ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Plant and soil 115 (1989), S. 43-52 
    ISSN: 1573-5036
    Keywords: adsorption ; ammonia volatilization ; basalt ; isotherm ; manure ; peat ; zeolite
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract The effectiveness of sphagnum peat, zeolite (clinoptilonite) and basalt in reducing ammonia losses during aerobic manure decomposition was determined in an incubation experiment. Peat placed in the spent air-stream adsorbed all of the ammonia volatilized during the first 8 days of decomposition, and reduced overall ammonia losses by 59%. Zeolite reduced total ammonia losses by 16%, and basalt by 6%. All adsorbents were considerably less effective in reducing ammonia losses when mixed with the manure. Reductions in ammonia losses of 24% and 1.5% were obtained with the peat and zeolite, respectively. The addition of basalt increased losses. Ammonia and ammonium adsorption isotherms were determined for the three materials. The adsorption capacities and affinity terms of the adsorbents calculated from the isotherms, reflected their ability to reduce ammonia losses in the incubation experiment. Zeolite had both the highest affinity for ammonium and the highest ammonium adsorption capacity. The peat had a very high affinity for ammonia and a high adsorption capacity (23.4 mg NH3−N g−1), whereas zeolite and basalt had a much lower adsorption capacity (1.8 and 0.05 mg NH3−N g−1, respectively) compared with their capacity to adsorb ammonium (18.1 and 0.18 mg NH4−N g−1).
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2024-02-13
    Description: bibliography
    Description: DFG, SUB Göttingen, DGMT
    Keywords: ddc:553.21 ; Moor ; Torf ; peat ; peatland ; Rezension
    Language: German
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 3
    Publication Date: 2024-03-06
    Description: Am Lago Argentino (Südpatagonien) wurden Moore entdeckt. Es erfolgte eine pflanzensoziologische Inventarisierung der rezenten Vegetation. Großrestuntersuchungen der Torfe ergaben Einblicke in die subfossile Vermoorung. Gegenwärtig werden die Moore von Kleinseggenrasen besiedelt, die auch in der Vergangenheit als torfbildende Vegetation vorhanden waren. Zusätzlich gab es moosreiche Quellfluren. Beide Pflanzengesellschaften haben mit der entsprechenden holarktischen Vegetation Übereinstimmungen.
    Description: At the Lago Argentino (South Patagonia) mires have been discovered. Plant associations have been examined. Macrofossil investigations produce the subfossil paludification. Mire are colonized by fine sedge associations. In the past there was the same peat forming vegetation. In addition there are spring pools with mosses. Both plant associations remind of the holarctic vegetation.
    Description: research
    Description: DFG, SUB Göttingen
    Keywords: ddc:553.21 ; ddc:581.7 ; Moor ; Torf ; Vegetation ; peatland ; peat
    Language: German
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Plant and soil 106 (1988), S. 65-72 
    ISSN: 1573-5036
    Keywords: actinorhiza ; Alnus glutinosa ; Alnus incana ; fine sand ; Frankia ; nitrogen fixation ; nodulation ; nodulation capacity ; peat ; persistence ; pH ; spore ; survival
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract Factors affecting the establishment of Alnus/Frankia symbioses were studied partly by following the survival ofFrankia strains exposed to different soil conditions, and partly by investigating the effect of pH on nodulation. TwoFrankia strains were used, both of the Sp− type (sporangia not formed in nodules). One of the strains sporulated heavily, while the other formed mainly hyphae. The strains originated fromAlnus incana root nodules growing in soils of pH 3.5 and 5.0. The optimum pH for their growth in pure culture was found to be 6.7 and 6.2, respectively. The strains were introduced into twoFrankia-free soils, peat and fine sand. Their survival, measured as the persistance of nodulation capacity using the plant infection technique, was followed for 14 months. The survival curves of the strains were similar despite the morphological differences between the strains in pure culture. The nodulation capacities declined over time both at 14 and 22°C. Survival was better in soils limed to a pH above 6 than in soils at their original pH (peat 2.9, fine sand 4.2). The effect of pH on nodule formation in Alnus seedlings by theFrankia strains was studied in liquid culture. The number of nodules increased linearly within the pH range studied (3.5–5.8). No nodules were formed at pH 3.5.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Plant and soil 108 (1988), S. 253-261 
