Transforming mylonitic metagranite by open-system interactions during melt flow   总被引：3，自引：2，他引：1  

P. HASALOVÁ  P. &#;TÍPSKÁ  R. POWELL  K. SCHULMANN  V. JANOU&#;EK  O. LEXA 《Journal of Metamorphic Geology》2008,26(1):55-80

Gneisses and migmatites of the Gföhl unit (Moldanubian Zone, Bohemian Massif) range from banded mylonitic orthogneiss with recrystallized monomineralic bands, through stromatic (metatexite) and schlieren (inhomogeneous diatexite) migmatite, to isotropic nebulite (homogeneous diatexite). This sequence was classically attributed to increasing degree of anatexis. Under the microscope, the evolution is characterized by progressive destruction of the monomineralic banding that characterizes the original mylonitic orthogneiss. Throughout, the mineral assemblage is biotite–K‐feldspar–plagioclase–quartz ± garnet ± sillimanite, but the mineral compositions exhibit systematic changes with progressive disintegration of the layering. From banded orthogneiss to nebulite, the garnet composition changes systematically, Alm_75→94Prp_17→0.8Grs_2.5→1.2Sps_2→11 and X_Fe = 0.45→0.99 and for biotite, X_Fe = 0.80→1. This is consistent with a decrease in equilibration temperature and pressure of 790 °C and 8.5–6 kbar, to 690 °C and 5–4 kbar respectively. There is also a systematic change of whole‐rock composition, marked by an increase in SiO₂ (71→77 wt%) and X_Fe (0.62→0.85) and by a decrease in Al₂O₃ (16→13 wt%) and CaO (1.50→0.43 wt%). Assuming that the rocks started with the same composition, these systematic changes indicate open‐system behaviour. The predicted consequences of various open‐system processes are assessed using thermodynamic modelling. The observed variations are interpreted as being a consequence of melt flow through, and interaction with the rocks, and, to change the rock composition sufficiently, a large volume of melt must have been involved.  相似文献   

Size of wild and hatchery-reared Atlantic salmon populations in the northern Baltic Sea estimated by a stratified mark-recapture method     

Siira  Antti; Suuronen  Petri; Kreivi  Petri; Erkinaro  Jaakko 《ICES Journal of Marine Science》2006,63(8):1477-1487

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Hydrogen isotope fractionation factors between hydrous minerals and ore fluids at low temperatures: evidence from the Granny Smith gold deposit,Western Australia     

V. J. Ojala  D. I. Groves  J. R. Ridley 《Mineralium Deposita》1995,30(3-4):328-331

There are no reported experimental data on hydrogen isotope fractionation between muscovite and water at low temperatures (< 400 °C). A fractionation curve derived from extrapolation of the high temperature calibration of Suzuoki and Epstein (1976) yields 20 to 40%. higher D values than the empirical graphical calibration of Bowers and Taylor (1985) at temperatures of about 300 °C. Data from natural hydrothermal systems formed at approximately 300 °C, where D analyses are available both from fluid inclusions and alteration muscovite/sericite, support the Bowers and Taylor (1985) calibration, thus indicating smaller fractionation factors at these temperatures than suggested by extrapolations from high-temperature experimental results.  相似文献   

Spatial variability of turbulent fluxes and roughness lengths in HAPEX-MOBILHY     

L. Mahrt  M. EK 《Boundary-Layer Meteorology》1993,65(4):381-400

Surface-based and aircraft measured fluxes over the heterogeneous surface in HAPEX-MOBILHY are analyzed for the ten flight days when cloud cover above the boundary layer was minimal. The fair-weather climatology of the spatial variation of surface fluxes is estimated to provide an assessment of the generality of previous case studies appearing in the literature. For the 10-day averages, greater heating over the forest generates a forest breeze which leads to rising motion and a modest increase of boundary-layer cloud cover at the forest edge. The exchange coefficients and effective roughness lengths are computed for local averages (15 km scale) and for regional averages (100 km scale) intended to represent a range of grid sizes in numerical models of the atmosphere. The effective roughness length for momentum over the mixed agricultural region for both scales is on the order of 1 m, apparently due to bluff roughness effects associated with scattered trees, edges of small woods and other obstacles. This roughness length value is an order of magnitude larger than values used in numerical models for the same region, which are based on the dominant vegetation type. The spatially varying effective roughness length for heat is computed for use in those models which use surface radiation temperature to estimate surface heat flux. The effective roughness lengths for heat are found to be smaller than those typically used in numerical models of the atmosphere.  相似文献   

