scholarly journals Non-destructive methods for peat layer assessment in oligotrophic peat bogs: a case study from Poiana Ştampei, Romania

2011 ◽  
Vol 75 (2) ◽  
pp. 157-163
Author(s):  
Iuliana F. Gheorghe ◽  
Cristina M. Vâlcu ◽  
Ion Barbu ◽  
Sorana Ţopa
Keyword(s):  
Vegetation Type ◽  
Depth Estimation ◽  
Peat Bogs ◽  
Peat Bog ◽  
Peat Layer ◽  
Layer Depth ◽  
Peat Deposits ◽  
Picea Excelsa ◽  
Sphagnum Fimbriatum ◽  
Non Destructive

Practices currently employed in the investigation and characterisation of peat deposits are destructive and may irremediable perturb peat bog development even in cases when exploitation is not carried out. We investigated the correlation between vegetation characteristics in the active area of Poiana Ştampei peat bog, Romania, and the underlying peat layer depth, aiming at establishing a non-destructive method of peat layer depth estimation. The presence of the <em>Sphagneto-Eriophoretum</em> vaginati association, dominated by <em>Sphagnum fimbriatum</em>, <em>Eriophorum vaginatum</em>, <em>Andromeda polifolia</em>, <em>Vaccinium oxycoccos</em>, <em>V. myrtillus</em>, <em>V. vitis-idaea</em>, <em>Polytrichum commune</em>, <em>Picea excelsa</em>, <em>Pinus sylvestris</em> and <em>Betula verrucosa</em> was found to predict the existence of the peat layer but not its depth. Out of the seven identified vegetation types, one type was associated with a very thin or no peat layer, one type was characterised by the presence of a thick (over 100 cm) peat layer and five types indicated the presence of variable average depths of the peat layer. pH values correlated with peat layer depth only within the vegetation type associated with thick peat layers.

scholarly journals Distribution of heavy metals in cutover peat bog soils

2019 ◽  
Vol 8 (3) ◽  
pp. 63-69
Author(s):  
Elena Sergeevna Novosyolova ◽  
Lyudmila Nikolaevna Shikhova ◽  
Evgeny Mikhailovich Lisitsin
Keyword(s):  
Heavy Metals ◽  
Chemical Elements ◽  
Control Site ◽  
Peat Bogs ◽  
Peat Bog ◽  
Peat Deposits ◽  
And Migration ◽  
Economic Use ◽  
Maximum Content ◽  
Migration Of Chemical Elements

The paper contains the research results on content of total and mobile heavy metals compounds (lead, cadmium, copper, and zinc) in soils of the cutover peat bog Zenginsky located in the central part of the Kirov Region. As a result of the conducted researches it is revealed that the content of elements in different peat layers in control site (zinc - up to 2,60; copper - up to 0,90; lead - up to 5,60; cadmium - up to 0,59 mg/kg of soil) does not exceed the level of their maximum-permissible concentration and background contents in soils of the Kirov Region. For the undeveloped site the increased content of total and mobile compounds of the studied metals in the top layers is noted; it can be caused by biogenous accumulation of these elements by plants. The developed soils (the drained sites) are characterized by considerable fluctuations of elements content both in different profiles, and in the different layers of the same profile. Here the maximum content of elements in separate layers is much higher than control (zinc - up to 126,0; copper - up to 34,0; lead - up to 17,0; cadmium - up to 1,2 mg/kg of soil). Economic use of the peat bogs leads to an active mineralization of the top part of the remained peat mass. As a result of these processes stability of biogeochemical cycles of separate elements is broken. At the same time, the received data allow to consider soils of control sites as indicators of surrounding environment condition. The good safety of peat deposits gives the opportunity to study processes of accumulation and migration of chemical elements.

scholarly journals Comparison of metals content in peatlands with different anthropopressure in Welski Landscape Park (Poland)

2021 ◽  
pp. 20-28
Author(s):  
Bartłomiej Igliński ◽  
Anna Iglińska ◽  
Urszula Kiełkowska ◽  
Dariusz Kamiński ◽  
Grzegorz Piechota
Keyword(s):  
Heavy Metals ◽  
Metal Content ◽  
Peat Bogs ◽  
Peat Bog ◽  
Plant Debris ◽  
Retrospective Monitoring ◽  
Calcium And Magnesium ◽  
Good Agent

