IInd sampling time) after fertilization. The laboratory experiment included determination of: catalase activity, dehydrogenase activity, microbial biomass, and basal respiration; pH and dissolved organic carbon (DOC) w

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27

Kondras, Marek, Danuta Czępińska-Kamińska, Paulina Sienicka, Anna Otręba, Karol Torzewski, and Lidia Oktaba. "The Stock of Organic Carbon in Forest Soils in Phytocenosis of the Continental Mixed Coniferous Forest in Kampinos National Park." Soil Science Annual 63, no. 4 (2012): 26–33. http://dx.doi.org/10.2478/v10239-012-0038-8.

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Abstract In this study physical and chemical analyses of soils were conducted in four areas of the habitat fresh mixed coniferous forest typical of the Kampinos National Park (20% forest area KPN). An attempt was made to evaluate the stock of organic carbon in every genetic horizon and the whole profiles of selected soils, and one counted the indicator ITGL (FSTI - Forest Soil Trophizm Index). In the examined soils, the particle size distributions, the content and ability to store organic carbon was analyzed as well as the amount of total nitrogen, C:N ratio, soil reaction and sorption propert

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Ziolkowska, Anna, Bozena Debska, and Magdalena Banach-Szott. "Content of Phenolic Compounds in Meadow Vegetation and Soil Depending on the Isolation Method." Molecules 25, no. 22 (2020): 5462. http://dx.doi.org/10.3390/molecules25225462.

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The aim of this paper was to determine the effect of the hydrolysis method on the amounts of phenolic compounds in the plant material in soil and, as a consequence, on the parameters to determine the degree of lignins transformation in soils. The study included the plant material (hay, sward, and roots) and soil—Albic Brunic Arenosol (horizon A, AE, and Bsv) samples. Phenolic compounds were isolated at two stages by applying acid hydrolysis followed by alkaline re-hydrolysis. The quantitative and qualitative analysis of phenolic compounds was performed with high-performance liquid chromatograp

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29

Konstantinov, Alexandr, Sergey Loiko, Alina Kurasova, et al. "First Findings of Buried Late-Glacial Paleosols within the Dune Fields of the Tomsk Priobye Region (SE Western Siberia, Russia)." Geosciences 9, no. 2 (2019): 82. http://dx.doi.org/10.3390/geosciences9020082.

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Buried soils within aeolian deposits are considered an important tool for diagnosing, determining the age, and estimating the intensity of aeolian processes at the transition from the Pleistocene to the Holocene in the Northern Hemisphere. Late Pleistocene aeolian coversands and ancient inland dunes are widely distributed in the periglacial zone of Western Siberia. In contrast to the territories of Central and Eastern Europe, the paleosol archive of the aeolian sands and dunes of Western Siberia has not yet been studied. This paper presents the first findings of late Pleistocene paleosols with

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Mącik, Mateusz, Agata Gryta, Lidia Sas‐Paszt, and Magdalena Frąc. "Composition, activity and diversity of bacterial and fungal communities responses to inputs of phosphorus fertilizer enriched with beneficial microbes in degraded Brunic Arenosol." Land Degradation & Development 33, no. 6 (2022): 844–65. http://dx.doi.org/10.1002/ldr.4179.

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Mącik, Mateusz, Agata Gryta, Lidia Sas-Paszt, and Magdalena Frąc. "The Status of Soil Microbiome as Affected by the Application of Phosphorus Biofertilizer: Fertilizer Enriched with Beneficial Bacterial Strains." International Journal of Molecular Sciences 21, no. 21 (2020): 8003. http://dx.doi.org/10.3390/ijms21218003.

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Regarding the unfavourable changes in agroecosystems resulting from the excessive application of mineral fertilizers, biopreparations containing live microorganisms are gaining increasing attention. We assumed that the application of phosphorus mineral fertilizer enriched with strains of beneficial microorganisms contribute to favourable changes in enzymatic activity and in the genetic and functional diversity of microbial populations inhabiting degraded soils. Therefore, in field experiments conditions, the effects of phosphorus fertilizer enriched with bacterial strains on the status of soil

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32

Rahmonov, Oimahmad, Leszek Majgier, and Małgorzata Rahmonov. "Chemical Composition of Tissues of Syringa vulgaris L. and Soil Features in Abandoned Cemeteries." Soil Systems 7, no. 1 (2023): 18. http://dx.doi.org/10.3390/soilsystems7010018.

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Abandoned anthropogenic sites are transformed when they come into use. In the present study, such objects were abandoned Evangelical cemeteries located in the Land of the Great Mazurian Lakes (northern Poland). This study aims to compare the concentrations of selected major (Ca, Na, Mg, Al, Fe) and potentially toxic elements (Zn, Cd, Pb) in the roots, leaves, and branches of Syringa vulgaris and buried necrosols and unburied soils in which this species grows. The soils analysed differ in their profile structure; in the case of burial necrosols, anthropogenic layers are present, while Brunic Ar

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Banach-Szott, Magdalena, Andrzej Dziamski, and Maciej Markiewicz. "Properties of Humic Acids in Meadow Soils Irrigated with the Slope-and-Flooding System." Agronomy 11, no. 12 (2021): 2553. http://dx.doi.org/10.3390/agronomy11122553.

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The still-advancing soil degradation and the related losses of soil organic carbon stocks due to the limited inflow of organic residues in agro-ecosystems encourage more and more soil protection. Establishing meadow ecosystems is one of the key methods of agricultural land use preventing losses of organic carbon in soils. Based on the research on the properties of humic acids, it is possible to determine the advancement of the processes of transformation and decomposition of soil organic matter. The obtained results may allow for the development of a soil protection strategy and more effective

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Jonczak, Jerzy, Lidia Oktaba, Edyta Pawłowicz, et al. "Soil organic matter transformation influenced by silver birch (Betula pendula Roth) succession on abandoned from agricultural production sandy soil." European Journal of Forest Research, December 24, 2022. http://dx.doi.org/10.1007/s10342-022-01527-8.

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AbstractA chronosequence approach was applied to evaluate the effects of silver birch succession on soil organic matter (SOM). The studies covered five plots (arable field [AF], fallow [FA] and three birch stands aged 8, 33 and 40 years), and all located in the same complex of Brunic Arenosols in central Poland. The O and A horizons of the soils were sampled and analysed using the standard procedures in soil science. It was found that the birch succession was accompanied by dynamic changes in the stock and quality of the SOM. The transition from AF to FA soils did not significantly change the

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Kołodziejek, Jeremi. "Growth performance and emergence of invasive alien Rumex confertus in different soil types." Scientific Reports 9, no. 1 (2019). http://dx.doi.org/10.1038/s41598-019-56068-9.

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AbstractRumex confertus is known to be one of the most serious invasive weed species infesting meadows, pastures and ruderal lands throughout the Central Europe. Rumex confertus was grown in pot experiments using 8 soil types at 5 concentrations of nitrogen (N) and phosphorus (P). Based on harvest data, the variables, seedlings emergence, root: shoot (R: S) ratio, N and P concentration, chlorophyll content, Relative Colimitation Index (RCI) and dry matter allocation to plant components, were determined. N and P addition stimulated the growth of plants in different soils, as reflected by a sign

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