Bayesian logistic regression for presence-only data     

Fabio Divino  Natalia Golini  Giovanna Jona Lasinio  Antti Penttinen 《Stochastic Environmental Research and Risk Assessment (SERRA)》2015,29(6):1721-1736

Presence-only data are referred to situations in which a censoring mechanism acts on a binary response which can be partially observed only with respect to one outcome, usually denoting the presence of an attribute of interest. A typical example is the recording of species presence in ecological surveys. In this work a Bayesian approach to the analysis of presence-only data based on a two levels scheme is presented. A probability law and a case-control design are combined to handle the double source of uncertainty: one due to censoring and the other one due to sampling. In the paper, through the use of a stratified sampling design with non-overlapping strata, a new formulation of the logistic model for presence-only data is proposed. In particular, the logistic regression with linear predictor is considered. Estimation is carried out with a new Markov Chain Monte Carlo algorithm with data augmentation, which does not require the a priori knowledge of the population prevalence. The performance of the new algorithm is validated by means of extensive simulation experiments using three scenarios and comparison with optimal benchmarks. An application to data existing in literature is reported in order to discuss the model behaviour in real world situations together with the results of an original study on termites occurrences data.  相似文献   

Comparative varve counting and magnetic properties of the 8400-yr sequence of an annually laminated sediment in Lake Valkiajärvi, Central Finland     

Antti E.K. Ojala  Matti Saarnisto 《Journal of Paleolimnology》1999,22(4):335-348

Two varve counts made nearly 20 yrs apart and by different authors in the small and well sheltered meromictic lake of Valkiajärvi were compared with a view to establishing how similar, or otherwise, these two independent varve chronologies might be. The results were significant, the difference between the two varve counts being less than 2% for most of the sediment length, even though the average varve thickness was only 0.3 mm. The continuous and essentially uniform varve record - so far the longest in Finland - covers 8400 yrs and could be applied for accurate dating of palaeoenvironmental indicators in the sediment. As an example, we present a varve-dated pollen diagram for Lake Valkiajärvi.In addition, some magnetic parameters (susceptibility, ARM, SIRM) were measured on the sediment sequence to support the stratigraphic division and correlation of the cores, and to outline the development of the basin since the last deglaciation. Magnetic variables reflected mainly the variation in minerogenic material in the sediment, and were therefore related to changes in the catchment. The magnetic parameters also showed a drastic change some 6000 yrs ago, the reason for which, unfortunately, is still not fully understood.  相似文献   

Modelling effects of spatial variability of saturated hydraulic conductivity on autocorrelated overland flow data: linear mixed model approach     

Antti Taskinen  Hannu Sirviö  Michael Bruen 《Stochastic Environmental Research and Risk Assessment (SERRA)》2008,22(1):67-82

The mixed linear model approach was introduced and applied in studying the effects of spatial variation of the saturated hydraulic conductivity (K _s ) on the variation of the overland flow. Analysis was carried out with 2,000 rainfall-runoff events, all generated through transformation of real, observed rainfall events and different spatially variable K _s fields in a small (12 ha) agricultural catchment. The parameters accounting for the variation in the generation method were the coefficient of variation (cv) and correlation length (L _x L _y ) of K _s both having two levels of values obtained from field measurements of other studies. The analysis showed that the combinations with both parameters having the smaller or bigger value during flow peaks only caused different response in the overland flow. However, the parameters were statistically significant only at the 10% level. Most of the flow variation was explained by the event dynamics. The mixed models were able to model the structure of the data efficiently with less restrictive assumptions than for example the analysis of variance, hence producing more reliable results. The method was able to take into account autocorrelation of the test series, correlation between the factors and unequal variances. The usefulness of the method was supported by the fact that the conclusions drawn by it were confirmed by simple, conventional methods of a previous study, added with statistical criteria and confidence levels for each calculation moment. The findings of the study can be utilized in practise for example when designing the field sampling experiments.  相似文献   