The metal content was determined using the WD-XRF method in the peat from the Wąpiersk bog and the Las Nadwelski bog (Welski Landscape Park, Poland). The results of the study show that the concentration of metals, especially heavy metals in peat bogs in Welski Landscape Park is low in general. In both bogs, the concentration of heavy metals was lower in the center than on the border. This shows that heavy metals are absorbed by the peat at the border and their further migration is limited. There are more elements such as iron, calcium and magnesium in the Las Nadwelski bog. There is more light on the border of the forest, which also plays an important role in decomposing plant debris, releasing metals. Heavy metals content was higher in Wąpiersk bog – a bog with higher anthropopressure. To sum up, the peat bog actively captures heavy metals, immobilizing them, and acts as a kind of “filter”. Peat is a good agent for retrospective monitoring of metals migration and accumulation in the environment.

scholarly journals Extension of the Thermographic Signal Reconstruction Technique for an Automated Segmentation and Depth Estimation of Subsurface Defects

2020 ◽  
Vol 6 (9) ◽  
pp. 96
Author(s):  
Alexander Schager ◽  
Gerald Zauner ◽  
Günther Mayr ◽  
Peter Burgholzer
Keyword(s):  
Signal Reconstruction ◽  
Computational Cost ◽  
Infrared Camera ◽  
Poor Performance ◽  
Depth Estimation ◽  
Reconstruction Technique ◽  
Destructive Testing ◽  
Cost Efficient ◽  
Non Destructive ◽  
Subsurface Defects

With increased use of light-weight materials with low factors of safety, non-destructive testing becomes increasingly important. Thanks to the advancement of infrared camera technology, pulse thermography is a cost efficient way to detect subsurface defects non-destructively. However, currently available evaluation algorithms have either a high computational cost or show poor performance if any geometry other than the most simple kind is surveyed. We present an extension of the thermographic signal reconstruction technique which can automatically segment and image defects from sound areas, while also estimating the defect depth, all with low computational cost. We verified our algorithm using real world measurements and compare our results to standard active thermography algorithms with similar computational complexity. We found that our algorithm can detect defects more accurately, especially when more complex geometries are examined.

scholarly journals Transformation of Lake Ecosystem into Peat Bog and Vegetation History Based on Durne Bagno Mire (Lublin Polesie, E Poland)

2007 ◽  
Vol 29 (-1) ◽  
pp. 23-43 ◽  
Author(s):  
Krystyna Bałaga
Keyword(s):  
Vegetation History ◽  
Chemical Elements ◽  
Late Glacial ◽  
Unique Element ◽  
Peat Bogs ◽  
Lake Ecosystem ◽  
Peat Bog ◽  
Mineral Material ◽  
Late Glacial And Holocene ◽  
Almost All

Transformation of Lake Ecosystem into Peat Bog and Vegetation History Based on Durne Bagno Mire (Lublin Polesie, E Poland)In this paper, the history of Durne Bagno, i.e. the largest peat bog in the Lublin Polesie, is shown. Peat bogs are a unique element of the Polesie landscape. They occur mostly in the subregion of the Łęczna-Włodawa Lake District occupying 1.07% of its area. They fill basin-shaped depressions without outflow, often in the immediate vicinity of dystrophic lakes. Based on interdisciplinary research, the changes of vegetation cover and the Durne Bagno lake-mire ecosystem in the Late Glacial and Holocene are presented. The environmental conditions are reconstructed from pollen analysis, detailed identification of algae ofPediastrumgenus and chemical composition of deposits, together with the results of Cladocera analysis. The distribution of archaeological artefacts in the surroundings of Durne Bagno peat bog gives the view on the intensity of settlement in this area. The duration of the limnic and mire stages during the development of the ecosystem was different in different parts of the examined depression. In its central part the limnic stage lasted about 8000 years and included the period from the Late Glacial to the middle Holocene (to about 6000 BP). It is represented by 7 pollen zones and 6 chemical zones. The mire stage contained a part the Atlantic period and on the Subboreal and Subatlantic periods. It is represented by 4 pollen zones and 5 chemical zones. Limnic and mire deposits differ widely in the concentrations of chemical elements. The contents of mineral material and almost all analyzed elements in limnic deposits are high. These deposits are characterized by positive correlation between the contents of Zn and Cr and the frequency of Cladocera fauna. Peat contains very low amount of mineral material. The contents of Ca, Sr and Ba are rather high in sedgemoss peat. The concentrations of these elements decrease upwards due to oligotrophic processes and sedentation of sedge-Eriophorum-Sphagnumpeat. Peat succession was modified by pastoral economy of prehistoric man.

scholarly journals Use of Bomb-Produced 14C to Evaluate the Amount of CO2 Emanating from Two Peat Bogs in Finland

Radiocarbon ◽  
1995 ◽  
Vol 37 (2) ◽  
pp. 567-573 ◽  
Author(s):  
Högne Jungner ◽  
Eloni Sonninen ◽  
Göran Possnert ◽  
Kimmo Tolonen
Keyword(s):  
Emission Rate ◽  
Climatic Factors ◽  
Peat Bogs ◽  
Peat Bog ◽  
Annual Variations ◽  
Temperature And Precipitation ◽  
Activity Peak ◽  
Sphagnum Fuscum ◽  
Ams Dating ◽  
Eastern Finland

