41. Factors influencing rehabilitation in patients with head and neck cancerIrena Hočevar-Boltežar, Alojz Šmid, Miha Žargi, Avgust Župevc, Igor Fajdiga, Janez Fischinger, Ana Jarc, 2000, original scientific article Abstract: Purpose. The purpose of the prospective study was to identify the factors adversely influencing the post-treatment rehabilitation in patients with head and neck cancer. Patients and methods. One hundred and ten patients with oral cavity, pharyngeal and laryngeal cancer were examined before surgical treatment in order to find unfavorable factors: hearing loss, defective teeth,impaired pulmonary function, and speech disorders. The patients evaluated the success of their rehabilitation 12 months after the treatment. The influence of possible unfavorable factors, tumor site, and type of surgeryon speech, swallowing and reintegration competence was determinated. Results. The site of the tumor and the type of surgery did not influence the quality of rehabilitation in general. Defective teeth influenced the ability of swallowing but not the speech. Hearing loss impaired the patient's reintegration in their home environment. Impaired pulmonary function did not affect patient's speech. Speech was the poorest in laryngectomized patients. However, about two thirds of the patients were satisfied with their capabilityof speech, swallowing and their rehabilitation in general. Conclusions. Early identification of unfavorable factors, and individually planned rehabilitation can ensure a suitable quality of life for patients thathave undergone surgery for head and neck cancer.
Published in DiRROS: 25.01.2024; Views: 163; Downloads: 44
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46. 5. poročilo o doseganju kazalnikov uspešnosti in napredka partnerjev projekta Life IP CARE4CLIMATE - akcija C8 in E3Boštjan Mali, Andreja Ferreira, Gal Kušar, Anica Simčič, Bernarda Krištof, 2022, treatise, preliminary study, study Keywords: projekt Life IP CARE4CLIMATE, raba tal, spremembe rabe tal, gozdarstvo, aktivnosti
Published in DiRROS: 16.01.2024; Views: 258; Downloads: 0 |
47. 4. poročilo o doseganju kazalnikov uspešnosti in napredka partnerjev projekta Life IP CARE4CLIMATE - akcija C8 in E3Boštjan Mali, Andreja Ferreira, Gal Kušar, Anica Simčič, Adrijana Trekman, 2022, treatise, preliminary study, study Keywords: projekt Life IP CARE4CLIMATE, raba tal, spremembe rabe tal, gozdarstvo, aktivnosti
Published in DiRROS: 16.01.2024; Views: 262; Downloads: 0 |
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49. Resections of pelvic bone and sacrum, Ljubljana experienceJanez Novak, Marjana Čuček-Pleničar, Darja Eržen, Franc Srakar, Mojca Senčar, Boštjan Baebler, Jožica Červek, Alenka Vodnik-Cerar, Matej Bračko, Živa Pohar-Marinšek, Jožica Anžič, 1997, original scientific article Published in DiRROS: 16.01.2024; Views: 221; Downloads: 48
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50. Transverse Dinaric zone of increased compression between the Kraški rob and Hrušica Regions, NE MicroadriaLadislav Placer, Igor Rižnar, Ana Novak, 2023, original scientific article Abstract: The Kvarner fault divides the Microadria (Adria microplate, the Adria stable core) into the Po and Adria segments. The Istra block, which is sandwiched between the right-lateral Kvarner Fault and the left-lateral Sistiana Fault lies at the extreme eastern edge of the Po segment. Both faults run transversely to the Dinarides and reach their thrust boundary in the east. The Microadria has been moving towards the Dinarides since the Middle Miocene. The movement of the Istra block is exposed in relation to the neighbouring blocks, so an extensive pushed area (the Istra Pushed Area) was formed in the External Dinarides, which is bent towards the northeast. It is defined by two flexural zones, one lying in the extension of the Sistiana Fault and the other in the extension of the Kvarner Fault. The structure of the Dinaric thrust border on the north-eastern side of the Istra block is complex. Its prominent structural element is the Črni Kal Anomaly, due to which a zone of increased compression developed within the Istra Pushed Area and transversely to the Dinarides (Kraški rob – Hrušica Traverse), which lies between the Sistiana and Kvarner Flexural Zones. In terms of kinematics, it differs greatly from these two, and various geomorphologically responsive deformations have occurred within it. Mt. Vremščica (1027 m), which represents a transpressive anticline within the wider zone of the Raša Fault is the most prominent. In order to understand the genesis of the Classical Karst relief, it is important to know that the Mt. Vremščica ridge rose from the levelled karst surface.
Keywords: NE Microadria (Adria Microplate), Istra peninsula, Istra Pushed Area, Črni Kal Anomaly, Kraški rob – Mt. Hrušica Traverse, stacked structure, envelope fault
Published in DiRROS: 15.01.2024; Views: 188; Downloads: 148
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