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3 edition of On the distribution of bogs and bog soils over the northwestern lake region of the USSR found in the catalog.

On the distribution of bogs and bog soils over the northwestern lake region of the USSR

L. I. Prasolov

On the distribution of bogs and bog soils over the northwestern lake region of the USSR

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Published by Academy of Sciences of the USSR in Leningrad .
Written in English


Edition Notes

StatementL.I. Prasolov.
Classifications
LC ClassificationsMLCS 84/00229 (Q)
The Physical Object
Pagination5 p., [1] folded leaf of plates : ill. ; 22 cm.
Number of Pages22
ID Numbers
Open LibraryOL2911513M
LC Control Number84142505

The Ahveninen Lake receives runoff from the mineral soil catchment, in the direction of the water flow path from the catchment towards the aapa mire (Figs 1 and 2). The small but relatively deep (5 m) lake lacks any outlet stream and it is bordered by an excentric bog dome, which does not have any minerotrophic vegetation.


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On the distribution of bogs and bog soils over the northwestern lake region of the USSR by L. I. Prasolov Download PDF EPUB FB2

On the Distribution of Bogs and Bog Soils over the Northwestern Lake region of the USSR + 1 map: Author(s) Prasolov, L. Publisher: Leningrad: The Academy of Sciences of the USSR: Publication year: Description: 4 p. Series title: Second International Soil Science Congress: Notes: Library holding:SU show all notes.

Within the Northern Lake States Forest and Forage Region (NLSFFR) are 17 Major Land Resource Areas (MLRAs), each of which is fairly internally homogeneous with respect to soils, landforms and land use (Fig.

).The focus of this chapter is on the characteristics, distribution, classification, and genesis of soils within the NLSFFR, as well as on issues related to management and land : Randall J. Schaetzl. In this relatively dry region, raised bogs preferentially develop over regional discharge zones for groundwater that upwells into the deeper portion of the peat profile.

During wet years, water-table mounds under the bogs drive flow downward into the deeper peat and deflect the upwelling groundwater laterally to the bog margins (Fig. ).Cited by: 5.

The total area of peatlands covers % of the entire territory and raised bogs occupy more than 41% of the peatlands. At present, about 9% of Latvia's raised bogs (ab ha) are affected. In contrast, a recent floristic study of known and potential bog turtle fens in the Lake Ontario coastal plain in New York found few plant species in common among occupied habitats and few plant.

bog massif varies over a signi cant range, soils and bogs as well as pollution control facilities and. the V asyugan peat-bog region of Western Siberia. Glebov, F.Z. Some tasks for forest bog investigations due to the peculiarities of forest and bog interaction in west Siberia, pp.

6–18 in Theory and Practice of Forest Bog Science and Hydroforest Amelioration, Institute of Forests and Timber, Krasnoyarsk, Russia. Trans-Palaearctic distribution: Austria (boggy areas in mountains, –m in Alps), Netherlands (sandy area with lake [“fen”] surrounded by forest), Byelorussia (boggy forests), Russia (northwestern Murmansk region; and Siberia - northern taiga, Kamchatka - boggy forests with lakes).

In Czech Republic, only from an upland peatbog. All Saints Bog is an approximately ha raised bog in County Offaly that is located 8 km north-northwest of Birr (7° 59′ W, 53° 9′ N; Figures and ; Valverde et al., ).The bog is a Special Area of Conservation (SACEC Habitats Directive (92/43/EEC) as amended).

The high bog has ha (%) that is currently classified as active raised bog and ha (%. Podzolic soils covered approximately 60% of the study area and according to Sanborn et al.

() Podzolic soils occupy over 14% of Canada and occur in two distinct areas, eastern Canada. The central part of the peat bogs is characterized by open-bog plain of stunted, thin trees (3–4 m high and bogs. Classification of organic soils Over the years many wetland and peatland classification schemes have evolved, each suited to a particular range of physiographic and climatic regimes.

Some of the criteria which have been used to classify organic soils are shown in Table   One split was pulverized in a tungsten carbide ring mill for min- utes. The second was hand-ground with a porcelain mortar and pestle and then ashed in a muffle furnace at C.