We used moss increment counting to obtain well-defined samples of the topmost peat layers of two Sphagnum fuscum hummocks. The two ombrotrophic bogs, Lakkasuo in central Finland and Korvinsuo in eastern Finland, are of different ages, covering 3 and 9 ka, respectively. Using AMS dating, we traced bomb-produced 14C through the topmost parts of the two peat profiles. A well-defined 14C activity peak was found in both sequences dating the corresponding layer to ad 1965. A comparison between the maximum peat activities and the corresponding atmospheric values for the period of interest provides an opportunity to evaluate the amount of CO2 emanating from the decaying peat bog, and taken up by the living sphagnum plants.Considerable variations in δ13C values were also observed. These variations indicate, at least partly, annual variations in the emission rate of CO2 from decomposition of older peat in the bog, and are connected with climatic factors such as temperature and precipitation.

scholarly journals METALS IN OILED PEAT (WESTERN SIBERIA)

2011 ◽  
pp. 67-79
Author(s):  
Yu. Vodianitsky ◽  
A. Savichev ◽  
S. Trofimov ◽  
E. Shishkonakova
Keyword(s):  
Condition Monitoring ◽  
Western Siberia ◽  
Soil Condition ◽  
The State ◽  
Peat Bog ◽  
Peat Layer ◽  
Geochemical Barriers ◽  
Artificial Geochemical Barriers

The study of metals in oil-contaminated peat has double meaning. Firstly, it is diagnostic as convenient and simple The method of soil condition monitoring, and secondly, the ecological method to predict the state of the peat bog as a biocenosis element. Every pollutant elements in contaminated peat are divided into two bands. Some of them (Ti, V, Cr, Ni, Zr, Ba, Y, La, Ce, Nd) accumulate in the upper, bituminous layer of peat. Other elements (halogen chlorine, as well as metals: Ca, Mp, Zn, Cu, Sr), on the contrary, migrate deep into the peat layer with light fractions hydrocarbons. For capturing particularly moving Cu metals, Zn needs to be equipped with artificial geochemical barriers to prevent pollutants from entering groundwater and open ponds.

scholarly journals Hydrological regime and physico-chemical water properties of various types of peat bog sites: case study of Mezilesní peat bog, Šumava Mts.

Geografie ◽  
2020 ◽  
Vol 125 (1) ◽  
pp. 21-46
Author(s):  
Tomáš Doležal ◽  
Lukáš Vlček ◽  
Jan Kocum ◽  
Bohumír Janský
Keyword(s):  
Hydrological Regime ◽  
Peat Bogs ◽  
Peat Bog ◽  
Rainfall Runoff ◽  
Study Objective ◽  
Water Properties ◽  
Hydrological Extremes ◽  
Physico Chemical ◽  
Chemical Water

In a period with frequently occurring hydrological extremes, research on areas with a high retention potential is brought into focus. The Šumava Mountains peat bogs are important parts of the landscape in the headwater area of the Otava river basin. The study objective is to describe the variability of discharges and the dynamics of groundwater level changes in various types of peat bogs, and to identify connections between observed physico-chemical water properties. This is assessed by basic statistical methods. The rainfall-runoff process and physico-chemical water properties can be affected by many factors. In this case, strong relations between the observed parameters were identified along with considerable differences in the involvement of various types of peat bog sites in the runoff process. It is evident that the peat bog pattern and its vegetation cover have an essential effect on the hydrological regime and water properties stored in a peat bog.

NATURAL RADIOISOTOPES AND 137CS IN THE SECTION OF THE SHERSTOBITOVO PEAT BOG OF THE BARABA FOREST-STEPPE (WESTERN SIBERIA)

2021 ◽  
pp. 96-109
Author(s):  
G. A. Leonova ◽  
◽  
M. S. Melgunov ◽  
K. A. Mezina ◽  
A. E. Maltsev ◽  
...  
Keyword(s):  
Forest Fires ◽  
Suspended Matter ◽  
Western Siberia ◽  
Coarse Grained ◽  
Dust Particles ◽  
Winter Period ◽  
Peat Bogs ◽  
Forest Steppe ◽  
Peat Bog ◽  
Additional Contribution

