共查询到10条相似文献，搜索用时 31 毫秒
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A. POULOVASSILIS 《European Journal of Soil Science》1974,25(1):27-33
Experiments, designed to test the non-uniqueness which has been reported in the relationship between moisture content and suction in porous materials during transient flow conditions, are escribed. When a vertical column of sand was brought to uniform moisture content and uniform suction in a draining condition by percolating a constant flow through it until apparent equilibrium conditions ensued and then placed horizontally at the same time as the flow was stopped, the suction was found to decrease with time over a period of a day, indicating that the sand was now wetting up. This decrease was smaller the drier the sand. However, when the column was left in a vertical position with the water percolating through it for three hours after apparent equilibrium conditions were reached, a small adjustment of moisture content and suction was observed; when it was then placed horizontally as in the previous experiments little decrease of suction was observed. No change in suction was observed in either case if the equilibrium condition was reached in a wetting porous material. These experimental results and those of previous workers are explained by the hypothesis that, during drainage, some water is left in pores from which the air-water interface has already retreated to drain through film flow, more slowly, subsequently to the continuous water body. Additional experiments showed that the release of entrapped air may have a small effect on the uniqueness of the moisture characteristics. 相似文献
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缺锰和多锰对番茄产量及风味品质的影响 总被引：2，自引：0，他引：2
通过设置不同的硫酸锰浓度并测定不同供锰水平下番茄的产量及与果实风味品质相关的指标,研究了缺锰和多锰对番茄产量和品质的影响。结果表明,无论缺锰还是多锰处理,番茄叶片叶绿素含量和产量都显著下降,叶绿素含量分别为正常处理的57.31%和61.50%,产量为58.25%和68.35%;叶片POD和SOD活性降低,以缺锰处理较为显著;缺锰和多锰处理的MDA含量分别高于对照71.07%和40.71%。缺锰和多锰处理导致果实的酸度分别增加37.4%和40.1%,可溶性固型物含量降低17.51%和13.19%,两者较正常锰处理均差异达到显著水平,Vc含量降低31.94%和9.45%;此外,2种处理果实中的活性物质番茄红素含量均下降34%左右,总酚和总黄酮含量下降30%~35%,总抗氧化力也明显降低,而且果实的芳香物质种类也少于正常处理。说明适宜的锰浓度是保证番茄高产、优质的重要因素。 相似文献
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上海郊区水田土壤,可以古岗为界分成东西两部分:浦东的沙泥、夹沙泥、黄泥头以及岗身的沟干泥是由长江沉积物发育起来的草甸土,地势较高(吴淞0.4米以上),地下水位较低(地面1米以下),质地偏中(轻壤-重壤),土壤通气孔隙较多,渗透性较好,因此土壤比较爽水,生产性能好,产量较高;浦西的青紫泥是由古太湖和其他许多湖荡港叉葑淤成陆的沼泽土,地势低洼(地面高程在吴淞零上2.2-3.5米),地下水位高(地面以下0.3-0.8米),质地偏粘(中壤-重壤),土壤通气孔隙少,毛管孔隙多,吸持力强,土壤透水性差,易于囊水,根系环境不良. 相似文献
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THE STUDY OF SOIL STRUCTURE IN THE FIELD AND THE LABORATORY 总被引：3，自引：0，他引：3
A.J. LOW 《European Journal of Soil Science》1954,5(1):57-74
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运用动态试验方法研究了久效磷在水及水生动植物内的吸收、转移、富集和排除的规律。水中久效磷随时间按Cow e~(-λwt)规律消失,面归方程为 _w=1.0000e~(-0.0749t).金鱼藻、螺蛳肉、鱼肉及底泥中久效磷及其代谢物按规律变化,各回归方程为:及水生动植物的生态富集系数按规律变化,各回归方程分别是:和。 相似文献