Analysis Soils, sediments and bogs Soils, stream sediments, moss mats, bank soils and bog samples were ana- lyzed at Acme Analytical Laboratories, Vancouver. A registry of productive peat bogs in the lake region. Hemispherics Polar Stud the proportional clay content of the soil was related to the distribution of patches.

at monthly intervals. Abstract. An ecological overview of seven years investigation of Braconidae, a family of parasitoid wasps (Hymenoptera: Ichneumonoidea) and a tyrpho-classifica.

This chapter reviews the literature on the ecology and geography of mires and their vegetation in the former Soviet Union.

In the “Introduction” mires are defined and the types of mire systems included in the review are described. In the first section mire classification systems are discussed with an emphasis on physiognomic, phytogeographical and multilevel systems of. The Western Siberian Lowlands (WSL) store a substantial amount of the global terrestrial carbon pool in widespread organic peat soils (Sheng et alSmith et al ).Soil carbon is largely immobilized by permafrost, but rising global air temperature is causing substantial thawing of permafrost, which is expected to have implications for carbon mineralization and release from peatlands.

The peat industry distinguishes four types of peat bogs: low-moor, transitional, high-moor, and mixed. The type of peat bog is the primary unit of classification (Figure 1).

Twenty-five primary types of peat bogs are distinguished in the European USSR and 32 in Western Siberia. Peat deposits. Search the history of over billion web pages on the Internet.

search Search the Wayback Machine. Featured texts All Books All Texts latest This Just In Smithsonian Libraries FEDLINK (US) Genealogy Lincoln Collection Full text of "The bogs and bog flora of the Huron River Valley.". The terms “bog” and “mire” were explicitly linked in scientific usage by Tansley and Godwin to the presence of a peat soil and with peat-forming y formally assigned the term “fen” to those peat-forming habitats which ranged from somewhat alkaline to moderately acid conditions as a result of their solute supply and assigned the term “bog” to habitats which were.

Large areas in Northern Russia are covered by extensive mires, which represent a complex mosaic of ombrotrophic raised bogs, minerotrophic and eutrophic fens, all in a close proximity to each other. In this paper, we compared microbial diversity patterns in the surface peat layers of the neighbouring raised bogs and eutrophic fens that are located within two geographically remote mire sites in.

Sustained by inputs of upstream lake exports, groundwater discharge (Hayashi et al ), as well as contributions from bogs connected directly, partially or seasonally, the channel fen water level remained effectively unchanged over the period (figure 3(b)), with a non-significant (p = ) decrease of 38 mm (table 1).

The main river in Ireland is the River Shannon. km ( mi) The longest river in Ireland, it separates the midlands of Ireland from the west of the river develops into three lakes along its course, Lough Allen, Lough Ree, and Lough these, Lough Derg is the largest.

The River Shannon enters the Atlantic Ocean in Limerick city in the Shannon Estuary. Mean soil organic carbon stocks by soil material for various successional stages (Yng =young, Int =intermediate, DL =drained lake) within four soil landscapes. Totals are for 0–2 m interval, except peaty–silty lowlands, which are for soils of variable depth above a common limnic horizon created after thaw-lake drainage.

The desert region in northwestern China exhibited the lowest Hg concentrations in soil because of the barren soils. In the western United States, the soil Hg distribution is strongly linked to vegetation greenness with the same order of Hg levels in land cover as that in China, and forested land had more than times higher soil Hg levels.

We evaluate soil carbon stocks and turnover rates, and the relationship between soil carbon loss with soil temperature and moisture, from an ensemble of eleven global land surface models. We focus on the region of NASA’s Arctic-Boreal vulnerability experiment (ABoVE) in North America to inform data collection and model development efforts.

Norway is a country located in Northern Europe on the northern and western parts of the Scandinavian majority of the country borders water, including the Skagerrak inlet to the south, the North Sea to the southwest, the North Atlantic Ocean (Norwegian Sea) to the west, and the Barents Sea to the north.

It has a land border with Sweden to the east and a shorter border with Finland. Climate warming, increased precipitation, and permafrost thaw in the Arctic are accompanied by an increase in the frequency of full or partial drainage of thermokarst lakes.

