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Journal articles on the topic 'Vegetation elements'

Author: Grafiati

Published: 4 June 2021

Last updated: 13 February 2022

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1

Yagci, Oral, Mehmet Furkan Celik, Vasileios Kitsikoudis, et al. "Scour patterns around isolated vegetation elements." Advances in Water Resources 97 (November 2016): 251–65. http://dx.doi.org/10.1016/j.advwatres.2016.10.002.

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2

Masing, Viktor. "Approaches, levels and elements of vegetation research." Folia Geobotanica et Phytotaxonomica 29, no. 4 (1994): 531–41. http://dx.doi.org/10.1007/bf02883149.

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3

Lézine, Anne-Marie. "Late Quaternary Vegetation and Climate of the Sahel." Quaternary Research 32, no. 3 (1989): 317–34. http://dx.doi.org/10.1016/0033-5894(89)90098-7.

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AbstractPollen and phytogeographic evidence provides a vegetational history of the Sahel for the period 0–18,000 yr B.P. The zonal vegetation fluctuated latitudinally and its most extreme positions occurred at 18,000 and 8500 yr B.P. The first involved a southward shift of the Sahelian wooded grassland to 10°N under the arid conditions of the last glacial maximum. The second change shows a rapid northward migration of humid vegetation: Guinean elements reach 16°N and Sahelo-Sudanian elements extend to the southern margin of the modern Sahara (21°N) when the Atlantic monsoon flux increased. In

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4

Berg, Christian, Jörg Ewald, Gabriele Berg, and Carsten Hobohm. "What are the organismic elements of vegetation science?" Applied Vegetation Science 21, no. 2 (2018): 341–44. http://dx.doi.org/10.1111/avsc.12371.

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5

Jeglum, John K., and Fangliang He. "Pattern and vegetation–environment relationships in a boreal forested wetland in northeastern Ontario." Canadian Journal of Botany 73, no. 4 (1995): 629–37. http://dx.doi.org/10.1139/b95-067.

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A forested wetland data set from northeastern Ontario, consisting of species cover and environmental measures in 43 stands, was analyzed with canonical correspondence analysis. Results showed two main vegetational gradients related to factor complexes of peat depth – moisture (mire margin to mire expanse) and pH–calcium. Stands within each of the vegetation types were positioned closely, and gradients of types were similar to those from earlier analyses, suggesting the validity of a previous classification. Axis I of the ordination was highly related to peat depth, several elements (Al, Fe, an

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6

Jiang, Qinhua, and Dolores R. Piperno. "Environmental and Archaeological Implications of a Late Quaternary Palynological Sequence, Poyang Lake, Southern China." Quaternary Research 52, no. 2 (1999): 250–58. http://dx.doi.org/10.1006/qres.1999.2070.

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Paleoecological data from Poyang Lake, southern China, indicate that significant natural and human-induced vegetational changes have occurred during the Late Quaternary in the Middle Yangtze River valley, the likely location of rice (Oryza sativa L.) domestication. During the late Pleistocene (from ca. 12,830 to ca. 10,500 yr B.P.), the climate was cooler and drier than today's. The subtropical, mixed deciduous–evergreen broad-leaved forest which constitutes the modern, potential vegetation was reduced and herbaceous vegetative cover expanded. A hiatus in sedimentation occurred in Poyang Lake,

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7

Sudimac, Budimir, Natasa Cukovic-Ignjatovic, and Dusan Ignjatovic. "Experimental study on reducing temperature using modular system for vegetation walls made of perlite concrete." Thermal Science 22, Suppl. 4 (2018): 1059–69. http://dx.doi.org/10.2298/tsci170612227s.

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The aim of this research is to examine and analyse the thermal characteristics of the fa?ade modular element. The possibility of optimization of the fa?ade coating with vegetation is examined experimentally in this research, with the aim of improving the thermal characteristics of the fa?ade wall. This element is made of perlite concrete in which the greenery is implanted. The scope of the research is experimental and theoretical testing the possibility for optimizing the fa?ade coating with vegetation. The energy specificities of modular vegetation elements and their contribution to the impro

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8

Miladinovic, Dragoljub, Budimir Ilic, and Violeta Milosavljevic. "Trace elements and antioxidants in Astragalus onobrychis L. var. chlorocarpus (Griseb.) S. Kozuharov et D.K. Pavlova." Chemical Industry 65, no. 3 (2011): 323–27. http://dx.doi.org/10.2298/hemind110110019m.

