A seven channel microwave radiometer has previously been developed for the Department of Energy Atmospheric Radiation Measurement Unmanned Aerospace Vehicle program. The instrument is designed to measure precipitable water vapor and cloud liquid water from board a DHC-6 (Twin Otter) chase plane for a remotely piloted vehicle. Five of the seven channels are centered about the 22.235 GHz water vapor absorption line. The other two channels are centered about 36.5 GHz and 89.0 GHz. Four calibration references exist for each channel within the radiometer. A digital computer is used to synchronize the switching of the circulators to the sampling of the analog-to-digital converters, thus, the timing of the data acquisition is programmable. By shortening the duty cycle of the calibration sequence and averaging the reference samples over an extended period of time radiometric precision approaching that of a total power radiometer is achieved. The channel selection along with its novel calibration scheme make this instrument a unique research tool.
An investigation and comparison has been made of exchange reactions in synthetic fluorhectorites of exchange capacities 150 and 90 mequiv. per 100 g. The exchanges studied were of Na+ by K+, Rb+, Cs+, Ca2+, Sr2+, Ba2+, Co2+, Ni2+, Cu2+, and Cu(NH3)42+. Isotherms for exchanges of Na+ by the alkaline earth metal ions and by Co2+, Ni2+, and Cu2+ were reversible, and were analysed to give thermodynamic equilibrium constants, standard free energies, and activity coefficients of the intracrystalline ions. The exchanges involving K+, Rb+, Cs+, and Cu(NH3)42+ were irreversible and resulted in ion fixation. The fluorhectorites were notable for the strong selectivities shown towards K+, Rb+, and especially Cs+. The latter ion was quantitatively removed up to the exchange capacities of the fluorhectorites. The fixation reactions resulted from preferential solvation of K+, Rb+, and Cs+ by lattice oxygens, so that the exchanged forms were anhydrous and the cations, partially recessed into sheets of oxygens, were immobilised.
Contents: Geology; Foundation and Abutments; Embankment; Settlement; Slope Stability; Seepage Control; Diversion and Closure; Instrumentation; Construction Notes; Operational Notes.
Plants release many strange and complex substances - such as terpenes, alkaloids and phenols - in response to attack, and Daedalus sees this as a splendid new source of herbal fuel. He proposes to enclose a plantation of shrubs or trees in a huge plastic-film greenhouse and to stimulate them to produce terpenes, which can then be extracted from the air.
Quarries and minesites are examples of extreme disturbance. Frequently, materials that form soil are scarce and ecological restoration is easier to achieve than productive land. Establishment of soil microbial function is critical to ecological restoration and a key objective of the study. An organic fertilizer containing a mix of sewage and paper sludges was designed to promote soil functioning during the revegetation of slate waste. We compared soil formation under naturally established birch trees (Betula pubescens) on slate waste with that of container-grown seedling birches of local provenance in slate waste amended with either organic or mineral fertilizer. Hypotheses that an organic nutrient source would lead to more rapid establishment of microbial communities and nutrient cycling than mineral fertilizer, and result in a substrate biochemically comparable to that under naturally established revegetation, were supported.
In terrestrial environments, soil organic matter (SOM) is the largest organic carbon (C) pool. The quantity and quality of organic carbon in soils can be affected by vegetation through influencing the inputs and outputs of SOM. We examined how storage and quality of C in SOM were affected by vegetation under grass cover or single and a polyculture plot of Betula pendula, Alnus glutinosa and Fagus sylvatica. An acid hydrolysis approach was used to quantify three SOM fractions differing in biodegradability. Tree species identity and stand composition had no significant effect on the total amount of C stored in different SOM fractions to a depth of one meter. However, when examining individual SOM fractions in the upper layers of the soil profile, significantly more C was stored in the putatively more labile fractions 1 and 2 under F. sylvatica and A. glutinosa, respectively. In deeper soil layers, the highest storage of recalcitrant organic C was found under the tree polyculture. The vertical distribution of these three soil organic C pools was compared to C inputs via decomposed leaf litter. Our data indicated that in the tree species polyculture, combining litter inputs of multiple species can have a positive impact on the accumulation of acid resistant recalcitrant C in deep soil layers in 4years. This C fraction has the greatest potential for long-term sequestration.
Routine monitoring of commercial shellfish beds in the European Union currently focuses on quantifying the bacterial content within shellfish flesh as an indicator of faecal contamination. Previous studies have documented the presence of other significant bacterial reservoirs within commercial shellfish beds e.g. sediments. This study examined the importance of epizoic barnacles as a potential bacterial reservoir across three intertidal mussel (Mytilus edulis) beds in North Wales, UK. Results demonstrated that over 80% of the total coliform reservoir was held within the epizoic barnacles in comparison to the mussel flesh, concluding that epizoic barnacles represent a significant bacterial reservoir within commercial shellfisheries. The implications for the shellfish industry are discussed.