After lake drainage, highly productive plant communities on nutrient-rich sediments may develop, thus increasing the influencing greening trends of Arctic tundra. However, the magnitude and extent of this process remain. Mineral Soil Bog Construction. This document is available for download as a pdf here.

Regulatory restrictions on development of new cranberry bogs in wetlands have resulted in a limitation on the sites where bogs may be constructed. This lowland bog vegetation type is most frequently found on raised bogs although it can be found on intermediate bogs and where blanket bog extend over saddles and deep depressions (see ).

Which of the following soils would you find associated with a peat bog. histosol. Which of the following soils would you find associated with the extensive grasslands of the Prairies. _____ are soils in which more than half of the parent mineral matter is volcanic ash.

This soil has a high carbon content so appears very dark in color. Andisols. Testate amoebae assemblages were investigated in the peat deposits of the floodplain terrace swamp located in the southern taiga subzone of Western Siberia.

It was revealed that tests of amoebae were well preserved in the minerotrophic peat. Variations in the structure of assemblages show that these bioindicators are sensitive to changes in the environment.

Drain Lake in Nova Scotia was previously described as a highly acidic (pH ) but eutrophic lake. Drain Lake is fishless but it has large populations of aquatic invertebrates and plants.

This habitat allows black ducks and ring-necked ducks to be more productive than is typical for lakes in the region (Kerekes et al., ).

Bogdanovskaya-Gienef I. Distribution of certain types of sphagnum mosses in Polistovsky bogs // Botanical Journal of the USSR. Vol. Iss. Bogdanovskaya-Gienef I. Stratigraphy of the Polisto-Lovatsky raised bog massif // Nature of the bogs and methods of their research.

Leningrad. A zone near the soil surface that is more or less cemented by secondary carbonates of calcium or magnesium precipitated from the soil solution. It may occur as a soft, thin soil horizon, a hard, thick bed, or a layer exposed by erosion.

calyptra: In mosses and liverworts, a thin hood fitting over the top of the spore capsule. capsule. Figure shows a map of the distribution of the most extensive terrestrial biomes. The distribution of biomes is determined by environmental conditions, which must be appropriate to support the dominant species.

Moisture and temperature are usually the most important environmental influences on the distribution of terrestrial biomes (Figure ). Print a read and math workbook with Bogs reading comprehension.

You need to use this workbook in your classroom. Great mix of reading and math. Yost Bog was the only site where subfossils of Polytrichum strictum were recovered.

The occurrence of P. strictum in the upper layers of the bog peat suggests xeric conditions at least on the tops of Sphagnum hummocks. The species is still common on the tops of hummocks in Yost Bog and other leatherleaf bogs. Such soils are widespread in the region.

They occur as stabilized dune sand on modern or ancient lake shores, and as glacial outwash, plains. The pines on these sites usually are widely space, the ground being covered with a thin mat of moss, reindeer lichen, and trailing heaths — much as in the parklike spruce forests described above.

On Wednesday, 12th of July, there was conference excursion to Melnais Lake Mire Nature Reserve, which is one of the LIFE project’s Raised Bogs () sites. During the project, the active raised bog habitats and natural hydrology were re-established.

Volume 2, No. 3, / Some aspects of the problem of geochemical methods of prospecting for concealed mineralization; Distribution of uranium in the crust of the northwestern Canadian Shield as shown by lake-sediment analysis; The geochemistry of arsenic and its use as an indicator element in geochemical prospecting, $ Kostomukshsky Zapovednik Facts: Animals • Vegetation • Geographical Features • Conservation Status • References.

Animals. Leaping over fallen logs in a remote conifer forest of Kostomukshsky Zapovednik, hungry wolves (Canis lupus) trail close behind a small herd of vigorous forest-dwelling reindeer (Rangifer tarandus fennicus), waiting for a young or weak animal to fall behind.GENERAL DISTRIBUTION: Lingonberry is a circumpolar, circumboreal species that occurs throughout parts of North America, Eurasia, and Japan [,].The New World subspecies (ssp.

minus) extends from northwestern Greenland across the Canadian Arctic southward to New England [].It grows westward to the Great Lakes and British Columbia and reaches islands in the Bering Sea [42,].