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Leaves of growing-wild species Astragalus onobrychis L. var. chlorocarpus (Griseb.) S. Kozuharov et D. K. Pavlova were collected during the different stages of growth and analyzed for iron (Fe), copper (Cu), zinc (Zn), manganese (Mn), soluble proteins, reduced glutathione (GSH), total flavonoid and total carotenoid contents. Iron, copper and manganese have shown similar seasonal pattern, increasing of metal content in leaves during the vegetative period. The highest values of the examined elements were in seed forming stage, except zinc. The highest value of this element was recorded in initia

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9

Leenders, Jakolien K., Geert Sterk, and John H. Van Boxel. "Modelling wind-blown sediment transport around single vegetation elements." Earth Surface Processes and Landforms 36, no. 9 (2011): 1218–29. http://dx.doi.org/10.1002/esp.2147.

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10

Zakharikhina, L. V., and Yu S. Litvinenko. "Volcanism and geochemistry of soil and vegetation cover of Kamchatka. Communication 3. Elemental composition of vegetation of volcanic ecosystems." Вулканология и сейсмология, no. 4 (July 8, 2019): 40–51. http://dx.doi.org/10.31857/s0203-03062019440-51.

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The link of the chemical composition of the plant with the active volcanism of Kamchatka, is determined by the stable occurrence into the composition of the priority chemical elements for plants, volcanic ashes and soils: Ca, Mg, Mn, P, Cu, Zn and Sr. An elevated geochemical background of Kamchatka plants relative to the bulk chemical composition of the peninsula’s soils was established. The contents of Br, Hg, Hf, Sb, Ga, W, K relative to the clarks for living matter in the plants of the region are exceeded by 3–5 times. Against the background of small variations in the contents of chemical e

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11

Krejčí, Markéta. "Function of the vegetative elements in contemporaneous interpretation of the architectonic work." Acta Universitatis Agriculturae et Silviculturae Mendelianae Brunensis 56, no. 4 (2008): 239–46. http://dx.doi.org/10.11118/actaun200856040239.

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The creative process during which a vegetation element finds itself in the position of a fundamental part of material design of the building can be found in the field of modern architectural production. Along with other building materials, it has its own task to participate in the composition of architectural space. This represents an authentic approach of the current production where the dominating position of the vegetation material determines the unique character of the final work. In these existing factors of practice, the vegetation material is treated, according to the three branches

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12

Hernández, Bernardo, and M. Carmen Hidalgo. "Effect of Urban Vegetation on Psychological Restorativeness." Psychological Reports 96, no. 3_suppl (2005): 1025–28. http://dx.doi.org/10.2466/pr0.96.3c.1025-1028.

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The present study analyzes the contribution which natural elements in the city make to restorativeness, that is, the potential of certain environments to help recover the capacity to focus attention, reduce mental fatigue, and reduce stress. We presented photographs of 12 urban scenes (streets, industrial areas, and buildings) with and without vegetation to 214 university students, divided into 12 groups who then completed the Perceived Restorativeness Scale. The results support the hypothesis, i.e., urban environments with natural elements yield higher restorativeness than urban environments

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13

Lucas, Chris, Willem Bouten, Zsófia Koma, W. Kissling, and Arie Seijmonsbergen. "Identification of Linear Vegetation Elements in a Rural Landscape Using LiDAR Point Clouds." Remote Sensing 11, no. 3 (2019): 292. http://dx.doi.org/10.3390/rs11030292.

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Modernization of agricultural land use across Europe is responsible for a substantial decline of linear vegetation elements such as tree lines, hedgerows, riparian vegetation, and green lanes. These linear objects have an important function for biodiversity, e.g., as ecological corridors and local habitats for many animal and plant species. Knowledge on their spatial distribution is therefore essential to support conservation strategies and regional planning in rural landscapes but detailed inventories of such linear objects are often lacking. Here, we propose a method to detect linear vegetat

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14

Yagci, O., and M. S. Kabdasli. "The impact of single natural vegetation elements on flow characteristics." Hydrological Processes 22, no. 21 (2008): 4310–21. http://dx.doi.org/10.1002/hyp.7018.

