Antiproliferative activities of citrus flavonoids against six human cancer cell lines

Citrus fruits contain high concentrations of several classes of phenols, including numerous hydroxycinnamates, flavonoid glycosides, and polymethoxylated flavones. The latter group of compounds occurs without glycosidic linkages and has been shown to inhibit the proliferation of a number of cancer cell lines. This antiproliferative property was further demonstrated against additional human cancer cell lines, and the antiproliferative actions of a series of synthetic methoxylated flavones were also studied. Similar to the naturally occurring compounds, the synthetic compounds exhibited strong antiproliferative activities. In many cases the IC(50) values occurred below 10 microm. Other hydroxylated flavone and flavanone aglycons also exhibited antiproliferative activities against the cancer cell lines, with the flavones showing greater activities than the flavanones. Glycosylation of these compounds removed their activity. The strong antiproliferative activities of the polymethoxylated flavones suggest that they may have use as anticancer agents in humans.     

Differentiation of physical from chemical toxicity in solid waste fish bioassays

This study showed that particulate (i.e., physical) toxicity was responsible for rainbow trout deaths in bioassays with two separate solid wastes. This conclusion was based on: (1) fish necropsies which indicated physical damage to gills but no evidence of chemical damage to liver or kidney, (2) chemical analyses which indicated that levels of Priority Pollutants and other target compounds were too low to cause the observed toxicity, (3) structural and chemical analyses of the waste particles which showed that these consisted of inert materials, and (4) the use of centrifugation techniques to remove most of the suspended particulate material in bioassay tanks resulting in an elimination of most of the toxicity. The particles associated with the lethal effects were approximately 5 to 10 μm in size. Regulatory testing of solid wastes must distinguish physical and chemical toxicity since disposal options can vary depending on the mode of toxicity. For instance, chemical toxicity raises concern regarding leaching through soils into groundwater, whereas if physical particles are responsible for toxicity, such leaching is not of concern.     

Quantitative relationships between morphology and current soil hydrology in some Alfisols in semiarid tropical Australia

The shallow groundwater hydrology of a sequence of red, yellow, and grey earths (Paleustalfs, Plinthustalfs and Ochraqualfs of “Soil Taxonomy”) was monitored over a 9-year period (1973–1982) along a drilled transect of 30 boreholes near Torrens Creek, in northeastern Australia. Climatic analysis shows an aridic soil moisture regime under which soil water surpluses should not occur, and thus significant hydromorphism would not be expected in the soils. The present study has demonstrated, however, that profile saturation and groundwater tables may be expected to develop at various depths in the soils as often as 1 year in 3. Besides, strong linear relationships were found between a number of morphological features of the soils and various hydrological regimes currently active in the profiles: the depths to the upper limits of brown, brownish red, or red mottles, to the upper limit of ironstone gravels, and to the maximum content of clay are all most closely related to the mean position of the shallowest water tables observed; the depths to grey mottles and to mottles with chromas of two or less are most directly related to the depths at which the soils are saturated for 5 weeks; the depth to the maximum content of ironstone gravels and to the base of the solum are most closely associated with the depth at which the soils are saturated for 10 to 15 weeks; and dominantly grey colours in the strongly mottled subsols are best related to profile saturations for at least 21 weeks. The results indicate that the gley features present in the soil profiles could have developed, at least in part, in response to the current soil hydrological regime.     

Toxicity of lead nitrate to algae

The fixation of radioactive C was used to mesaure the toxicity of Pb(NO₃)₂ to five species of freshwater algae. Portions of unialgal cultures were inoculated into low salt medium and were used to test all species at 10, 20 and 30 ppm Pb. This medium approximated the salt concentrations of natural aquatic environments. Three different cell weights were used for each concentration of Pb and for the control to determine a relationship between cell weight and toxicity. The concentration of Pb causing a 50% reduction of¹⁴CO₂ fixation as compared to the control was called the ED₅₀ (median effective dose). These values were extrapolated from graphs of ppm Pb vs dpm mg^?1 dry cell weight. The ED₅₀ for three of the species tested (Anabaena, Chlamydomonas andNavicula) was between 15 and 18 ppm Pb. A desmid,Cosmarium, had an ED₅₀ of 5 ppm. This species has a higher surface: volume ratio than the other species tested and this may account for its increased sensitivity. An ED₅₀ forOchromonas was not obtained. Throughout this experiment the fixation of¹⁴CO₂ increased with increasing Pb concentrations and is not readily explained.     

Effects of increasing acidity on aquatic protozoan communities

Laboratory tests were conducted to evaluate the chronic effects of increased acidity on protozoan communities. Taxonomic richness of the protozoan component of these communities was severely affected at pH ≤ 5.33. Taxonomic composition was significantly affected at much higher pH. A permissible concentration was defined as the pH affecting no more than 20% of the species and estimated from concentration-response regression as 6.92 (5.92 to 8.04) pH units. A similar value estimated from more conventional chronic toxicity tests was 6.28 (6.16 to 6.45) pH units. Bacterial abundance decreased at pH levels ≤ 5.34 pH units. Other nontaxonomic responses (e.g., biomass, algal biomass, fungal biomass, net oxygen metabolism) were not sensitive to increases in acidity.     

