王辉, 黄正忠, 谭帅, 胡传旺, 武芸. 再生水灌溉对红壤水力特性的影响[J]. 农业工程学报, 2019, 35(17): 120-127. DOI: 10.11975/j.issn.1002-6819.2019.17.015
    引用本文: 王辉, 黄正忠, 谭帅, 胡传旺, 武芸. 再生水灌溉对红壤水力特性的影响[J]. 农业工程学报, 2019, 35(17): 120-127. DOI: 10.11975/j.issn.1002-6819.2019.17.015
    Wang Hui, Huang Zhengzhong, Tan Shuai, Hu Chuanwang, Wu Yun. Effects of irrigation with reclaimed water on hydraulic characteristics of red soil[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of the CSAE), 2019, 35(17): 120-127. DOI: 10.11975/j.issn.1002-6819.2019.17.015
    Citation: Wang Hui, Huang Zhengzhong, Tan Shuai, Hu Chuanwang, Wu Yun. Effects of irrigation with reclaimed water on hydraulic characteristics of red soil[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of the CSAE), 2019, 35(17): 120-127. DOI: 10.11975/j.issn.1002-6819.2019.17.015

    再生水灌溉对红壤水力特性的影响

    Effects of irrigation with reclaimed water on hydraulic characteristics of red soil

    • 摘要: 再生水长时间灌溉是诱发土壤水力特性演变的关键因素之一。该文采用再生水原液(reclaimed water,RW)以及再生水原液稀释2倍(RW-2)、4倍(RW-4)、6倍(RW-6)等4种不同浓度再生水水源,设置再生水连续灌溉与再生水-蒸馏水交替灌溉(ARW、ARW-2、ARW-4、ARW-6)2种灌溉模式,以蒸馏水连续灌溉(CK)为对照,持续对第四纪红壤进行干湿循环模拟灌溉,直到土壤入渗趋于稳定为止。采用压力膜仪法测定各灌溉处理后的土壤水分特征曲线,选择van Genuchten(VG)模型对其参数提取,分析了红壤水力特性的演变特征及其参数影响。结果表明:再生水灌溉显著影响了红壤的持水特性,促使红壤孔隙大小、数量及其分布发生演变,该变化规律与再生水水质浓度、灌溉模式关系密切。与CK相比,再生水连续灌溉模式RW、RW-2、RW-4、RW-6处理下,红壤有效水分别提高了5.4%、3.6%、14.6%、-8.1%;再生水-蒸馏水交替灌溉模式ARW、ARW-2、ARW-4、ARW-6处理下,红壤有效水分别降低了9.9%、23.3%、26.5%、16.9%。与CK相比,连续灌溉对红壤水力传导性无显著影响;而交替灌溉则影响显著,其土壤非饱和导水率、水分扩散度大体表现为CK>ARW-6?ARW-4>ARW>ARW-2。再生水灌溉对VG模型参数θs'、θr'、α、n均有显著影响;再生水的pH值、电导率及钠吸附比均与红壤有效水存在显著的相关性。该研究结果对红壤地区再生水长期灌溉利用风险评估提供了一定理论基础和技术支撑。

       

      Abstract: Abstract: With the rapid development of China's economy, the requirement for water resources from all walks of life is increasing. Using reclaimed water and other unconventional sources can greatly alleviate the contradiction between supply and demand for fresh water. However, long-term reclaimed water irrigation is one of the key factors that leads to the evolution of hydraulic characteristics of soil, and likely to increase the risk of soil degradation due to the high salt content of reclaimed water. As the irrigating water source, the reclaimed water discharged from the sewage treatment plant was selected in this test .During the wetting-drying cycle irrigation test, tested red soil was irrigated persistently with four kinds of reclaimed water with different concentrations, which were original reclaimed water (RW) and diluted concentration of 2 (RW-2), 4(RW-4), 6(RW-6) times. The selecting distilled water irrigation was control treatment (CK). Meanwhile, two irrigation modes applied to this study, such as continuous irrigation and alternate irrigation (irrigation with reclaimed water and distilled water alternately/ the corresponding treatments were expressed as: ARW, ARW-2, ARW-4, ARW-6). Finally, sampling was not started until the infiltration rate tended to stabilize after three times under the same treatment. In order to analyze the hydraulic characteristics of red soil, the soil water characteristic curve was measured by pressure membrane method, relying on van Genuchten (VG) model to extract the parameters of the water characteristic curve after fitting it. The results indicated that reclaimed water irrigation significantly affected the water retention of red soil and accelerated the evolution of pore's size, quantity and distribution in red soil. The variation law was closely related to the concentration of reclaimed water and irrigation mode. Compared with CK treatment, continuous irrigation RW, RW-2, RW-4, RW-6 treatments, available water content in turn increased by 5.4%, 3.6%, 14.6%, -8.1%;Alternate irrigation ARW, ARW-2, ARW-4, ARW-6 processing, available water content reduced by 9.9%, 23.3%, 26.5%, 16.9%, respectively. Compared with the control group, continuous irrigation had no significant effect on the unsaturated hydraulic conductivity of red soil, while alternate irrigation had significant effect. In the same moisture content, red soil unsaturated hydraulic conductivity and water diffusivity from big to small both could be described as CK?ARW-4>ARW-6>ARW>ARW-2 under alternative irrigation generally. Reclaimed water irrigation had significant influence on VG model parameters (θs', θr', α, n ), the pH, conductivity and sodium-adsorption ratio of reclaimed water were significantly correlated with the available water content of red soil. These results provided theoretical basis and technical support for the long-term utilization and risk assessment of reclaimed water in red soil areas. At present, reclaimed water and other low-quality water have not been put into agricultural production in south China. The change rules of water movement and retention in red soil under reclaimed water irrigation analyzed in this paper will have certain value and significance for the sustainable and efficient utilization and development of water resources, and also provide reference for the scientific irrigation of reclaimed water in south China because the red soil is the typical farming soil in this region.

       

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