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15

Mani, Francesco, and Claude Oestges. "A Ray Based Method to Evaluate Scattering by Vegetation Elements." IEEE Transactions on Antennas and Propagation 60, no. 8 (2012): 4006–9. http://dx.doi.org/10.1109/tap.2012.2201123.

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16

Bakiev, S. A., J. Rakhmanov, Z. M. Khakimov, and S. Turaev. "Peculiarities of the distribution of some elements in vegetation samples." Journal of Radioanalytical and Nuclear Chemistry 272, no. 2 (2007): 281–84. http://dx.doi.org/10.1007/s10967-007-0516-3.

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17

Кулик, М. І., та І. І. Рожко. "Вплив погодних умов веґетаційного періоду на елементи продуктивності та урожайність проса прутоподібного". Вісник Полтавської державної аграрної академії, № 4 (28 грудня 2017): 50–55. http://dx.doi.org/10.31210/visnyk2017.04.09.

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З'ясовано вплив погодних умов веґетації на мінливість елементів продуктивності (висоти та густоти стеблостою) проса прутоподібного. Визначено вплив середньодобової температури повітря та суми опадів під час веґетації рослин на урожайність фітомаси культури в розрізі років дослідження. Наведено кореляційні залежності між кількісними показниками рослин (елементами продуктивності) третього–шостого років веґетації та урожайністю фітомаси проса прутоподібного. Встановлено, що урожайність сухої надземної веґетативної маси проса прутоподібного в більшій мірі обумовлюється кількістю стебел на одиницю

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18

Lenz, Olaf K., Walter Riegel, and Volker Wilde. "Greenhouse conditions in lower Eocene coastal wetlands?—Lessons from Schöningen, Northern Germany." PLOS ONE 16, no. 1 (2021): e0232861. http://dx.doi.org/10.1371/journal.pone.0232861.

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The Paleogene succession of the Helmstedt Lignite Mining District in Northern Germany includes coastal peat mire records from the latest Paleocene to the middle Eocene at the southern edge of the Proto-North Sea. Therefore, it covers the different long- and short-term climate perturbations of the Paleogene greenhouse. 56 samples from three individual sections of a lower Eocene seam in the record capture the typical succession of the vegetation in a coastal wetland during a period that was not affected by climate perturbation. This allows facies-dependent vegetational changes to be distinguishe

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19

Li, Zhan, Michael Schaefer, Alan Strahler, Crystal Schaaf, and David Jupp. "On the utilization of novel spectral laser scanning for three-dimensional classification of vegetation elements." Interface Focus 8, no. 2 (2018): 20170039. http://dx.doi.org/10.1098/rsfs.2017.0039.

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The Dual-Wavelength Echidna Lidar (DWEL), a full waveform terrestrial laser scanner (TLS), has been used to scan a variety of forested and agricultural environments. From these scanning campaigns, we summarize the benefits and challenges given by DWEL's novel coaxial dual-wavelength scanning technology, particularly for the three-dimensional (3D) classification of vegetation elements. Simultaneous scanning at both 1064 nm and 1548 nm by DWEL instruments provides a new spectral dimension to TLS data that joins the 3D spatial dimension of lidar as an information source. Our point cloud classific

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20

Kholod, S. S. "Large-scale mapping of the catenas vegetation in Subarctic tundra." Geobotanical mapping, no. 1993 (1995): 3–21. http://dx.doi.org/10.31111/geobotmap/1993.3.

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One of the most difficult tasks in large-scale vegetation mapping is the clarification of mechanisms of the internal integration of vegetation cover territorial units. Traditional way of searching such mechanisms is the study of ecological factors controlling the space heterogeneity of vegetation cover. In essence, this is autecological analysis of vegetation. We propose another way of searching the mechanisms of territorial integration of vegetation. It is connected with intracoenotic interrelation, in particular, with the changing role of edificator synusium in a community along the altitudi

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21

Siepel, Adam C., Tammo S. Steenhuis, Calvin W. Rose, J. Yves Parlange, and Gregory F. McIsaac. "A simplified hillslope erosion model with vegetation elements for practical applications." Journal of Hydrology 258, no. 1-4 (2002): 111–21. http://dx.doi.org/10.1016/s0022-1694(01)00569-8.

