Variations of well water radon in Virginia and Maryland.

In north-central Virginia and south-central Maryland, municipal water supplies obtained from reservoirs provide radon-free potable water. However, about 10 percent of the population consumes well water. Radon in drinking water from some wells exceeds 4,000 pCi/L. Only about 30% of the radon is lost between the well storage tanks and the homes. The average radon concentration is about 2,000 pCi/L, which greatly exceeds the U.S. Environmental Protection Agency's recommended Maximum Contamination Level of 300 pCi/L. In this study of a geologically diverse area, the well water comes from granite (radon averages about 3,000 pCi,/L), schist and phyllite (about 2,000 pCi/L), sandstone (about 1,500 pCi/L), and quartzite (about 1,100 pCi/L). Aeration experiments on well water in storage tanks indicated that about 60-70% can be removed using a splash box with an exhaust fan on the storage tank, and about 60-70% can be removed using bubble aeration. About 90% of the radon can be removed by the simultaneous use of bubble aeration, splash box, and an exhaust fan. However, this combination does not become less efficient through time. Passing the water through tanks of activated charcoal can remove about 90% of the radon, though the charcoal becomes less efficient over an interval of a few months.

An environmentally benign soybean derived fuel as a blending stock or replacement for home heating oil.

The use of bio-derived materials both as fuels and/or as blending stocks becomes more attractive as the price of middle distillate fuels, especially home heating oil, continues to rise. Historically, many biomass and agricultural derived materials have been suggested. One of the most difficult problems encountered with home heating oil is that of storage stability. High maintenance costs associated with home heating oil are, in large part, because of this stability problem. In the present research, Soygold, a soybean derived fuel, was added in concentrations of 10%-20% to both a stable middle distillate fuel and an unstable home heating oil. Fuel instability in this article will be further related to the organo-nitrogen compounds present. The soy-fuel mixtures proved stable, and the addition of the soy liquid enhanced both the combustion properties, and dramatically improved the stability of the unstable home heating oil.

A two-year study of seasonal indoor radon variations in southern Maryland.

The concentrations of indoor radon in the basements of homes located in southern Maryland average about 1.3 times the first floor radon concentrations. Particular geological units tend to be associated with higher indoor radon. In the study area, homes underlain by phyllite were mostly above 4 pCi/liter (the US Environmental Protection Agency 'action level'). Comparative studies between indoor radon and total-gamma aeroradioactivity show that aeroradioactivity can be accurately used to estimate community radon hazards. When combined, geology and aero radioactivity can be used to identify problem homes.

A 2-year study of seasonal indoor radon variations in northern Virginia.

The concentrations of indoor radon in the basements of homes located in northern Virginia average about 1.4 times the first-floor radon concentrations. Basement indoor radon concentrations exhibit seasonal variations that can be related to home use patterns of the occupants. Little indoor radon difference was seen between homes that have concrete block basement walls and poured concrete basement walls, but homes that use oil or gas furnaces for heating have approximately 25% lower indoor radon than homes that use electrical heating systems. Particular geological units seem to be associated with elevated indoor radon concentrations, and several units are associated with indoor radon concentrations that exceed 4 pCi/l (the U.S. Environmental Agency "action level") at some time in more than 40% of the homes. Comparative studies between indoor radon and total gamma aeroradioactivity show that aeroradioactivity can be accurately used to estimate community radon hazards. When combined with information about the home heating system, geology and aeroradioactivity can be used to identify problem homes.

Seasonal indoor radon variations related to precipitation.

Indoor radon concentrations show a strong dependence on weather. Winter tends to be associated with higher than average indoor radon, and summer with lower than average. However, in northern Virginia, the summer of 1988 was wetter than the summer of 1987. Consequently, the regional indoor radon during the summer of 1988 was about 30% higher than during the summer of 1987, and indoor radon during the summer of 1988 actually exceeded the indoor radon level of the 1987-1988 winter.

Indoor radon and well water radon in Virginia and Maryland.

The domestic use of radioactive water has long been a cause for concern, but only a few studies have examined prolonged exposure to radionuclide concentrations found in natural settings. This paper reports on the indoor radon concentrations from 1,500 homes in northern Virginia and southern Maryland and well water radon from 700 homes in the same area. Indoor radon concentrations are almost all between 1 and about 40 pCi/L. The winter season shows the highest values with about 40% of the homes over the US EPA action level of 4.0 pCi/L. The summer season shows the lowest values with about 25% of the homes over this level. This seasonal variation is related to home ventilation. Waterborne radon in homes with private well ranges from about 100 pCi/L to about 8,000 pCi/L. In small homes, indoor radon can be significantly increased by outgassing of the home water supply, even at water radon levels of less than 10,000 pCi/L.

