Corrosion Resistance and Thermal Conductivity Enhancement of Reduced Graphene Oxide-BaSO4-Epoxy Composites.

The results of studies on the corrosion protectiveness and thermal conductivity of reduced graphene oxide-BaSO4 epoxy composites are reported here. A commercial epoxy resin and reduced graphene oxide (rGO) were blended with a hardening reagent and then mixed with prepared BaSO4-epoxy resin (B-epoxy). The reduced graphene oxide-BaSO4-epoxy composite (rGO-B-epoxy) paste was used to coat the surfaces of Al 7205 alloy and the corrosion and thermal properties were investigated. A corrosion test in a 3.5 wt% synthetic sea water solution showed that the composite coating containing BaSO4 had the best corrosion resistance. Moreover, the rGO-B-epoxy composite showed better protection against corrosion than the epoxy alone. The rGO-B-epoxy composite with 5 wt% BaSO4 had an in-plane coefficient of thermal conductivity of approximately 165.0 W/m K, and the in-plane thermal diffusivity was 71.38 mm2/s. In standard thermal conductivity tests, all three samples had values below 40 W/m K. The rGO-B-epoxy composites showed good surface corrosion protection and in-plane thermal conductivity.

High-precision iron isotope analysis of whole blood, erythrocytes, and serum in adults.

BACKGROUND: Iron isotopic composition serves as a biological indicator of Fe metabolism in humans. In the process of Fe metabolism, essential carriers of Fe circulate in the blood and pass through storage organs and intestinal absorptive tissues. This study aimed to establish an analytical method for high-precision Fe isotopic measurement, investigate Fe concentration and isotopic composition in different parts of whole blood, and explore the potential of Fe isotopic composition as an indicator for Fe status within individuals. ANALYTICAL METHODS: A total of 23 clinically healthy Taiwanese adults of Han descent were enrolled randomly and Fe isotopic compositions of their whole blood, erythrocytes, and serum were measured. The Fe isotopic analysis was performed by Neptune Plus multiple-collector inductively coupled plasma mass spectrometry with double-spike technique. The precision and reproducibility of the Fe isotopic analysis were monitored by international biological and geological reference materials. MAIN FINDINGS: High-precision Fe isotopic measurements were achieved alongside with high consistency in the isotopic data for well-characterized reference materials. The Fe isotopic signatures of whole blood and erythrocytes were resolvable from that of serum, where both whole blood and erythrocytes contained significantly lighter Fe isotopic compositions compared to the case of serum (P = 0.0296 and P = 0.0004, respectively). The δ56/54Fe value of the serum sample was 0.2‰ heavier on an average than those of whole blood or erythrocytes. This isotopic fractionation observed in different parts of whole blood may indicate redox processes involved in Fe cycling, e.g. erythrocyte production and Fe transportation. Moreover, the δ56/54Fe values of whole blood and serum significantly correlated with the hemoglobin level (P = 0.0126 and P = 0.0020, respectively), erythrocyte count (P = 0.0014 and P = 0.0005, respectively), and Mentzer index (P = 0.0055 and P = 0.0011, respectively), suggesting the Fe isotopic composition as an indicator of functional Fe status in healthy adults. The relationships between blood Fe isotopic compositions and relevant biodemographic variables were also examined. While the average Fe concentration of whole blood was significantly higher in males than in females (P = 0.0028), females exhibited a heavier Fe isotopic composition compared to that of males in whole blood (P = 0.0010) and serum (P < 0.0001). A significantly inverse correlation of the whole blood δ56/54Fe value with body mass index of individuals (P = 0.0095) was also observed. CONCLUSION: The results presented herein reveal that blood Fe isotopic signature is consequentially linked to baseline erythrocyte parameters in individuals and is significantly affected by the gender and body mass index in the adult population. These findings support the role of Fe isotopic composition as an indicator for the variance of Fe metabolism among adult individuals and populations and warrant further study to elucidate the underlying mechanisms.