The luminescent properties of Sm2+ in strontium tetraborates (SrB4O7 : Sm2+)

The luminescence of Sm2+ in SrB4O7 was studied as a function of temperature from 10 K up to 600 K. According to the high-resolution spectra of Sm2+ in matrix at 10 K, the line numbers of D-5(0)-F-7(J) transitions were 1, 3, 5 for J = 0, 1, 2, respectively. The D-5(1)-F-7(J) (J = 0, 1, 2) transitions were observed at high temperature. The intensities of D-5(0)-F-7(J) transitions increased up to 400 K and then decreased with increase in temperature. 4f(5)d(1)-4f(6) transition of Sm2+ appeared at high temperature. (C) 1999 Elsevier Science Ltd. All rights reserved.

PREPARATION AND ELECTRICAL-PROPERTIES OF BISMUTH STRONTIUM DIMANGANESE HEXOXIDE [BISRMN2O6]

BiSrMn2O6 is prepared by solid state reaction at 850 degrees C. It is tetragonal with a= 0.7821nm c= 0.3790 nm. It is a black n-type semiconductor below 820K. Its resistivity is 3 Omega-CM at room temperature. A semiconductor -metal transition is observed around 820K, Bi1+xSr1-xMn2O6-y is a solid solution for -0.2 less than or equal to x less than or equal to 0.2. Its unit cell dimensions increase but resistivity decreases when the Bi contents increase.

Boron and strontium isotopic characterization of coal combustion residuals: validation of new environmental tracers.

In the U.S., coal fired power plants produce over 136 million tons of coal combustion residuals (CCRs) annually. CCRs are enriched in toxic elements, and their leachates can have significant impacts on water quality. Here we report the boron and strontium isotopic ratios of leaching experiments on CCRs from a variety of coal sources (Appalachian, Illinois, and Powder River Basins). CCR leachates had a mostly negative δ(11)B, ranging from -17.6 to +6.3‰, and (87)Sr/(86)Sr ranging from 0.70975 to 0.71251. Additionally, we utilized these isotopic ratios for tracing CCR contaminants in different environments: (1) the 2008 Tennessee Valley Authority (TVA) coal ash spill affected waters; (2) CCR effluents from power plants in Tennessee and North Carolina; (3) lakes and rivers affected by CCR effluents in North Carolina; and (4) porewater extracted from sediments in lakes affected by CCRs. The boron isotopes measured in these environments had a distinctive negative δ(11)B signature relative to background waters. In contrast (87)Sr/(86)Sr ratios in CCRs were not always exclusively different from background, limiting their use as a CCR tracer. This investigation demonstrates the validity of the combined geochemical and isotopic approach as a unique and practical identification method for delineating and evaluating the environmental impact of CCRs.