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22

Lashchinskiy, N. N., M. P. Tishchenko, O. Yu Pisarenko, and N. V. Lashchinskaya. "Vegetation cover of subtaiga landscapes in premountain plain on a right bank of the Ob river." Vegetation of Russia, no. 24 (2014): 63–85. http://dx.doi.org/10.31111/vegrus/2014.24.63.

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Vegetation of the right bank of the Ob River in the limits of Novosibirsk area consists of southern taiga, subtaiga and forest-steppe elements. More over, in comparison with neighboring areas on the West Siberian Plain, it contains the significant amount of mountain elements (Kuminova, Vagina, Lapshina, 1963). Natural vegetation of the area belongs to the forest-steppe subzone of the West Siberian province (Il’ina, 1985). Low percentage of forest coverage is caused by anthropogenic deforestation and wide distribution of meadows (Lapshina, 1963). This is the most endangered vegetation in Novosi

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23

Středa, Tomáš, Tomáš Litschmann, and Hana Středová. "Relationship between tree bark surface temperature and selected meteorological elements." Contributions to Geophysics and Geodesy 45, no. 4 (2015): 299–311. http://dx.doi.org/10.1515/congeo-2015-0026.

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Abstract The results were obtained by measurements in 2014 and 2015 in an apple orchard in Starý Lískovec and Těšetice (South Moravia, Czech Republic, Central Europe) into fertile planting of apple trees. The results show that the bark surface temperature during the year slightly differs from the surrounding air temperature. In addition, it is in average a few tenths of a °C higher in the period before the onset of the vegetation and several tenths of a degree lower during vegetation. Causes of these differences appear to be associated with the flow of sap as well as with foliage. Although it

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24

Nikiforov, A. R. "Meadows of the Crimean Yaila." Plant Biology and Horticulture: theory, innovation, no. 149 (December 10, 2019): 124–31. http://dx.doi.org/10.36305/0201-7997-2019-149-124-131.

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A comparative analysis of the vegetation composition in the meadow steppe community and the meadow in the middle in a karst sinkhole was made. The appearance of the meadow, which is formed by its coenogenous elements, is contrasted with the steppe. The compositions of the elements in two neighboring coenoses are also not similar. Obviously, the examined communities have different genesis. These differences are due to environmental conditions of karst depression. Yaila meadows are here indigenous primary vegetation of azonal origin.

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25

Kowalska, Joanna Beata, Michał Gąsiorek, Paweł Zadrożny, Paweł Nicia, and Jarosław Waroszewski. "Deep Subsoil Storage of Trace Elements and Pollution Assessment in Mountain Podzols (Tatra Mts., Poland)." Forests 12, no. 3 (2021): 291. http://dx.doi.org/10.3390/f12030291.

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Research highlights: this article refers to the deep storage of trace elements as a result of the podzolization process under different types of vegetation cover. This is also an attempt to trace differentiation in the distribution of trace elements in mountain soils under the podzolization process. Background and objectives: we focused on estimating whether the podzolization process of soils under various vegetation covers led to the deep storage of trace elements in the subsoil. Furthermore, the potential contamination of studied soils with trace elements using pollution indices was assessed

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26

Plit, Joanna. "The map of potential natural vegetation as a basis for comparative studies and geobotanical regionalization." Acta Societatis Botanicorum Poloniae 50, no. 3 (2014): 515–40. http://dx.doi.org/10.5586/asbp.1981.073.

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A method of typology and regionalization of landscape units of vegetation on the basis of a map of potential natural vegetation is presented. Particular attention has been paid to the methodical basis of the conducted division. The map of potential natural vegetation was subsequently compared with maps of other elements of the natural environment and the result of geobotanical botanical regionalization was compared to the complex physicogeographical regionalization.

