DasT-P-Feld der Diagenese und niedrigtemperierten Metamorphose aufgrund von Mineralreaktionen     

Prof. Dr. Helmut G. F. Winkler 《Contributions to Mineralogy and Petrology》1964,10(1):70-93

It is attempted to determineT, P values for the lowgrade metamorphic facies. From geologic-petrographic observations and from experiments mineralreactions are outlined which characterize the zeolitic-, the glaucophane- and the greenschistfacies, respectively. Only such reactions are considered which are univariant if P_f=P_s; thus aP-T grid can be arrived at. Experimental data on the equilibria of the relevant reactions is taken from the literature and from own experiments. Experimental results are always checked against known field-observations. Contrary to current opinium, we arrive at rather higher temperatures for the beginning of the lowgrade metamorphic facies: Diagenesis. From sedimentation up to slightly below 300° C. Zeolitic facies. From slightly below 300° C up to about 400° C. Greenschistfacies. From about 400° C up to about 550° C. Glaucophaneschistfacies. Under pressures of at least 6–7 kb this facies begins somewhat above 300° C, probably at about 330° C, grading into high-pressure greenschistfacies.  相似文献   

Der orographische Einfluss der Alpen auf eine westliche Höhenströmung     

Helmut Pichler 《Pure and Applied Geophysics》1964,59(1):185-190

Zusammenfassung In der vorliegenden Arbeit wurde der orographische Einfluss der Alpen auf eine westliche Höhenströmung untersucht. Dabei hat sich herausgestellt, dass bei westlicher Anströmung des Alpenmassivs die Luftpartikelchen nach rechts abgelenkt werden. Durch einen Radiosondenvergleich zwischen Payerne und Zagreb in 500 mb konnte diese von der Theorie her aufgestellte Forderung bekräftigt werden.

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Summary The author investigates the orographic influence of the chain of the Alps on a westerly upper air stream. The theory shows that air particles are deflected to the right, if they come with a westerly stream of air. A comparison between the 500 mb winds of Payerne (Switzerland) and Zagreb (Yugoslavia) could confirm this theory.

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Diese Arbeit stellt den Beitrag FRP Alpenwetter Nr. 2/64 eines vom Österreichischen Forschungsrat subventionierten Forschungsvorhabens dar.  相似文献   

Land management impacts on runoff sources in small Amazon watersheds     

Joaquín Chaves  Christopher Neill  Sonja Germer  Sérgio Gouveia Neto  Alex Krusche  Helmut Elsenbeer 《水文研究》2008,22(12):1766-1775

Forest clearing and conversion to cattle pasture in the lowland Amazon region has been linked to soil compaction and increased soil water storage, which combine to diminish soil infiltration, enhance quick lateral flows and increase the stream flow response to precipitation. Quantifying the importance of quick surficial flow in response to this land use change requires identification of water sources within catchments that contribute to stream flow. Using an end member mixing analysis approach, potential contributing sources of stream flow were evaluated during an entire rainy season in a forest and a pasture watershed drained by ephemeral‐to‐intermittent streams in the south‐western Amazon. Water yield was 17% of precipitation in the pasture and 0·8% of precipitation in the forest. During the early rainy season, throughfall, groundwater, and soil water contributed 79%, 18%, and 3%, respectively, to total forest stream flow. Over the entire rainy season, throughfall, groundwater, and shallow soil water provided 57%, 24%, and 19%, respectively, of stream flow. In the pasture watershed, overland flow dominated stream flow both in the early (67%) and late (57%) rainy season, with a mean contribution of 60% overland flow, 35% groundwater, and 5% soil water. The uncertainty associated with those estimates was studied using a Monte Carlo approach. In addition to large changes in total surface flow, marked differences were found in the proportions of total stream flow in the second half of the rainy season between the forest and pasture watershed. These results suggest that (1) there is great potential for alteration of the hydrological budgets of larger watersheds as the proportion of deforested land in the Amazon increases, and (2) as more rainfall is diverted into fast flowpaths to streams in established pastures, the potential to deliver water with higher solute concentrations generated by erosion or by bypassing sites of solute removal increases. Copyright © 2007 John Wiley & Sons, Ltd.  相似文献   

