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生化黃腐酸對鹽堿土水鹽運(yùn)移特征的影響
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國家自然科學(xué)基金重點(diǎn)項(xiàng)目(41830754),、國家自然科學(xué)基金青年科學(xué)基金項(xiàng)目(41907010),、國家自然科學(xué)基金面上項(xiàng)目(41977043)和中國博士后科學(xué)基金面上項(xiàng)目(2019M653708)


Effect of Biochemical Fulvic Acid on Water and Salt Transport Characteristics in Saline-alkali Soil
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    摘要:

    為改善鹽堿脅迫農(nóng)田土壤水鹽環(huán)境,、緩解西北干旱地區(qū)土地次生鹽漬化,通過一維垂直入滲試驗(yàn),,對不同生化黃腐酸施加量(0,、1,、2,、4、8g/kg)條件下新疆地區(qū)中度鹽堿土的水鹽運(yùn)移特征及入滲模型參數(shù)進(jìn)行了研究,。結(jié)果表明:在入滲結(jié)束后,,與未施加生化黃腐酸相比,施加量為1,、2,、4、8g/kg條件下的土壤累積入滲量分別增加了1.00%,、4.67%,、7.14%、3.44%,,土壤水分入滲速率隨著生化黃腐酸施加量的增加呈現(xiàn)先減小后增大的變化趨勢,,土壤剖面平均體積含水率分別增加了8.90%、17.70%,、20.41%,、11.67%;在0~20cm土層,,土壤平均脫鹽率分別為5.29%,、27.04%、42.77%,、14.74%,。Philip、Green-Ampt模型和代數(shù)模型均能較好地模擬不同生化黃腐酸施加量下土壤水分入滲特征,,且模型參數(shù)與生化黃腐酸施加量間存在函數(shù)關(guān)系,。與未施加生化黃腐酸相比,施加生化黃腐酸后土壤吸滲率S和土壤飽和導(dǎo)水率Ks均減小,,且隨著施加量的增加均呈現(xiàn)先減小后增大的變化趨勢,,施加量4g/kg時(shí)S、Ks最??;濕潤鋒處吸力Sf和綜合形狀系數(shù)α呈現(xiàn)先增大后減小的變化趨勢,施加量4g/kg時(shí)Sf,、α最大,。施加生化黃腐酸能夠顯著影響土壤水分入滲和水鹽運(yùn)移特征,,且施加量4g/kg對于中度鹽堿土具有較好的保水和脫鹽效果。

    Abstract:

    Chemical amendment is an effective measure to improve soil water and salt environment under saline alkali stress and alleviate land secondary salinization in arid areas of Northwest China. The water and salt transport characteristics and infiltration model parameters of medium saline-alkali soil at different biochemical fulvic acid (BFA) application rates (0g/kg, 1g/kg, 2g/kg, 4g/kg and 8g/kg) were investigated through the one-dimensional vertical infiltration test. The results showed that after the infiltration, compared with no application of BFA, the cumulative infiltration amount at the BFA application rates of 1g/kg, 2g/kg, 4g/kg and 8g/kg was increased by 1.00%, 4.67%, 7.14% and 3.44%. The soil water infiltration rate was decreased first and then increased with the increase of BFA application, respectively, the average volumetric water content of soil profile was increased by 8.90%, 17.70%, 20.41% and 11.67%, respectively. In addition, at the 0~20cm soil layer, the average desalination rates were 5.29%, 27.04%, 42.77% and 14.74%, respectively. At the same time, the Philip model, Green-Ampt model and algebraic model could well simulate the soil water infiltration regulation at different BFA application rates, and there was a functional relationship between model parameters and BFA application rates. Compared with no application of BFA, the soil infiltration rate S and the soil saturated hydraulic conductivity Ks were decreased, and showed a trend of first decrease and then increase with the increase of the BFA application amount, and the minimum value was obtained at application rate of 4g/kg. The suction Sf at the wetting front and comprehensive shape factor α were increased first and then decreased, and the maximum value was obtained at application rate of 4g/kg. Therefore, the application amount of BFA significantly affected the characteristics of soil water and salt transport, and the application amount of 4g/kg had obvious effects on water conservation and desalination of medium salinealkali soil in Xinjiang.

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孫燕,王建,王全九,曲植,王春宏,張曦元.生化黃腐酸對鹽堿土水鹽運(yùn)移特征的影響[J].農(nóng)業(yè)機(jī)械學(xué)報(bào),2022,53(1):302-310. SUN Yan, WANG Jian, WANG Quanjiu, QU Zhi, WANG Chunhong, ZHANG Xiyuan. Effect of Biochemical Fulvic Acid on Water and Salt Transport Characteristics in Saline-alkali Soil[J]. Transactions of the Chinese Society for Agricultural Machinery,2022,53(1):302-310.

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  • 收稿日期:2021-10-16
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  • 在線發(fā)布日期: 2022-01-10
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