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Wyszukujesz frazę "Rudowski, M." wg kryterium: Wszystkie pola


Wyświetlanie 1-2 z 2
Tytuł:
An expert system supporting risk stratification in acute coronary syndromes
Autorzy:
Grabowski, M.
Filipiak, K. J.
Rudowski, R.
Opolski, G.
Powiązania:
https://bibliotekanauki.pl/articles/1965787.pdf
Data publikacji:
2004
Wydawca:
Politechnika Gdańska
Tematy:
expert system
decision making
acute coronary syndrome
risk stratification
Opis:
The aim of the project was to create a computer program, an expert system (ES), which would support physicians when a management for patients with acute coronary syndrome needs to be chosen. A knowledge database was created with the support of clinical experts, based on the current management standards. Data from new patients are added to the case database. The inference engine integrates two types of reasoning rule-based and case-based. The ES gives unambiguous and objective answers, its recommendation are reliable. At present, the ES is tested in clinical practice. Strategies recommended by the ES are compared with the management applied in a clinic.
Źródło:
TASK Quarterly. Scientific Bulletin of Academic Computer Centre in Gdansk; 2004, 8, 2; 281-286
1428-6394
Pojawia się w:
TASK Quarterly. Scientific Bulletin of Academic Computer Centre in Gdansk
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Submarine landslides on the slope of a sandy barrier : A case study of the tip of the Hel Peninsula in the Southern Baltic
Autorzy:
Rudowski, R.
Rucińska-Zjadacz, M.
Wróblewski, R.
Sitkiewicz, P.
Powiązania:
https://bibliotekanauki.pl/articles/2059851.pdf
Data publikacji:
2016
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
underwater mass movements
sandspit
digital terrain model (DTM)
side-scan sonar
sub–bottom profiling
Opis:
The aim of the study is to present the occurrence of landslides on the submarine slope of a sandy barrier. The scale and significance of this phenomenon is discussed. The study area is the Hel Peninsula. It is a 35 km long young sandy spit. The landform is prograding into the deep part of Gdańsk Bay, and the underwater extension of its tip is a steep sandy slope. The tip is still poorly investigated, as it was a military area closed to researchers until 2003. The first detailed survey of the tip on the seabed was conducted aboard the research vessel “IMOR”. A multibeam echosounder, a sub-bottom profiler and a side-scan sonar were used, while grab and core samples of sediment were obtained. Many forms, commonly created as the result of underwater mass movement, were recognized and determined (main scarps, main bodies, landslide steps, landslide foots, series of small slides, “sheet” slides and structural slides). On the one hand, the landslide processes that occur in the tip of the Hel Peninsula are related to the natural development of sandy spits. On the other hand, they threaten the shore’s stability. The genesis of the landslides is still not known.
Źródło:
Geological Quarterly; 2016, 60, 2; 407--416
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-2 z 2

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