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27

Ibrahim Rzayeva, Ilhama. "Study of the effect of physical mutagens on the elements of cotton varieties Summary." NATURE AND SCIENCE 04, no. 05 (2020): 40–43. http://dx.doi.org/10.36719/2707-1146/05/40-43.

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The effect of different doses of gamma rays of the Co60 isotope on the seeds of cotton varieties AzNIXI-104 and AzNIXI-195 before sowing caused changes in the growing season, plant height, sympodial branches and the number of bolls on the bush. At low doses of gamma rays (500 r, 5000 r) the vegetation period was shortened, the number of sympodial branches and bolls in the branch increased, and at high doses of mutagen a decrease in biomorphological features was observed. Key words: cotton, sort, gamma ray, mutagen, sympodial branch, vegetation period.

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28

Vasile, Gabriela Geanina, Cristina Dinu, Lidia Kim, et al. "Platinum Group Elements in Road Dust and Vegetation from Some European and National Roads with Intensive Car Traffic in Romania." Revista de Chimie 70, no. 1 (2019): 286–92. http://dx.doi.org/10.37358/rc.19.1.6901.

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The paper presents a monitoring study of the platinum group metals concentrations in 17 samples of road dust and vegetation from areas with heavy car traffic on several European and national roads in eastern Romania. The Ir, Pd, Pt, Rh, Ru concentrations were determined by the ICP-MS technique, the reported values being below the method�s limit of determination for Ir, Pt and Ru both in soil and vegetation. As regards the Pd content, it showed a maximum of 794 mg / kg dry matter in Focsani area (DN2), an area where, according to national data published by National Road Infrastructure Managemen

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29

Mohammed, I., and I. M. Abubakar. "The Rerelationship Between Climatic Elements and Vegetation Cover in Adamawa State, Nigeria." Agricultural Journal 14, no. 5 (2020): 94–103. http://dx.doi.org/10.36478/aj.2019.94.103.

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30

Rope, Susan K., W. John Arthur, Timothy H. Craig, and Erica H. Craig. "Nutrient and trace elements in soil and desert vegetation of southern Idaho." Environmental Monitoring and Assessment 10, no. 1 (1988): 1–24. http://dx.doi.org/10.1007/bf00394252.

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31

Bhandari, Sudarshan, Khum N. Paudayal, and Arata Momohara. "Late Pleistocene plant macrofossils from the Thimi Formation (Madhyapur Thimi section) of the Kathmandu Valley, central Nepal." Journal of Nepal Geological Society 40 (December 1, 2010): 31–48. http://dx.doi.org/10.3126/jngs.v40i0.23594.

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The Late Pleistocene plant macrofossils from the Thimi Formation of the Kathmandu Valley have been reported in this paper. On the basis of 71 taxa from 39 families, seven plant macrofossil assemblages T-1 to T-7 were described from 18.5 m thick section of the Thimi Formation exposed at Madhyapur Thimi, Bhaktapur. Pinus, Abies, Tsuga, Carpinus, Sambucus, Rubus, Eurya, Potentilla and Scirpus are the common elements in the Thimi Formation. It is found that the cool temperate elements (Abies, Pinus, Tsuga, Picea, Taxus) were dominated over warm climatic elements (Quercus, Eurya, Pyracantha, etc.)

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32

Kyrylchuk, Andriy. "Geography of rendzina in Western region of Ukraine." Visnyk of the Lviv University. Series Geography, no. 44 (November 28, 2013): 133–39. http://dx.doi.org/10.30970/vgg.2013.44.1213.

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Geographic regularities of rendzina distribution in Western Ukrainian region were analyzed as well as their correspondence to a variety of relief elements and the way soil formation parent materials and vegetation effects on the morphogenetic properties of these soils. Key words: rendzina, relief, soil formation parent materials, vegetation, morphogenetic properties.

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33

Mareček, J. "Folk landscape architecture as a significant value of Czech landscape." Horticultural Science 34, No. 1 (2008): 42–46. http://dx.doi.org/10.17221/1846-hortsci.