Fish assemblages in coastal lagoons in land-uplift succession: The relative importance of local and regional environmental gradients     

Martin Snickars  Alfred Sandström  Antti Lappalainen  Johanna Mattila  Kajsa Rosqvist  Lauri Urho 《Estuarine, Coastal and Shelf Science》2009

The assemblages of young-of-the-year fish were studied in coastal lagoons in an archipelago with post-glacial land-uplift, which affects environmental gradients at local and regional scale, i.e. lagoon habitat isolation and archipelago position, respectively. The categorisation of 40 undisturbed lagoons into nine habitat types based on habitat isolation and archipelago position was supported by clear relationships with spring temperature and total fish abundance. Rutilus rutilus, breams (Abramis/Blicca sp.) and Perca fluviatilis were the most abundant and frequently occurring species. The fish assemblage differed among the nine habitat types. Rutilus rutilus, P. fluviatilis and breams were discriminating species in the majority of habitat types with low physical harshness, whereas Alburnus alburnus and Gasterosteus aculeatus increased their contributions in habitat types with high physical harshness. Rutilus rutilus and breams were thus common in lagoons with high habitat isolation situated in the inner archipelago. These lagoons were characterised by warm water and high vegetation coverage. Gasterosteus aculeatus was restricted to lagoons with low habitat isolation and exposure and low vegetation coverage, situated in the outer archipelago. Perca fluviatilis had the widest distribution of all species. The coverage of two macrophytes, Potamogeton perfoliatus and Zannichellia palustris, and salinity matched best the distance among habitat types. These habitat characteristics, as well as the fish abundances and assemblages differed most across the habitat types in the outer and mid archipelago zones and in the lowest habitat isolation. These patterns suggest that the structuring effect of habitat isolation increases along the archipelago gradient as differences between local and regional conditions increase. In the inner archipelago, overall low physical harshness induces homogeneous conditions and the habitat isolation is less important here than in the other zones. We suggest that this difference in the relative importance of the two gradients depending on the level of respective gradient ultimately forms these heterogeneous coastal habitats in a successional landscape. Rutilus rutilus and P. fluviatilis were responsible for large parts of the assemblage patterns. Although sympatric due to similar habitat requirements, differences in dispersal capability, competitive ability and predation vulnerability may add explanation to detected differences in distribution and abundance in these two species in an open system. Our results also stress the structuring role of vegetation in terms of total coverage and species composition, as these two aspects of macrophyte diversity may act as complementary habitat modifiers across gradients of physical harshness.  相似文献   

Computations with finite element methods for the Brinkman problem     

Antti Hannukainen  Mika Juntunen  Rolf Stenberg 《Computational Geosciences》2011,15(1):155-166

Various finite element families for the Brinkman flow (or Stokes–Darcy flow) are tested numerically. Particularly, the effect of small permeability is studied. The tested finite elements are the MINI element, the Taylor–Hood element, and the stabilized equal order methods. The numerical tests include both a priori analysis and adaptive methods.  相似文献   

Early Farming in the Northern Boreal Zone: Reassessing the History of Land Use in Southeastern Finland through High‐Resolution Pollen Analysis     

Teija Alenius  Teemu Mkknen  Antti Lahelma 《Geoarchaeology》2013,28(1):1-24

The early stages of agriculture in the Boreal forests of Northern Europe remain poorly understood. Although pottery appeared during the 6th millennium B.C., this has not been seen as an indication of a true Neolithic in the north. In later prehistory, vast parts of the region are thought to have remained a wilderness. In order to test these assumptions, a high‐resolution pollen analysis and an archaeological survey were carried out at Lake Huhdasjärvi, SE Finland. The results indicate signs of cultivation already by the early Neolithic, 5260–4260 B.C., and slash‐and‐burn cultivation concentrated on deciduous forests is recorded from ca. A.D. 600 onwards. By A.D. 930, an intensive form of swidden cultivation began in the coniferous forests, indicating a well‐established agricultural settlement. The discovery of Neolithic (late 6th millennium B.C.) buckwheat pollen suggests that the roots of agriculture in northernmost Europe may have to be searched for in China rather than the Near East.  相似文献