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EN
Sedimentological analysis of the Missão Velha Formation (Araripe Basin, northeast Brazil) is the aim of this paper through detailed facies analysis, architectural elements, depositional systems and paleocurrent data. The main facies recognized were: (i) coarse-grained conglomeratic sandstones, locally pebbly conglomerates, with abundant silicified fossil trunks and several large-to-medium trough cross-stratifications and predominantly lenticular geometry; (ii) lenticular coarse-to-medium sandstones with some granules, abundant silicified fossil wood, and large-to-medium trough cross-stratifications, cut-and fill features and mud drapes on the foresets of cross-strata, (iii) poorly sorted medium-grained sandstones with sparse pebbles and with horizontal stratification, (iv) fine to very fine silty sandstones, laminated, interlayered with (v) decimetric muddy layers with horizontal lamination and climbing-ripple cross-lamination. Nine architectural elements were recognized: CH: Channels, GB: Gravel bars and bed forms, SB: Sand bars and bedforms, SB (p): sand bedform with planar cross-stratification, OF: Overbank flow, DA: Downstream-accretion macroforms, LS: Laminated sandsheet, LA: Lateral-accretion macroforms and FF: Floodplain fines. The lithofacies types and facies associations were interpreted as having been generated by alluvial systems characterized by (i) high energy perennial braided river systems and (ii) ephemeral river systems. Aeolian sand dunes and sand sheets generated by the reworking of braided alluvial deposits can also occur. The paleocurrent measurements show a main dispersion pattern to S, SE and SW, and another to NE/E. These features imply a paleodrainage flowing into the basins of the Recôncavo-Tucano-Jatobá.
PL
W pracy przedstawiono analize numeryczną przepływu strumienia powietrza o różnej prędkości i intensywności turbulencji w strefie przypowierzchniowej elementu architektonicznego o rozwiniętej geometrii. Określono pola prędkości na wyodrębnionym fragmencie elewacji oraz określono kąt napływu. Uzyskane wyniki poddane zostały weryfikacji poprzez badania w tunelu aerodynamicznym.
EN
The paper presents numerical analyses of air flow in surface layer of architectural element. The flow was characterized by different speed and turbulence intensity. The obtained flow field were verified by wind tunnel measurement.
PL
W pracy podjęta została próba oszacowania podstawowych parametrów związanych z opisem turbulentnego przepływu w strefach napływu i odpływu powietrza, w sąsiedztwie elementu architektonicznego. Badania zostały przeprowadzone w tunelu aerodynamicznym. Do rejestracji zastosowany został układ elektro - optyczny z wykorzystaniem wąskiej wiązki światła laserowego. W celu wyznaczenia podstawowych wielkości, charakteryzujących przepływ turbulentny wykorzystano równania, zaproponowane w pracy [1] przez Consortini.
EN
The paper presents the first attempt in estimation of basic parameters describing turbulent air flow in windward and leeward side of architectural element. Measurement were carried out in wind tunnel with the aid of electro - optic system based on laser beam. In order to determine basic parameters equations proposed by Consortini were used.
EN
Detailedanalysis of lithofacies and their distribution in the Magura Beds in 11 transects in the eastern part of the Siary zone, revealed 16 facies and 6 associations of genetically and spatially related facies. The facies spectrum evidences deposition from a variety of mass gravity processes and subordinately by hemipelagic rain. The facies associations reveal depositional patterns of submarine fans and include: channels, channel-levees, channel-lobe transitions, depositional lobes and slump bodies. Correlation results (9 sections) and facies distribution together with paleocurrent directions suggest that the deposition of this part of Magura Beds took place in a submarine ramp/apron hybrid setting fed from a multipoint source. The depositional pattern of the Magura Beds in the study area records a two-stage development, which began with the emplacement of a sand/mud-rich type system and was followed by a mud-dominated system.
6
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