首页> 外文期刊>International Agrophysics >Possible effects of soil contamination by light non-aqueous phase liquids (LNAPLs) on soil water parameters and their consequences.
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Possible effects of soil contamination by light non-aqueous phase liquids (LNAPLs) on soil water parameters and their consequences.

机译:轻质非水相液体(LNAPL)污染土壤对土壤水分参数及其后果的可能影响。

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摘要

In central Germany, a loess derived site contaminated with very different light non-aqueous phase liquids (LNAPLs) emanating from production of mineral oils, was evaluated with respect to soil water retention to investigate the conditions and possibilities of deep percolation. At 4 subsites, undisturbed cores (100 cm3) were sampled from profile depths ranging between 2 and 9 m. The water retention characteristics and bulk density were determined. Results indicate that in most cases > 50% of the pore volume (PV) is occupied by water held at matrix potentials of ?15000 hPa and only approximately 10% of PV may be occupied by quickly draining water (matrix potential > -60 hPa). LNAPLs strongly decrease the surface tension gamma to values ranging from20 to 45 m.Nm-1 and increase the angle of contact alpha to 20-45?(from literature) as compared to values of 72.75 mN.m-1 and 0?for pure water. Thus, it is almost impossible to derive the correct pore size distributions of the material studied and other contaminated material from the water retention characteristics. The effect of the changed surface tension and angle of contact on the water regime (deep percolation, capillary rise) of contaminated profiles results in an enhancement of deep percolationand a restriction in capillary rise.
机译:在德国中部,对黄土衍生场地的土壤保水能力进行了评估,以研究其深度渗滤的条件和可能性,该场地受到矿物油生产中产生的非常不同的轻质非水相液体(LNAPL)的污染。在4个子站点上,从2到9 m的剖面深度采样了未受干扰的岩心(100 cm3)。测定保水特性和堆积密度。结果表明,在大多数情况下,> 50%的孔体积(PV)被保持在?15000 hPa的基质电势下的水占据,而快速排干的水(矩阵电势> -60hPa)只能占据大约10%的PV。 。与纯净的72.75 mN.m-1和0°的值相比,LNAPLs极大地降低了表面张力gamma的值,范围从20到45 m.Nm-1,并将接触角α增加到20-45°(来自文献)。水。因此,几乎不可能从保水特性中得出研究材料和其他受污染材料的正确孔径分布。改变的表面张力和接触角对被污染轮廓的水分状况(深层渗透,毛细管上升)的影响导致深层渗透的增强和毛细管上升的限制。

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