    ISSN: 1573-5036
    Keywords: Cu-deficiency ; Histosols ; nutrients ; peat ; reclamation
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract Legislation is being considered in Minnesota to broaden existing strip-mine reclamation laws to include the expanding peat harvesting industry, but the lack of information on plant-residual organic soil relationships will make compliance with such guidelines difficult. A greenhouse study was established to provide basic information on three representative residual organic soils and their capacity to support Scotch pine, black spruce, Norway spruce, and white spruce seedlings under different fertilizer regimes. The nature of the residual soil, the species grown upon it, the amount and type of fertilizer added, and the interactions between these factors significantly affected seedling growth, emphasizing the importance of treating each mined site as an individual case. Poor growth on a Fibrist was attributed to soil acidity, with added fertilizer further reducing growth. Seedling performance was excellent on a Hemist, particularly when fertilized with micronutrients and a high rate of NPK. A strong relationship was identified between spruce growth and foliar Cu levels, and a critical value of 3.7 μg g−1 was estimated for spruce on this Cu-deficient soil. Seedling performance was satisfactory on a Saprist, with all species responding to low rates of NPK and some to high rates of NPK plus micronutrients. The non-factorial arrangement of the fertilizer treatments made it difficult to determine which element or elements were limiting on this soil. The results of soil chemical analyses could be used to make general statements on the relative fertility of the residual soils. However, they could not be used to make statements on the availability of specific nutrients.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 6
    ISSN: 1573-5036
    Keywords: acid brown earth ; Alnus glutinosa ; Alnus rubra ; Frankia ; nitrogen fixation ; nodule ; peat
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract The effects of soil type (an acid peat and 2 acid brown earths) andFrankia source (3 spore-positive crushed nodule inocula and spore-negative crushed nodules containing the singleFrankia ArI5) on nodulation, N content and growth ofAlnus glutinosa andA. rubra were determined in a glasshouse pot experiment of two years duration. Plants on all soils required additional P for growth. Growth of both species was very poor on peat withA. glutinosa superior toA. rubra. The former species was also superior toA. rubra on an acid brown earth with low pH and low P content. Some plant-inoculum combinations were of notable effectivity on particular soils but soil type was the major source of variation in plant weight. Inoculation with crushed nodules containingFrankia ArI5 only gave poor infection of the host plant, suggesting that inoculation with locally-collected crushed nodules can be a preferred alternative to inoculation withFrankia isolates of untested effectivity. Evidence of adaptation ofFrankia to particular soils was obtained. Thus, while the growth of all strains was stimulated by mineral soil extracts, inhibitory effects of peat extracts were more apparent with isolates from nodules from mineral soils than from peat, suggesting that survival ofFrankia on peat may be improved by strain selection.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 7
    Publication Date: 2024-02-28
    Description: Der 8 . Internationale Torfkongreß fand vom 14. - 21. August 1988 in Leningrad statt. Es war eine "Jubiläumstagung", denn bereits vor 25 Jahren entzückte die berühmte und ehemalige Metropole Peter des Großen zahlreiche Torffachleute aus aller Welt. Wenn nicht alle Veranstaltungen und Vorträge der Tagung immer gut besucht waren, so ist das unter anderem auch auf das Bedürfnis vieler Teilnehmer zurückzuführen, die zahllosen Schönheiten dieser Stadt kennenzulernen. Alle Stadtrundfahrten, Besichtigungen und Damentouren waren ausgebucht!
    Description: conference
    Description: DFG, SUB Göttingen
    Keywords: ddc:553.21 ; Moor ; Torf ; peat ; peatland ; Tagungsbericht ; conference report
    Language: German
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 8
    facet.materialart.
