Wolery and Wang[6] used the EQ3/6 geochemical code and the Yucca Mountain Project high-temperature Pitzer model to predict the deliquescence of salt mixtures found in Yucca Mountain dust samples collected from exploratory tunnels.
The assignment of elutrition samples collected every 30 minutes to mixture components provided a good example of a slow transition of the network behavior across time.
Figures 5A and 5B show spectra from two clinical samples, each containing a mixture of two different viral BC types observed in samples collected during the 2005 2006 season.
These major congeners of the three commercial mixtures were detected in nearly all of the dust samples collected.
The mixture used in specimen preparation was designed to simulate the properties of the samples collected from depths up to 200 m at a drilling site in South Australia.
The first six samples collected between 0 and 150 minutes were assigned to one mixture component and six samples obtained from 240 to 390 minutes were assigned to the other mixture component.
All samples collected at the time of autopsy were snap frozen in a mixture of absolute ethanol and dry ice and subsequently stored at –70°C until tested.
Samples collected at intermediate time points (between 180 and 210 minutes) had a similar odds ratio to pertain to either mixture component.
Accordingly, for subsequent exposures to mixtures, water samples were collected only at t = 0. Throughout this article, pesticide exposures are reported in terms of nominal concentrations.
Samples of this mixture were collected using a precipitation funnel where components of the mixed plumes were discharged from the atmosphere with the rainfall.