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In the past the image of Czech countryside was created by agricultural and social activities of the rural population in a significant manner. These activities related to natural elements and to the creation of landscape in a wider sense can be described as folk landscape architecture. Its object is mainly the spatial arrangement and assortment composition of vegetation and its functionality in villages and in their landscape environment. This study defines these activities as time limited regional (local) customary practices of agricultural and cultural and social character, reflected especial

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34

Tahvildari, Navid, Ramin Familkhalili, and Gangfeng Ma. "NONHYDROSTATIC MODELING OF FLOW INTERACTIONS WITH HIGHLY FLEXIBLE VEGETATION." Coastal Engineering Proceedings, no. 36v (December 28, 2020): 59. http://dx.doi.org/10.9753/icce.v36v.waves.59.

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Improving our understanding of the interactions between gravity waves, currents, and coastal vegetation, which are nonlinear in nature, enables coastal engineers and managers to better estimate hydrodynamic forces on coastal infrastructure and utilize natural elements to mitigate their impacts. Aquatic vegetation is ubiquitous in coastal waters and it is well-known that flow loses energy over vegetation. Computational modeling of wave-vegetation interaction has been the subject of numerous recent studies and many improvements have been achieved in reducing limitations applied on wave and veget

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35

Ali, Ahmed Khairadeen, Hayub Song, One Jae Lee, Eun Seok Kim, and Haneen Hashim Mohammed Ali. "Multi-Agent-Based Urban Vegetation Design." International Journal of Environmental Research and Public Health 17, no. 9 (2020): 3075. http://dx.doi.org/10.3390/ijerph17093075.

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Urban vegetation is an essential element of the urban city pedestrian walkway. Despite city forest regulations and urban planning best practices, vegetation planning lacks clear comprehension and compatibility with other urban elements surrounding it. Urban planners and academic researchers currently devote vital attention to include most of the urban elements and their impact on the occupants and the environment in the planning stage of urban development. With the advancement in computational design, they have developed various algorithms to generate design alternatives and measure their impa

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36

Kulachkovskyy, Roman. "Geoecological modelling of potential natural vegetation in the Limnytsia source area." Visnyk of the Lviv University. Series Geography, no. 48 (December 23, 2014): 32–38. http://dx.doi.org/10.30970/vgg.2014.48.1291.

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The concept of a natural morphogenic geoecosystem was used to model the vegetation in the GIS environment. The edaphic factors used in modeling included landform elements characteristics (slope and concavity/convexity) as well as the soil and the parent rock properties that define drainage. The climatic factors influencing the distribution of the vegetation embraced annual sums of precipitation and of active temperature. The information about the ecological interrelations between the factors and the vegetation was taken from the regional literature as well as from the field observations. Key w

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37

Pan, Tong, Xiao Jing Li, Hao Peng Wang, and Kai Zhao. "Research on LAI Retrieving Applied for Virtual Reality Simulation of Vegetation." Applied Mechanics and Materials 263-266 (December 2012): 1473–77. http://dx.doi.org/10.4028/www.scientific.net/amm.263-266.1473.

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It is the key process for developing usability of virtual reality simulation of vegetation taking into account soil, chemistry elements of water, temperature and humidity of land surface, and lighting. Retrieving the characteristics of vegetation from remote sensing data effectively and exactly, building the relationship between remote sensing data and interfaces of VR-vegetation models are important. The paper discusses dense vegetation model, nondense vegetation model, and two-stream approximation model applied for LAI retrieving, analyzes the efficiency of the methods; presents the process

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38

Hansen, Barbara C. S., and Daniel R. Engstrom. "Vegetation History of Pleasant Island, Southeastern Alaska, since 13,000 yr B.P." Quaternary Research 46, no. 2 (1996): 161–75. http://dx.doi.org/10.1006/qres.1996.0056.

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A 13,000-year history of late-Quaternary vegetational and climatic change has been derived from lacustrine sediments from Pleasant Island in the Glacier Bay region of southeastern Alaska. Early arrival of lodgepole pine and mountain hemlock, indicated by the presence of pollen and conifer stomata, suggests expansion from refugia in the Alexander Archipelago. A short-term climatic reversal, possibly correlated with the European Younger Dryas, is inferred from the expansion of tundra elements and deposition of inorganic sediments between 10,600 and 9900 14C yr B.P. Two peat cores from the lake c

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39

Hillman, Samuel, Luke Wallace, Karin Reinke, Bryan Hally, Simon Jones, and Daisy S. Saldias. "A Method for Validating the Structural Completeness of Understory Vegetation Models Captured with 3D Remote Sensing." Remote Sensing 11, no. 18 (2019): 2118. http://dx.doi.org/10.3390/rs11182118.