The hydrolysis of kaolinitic soils as affected by the type of the exchangeable cation

The hydrolysis of four kaolinitic soils from the Transvaal (RSA), and the effects of exchangeable Na, Ca and Mg were studied by monitoring the changes in the electrical conductivity of the soil suspension with time. The rate of the hydrolysis was found to be linearly related to the square root of time. The rates of the hydrolysis of the Half-Way House and Krugersdorp soils were appreciably lower than those of the Potchefstroom and Amsterdam soils, and rates reported in the literature for smectite soils. This was probably because of the low content of hydrolysable bases in the Half-Way House and Krugersdorp soils, resulting from the low cation exchange capacity of their clay fraction. The extensive hydrolysis observed in the Potchefstroom and Amsterdam soils could be ascribed to the presence of significant amounts of smectite in the former and high silt content in the latter; both factors are known to enhance the rate of weathering and hydrolysis. With the exception of the Potchefstroom soil, the rate of hydrolysis was not affected by the cationic composition of the adsorbed phase. Contrary to expectations, exchangeable Mg did not inhibit hydrolysis in the soils studied, probably because of the limited isomorphic substitutions in kaolinite which lead to very small amounts of octahedral Mg in the crystal. The hydrolysis of the Potchefstroom soil was enhanced in the presence of exchangeable Mg compared to exchangeable Ca; the reason for this is not fully understood.     

Influence of soil properties on the vertical movement of genetically-marked Pseudomonas fluorescens through large soil microcosms

Summary Vertical translocation of the introduced transposon Tn5-tagged Pseudomonas fluorescens cells was studies after irrigation of 50-cm long soil columns of loamy sand. The soil in the columns was slowly brought to saturation using groundwater, and enough water was then slowly added to permit collection of the percolated water. Introduced bacteria were transported to lower soil layers to a significantly higher degree in undisturbed soil cores than in repacked cores; water transport was hampered in both core types due to high soil bulk densities. Soil bulk density affected the degree of transport of the introduced cells; progressively more cells were translocated to deeper soil layers and into the percolation water at decreasing soil bulk densities. Repeated percolation of soil at a bulk density of 1.25 caused an increase in Tn5-tagged cell numbers in the lower soil layers and in the percolated water. Further, cells initially introduced into a dry (5.3% moisture) soil were translocated to a lesser extent than cells introduced into a wetter (13% moisture) soil. Finally, wheat roots enhanced the water-induced transport of introduced cells to the 40- and 50-cm deep soil layers and into the effluent, but not to the remaining soil layers. Large soil columns such as those used in the present study are useful in assessing the transport and survival of introduced bacterial cells in soils under a variety of simulated environmental conditions.     

Flavor release measurement from gum model system

Flavor release from a mint-flavored chewing gum model system was measured by atmospheric pressure chemical ionization mass spectroscopy (APCI-MS) and sensory time-intensity (TI). A data analysis method for handling the individual curves from both methods is presented. The APCI-MS data are ratio-scaled using the signal from acetone in the breath of subjects. Next, APCI-MS and sensory TI curves are smoothed by low-pass filtering. Principal component analysis of the individual curves is used to display graphically the product differentiation by APCI-MS or TI signals. It is shown that differences in gum composition can be measured by both instrumental and sensory techniques, providing comparable information. The peppermint oil level (0.5-2% w/w) in the gum influenced both the retronasal concentration and the perceived peppermint flavor. The sweeteners' (sorbitol or xylitol) effect is less apparent. Sensory adaptation and sensitivity differences of human perception versus APCI-MS detection might explain the divergence between the two dynamic measurement methods.     

Solvent-extractable lipids in an acid andic forest soil; variations with depth and season

Total lipid extracts from an acid andic soil profile located on Madeira Island (Portugal) were analysed using gas chromatography (GC) and GC-mass spectrometry (GC/MS). The profile was covered mainly by grass. Bulk soil characteristics determined included soil pH (H₂O) ranging from 4.5 to 4.0 and TOC, ranging from 84 to 30 g kg⁻¹. A decrease of the contribution of lipids per TOC with depth was observed. The absence of typical bacterial markers might be an indication for reduced bacterial activity, most likely related to the low soil pH and the presence of Al and Fe (oxides). The distribution observed in the top layer with a dominant C₂₆n-alkanol, steroids and triterpenoids, reflected mainly an input by grass leaves. A strong decrease in both relative and absolute concentration of these leaf-derived compounds was observed when comparing the litter layer with the mineral soil. The presence of C₂₂-C₃₂n-alkanoic acids, C₂₂-C₂₆ ω-hydroxy acids, C₃₁n-alkane and C₂₂-C₃₂n-alkanols observed in the sub-soil is indicative of an important contribution by (grass) roots. In summer, a signal most likely reflecting the leaching of microbially derived products from the litter and/or aerial vegetation at the surface was observed.