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Postoperative morbidity after colorectal surgery was retrospectively investigated, comparing 32 alcoholics (≥60 gm of alcohol a day) to 32 controls (<25 gm of alcohol a day). The material originated from 260 male patients and the two groups were paired with respect to operative procedure, diagnosis, age-complicating cardiopulmonary diseases, weight, and smoking habits. Postoperative morbidity was
ABSTRACT. Erythrocyte mean cell volume (MCV) correlates well to alcohol intake in moderate alcoholism, but only about 50% of heavy drinkers have increased MCV. To evaluate the influence of the duration and extent of a drinking episode on MCV, 64 addictive alcoholics were investigated prospectively within two weeks after a drinking period. Their daily alcohol intake was 120–480 g and the actual dri
On the basis of the theory that malnutrition leads to zinc deficiency, 36 severe alcohol addicts were investigated in a large clinic for alcoholism in Copenhagen. The serum zinc levels were registered on commencement/recommencement of treatment with disulphiram and one month later. A total of 16 patients completed the entire investigation. All of the participants in the trial were without clinical
Background: Distinguishing behavioural variant frontotemporal dementia (bvFTD) from non-neurodegenerative ‘non-progressor’ mimics of frontal lobe dysfunction, can be one of the most challenging clinical dilemmas. A biomarker of neuronal injury, neurofilament light chain (NfL), could reduce misdiagnosis and delay. Methods: Cerebrospinal fluid (CSF) NfL, amyloid beta 1–42 (AB42), total and phosphory
We report a spatially resolved spectroscopic study of the visible chemiluminescence emission from different premixed ammonia-air-oxygen flames stabilized on a laminar flat flame burner, with equivalence ratio ranging from 0.7 to 1.35 and an O2/N2 ratio of 0.4. In the reaction zone of the observed flames, the visible emission was recognized to be the chemiluminescence of excited NH2* radicals, whil
Global warming may lead to carbon transfers from soils to the atmosphere, yet this positive feedback to the climate system remains highly uncertain, especially in subsoils . Using natural geothermal soil warming gradients of up to +6.4C in subarctic grasslands , we show that soil organic carbon (SOC) stocks decline strongly and linearly with warming (-2.8tha-1C-1). Comparison of SOC stock changes