Intracluster light and the extended stellar envelopes of cD galaxies: an analytical description     

Marc S. Seigar †  Alister W. Graham  Helmut Jerjen 《Monthly notices of the Royal Astronomical Society》2007,378(4):1575-1588

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Tying platform drowning to perturbations of the global carbon cycle with a δ¹³C_Org-curve from the Valanginian of DSDP Site 416     

Ulrich G. Wortmann  & Helmut Weissert 《地学学报》2000,12(6):289-294

The carbonate carbon isotope record of the Phanerozoic is marked by repeated high-amplitude excursions towards more positive values. Although the interpretation of C-isotope events remains controversial, they are regarded as a proxy of the global C-cycle. Using δ¹³C_Org-measurements of samples from DSDP Site 416, it is shown that a classic example of platform drowning coincided with the onset of the mid-Valanginian carbon-cycle excursion. Widespread carbonate platform drowning would have contributed to the observed positive shift in the C-isotope record. As choking of carbonate production was compensated by increased organic production, both processes favoured a shift in marine carbon partitioning from the oxidized to the reduced carbon reservoir. This would have resulted in an increased flux of CO₂ from the atmosphere into the marine and sedimentary carbon reservoir.  相似文献   

Korallenriffe—Bedrohungen,Schutzkonzepte und Rehabilitationsmaßnahmen     

Schuhmacher  Helmut 《Ocean Dynamics》1999,51(10):17-23

Ocean Dynamics - Korallenriffe sind der artenreichste Lebensraum im Meer und zugleich der wirkungsvollste Schutz tropischer Küsten. Die hermatypischen Organismen konvertieren durch die...  相似文献   

Climatic bisection of the last interglacial warm period in the Polar North Atlantic     

Henning A. Bauch  Evguenia S. Kandiano  Jan Helmke  Nils Andersen  Antoni Rosell-Mele  Helmut Erlenkeuser 《Quaternary Science Reviews》2011,30(15-16):1813-1818

New multiproxy marine data of the Eemian interglacial (MIS5e) from the Norwegian Sea manifest a cold event with near-glacial surface ocean summer temperatures (3–4 °C). This mid-Eemian cooling divided the otherwise relatively warm interglacial climate and was associated with widespread expansions of winter sea-ice and polar water masses due to changes in atmospheric circulation and ocean stability. While the data also verify a late rather than early last interglacial warm peak, which is in general disharmony with northern hemisphere insolation maximum and the regional climatic progression of the early Holocene, the cold event itself was likely instrumental for delaying the last interglacial climate development in the Polar North when compared with regions farther south. Such a ‘climatic decoupling’ of the Polar region may bear profound implications for the employment of Eemian conditions to help evaluate the present and future state of the Arctic cryosphere during a warming interglacial.  相似文献   

Book Review A Mathematical Approach by F. Cap     

Helmut Kirchner 《Pure and Applied Geophysics》2009,166(4):723-724

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The soil hydrologic response to forest regrowth: a case study from southwestern Amazonia     

Sarah Godsey  Helmut Elsenbeer 《水文研究》2002,16(7):1519-1522

As a large and dynamic land‐use category, tropical secondary forests may affect climate, soils, and hydrology in a manner different from primary forests or agricultural areas. We investigated the saturated hydraulic conductivity K_sat of a Kandiudult under different land uses in Rondonia, Brazil. We measured K_sat at four depths (12·5, 20, 30 and 50 cm) under (a) primary forest, (b) a former banana–cacao plantation (SF1), and (c) an abandoned pasture (SF2). At 12·5 cm, all three land uses differ significantly (α = 0·1), but not at the 20 and 30 cm depths. At 50 cm, K_sat was significantly greater in the former pasture than in other land uses. Lateral subsurface flow is expected during intense rainfall (about 30 times per year) at 30 cm depth in SF1 and at 50 cm depth in the forest, whereas the relatively low permeability at shallow 12·5 cm in the SF2 may result not only in lateral subsurface flow, but also saturation overland flow. For modelling purposes, recovering systems seem to have K_sat values distinct from primary forest at shallow depths, whereas at deeper layers (>20 cm) they may be considered similar to forests. Copyright © 2002 John Wiley & Sons, Ltd.  相似文献