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Influence of Anionic Surfactant on Saturated Hydraulic Conductivity of Loamy Sand and Sandy Loam Soils

机译:阴离子表面活性剂对壤土和砂质壤土饱和导水率的影响

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Surfactants released into the terrestrial environment in large amounts can potentially alter the physical, chemical and biological properties of soils, particularly the saturated hydraulic conductivity ( K s ). Unfortunately findings regarding this process are quite limited. In this study, column tests were used to analyze the effects of Aerosol 22, a widely used anionic surfactant, on K s of loamy sand and sandy loam soils. Solutions were injected into columns from the bottom with controlled pressure heads. Both the overall K s of columns and the K s of 6 layers at distances of 0–1 cm, 1–3 cm, 3–5 cm, 5–7 cm, 7–9 cm, and 9–10 cm from the bottom, were continuously monitored before and after the surfactant injections. Results showed that the overall K s of all columns decreased after 2–4 pore volumes of the surfactant injections. However, stabilization and even increase at the beginning of the surfactant injection was also observed due to the different K s variations in different layers. Specifically, a surfactant injection of 2–4 pore volumes continuously decreased the K s of the 0–1 cm layers which yielded a K s reduction of two orders of magnitude and dominated the K s variations of the column. In contrast, an increase in the K s of the 1–3 cm and 3–5 cm layers was more likely, while K s variation of the 5–10 cm layers was less likely. We hypothetically attributed the K s variations to the swelling of clay, the collapse of soil aggregates and subsequent particle displacements from surfactant adsorption, which caused pore clogging in the bottom 0–1 cm layer and higher porosities in the layers above. The adsorption of the surfactant aggregates and crystallization were also possibly thought to cause a pore clogging in the bottom layer thus decrease the surfactant concentration from the inlet, the severity of which affects these layers less at greater distances from the inlet. In view of the uncertainty showed by the experimental results, we also suggest to include more replicate columns in future studies, so as to increase the repeatability of the measurements.
机译:大量释放到地面环境中的表面活性剂可能会改变土壤的物理,化学和生物学特性,尤其是饱和导水率(K s)。不幸的是,有关此过程的发现非常有限。在这项研究中,使用柱测试分析了广泛使用的阴离子表面活性剂Aerosol 22对壤土和砂质壤土K s的影响。用可控压力头从底部将溶液注入到色谱柱中。距底部0–1 cm,1–3 cm,3–5 cm,5–7 cm,7–9 cm和9–10 cm的列的总K s和6层的K s在注射表面活性剂之前和之后,连续监测。结果表明,在注入表面活性剂的2-4个孔体积后,所有色谱柱的总K s均降低。然而,由于在不同层中不同的K s变化,在表面活性剂注入开始时也观察到稳定甚至增加。具体而言,注入2-4个孔体积的表面活性剂会连续降低0-1 cm层的K s,这会使K s降低两个数量级,并主导了色谱柱的K s变化。相反,1-3 cm和3-5 cm层的K s增大的可能性更大,而5-10 cm层的K s减小的可能性较小。假设我们将K s的变化归因于粘土的膨胀,土壤团聚体的崩塌以及随后由于表面活性剂的吸附而引起的颗粒位移,这些位移导致底部0–1 cm层的孔堵塞和上面各层的较高孔隙度。表面活性剂聚集体的吸附和结晶也可能被认为引起底层的孔堵塞,从而降低了来自入口的表面活性剂浓度,其严重性在距入口更大的距离处对这些层的影响较小。考虑到实验结果显示的不确定性,我们还建议在以后的研究中包括更多的重复色谱柱,以提高测量的可重复性。

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