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Characteristics describing below canopy vegetation are important for a range of forest ecosystem applications including wildlife habitat, fuel hazard and fire behaviour modelling, understanding forest recovery after disturbance and competition dynamics. Such applications all rely on accurate measures of vegetation structure. Inherent in this is the assumption or ability to demonstrate measurement accuracy. 3D point clouds are being increasingly used to describe vegetated environments, however limited research has been conducted to validate the information content of terrestrial point clouds of

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40

Тихонова, Elena Tikhonova, Трещевская, et al. "Chemical composition of vegetation in man-made landscapes Kursk magnetic anomaly." Forestry Engineering Journal 6, no. 3 (2016): 48–53. http://dx.doi.org/10.12737/21679.

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The open-mining leads to the formation of the post-miningo or disturbed lands, which are characterized by extreme conditions. The largest area of the post-mining and disturbed lands in Central Black Soil Region are situated near the Kursk magnetic anomaly enterprises. The main direction of the restoration of the post-mining lands is the forestry reclamation. The biocenosis contribute to changes of substrates properties and their transformation into primary soil (“em-bryonic soils”). The dumps vegetation absorbs nitrogen, ash elements and heavy metals from the substrate and air and returns the

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Osuch, Bolesław, Wiesław Gądek, Anna Homa, Marta Cebulska, Robert Szczepanek, and Anna Hebda-Małocha. "Methods of estimating the elements of water balance in a forested catchment basin." Journal of Water and Land Development 13a, no. 1 (2009): 19–40. http://dx.doi.org/10.2478/v10025-010-0017-6.

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Methods of estimating the elements of water balance in a forested catchment basin The paper presents basic hydrological processes of rainfall-runoff transformation in experimental watershed of the Trzebuńka stream. Several field experiments were made to determine basic hydrological parameters, The influence of atmospheric circulation on spatial distribution of precipitation was investigated. Attempt was made to determine the influence of forest vegetation, undergrowth, forest litter retention and surface retention on water loss in the catchment. Water retention capacity of soil was also estima

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Najwer, Alicja, Janina Borysiak, Joanna Gudowicz, Małgorzata Mazurek, and Zbigniew Zwoliński. "Geodiversity and Biodiversity of the Postglacial Landscape (Dębnica River Catchment, Poland)." Quaestiones Geographicae 35, no. 1 (2016): 5–28. http://dx.doi.org/10.1515/quageo-2016-0001.

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Abstract The preparation of a proper zoning plan or landscape-ecological plan requires taking into account recognition of the natural values of an area covered by the plan and evaluating its abiotic and biotic diversities. The aim of the paper is to present the new approach to the procedure of geodiversity and biodiversity assessment. This procedure is used to characterise abiotic and biotic heterogeneity of the postglacial landscape modified by a man, tested on Dębnica River catchment (Western Pomerania, Poland). This catchment is a representative example illustrating the landscape of Central

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Handford, Paul. "Trill rate dialects in the Rufous-collared Sparrow, Zonotrichia capensis, in northwestern Argentina." Canadian Journal of Zoology 66, no. 12 (1988): 2658–70. http://dx.doi.org/10.1139/z88-391.

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Geographical variation in trill rate of Zonotrichia capensis was assessed in a sample of about 2300 individuals from nearly 600 sites distributed throughout northwestern Argentina, from 22 to 34°S. The variation was partitioned among the following site characteristics: original (natural) vegetation, contemporary vegetation structure, latitude, longitude, and altitude. About 45% of the variation was attributable to the original vegetation (p < 0.0001): the other site characteristics explained a further 4%. Thus the geographical distribution of trill rate closely paralleled that of the natura

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Judt, Guzmán, Gómez, et al. "Diverging Effects of Landscape Factors and Inter-Row Management on the Abundance of Beneficial and Herbivorous Arthropods in Andalusian Vineyards (Spain)." Insects 10, no. 10 (2019): 320. http://dx.doi.org/10.3390/insects10100320.