Winter-to-winter variations in indoor radon.

Indoor radon concentrations in northern Virginia and central Maryland show a strong dependence on weather. Winter tends to be associated with higher than average indoor radon, and summer with lower than average. However, compared to the winter of 1986-1987, the winter of 1987-1988 was warmer and drier. Consequently, winter-to-winter indoor radon decreased by about 25%. This winter-to-winter decrease is unexpectedly large, and simulates winter-to-summer variations that have been reported.

Terbium as a solid-state probe for RNA.

This paper continues previous work on the analysis of nucleic acid-terbium complexes in the solid state. The fluorescence excitation and emission spectra of the RNA-terbium(III) complex is reported. The fluorescence excitation and emission spectra of both the RNA-terbium(III) and DNA-terbium(III) complexes as trapped on millipore filters is reported. One hundred percent of the DNA combined with terbium was trapped on millipore filters. Deoxyribonucleic acid was recovered from DNA-terbium(III) complexes trapped on millipore filters using SDS-extraction. Energy transfer was shown to occur from the bases in nucleic acids to the terbium ion, whereas the actual binding of terbium to nucleic acids was due to phosphate groups. The relative fluorescence of homopolyribonucleotide-terbium complexes showed that the guanine moiety was responsible for most of the observed fluorescence. Binding studies showed an equal affinity of radioactive terbium for all the homopolyribonucleotides. The fluorescence of solid-state DNA and RNA terbium complexes was used to measure picomole quantities of DNA or RNA.

Measurement of binding of terbium to DNA.

This communication demonstrates further that terbium(III) can be used as a probe for DNA. The stoichiometry of terbium binding to DNA was measured by two new methods. In the first method, calf-thymus DNA was titrated with radioactive terbium-160, which is an isotope of the common terbium-159. The resulting DNA-terbium complex was trapped and measured on millipore filters. In the second method, a peak of UV absorption of terbium was found at 219 nm and was used to measure stocichiometry. By both methods, the stoichiometry of binding was one Tb(III) for each three available phosphate groups in DNA. Finally, a rapid method was developed using terbrium-160 to measure the amount of nucleic acid in a solution.

Terbium as a fluorescent probe for DNA and chromatin.

Terbium reacted with DNA and chromatin to form a complex in which terbium acted as a sensitive fluorescent probe. By measuring the narrow-line emission of Tb-3+ when DNA is selectively excited, the relative amount of Tb-3+ bound to the DNA can be calculated. Terbium was bound to DNA until one Tb-3+ was present for each phosphate group. After this point no more terbium was bound. TbCl3 was bound to chromatin in a linear manner until approximately 0.48 TbCl3 was added for each phosphate group in the chromatin-DNA solution. From these data it appears that 52% of the phosphate groups in chromatin were unavailable for binding. The binding of Tb-3+ to DNA can be reversed by prolonged dialysis against 0.5 M NaCl and chelating agents. The terbium ion is ideal in that it binds DNA tight enough so that completion of the reaction can be assumed but loose enough so that it can be removed by gentle means. Low concentrations of salt (up to 2 mM NaCl) enhance the quantum efficiency. Below pH 3 and above pH 7 the DNA-terbium complex will not form. Between pH 3 and pH 7 the quantum efficiency of the DNA terbium complex increases from either pH to a maximum at pH 5.5 to 5.6. Several biochemical uses for Tb-3+ ion are suggested.

Growth hormone responses to L-dopa in depressed patients.

Plasma human growth hormone responses to oral administration of 500 milligrams of L-dopa were analyzed in three groups of subjects: normals, age 20 to 32; normals, age 48 to 68; and unipolar depressed patients, age 45 to 68. While only 7 percent of the young normals had deficient human growth hormone responses to this stimulus, 36 percent of the older normals and 77 percent of the depressed patients failed to have adequate responses, suggesting an effect of age and a further effect of depressive illness. Because the release of human growth hormone appears to be closely related to brain catecholamine metabolism, the deficient responses in the depressed patients may provide further support to the concept of a neurochemical defect in depressive illness.