    Unknown
    In:  Herausgeberexemplar
    Publication Date: 2024-03-06
    Description: Die Sanierung der hypertrophierten, zunehmend verschlammenden Flachseen gelingt nur, wenn die verschiedenen Quellen des Nährstoffeintrags eingegrenzt werden können. Niedermoore sind während ihrer Entstehung durch Verlandung und/oder Versumpfung eine Falle (sink) für die im Torf akkumulierten Nährstoffe. Mit zunehmender Entwässerung und Nutzungsintensität werden die Torfe jedoch zur Quelle (source)von remineralisierten Nährstoffen. Es wird über die freisetzbaren Mengen an NO3-N und PO4-P unter Bezug auf langjährige Feldversuche des Bodentechnologischen Institutes Bremen berichtet. Bei intensiver landwirtschaftlicher Nutzung der Niedermoorböden werden mehr Nährstoffe freigesetzt als auch durch die Dauerkultur Grünland jährlich entzogen werden können. Bei relativ geringer Nitrat- und Phosphatauswaschung wird die Bedeutung der N-Inkorporierung bei der Humifizierung und der Denitrifizierung bei der Zersetzung der Torfe diskutiert. Der P-Austrag aus Niedermoorböden in das Grundwasser ist ähnlich niedrig wie aus Mineralböden. Hier gilt es vor allem die Verlagerung in die Oberflächengewässer durch Erosion zu vermeiden. Eine Torfsubstanz schonende Wirtschaftsweise ist eine Boden- und Gewässerschutzmaßnahme. Sie verlangt eine begrenzte Nutzungsintensität.
    Description: The rehabilitation of hypertrophied shallow lakes in which more and more sludge accumulates will be successful only if the nutrient input from different sources might be reduced. During their formation by sedimentation and subsequent peat formation or peat formation on paludified soils fens are a sink for nutrient accumulating in the peat. Due to increasing drainage and intense farming they become however a source of remineralized nutrients. Based on long-term trials of the Institute for Soil Technology Bremen an account is given of the remineralizable quantities of NO3-N and PO4-P. More nutrients are mineralized by intense agricultural use of fen soils than might be withdrawn annually even by permanent grassland. Considering the relatively low leaching of nitrate and phosphate the importance of N-incorporation during humification as well as the denitrification during peat decomposition is discussed. The P-leaching from fen soils into the ground water is similarly low as in mineral soils. The main task is above all to avoid a transfer into surface waters by erosion. Soil and water conservation means conservation of the peat substance. This demands a restricted intensity of land use.
    Description: research
    Description: DFG, SUB Göttingen
    Keywords: ddc:553.21 ; ddc:631.4 ; Bodenkunde ; Moor ; Torf ; soil ; peatland ; peat
    Language: German
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 9
    ISSN: 1573-5095
    Keywords: medium porosity ; mineral wool ; peat ; perlite ; plant dry weight ; plant stem length ; standardized time method
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract Effects of growth medium physical conditions were studied. Peat and two series of peat mixed with hydrophobic mineral wool or perlite in three mixing ratios were prepared. Growth media porosities were characterized by the “standardized time method” and seedling development by measurements of stem length and fresh and dry weight. Seedlings grown in media containing mineral wool showed less mortality, were larger and had more living root apices than seedlings in media lacking mineral wool. Growth media influenced most the stem length and dry weights and was best at higher porosity. The difference between mineral wool and perlite amendments was greater for dry weight than stem length, although the effect of mixing ratio was observed for mineral wool only. The media induced qualitative differences in shoots (foliage spiralling) and roots (branching, number of living root apices, lenticel intumescence).