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Land use at landscape and field scales can increase the diversity and abundance of natural enemies for pest control. In this study, we investigated interactions between landscape elements (semi-natural vegetation, olive orchards, vineyards, other agricultural areas) and inter-row management (vegetation cover vs. bare soil) in relation to arthropod populations in Andalusian vineyards. Arthropods were collected from grapevine foliage in 15 vineyards using suction sampling. Landscape structure was analyzed within a 750 m radius surrounding the studied vineyards. Arthropods were categorized into f

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Ханина, Л. Г., and L. G. Khanina. "Ground Vegetation Modeling through Functional Species Groups and Patches in the Forest Floor." Mathematical Biology and Bioinformatics 10, no. 1 (2015): 15–33. http://dx.doi.org/10.17537/2015.10.15.

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We have developed a system of plant functional groups for modeling dynamics of forest ground vegetation. Ecological and coenotic traits of species together with species life form and biomass values were used to classify species into the functional groups. Ground vegetation patches dominated by species of different plant functional groups were distinguished in the forest floor. We have characterized biomass of these patches by applying of statistical analysis of published data and results of our own field investigations combined into the database "Biomass". Biomass of vascular plants and bryoph

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Raison, R. J., P. K. Khanna, and P. V. Woods. "Mechanisms of element transfer to the atmosphere during vegetation fires." Canadian Journal of Forest Research 15, no. 1 (1985): 132–40. http://dx.doi.org/10.1139/x85-022.

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Published data and newly presented evidence demonstrate that the proportion of N or P lost from plant material during combustion under a wide range of conditions increases linearly with percentage loss of fuel weight during combustion. For N the correlation is strong, and the slope (β) of the regression line approaches unity for combustions under field or simulated-field conditions, but reduces to 0.78 for materials combusted in a muffle furnace. Almost all of the losses of N are due to volatilization. The relationship for P is less well defined, and β is lower (0.56 for field studies; about 0

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Freydier, Rémi, Bernard Dupré, Jean-Louis Dandurand, Jean-Pol Fortune, and Luc Sigha-Nkamdjou. "Trace elements and major species in precipitation at African stations: concentrations and sources." Bulletin de la Société Géologique de France 173, no. 2 (2002): 129–46. http://dx.doi.org/10.2113/173.2.129.

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Abstract The chemical composition of rainwaters is important in obtaining information on the aerosols and gaseous species present in the atmosphere. Original data on the concentrations of trace elements and major species in the dissolved and particulate fractions of rainwater samples collected in intertropical Africa were used to determine the potential sources of chemical species. The photographic and mineralogical characterization of rainwater particles using scanning electron microscopy allow to identify the various origins of aerosols and the associated chemical elements: (i) the crustal s

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Demková, Katarína, Martin Hais, and Magda Edwards-Jonášová. "Cross-Border Comparison of Non-Forest Woody Vegetation in the White Carpathians (Central Europe) Over Last 65 Years." Journal of Landscape Ecology 12, no. 2 (2019): 64–78. http://dx.doi.org/10.2478/jlecol-2019-0010.

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Abstract Landscape structure is determined by human activities and natural processes. Despite both influences are described in many studies, there remains still question, how the landscape structure reflects the individual socio-economic predictors. To answer this question we compared landscape structure, with emphasis on non-forest woody vegetation, of two states, however, with common socio-economic and political history. Non-forest woody vegetation represents characteristic feature in rural landscape, which increases water retention, biodiversity and bio-migration using green structures. In

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Khomutova, V. I. "The Significance of Zonal, Regional and Local Vegetation Elements in Lacustrine Pollen Spectra." Grana 34, no. 4 (1995): 246–50. http://dx.doi.org/10.1080/00173139509429053.

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Gorbunov, A. V., M. V. Frontasyeva, S. F. Gundorina, T. L. Onischenko, B. B. Maksjuta, and Chen Sen Pal. "Effect of agricultural use of phosphogypsum on trace elements in soils and vegetation." Science of The Total Environment 122, no. 3 (1992): 337–46. http://dx.doi.org/10.1016/0048-9697(92)90051-s.

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