首页> 外文会议>IFIP WG 5.14 International conference on computer and computing technologies in agriculture >Impact of Simulated Irrigation with Treated Wastewater and Saline-Sodic Solutions on Soil Hydraulic Conductivity, Pores Distribution and Fractal Dimension
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Impact of Simulated Irrigation with Treated Wastewater and Saline-Sodic Solutions on Soil Hydraulic Conductivity, Pores Distribution and Fractal Dimension

机译:经处理的废水和盐碱溶液模拟灌溉对土壤水力传导率,孔隙分布和分形维数的影响

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Irrigation with treated wastewater which has the characteristics of higher salt content, larger sodium adsorption ratio (SAR), and more organic matter and suspended particles can cause the deterioration of the soil environment. Ordinary water, treated wastewater, and saline-sodic solutions with SAR = 3, 10 and 20 (mmol_cL~(-1))~(0.5), respectively, were used as five irrigation water types, and the changes of soil saturated hydraulic conductivity (K_s), soil pores distribution, and soil pores single fractal dimension (D_m) were studied after simulated irrigation for 1 and 2 years with simulated irrigation systems, which consisted of soil bins and simulated evaporation systems. The results showed that soil K_s in the following descending order: CK > SAR3 > WW > SAR10 > SAR20, and the adverse effects on soil K_s caused by suspended solid particles and dissolved organic matter might play a more significant role than sodium in treated wastewater. The 0-5 cm soils had a smaller single soil pore area but larger pores quantity after simulated irrigation, the distribution of soil pores which was irrigated with treated wastewater had a smaller change compared with saline-sodic solutions treatments, and it showed the soil pores structure binary image was an effective method to analysis soil pores distribution. Soil D_m increased after simulated irrigation, and the smallest was the soil simulated irrigation with treated wastewater for 1 year, because the plugging and filling of suspended particles and dissolved organic matter in treated wastewater made the soil pores well distributed, but the soil D_m did not increase with increasing of SAR levels in irrigation waters. The relative SAR levels irrigation to soils and soil K_s had a good linear correlation relationship, while the relationship between soil D_m and the relative SAR levels irrigation to soils was very complicated. The soil D_m which calculated from soil binary images could not well reflect the hydraulic conductivity of saturated soil. Irrigation with treated wastewater had a greater effect on soil K_s than soil D_m, comparing with saline-sodic solutions which had the similar SAR value. It was suggested that the future research should consider both the horizontal and vertical directions of soil D_m to well reflect the soil K_s.
机译:经过处理的废水的灌溉具有较高的盐含量,较大的钠吸附率(SAR),更多的有机物和悬浮颗粒,这会导致土壤环境恶化。分别将SAR = 3、10和20(mmol_cL〜(-1))〜(0.5)的普通水,处理后的废水和盐碱溶液作为五种灌溉水类型,并分析了土壤饱和导水率的变化在模拟灌溉系统(包括土壤箱和模拟蒸发系统)模拟灌溉1年和2年后,研究了土壤的K_s,土壤孔隙分布和土壤孔隙的单分形维数(D_m)。结果表明,土壤K_s按以下降序排列:CK> SAR3> WW> SAR10> SAR20,悬浮固体颗粒和溶解有机物对土壤K_s的不利影响可能比钠在处理废水中起更大的作用。 0-5 cm土壤模拟灌溉后单孔面积较小,但孔隙数量较大,与盐溶液处理相比,用处理过的废水灌溉的土壤孔隙分布变化较小,表明土壤孔隙结构二值图像是分析土壤孔隙分布的有效方法。模拟灌溉后,土壤D_m增加,最小的是处理废水为1年的模拟灌溉,因为处理后的废水中悬浮颗粒和溶解性有机物的堵塞和填充使得土壤孔隙分布均匀,但土壤D_m没有随灌溉水中SAR值的增加而增加。土壤相对SAR水平与土壤K_s的灌溉具有良好的线性相关关系,而土壤D_m与土壤相对SAR水平的灌溉与土壤的关系非常复杂。由土壤二值图像计算得到的土壤D_m不能很好地反映饱和土壤的水力传导率。与具有类似SAR值的盐溶液相比,用处理过的废水灌溉对土壤K_s的影响要大于对土壤D_m的影响。建议未来的研究应考虑土壤D_m的水平和垂直方向,以很好地反映土壤K_s。

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