Hydrophysics of bogs. (Gidrofizika bolot). by V. V. Romanov

Cover of: Hydrophysics of bogs. | V. V. Romanov

Published by Israel Program for Scientific Translations [available from the U.S. Dept. of Commerce for Federal Scientific and Technical Information, Springfield, Va.] in Jerusalem .

Written in English

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Subjects:

  • Peat bogs.,
  • Hydrology.

Edition Notes

Bibliography: p. 237-248.

Book details

Statement[By] V. V. Romanov. Translated from Russian [by N. Kaner. Edited by Heimann]
Classifications
LC ClassificationsGB622 .R613
The Physical Object
Paginationviii, 299 p.
Number of Pages299
ID Numbers
Open LibraryOL5634937M
LC Control Number68062028

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Abstract. The hydrology of bog relicts differs from that in undisturbed bogs. The surface layers of these relicts mostly consist of moderately to strongly humified, secondary weathered peat as a result of drainage and Hydrophysics of bogs.

book by: Publishing History This is a chart to show the when this publisher published books. Along the X axis is time, and on the y axis is the count of editions published. Click here to skip the chart. Reset chart or continue zooming in.

This graph charts editions from this publisher over time. Summary. The main results of a long-term ecological study from to are presented. Aspects of vegetation dynamics and hydrology of a South German ombrogenous bog were analysed in different spatial scales and temporal periods.

Vegetation change from to was documented by Permanent plots and comparison of vegetation by:   The development of the acrotelm on two Irish Midland raised bogs, Raheenmore Bog and Clara Bog East, where drains were blocked in – is described.

The acrotelm of both bogs was surveyed in and before the blocking and again in late and earlywhen effects Hydrophysics of bogs.

book visually clear. Bogs may also form much thicker peat layers than fens, up to 7 m in the Netherlands and up to 20 m in some bogs in Canada. This is possible because bogs can in principle grow to unlimited heights above the original ground water table, which fens can not. Hydroponics and Greenhouse Gardening: 3-in-1 Gardening Book to Grow Vegetables, Herbs, and Fruit All-Year-Round (Urban Homesteading) by Richard Bray | out of 5 stars Paperback $ $ 00 $ $ Get it as soon as Tue, Dec 1.

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$ Free with Audible trial # This paper considers three topical problems—the definition of peat soils as natural-historical formations and the estimation of their profile thickness, the analysis of the genesis of organic soils, and the principles of the classification of peat soils.

Based on the experimental data of long-term studies, it was concluded that peat soils may include the whole peat layer and the upper.

Hydrophysics of Bogs. (Israel Programme for Scientific Translations, ) Publ. for US Dept of Agric. & NSF: pp., illustr.

Bogs and fens are, in a sense, hydrobiologic systems, and any evaluation of cumulative impacts will have to (1) consider the complicated and little understood interactions among wetland hydrology, water chemistry, and biota, and (2) place the effect of individual wetland impacts within the context of the cumulative impacts contributed to the watershed from other geomorphic areas and land uses.

ASTM Book of Standards, STP, vol. pp. 21 – Hydraulic conductivity. Basic Studies of Water-binding in Peat Hydrophysics of Bogs The trans-mission of water through peat: II. Field. The following article is from The Great Soviet Encyclopedia ().

It might be outdated or ideologically biased. Hydrophysics a branch of geophysics in which the physical processes taking place in the water envelope (hydrosphere) of the earth are studied.

Among the general problems covered by hydrophysics are the molecular structure of water in all. Hydrophysics of bogs. Monson Bindery Ltd., Jerusalem.

Schouwenaars, J.M., De Deurnese en Liesselse Peel; verslag van een onderzoek naar vegetatie en waterhuishouding. MSc-thesis, Dept. of Land and Water Use, Agric. Univ. Wageningen. COLOG’S hydrophysical and water well logging division offers clients the widest range of flow-logging capabilities of any downhole service provider.

These advanced hydrophysical evaluation methods and technologies allow for an entire aquifer to be tested as one working unit yielding sensitive and accurate assessments of the vertical distribution of flow, water quality, permeability and head. The behaviour of the water table in re-wetted bogs varies widely between different locations so that recolonising Sphagnum is vulnerable to water stress, especially when the water table is drawn down in summer.

It is important to understand how physical site conditions influence the occurrence of water stress so that adequate management measures may be applied. We report the results of continuous temperature monitoring ( days, from 28 June to 26 September ) in a 80 cm layer of peat soil in Bakchar bog (West Siberia), at sampling rates of 60 min in wintertime and 15 min in summertime.

Both annual and daily temperature patterns are controlled by water table position and weather conditions. Bog, type of wetland ecosystem characterized by wet, spongy, poorly drained peaty soil.

Bogs can be divided into three types: (1) typical bogs of cool regions, dominated by the growth of bog mosses, Sphagnum, and heaths, particularly Chamaedaphne (northern bogs with trees growing on them are often called muskegs); (2) fens, dominated by grasslike plants, grasses, sedges, and reeds; and (3 Missing: Hydrophysics.

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The author shows you in pictures, words, and even material lists for that matter on how to build each system individually and how to maintain it in good running s:   It appears that evaporation from a sphagnum bog could be reduced somewhat, making more water available for streamflow, by flooding the surface, or by lowering the water table to more than cm below the surface.

REFERENCES Bay, R.R., Evaluation of an evapotranspirometer for peat bogs. Water Resour. Res., 2: Bay, R.R., Book. Jan ; Atmospheric Environment Service; V.

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HUBBARD and YORAM RUBIN 1 Lawrence Berkeley National Laboratory, Earth Sciences Division, Berkeley, CA USA.

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Part B contains a comparison of the contents of the hydrological. Introduction. Mire and peatland ecosystems play a significant role in the global carbon cycle as they are sources or sinks of greenhouse gases (GHG), depending on how they are managed (Günther et al., ; Joosten et al., ; Leifeld et al., ; Rydin and Jeglum, ).Although, peatlands cover a small portion of the Earth's land surface (around 3%), they store about 20% of the global.

Raised mires are ecosystems in which waterlogged peat accumulates above the level of the surrounding stream system. It has been suggested that waterlogging is maintained by matric forces, but a. Hydrophysics of Bogs. Israel Program of Scientific Translations, Jerusalem, pp.

Methods for estimating the reliability of experimentally determined major hydrologic characteristics of bogs. (1) The hydrogeology of a spring-fen mound, water track, and raised bog in the remote Lost River peatland, northern Minnesota, was investigated by measurements of the groundwater levels and.

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Bogs are sometimes called quagmires (technically all bogs are quagmires while not all quagmires are necessarily bogs) and the soil which composes them is sometimes referred to as muskeg; alkaline mires are called fens rather than g: Hydrophysics.Look Inside.

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