Specific activities of natural (7Be, 210Pb) and technogenic (137Cs) radioisotopes in the suspended matter of snow melted water have been determined and the density of their fallout on the surface of the Sherstobitovo and Ubinskoye peat bogs of the Baraba forest-steppe at the points of snow flow in winter period is estimated. It has been established that the main concentrator of the 7Be radioisotope is a finely dispersed fraction of suspended matter (<0.45 μm), consisting of colloids and dissolved component, 210Pbatm is a coarse-grained fraction (> 3 μm), consisting of dust particles. On the example of vertical profile of the Sherstobitovo peat bog, the first data on the distribution of natural (238U, 210Pb, 226Ra, 40K) and technogenic (137Cs) isotopes were obtained for peat bogs of forest –steppe zone of the Western Siberia. Both 226Ra and 238U show the same pattern of vertical distribution that is also usual for 137Cs and 40K. The increase of activity of these radionuclides is observed in the horizon of 6-12 cm as well as in the lower section part (25-35 cm). According to our assumption it is due to the same processes. Migration of 37Cs deep into peat accumulation is significantly determined by moor water fluctuations in the seasonal and long-term cycle, and it is closely related to the microrelief of bog surface. Besides, 137Cs, being a geochemical analogue of the 40K biophile, is pulled up from the underlying peat horizons by plant roots during the dry season. An additional contribution to the high activity of 137Cs in upper horizons is probably due to the input of 137Cs to the surface of the Sherstobitovo peat bog as a result of peat and forest fires.

scholarly journals Convective Boundary Layer Depth Estimation from S-Band Dual-Polarization Radar

2018 ◽  
Vol 35 (8) ◽  
pp. 1723-1733 ◽  
Author(s):  
John R. Banghoff ◽  
David J. Stensrud ◽  
Matthew R. Kumjian
Keyword(s):  
Boundary Layer ◽  
New York ◽  
Convective Boundary Layer ◽  
Depth Estimation ◽  
Dual Polarization ◽  
Layer Depth ◽  
Reasonable Estimate ◽  
Convective Boundary ◽  
Using Data ◽  
Differential Reflectivity

AbstractThis study investigates Bragg scatter signatures in dual-polarization radar observations, which are defined by low differential reflectivity values, as a proxy for convective boundary layer (CBL) depth. Using data from the WSR-88D in Twin Lakes, Oklahoma (KTLX), local minima in quasi-vertical profiles of are found to provide a reasonable estimate of CBL depth when compared with depth estimates from upper-air soundings from Norman, Oklahoma (KOUN), during 2014. The 243 Bragg scatter and upper-air sounding CBL depth estimates have a correlation of 0.90 and an RMSE of 254 m. Using Bragg scatter as a proxy for CBL depth was expanded to other seasons and locations—performing well in Wilmington, Ohio; Fairbanks, Alaska; Tucson, Arizona; Minneapolis, Minnesota; Albany, New York; Portland, Oregon; and Tampa, Florida—showing its potential usefulness in monitoring CBL depth throughout the year in a variety of geographic locations and meteorological conditions.

scholarly journals Multi-Tool (LA-ICPMS, EMPA and XRD) Investigation on Heavy Minerals from Selected Holocene Peat-Bog Deposits from the Upper Vistula River Valley, Poland

Minerals ◽  
2019 ◽  
Vol 10 (1) ◽  
pp. 9 ◽  
Author(s):  
Krzysztof Szopa ◽  
Sylwia Skreczko ◽  
David Chew ◽  
Tomasz Krzykawski ◽  
Artur Szymczyk
Keyword(s):  
Iron Oxides ◽  
Heavy Minerals ◽  
Peat Bogs ◽  
Peat Bog ◽  
Textural Features ◽  
Vistula River ◽  
Mineral Phases ◽  
Magmatic Body ◽  
Provenance Areas ◽  
Basin Area

Peat sediments represent important environmental and climatic archives, as well as recording information on the processes affecting the formation of these deposits; combined these data can be used for paleoreconstruction of peat-bogs. In this paper we characterize heavy mineral-rich sandy layers from two peat-bog sites in Mizerów and Strumień (Poland). In both cases, the most common identified mineral suite is: epidote, staurolite, tourmaline (dravite and schörl), garnet, spinel, Al2SiO5 polymorphs (sillimanite, kyanite, andalusite), amphibole (mainly hornblende), pyroxene (e.g., richterite, diopside), perovskite, topaz, cordierite, apatite, monazite, chromite, ilmenite, chlorite, iron oxides, rutile and siderite. This mineral suite is characteristic of a metamorphic aureole surrounding a magmatic body. Pyrite is likely authigenic in origin. Apatite and monazite were employed for U-Pb and CHIME dating, respectively. Based on the U-Pb age information composition and textural features of selected minerals, different provenance areas were indicated: the Tatra Massif, the Bohemian Massif, and the Silesian Basin area. Transport of the investigated mineral phases was linked to development of both the Odra (praOdra) and the Vistula valleys.

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