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Tytuł:
Lotniczy skaning laserowy (LiDAR-ALS) jako źródło danych do obliczeń stateczności skarp na terenach zadrzewionych i zakrzewionych
Airborne laser scanning (LiDAR-ALS) as a source of data for calculations of escarpment stability in wooded and bushy areas
Autorzy:
Piechota, A.
Powiązania:
https://bibliotekanauki.pl/articles/2075700.pdf
Data publikacji:
2017
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
lotniczy skaning laserowy
ALS
skaning laserowy
LiDAR
globalny system nawigacji satelitarnej
GNSS
cyfrowy model terenu
DTM
pomiar nachylenia
kontrola jakości
Airborne Laser Scanning
Light Detection And Ranging
Global Navigation Satellite System
digital terrain model
slope measurement
quality control
Opis:
The paper discusses the problem of quick acquire height data for calculation of escarpment stability. In past the slope of profile was obtainedfrom classical land survey methods (like Total Station, GNSS, etc.), carto- metric measurement on maps or measurements based on a Digital Terrain Modelfrom aerial photography. Now we have a new method that is Airborne Laser Scanning (LiDAR-ALS). In 2011-2014 almost all country was measured in this method. The declared accuracy of height measurement on the durable surfaces is about 0.10-0.15 m. Author compared this method with classical method Global Navigation Satellite System - Real Time Network (GNSS-RTN) on two wooded and bushy areas. The comparison was based on the measurement characteristic points on the profiles and acquisition of height data from LiDAR-ALS data. Data in this method were obtained in two ways: from point cloud and from DTM createdfrom this point cloud. In the next step, height differences were calculated and these data were subjected to basic statistical calculations. The result of the study was a mean error of height data from LiDAR-ALS and conclusions about its usefulness in acquire height data for calculation of escarpment stability.
Źródło:
Przegląd Geologiczny; 2017, 65, 10/2; 811--816
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
CFD simulations of blood flow through abdominal part of aorta
Autorzy:
Polanczyk, A.
Piechota, A.
Powiązania:
https://bibliotekanauki.pl/articles/115686.pdf
Data publikacji:
2010
Wydawca:
Fundacja na Rzecz Młodych Naukowców
Tematy:
CFD
abdominal aorta
computer simulations
computer tomography
geometry
Opis:
The aim of this research was to show superiority of using real geometries in simulations of blood fl ow through cardiovascular system. Our model compared blood fl ow through an abdominal part of aorta reconstructed with a use of data from an AngioTK research with the 3DDoctor software to geometries with the same diameters at inlet and outlet as mention before but created only with the Gambit 2.2.30 software without data from AngioTK. Blood fl ow simulations were prepared with the Fluent 6.2.16 software. Calculations of fl ow through a real geometry allows to obtain realistic results of values connected with process of blood fl ow. Results showed that calculations blood fl ow through a virtual geometry lasted two times longer than for a real geometry. Mesh for a real geometry consist about 600.000 elements and for a virtual geometry about 900.000 elements. Wall shear stress and blood velocity was higher for a real geometry and closer to that in human organism. It was shown that calculating a virtual geometry vessel was to big simplifi cation when investigating blood fl ow through a vessel. Application of mathematical models based on real geometries gives more realistic results than artifi cial geometries. Virtual models have lots of simplifi cations which results are far away from expectations. Simplifi cations depend on the model that is used.
Źródło:
Challenges of Modern Technology; 2010, 1, 1; 34-39
2082-2863
2353-4419
Pojawia się w:
Challenges of Modern Technology
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The first Devonian holocephalian tooth from Poland
Autorzy:
Ginter, M
Piechota, A.
Powiązania:
https://bibliotekanauki.pl/articles/22410.pdf
Data publikacji:
2004
Wydawca:
Polska Akademia Nauk. Instytut Paleobiologii PAN
Tematy:
Famennian
phylogenesis
Cochliodontiformes
Holocephali
holocephalian tooth
tooth
paleontology
Chondrichthyes
Opis:
A recently found “bradyodont” holocephalian tooth from bituminous shales of the Kowala Quarry, south−western Holy Cross Mountains, Poland, dated as the middle Famennian Palmatolepis trachytera conodont Zone, is described. In spite of its resemblance to the forms often attributed to Helodus, the tooth is referred to as Psephodus cf. magnus (Agassiz, 1838), and supposed to represent the anterior part of the dentition, based on a partly articulated specimen of Psephodus from the Carboniferous of Scotland. The analysis of early helodonts and psephodonts, and other Famennian chondrichthyan crushing teeth, shows numerous similarities in tooth−base structure, such as the reduction of lingual basal extension, loss of articulation devices, development of numerous nutritive foramina, and the tendency to fusion between the teeth in a tooth−family. Based on these shared characters, close phylogenetic relationships between the Protacrodontoidea, Hybodontoidea, and the Holocephali are postulated.
Źródło:
Acta Palaeontologica Polonica; 2004, 49, 3
0567-7920
Pojawia się w:
Acta Palaeontologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Drenaż subglacjalny lądolodu skandynawskiego (Polska NW) w świetle modelowania numerycznego
Subglacial drainage of the Scandinavian Ice Sheet (NW Poland) from numerical modelling
Autorzy:
Piechota, A. M.
Piotrowski, J. A.
