Enhancement of cation diffusion rates across the 410-kilometer discontinuity in Earth's mantle

Rates of cation diffusion (magnesium, iron, and nickel) have been determined in olivine and its high-pressure polymorph, wadsleyite, at 9 to 15 gigapascals and 1100 degrees to 1400 degreesC for compositions that are relevant to Earth's mantle. Diffusion in olivine becomes strongly dependent on composition at high pressure. In wadsleyite, diffusion is one to two orders of magnitude faster than in olivine, depending on temperature. Homogenization of mantle heterogeneities (chemical mixing) and mineral transformations involving a magnesium-iron exchange will therefore occur considerably faster in the transition zone than at depths of less than 410 kilometers.     

Factors affecting the use of chlorine in the spin‐chilling of eviscerated poultry

Conditions have been determined under which chlorination can be used to eliminate both faecal and spoilage bacteria from the water used for chilling eviscerated poultry carcasses, thus avoiding any hazard from cross‐contamination.

All combinations of three rates of water usage (2.5, 5 or 8 1 per carcass) and three concentrations of total residual chlorine (10 to 15, 25 to 30 or 45 to 50 ppm), obtained by the addition of sodium hypochlorite, were compared. It was found that the majority of bacteria present were destroyed by the use of 45 to 50 ppm of total chlorine in conjunction with 5 1 of water per carcass. When the rate of water usage was increased to 8 1 per carcass it was found that 25 to 30 ppm of residual chlorine in the chill‐water gave comparable results.

The effect of water usage on the concentrations of free residual chlorine present in the chill‐water during processing is discussed. When chlorine gas was added continuously at a fixed concentration to the input water the concentration of total residual chlorine decreased in each chiller. This method of chlorination was found to be less effective in destroying bacteria than the hypochlorite method which could be used to vary the amount of added chlorine in order to maintain the required total residual concentration during processing.     

Lipids of the living coelacanth, Latimeria chalumnae

The muscle of Latimeria chalumnae contains 30 to 71 percent (dry weight) of lipid deposited extracellularly. Wax esters constituted 90 percent or more of the lipids from muscle and fat storage tissues. These esters, by gaschromatographic analysis, consisted of C(30) to C(40) homologs with one or two double bonds.     

Pulmonary ventilation measured from body surface movements

Changes in anteroposterior diameters of the rib cage and abdomen are sensed with magnetometers and summed to give outputs which are very nearly linearly related to changes in lung volume. The volume events of breathing can be measured without recourse to a mouthpiece or face mask, other than for calibration, and with minimal encumbrance to the subject.     

天津市种植业现代化的对策研究

经济体制改革以来,天津农业、农村经济社会有了长足发展,提前完成了党中央提出的第二步战略发展目标,基本实现小康,为农业、农村现代化建设提供了良好的经济社会环境、物质基础和物质技术条件。为落实党的十五届三中全会 决定 和江泽民同志关于 沿海发达地区要率先基本实现农业现代化"的指示精神,本文仅就天津种植业现代化的对策谈点粗浅看法。基本思路是:在加大政府组织推动和扶持力度的同时,采取 一个稳定、二个加大、三个完善、四个提高"的综合对策措施,整体推进种植业现代化进程     

Water movement and macroporosity of an Australian Alfisol under different tillage and pasture conditions

We assessed the effect of different tillage practices (i.e. conventional tillage and direct drilling) and pasture conditions on the infiltration and distribution of infiltrated rain water in an Australian Alfisol. Bromide was used as a tracer for the infiltrated rain under simulated rainfall conditions. The different infiltration patterns were then related to the macroporosity of the soils.

A 25-year-old permanent pasture was found to have the highest density (number per area) of macropores and percentages of transmitting macropores. A 9-year-old pasture phase in a pasture/crop rotation did not fully restore the macroporosity of the soil. Conventional cultivation by scarifying to 0.1 m for 4 years significantly reduced macropore density as well as continuity when compared with the pasture soil. The reduced macroporosity led to increased run-off by reducing preferential flow and altered the pathway of infiltrated water movement. As a consequence, the increase in water content below 0.1 m in the cultivated soil was predominantly from downward displacement of original soil solution, resulting in more leaching. The infiltrated rain water largely remained on the surface 0.1-m layer. In contrast, macroporosity found under direct drilling was similar to that of the pasture soil.