Jana Herrmann

Biotechnological hydrogen production by photosynthesis

Microbiological photosynthesis is a promising tool for producing hydrogen in an ecologically friendly and economically efficient way. Certain microorganisms (e.g. algae and bacteria) can produce hydrogen using hydrogenase and/or nitrogenase enzymes. However, their natural capacity to produce hydrogen is relatively low. Thus, there is a need to optimize their core photosynthetic processes as well as their cultivation, for more efficient hydrogen production. This review aims to provide a holistic overview of the recent technological and research developments relating to photobiological hydrogen production and downstream processing. First we cover photobiological hydrogen synthesis within cells and the enzymes that catalyze the hydrogen production. This is followed by strategies for enhancing bacterial hydrogen production by genetic engineering, technological development, and innovation in bioreactor design. The remaining sections focus on hydrogen as a product, that is, quantification via (in‐process) gas analysis, recent developments in gas separation technology. Finally, a discussion of the sociological (market) barriers to future hydrogen usage is provided as well as an overview of methods for life cycle assessment that can be used to calculate the environmental consequences of hydrogen production.

Role of Cellular Oxalate in Oxalate Clearance of Patients With Calcium Oxalate Monohydrate Stone Formation and Normal Controls

OBJECTIVES To examine the cellular, plasma, and urinary oxalate and erythrocyte oxalate flux in patients with calcium oxalate monohydrate (COM) stone formation vs normal controls. Pathologic oxalate clearance in humans is mostly integrated in calcium oxalate stone formation. An underlying cause of deficient oxalate clearance could be defective transmembrane oxalate transport, which, in many tissues, is regulated by an anion exchanger (SLC26). METHODS We studied 2 groups: 40 normal controls and 41 patients with COM stone formation. Red blood cells were divided for cellular oxalate measurement and for resuspension in a buffered solution (pH 7.40); 0.1 mmol/L oxalate was added. The supernatant was measured for oxalate immediately and 1 hour after incubation. The plasma and urinary oxalate were analyzed in parallel. RESULTS The mean cellular oxalate concentrations were significantly greater in the normal controls (5.25 +/- 0.47 micromol/L) than in those with COM stone formation (2.36 +/- 0.28 micromol/L; P < .01). The mean urinary oxalate concentrations were significantly greater in those with COM stone formation (0.31 +/- 0.02 mmol/L) than in the controls (0.24 +/- 0.02 mmol/L; P < .01). The cellular oxalate concentrations correlated significantly with the plasma (r = 0.49-0.63; P < .01) and urinary oxalate (r = -0.29-0.41; P < .03) concentrations in both groups. The plasma oxalate concentrations correlated significantly with the urinary oxalate concentrations (r = -0.30; P < .03) in the controls and with the erythrocyte oxalate flux (r = 0.25; P < .05) in those with COM stone formation. CONCLUSIONS Our data implicate the presence of a cellular oxalate buffer to stabilize plasma and urinary oxalate concentrations in normal controls.

Importance of Erythrocyte Band III Anion Transporter (SLC4A1) on Oxalate Clearance of Calcium Oxalate Monohydrate Stone-formering Patients vs. Normal Controls

OBJECTIVES To examine erythrocyte band III transport protein (SLC4A1), erythrocyte oxalate flux, and plasmatic, cellular, and urine oxalate concentrations and blood gas analyses in calcium oxalate monohydrate stone-forming patients (COM) in comparison with normal controls (NC). METHODS Isolated red cells from 51 NC and 25 COM cases were divided for cellular oxalate measurement and for measurement of transcellular erythrocyte oxalate flux (pH 7.48-8.24). SLC4A1 protein levels were determined by Western blot analyses. Plasmatic and urinary oxalate levels and the venous blood gas analysis were measured simultaneously. RESULTS SLC4A1 protein levels were significantly higher in COM (8.76 ± 2.12) than in NC (4.17 ± 0.61; P < .02). Cellular oxalate and venous HCO(3)(-) were significantly lower in COM (2.35 ± 0.26 μmol/L) and (24.06 ± 0.24 mmo/l) than in NC (4.03 ± 0.49 μmol/L; P < .05) and (24.93 ± 0.17 mmol/L; P < .01). Urinary oxalate was significantly higher in COM (0.31 ± 0.02 mmol/L) than in NC (0.25 ± 0.01 mmol/L; P < .04). The erythrocyte transmembrane oxalate flux correlated with the pH value and with the urinary oxalate in both groups (r = .25-.55; P = .01). With increased pH values, the oxalate flux showed inverse effects in both groups. CONCLUSIONS SLC4A1 associated changes of HCO(3)(-) and pH levels influenced the cellular oxalate levels and urinary oxalate clearance. Under normal conditions (pH 7.55) the oxalate efflux in COM was comparable with the acid stimulated oxalate efflux in NC. The addition of HCO(3)(-) compensated the flux of COM stone formers to the levels of normal controls.