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 10
    Publication Date: 2024-02-12
    Description: Zur Wiedervernässung von Hochmooren wird ein Staukörper aus gewachsenem Hochmoortorf gefordert. Mit repräsentativen Werten der gesättigten Wasserdurchlässigkeit wurden für statische Bedingungen Berechnungen der Sickerwasserverluste in Abhängigkeit unterschiedlicher Staukörpermächtigkeiten vorgenommen. Folgende Ergebnisse lassen sich aus diesen Modellen ableiten: 1. Staukörpermächtigkeiten 〉 0,5 m reduzieren die Sickerwasserverluste nur noch unwesentlich. 2. Erst Humositätsgrade H ≥ 7 nach v. POST bewirken ausreichenden Wasserstau. 3. Schrumpfrisse im ausgetrockneten Staukörper aus stark zersetztem Hochmoortorf können die Stauwirkung beeinträchtigen. Eine Staukörpermächtigkeit von 0.5 m sollte daher nicht unterschritten werden. Als Verdunstungsschutz werden mindestens 0,3 m Bunkerde bzw. Weißtorf über dem Staukörper gefordert. 4. Unter klimatisch ungünstigen Bedingungen ist ein Grundwasseranschluß des Staukörpers erforderlich.
    Description: Rewetting requires an impermeable layer of undisturbed raised-bog peat. For static conditions calculations of seepage dependent on the thickness of the impermeable layer have been carried out by means of representative data of saturated water permeability. The results of these model calculations are: 1. An increase of the impermeable ayer over 0,5 m insignificantly reduces the seepage. 2. Only a degree of decomposition H 2:7 according to v. POST causes a sufficient water rise. 3. An impermeable layer of highly decomposed raised-bog peat can be destroyed by crack formation after drying up. Therefore, the thickness of this layer should not be less than 0,5 m. A top spit or white peat layer of at least 0,3 m is required to prevent evaporation. 4. Under unfavourable climatic conditions contact of the impermeable layer with the ground water is necessary.
    Description: research
    Description: DFG, SUB Göttingen
    Keywords: ddc:553.21 ; Moor ; Torf ; peat ; peatland ; Wiedervernässung
    Language: German
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 11
    Publication Date: 2024-03-06
    Description: Jeweils zwischen den IMTG-Kongressen finden Kommissionssitzungen mit fachlichen Schwerpunktthemen statt. Aufgabe der Kommission III ist es, regionale Probleme der Kultivierung und Nutzung der verschiedenen Moorböden durch Landwirtschaft, Forstwirtschaft und Gartenbau zu behandeln. Bereits 1974 hatte ein solches erfolgreiches Internationales Moorsymposium am gleichen Ort unter dem Leitthema "Probleme der Wasserregulierung auf Niedermoor" stattgefunden. Darüber hat W. BADEN in der Zeitschrift für Kulturtechnik und Flurbereinigung 16, 110-123, 1975, eine Nachlese veröffentlicht. [...]
    Description: conference
    Description: DFG, SUB Göttingen
    Keywords: ddc:553.21 ; ddc:333.7313 ; ddc:631.4 ; Moor ; Torf ; Bodenkunde ; Landnutzung ; Landwirtschaft ; peat ; peatland ; soil ; land use ; agriculture
    Language: German
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 12
    facet.materialart.
    Unknown
    In:  SUB Göttingen | ZA 34278
    Publication Date: 2024-03-06
    Description: Es wird über 5 Jahrzehnte Erfahrungen mit deutschem Sandmischkulturboden − einem anthropogenen Bodentyp − berichtet. Aus dem Ertragsverlauf werden die bodenbildenden Prozesse − Setzung, Homogenisierung, Humifizierung − deutlich. Der jeweilige Grad der Bodenentwicklung − von der rohen Mischung aus Torf und Sand zum ± humosen Sand − kann durch bodenchemische Untersuchungen z.B. Schweretrennung in CCl4‚C/N-Verhältnis‚ N-Fraktionierung, aktuelle/potentielle KAK dargestellt werden. Solche Untersuchungen können der objektiven Bewertung von Neukulturen und zur Steuerung ihrer Bodenentwicklung dienen.
