Plasma free amino acid profiles and nutrition proteins in chronic renal failure; effect of dialysis treatment

Summary A well preserved nutritional status is beneficial in chronically uremic patients for slowing the pace of deterioration of renal function, and delaying the need for dialysis therapy. The purpose of this study was to assess the nutritional profile of 10 patients in a steady state of advanced CRF, and of 15 patients with terminal renal failure immediately prior to their first hemodialysis session (J0), and 7, 14, 45, 60, days post start of dialysis. Patients were 18 to 65 years old with total plasma proteins 60g/1. Plasma concentrations of amino acids, nutrition proteins, apolipoproteins A1, and B were evaluated. Non inflammatory reaction was evaluated by determination of alpha-1-acid glycoprotein, and C reactive protein. The data (mean ± 1 SD) were compared with mean values of 15 healthy individuals.     

Direct mass spectrometric measurement of gases in peat cores

Abstract Dissolved gas concentrations (O₂, CH₄, CO₂) in peat cores were monitored simultaneously using a fine (1.56 mm diameter) membrane inlet probe connected to a quadrupole mass spectrometer. This technique allows direct measurements at specific locations within the sample with minimal disturbance. Detailed gas profiles in completely waterlogged peat samples (hollows) and samples in which the water table was several cm below the vegetation surface (hummocks) were compared. The depth of the water table played a central role in the distribution of gases. In a hollow, oxygen was present (90 μM) at the surface but was not detectable (<0.5 μM) at depths greater than 2 cm. Concentrations of CH₄ and CO₂ increased from 6 and 300 μM respectively at the surface to maxima of 450 and 3900 μM at 13 cm depth. At a hummock, O₂ and CO₂ were present above the water table but CH₄ was not detectable. CH₄ was measurable 2 cm below the water table. Both CH₄ and CO₂ concentrations increased with depth but maxima were not attained in the sampled cores.