Powiązania:
https://bibliotekanauki.pl/articles/295104.pdf
Data publikacji:
2010
Wydawca:
Stowarzyszenie Geomorfologów Polskich
Tematy:
drenaż subglacjalny
vistulian
modelowanie numeryczne
subglacial drainage
Weichelian glaciation
numerical modelling
Opis:
W niniejszym artykule autorzy przedstawiają wyniki badań nad drenażem subglacjalnym lądolodu skandynawskiego podczas maksymalnego postoju w fazie poznańskiej i pomorskiej vistulianu w Polsce NW. Podczas numerycznychsymulacji dwuwymiarowychi trójwymiarowychprzepływu wód podziemnychpod lądolodem stwierdzono, że tworzyły się znaczne nadwyżki wód subglacjalnychna kontakcie lód-podłoże. Zaledwie od około 15-25% wód subglacjalnychbyło w stanie wpłynąć pod stopę lądolodu jako wody podziemne. W symulacjachdla warunków ustalonychwody te wpływały na głębokość około 220 m, często nie przekraczając jednak wartości 100 m, osiągając średnie prędkości około 110 m/rok.
Here we present the results of research on subglacial drainage of Scandinavian Ice Sheet during Poznan and Pomeranian phases of Weichelian glaciation in NW Poland. On the basis of two- and three-dimensional numerical simulation of groundwater flow under the ice sheet it is suggested that a surplus of subglacial water at the ice-bed interface occurred. Only about 15–25% of subglacial water had been able to drain through the bed as groundwater. In steady-state simulations, this water penetrated the bed to the depth of approximately 220 m but often not exceeding the value of 100 m, and reached an average flow velocity of approximately 110 m/year.
Źródło:
Landform Analysis; 2010, 13; 91-106
1429-799X
Pojawia się w:
Landform Analysis
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Analiza możliwości zastosowania metody tomografii elektrooporowej (ERT) do rozpoznania miąższości pokrywy laterytowej
Applicability analysis of the electrical resistivity tomography (ERT) method for the diagnosis of laterite cover thickness
Autorzy:
Pacanowski, G.
Czarniak, P.
Piechota, A.
Mieszkowski, R.
Powiązania:
https://bibliotekanauki.pl/articles/2075560.pdf
Data publikacji:
2016
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
tomografia elektrooporowa
VES
oporność właściwa
lateryty
złoża niklu
złoża kobaltu
electrical resistivity tomography
electrical resistivity sounding
laterite
nickel and cobalt deposit
Opis:
The paper discusses the problem of determining the thickness of a laterite cover using electrical resistivity tomography (ERT) in a selected area of the Seram Island in Indonesia. Seram Island lies in the tropical zone between the Seram and Banda seas. The laterite covers are rich in nickel, cobalt, iron and other metals. Concentrations of these metals in the laterites are high enough to form economic deposits. A significant part of the report concerns the measurement technique (ERT method) in difficult climatic (high humidity and temperature) and topographic conditions (equatorial jungle with significant variations in elevation) and the methods of processing and interpretation of the acquired data. The problem seems very interesting, because geophysical prospecting is currently more and more often conducted in poorly accessible regions of the world. Additionally, there are no sufficient and commonly available publications that would allow us to get acquainted with local measurement problems by potential contractors of similar geophysical investigations. The primary result of the geophysical survey was to determine the electrical resistivity of bedrock and laterite. This was the basis for the development of sections of electrical resistive distribution for the ERT profiles, which enabled to estimate the depth to the crystalline basement and the laterite thickness. It also facilitated to produce a map of laterite thickness, which may be an important material to develop the concept of searching and mining of nickel and cobalt ore.
Źródło:
Przegląd Geologiczny; 2016, 64, 4; 245--253
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Geochemical and ecological aspects of lower Frasnian pyrite-ammonoid level at Kostomłoty (Holy Cross Mountains, Poland)
Autorzy:
Racki, G.
Piechota, A.
Bond, D.
Wignall, P. B.
Powiązania:
https://bibliotekanauki.pl/articles/2060630.pdf
Data publikacji:
2004
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Holy Cross Mountains
Frasnian
pyritic fossils
geochemical proxies
anoxia
Timan Event
Opis:
The lower Frasnian (transitans Zone with Ancyrodella priamosica = MN 4 Zone) rhythmic basin succession of marly limestones and shales (upper Szydłówek Beds) at Kostomłoty, western Holy CrossMts., Central Poland, contains a record of the transgressive-hypoxic Timan Event in this drowned part of southern Laurussian shelf. The unique facies consists of organic-rich marly shales and a distinctive pyritic, goniatite level, 1.6mthick. The faunal assemblage is dominated by pyritized shells of diminutivemollusks with cephalopods (including goniatites Epitornoceras and Acanthoclymenia), buchioline bivalves (Glyptohallicardia) and styliolinids. This interval is marked by moderately low Th/U ratios and pyrite framboid size distributions suggestive of dysoxic rather than permanent euxinic conditions. The scarcity of infauna and bioturbation resulted in finely laminated sedimentary fabrics, as well as the low diversity of the presumed pioneer benthos (mostly brachiopods). In the topmost part of the Szydłówek Beds, distinguished by the Styliolina coquina interbedded between limestone-biodetrital layers, the above geochemical proxies and C-isotope positive shift indicate a tendency to somewhat increased bottom oxygen deficiency and higher carbon burial rate linked with a bloom of pelagic biota during high-productivity pulse. The geochemical and community changes are a complex regional record of the initial phase of a major perturbation in the earth-ocean system during a phase of intermittently rising sea level in the early to middle Frasnian, and associated with the highest positive C-isotope ratios of the Devonian.
Źródło:
Geological Quarterly; 2004, 48, 3; 267--282
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Wyświetlanie 1-10 z 131

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