    Description: It is reported on experiences with German sand-mix-culture soils within 50 years. The soil-forming processes − subsidence, homogenization, humification − are correlated with the development of the yields. The corresponding degrees of soil development − from a rough mixture of peat and sand to a ± humic sandy soil − can be shown by soil-chemical analyses like separation of particles with different densities in CCl4, C/N-ratio, N-fractionation, actual/potential CEC. Such investigations can be useful for the actual estimation of new cultures and the control of their development.
    Description: research
    Description: DFG, SUB Göttingen
    Keywords: ddc:553.21 ; ddc:631.4 ; Moor ; Torf ; Bodenkunde ; peatland ; peat ; soil
    Language: German
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 13
    Publication Date: 2024-03-06
    Description: In den Sanduntergrund einschneidende Entwässerungsgräben behindern eine Wiedervernässung von teilabgetorften Hochmooren. In Modellversuchen wurden verschiedene Materialien (Schwarztorf, Bunkerde, Bentonit) auf ihre Eignung als Material zur Grabenabdichtung überprüft. Dabei wurden verschiedene Abdichtungsprozesse - Verdichtung des Abdichtmaterials, - SenkundäreAbdichtumgdes Sanduntergrundes durch infiltriertes Material (mechanische Filterwirkung) untersucht. In den Modellversuchen erwiesen sich die Varianten "Schwarztorf, verdichtet" und "Sand/Bentonit-Gemisch" als praktikable Verfahren zur Grabenabdichtung. Sekundäre Abdichtungsprozesse konnten bei einigen Materialien (Schwarztorf-Suspension; Bunkerde) beobachtet werden, sie erwiesen sich bei kurzfristiger Betrachtung (10 Jahre) jedoch als zu uneffektiv.
    Description: Ditches cut into the sandy subsoil impede a rewetting of cutover peatlands. Different materials (black peat, top spit, bentonite)were tested for their suitability of sealing these ditches. Different sealing processes were examined - compaction of the material, - secondary sealing of the sandy subsoil by clogging with infiltrated material. The treatments "black peat-compacted" and "sand/bentonite-mixture"showed the best sealing properties. Secondary sealing by mechanical filtering was also observed for some other materials ("black peat-suspension", "top spit"), however the process of mechanical filtering is too ineffective in the short-term view (~10 years).
    Description: research
    Description: DFG, SUB Göttingen
    Keywords: ddc:553.21 ; ddc:333.72 ; Moor ; Torf ; Naturschutz ; Wiedervernässung ; peatland ; peat ; nature conservation
    Language: German
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 14
    Electronic Resource
    Electronic Resource
    Springer
    Biogeochemistry 1 (1985), S. 277-302 
    ISSN: 1573-515X
    Keywords: Appalachian mountains ; biogeochemistry ; peat ; Sphagnum ; water chemistry ; West Virginia ; wetlands
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences
    Notes: Abstract At Big Run Bog, aSphagnum-dominated peatland in the unglaciated Appalachian Plateau of West Virginia, significant spatial variation in the physical and chemical properties of the peat and in surface and subsurface (30 cm deep) water chemistry was characterized. The top 40 cm of organic peat at Big Run Bog had average values for bulk density of 0.09 g · cm−3, organic matter concentration of 77%, and volumetric water content of 88%. Changes in physical and chemical properties within the peat column as a function of depth contributed to different patterns of seasonal variation in the chemistry of surface and subsurface waters. Seasonal variation in water chemistry was related to temporal changes in plant uptake, organic matter decomposition and element mineralization, and to varying redox conditions associated with fluctuating water table levels. On the average, total Ca, Mg, and N concentrations in Big Run Bog peat were 33, 15, and 1050 μmol · g−1, respectively; exchangeable Ca and Mg concentrations were 45 and 14 μeq · g−1 , respectively. Surface water pH averaged 4.0 and Ca++ concentrations were less than 50 μeq · L−1 . These chemical variables have all been used to distinguish bogs from fens. Physiographically, Big Run Bog is a minerotrophic fen because it receives inputs of water from the surrounding forested upland areas of its watershed. However, chemically, Big Run Bog is more similar to true ombrotrophic bogs than to minerotrophic fens.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...