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Funktionelle Langzeitergebnisse nach Hüftgelenksprothesenexplantation (Girdlestone-Situation)
(2004)
- Studienziel: Ziel der Arbeit war die Identifikation prognostischer Faktoren, die die zu erwartende Funktion einer Girdlestone-Arthroplastik vorhersagen. Methode: Retrospektiv wurde das Kollektiv einer Klinik von 87 Patienten, 90 Hüften analysiert, die zwischen 1983 und 2000 mit Anlage einer Girdlestone-Hüfte behandelt worden waren. Ergebnisse: Hüftscores ergaben durchschnittlich 38.7 Punkte (Harris Hip Score) und 3.5 Punkte (Score nach Merle d’Aubigné und Postel). Die Standzeit der Girdlestone-Hüfte, im Durchschnitt 90.6 Monate, und das funktionelle Ergebnis korrelierten nicht (r = 0.0920; p = 0.6289). D.h. die Funktion einer Girdlestone-Arthroplastik wurde mit zunehmender Zeit nicht schlechter. Die Anzahl der implantierten Hüftprothesen vor Girdlestone-Anlage korrelierte nicht mit dem funktionellen Ergebnis der Girdlestone-Hüfte bei Nachuntersuchung (r = - 0.1400; p = 0.4524). Die Standzeit der letzten explantierten Hüftprothese, im Mittel 44.6 Monate, und die Funktion der Girdlestone-Hüfte korrelierten nicht (r = - 0.0705; p = 0.7065). Lebensalter bei Erstimplantation der Hüftprothese, Lebensalter zum Zeitpunkt der Nachuntersuchung oder Lebensalter bei Anlage der Girdlestone-Hüfte korrelierten nicht mit dem Harris Hip Score (r = - 0.0367; p = 0.8418 sowie r = 0.1527; p = 0.4121 sowie r = - 0.0151; p = 0.9356). Die Notwendigkeit einer Revision der Girdlestone-Hüfte und das Vorhandensein eines Diabetes korrelierten (p = 0.0104). Die Korrelation zwischen verbliebenem Knochenzement und radiologischen Zeichen eines persistierenden Infektes war signifikant (p = 0.0572). Schlussfolgerung: Das Lebensalter des Patienten, der Zeitraum seit Girdlestone-Anlage, die Zahl vorangegangener HTEP-Wechsel waren keine geeigneten prognostischen Merkmale, die Funktion einer Girdlestone-Hüfte vorherzusagen.
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Ozone loss derived from balloon-borne tracer measurements in the 1999/2000 Arctic winter
(2005)
- Balloon-borne measurements of CFC11 (from the DIRAC in situ gas chromatograph and the DESCARTES grab sampler), ClO and O3 were made during the 1999/2000 Arctic winter as part of the SOLVE-THESEO 2000 campaign, based in Kiruna (Sweden). Here we present the CFC11 data from nine flights and compare them first with data from other instruments which flew during the campaign and then with the vertical distributions calculated by the SLIMCAT 3D CTM. We calculate ozone loss inside the Arctic vortex between late January and early March using the relation between CFC11 and O3 measured on the flights. The peak ozone loss (~1200ppbv) occurs in the 440-470K region in early March in reasonable agreement with other published empirical estimates. There is also a good agreement between ozone losses derived from three balloon tracer data sets used here. The magnitude and vertical distribution of the loss derived from the measurements is in good agreement with the loss calculated from SLIMCAT over Kiruna for the same days.
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Ozone loss derived from balloon-borne tracer measurements and the SLIMCAT CTM
(2004)
- Balloon-borne measurements of CFC-11 (on flights of the DIRAC in situ gas chromatograph and the DESCARTES grab sampler), ClO and O3 were made during the 1999/2000 winter as part of the SOLVE-THESEO 2000 campaign. Here we present the CFC-11 data from nine flights and compare them first with data from other instruments which flew during the campaign and then with the vertical distributions calculated by the SLIMCAT 3-D CTM. We calculate ozone loss inside the Arctic vortex between late January and early March using the relation between CFC-11 and O3 measured on the flights, the peak ozone loss (1200 ppbv) occurs in the 440–470 K region in early March in reasonable agreement with other published empirical estimates. There is also a good agreement between ozone losses derived from three independent balloon tracer data sets used here. The magnitude and vertical distribution of the loss derived from the measurements is in good agreement with the loss calculated from SLIMCAT over Kiruna for the same days.
