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濕黏地播后鎮(zhèn)壓過程土壤-小麥交互模型參數(shù)標定
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江蘇省自然科學基金項目(BK20221187)和中國農(nóng)業(yè)科學院創(chuàng)新工程項目


Parameter Calibration of Discrete Element Model for Wet Clay Soil- Wheat Mixture for Simulating Compaction Process
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    摘要:

    離散元仿真是研究播后鎮(zhèn)壓過程中土下種子受力特性與移位規(guī)律的有效途徑,,土壤-種子離散元模型及其參數(shù)顯著 影響仿真結(jié)果,。但長江中下游濕黏地土壤含水率高、黏性強,,常規(guī)土壤參數(shù)無法與其物理性質(zhì)相匹配,缺乏準確的土壤- 小麥離散元模型參數(shù),。本研究對播后鎮(zhèn)壓過程中濕黏土與小麥交互模型的接觸參數(shù)進行標定,。基于物理實測試驗與顯著性分析試驗,,初步獲取參數(shù)取值范圍,,篩選出對自然堆積坡度系數(shù)影響顯著的參數(shù);通過響應面試驗,獲取各關(guān)鍵參數(shù)與坡 度系數(shù)的回歸模型和多組較優(yōu)土壤-土壤參數(shù)、土壤-小麥參數(shù)組合方案,,對比實際壓縮試驗與仿真試驗的位移-力曲線誤差,,篩選出最佳參數(shù)組合方案;通過對比準靜態(tài)壓縮試驗、滾動壓縮試驗及田間試驗的模擬值與實際值,,評估參數(shù)模型的準確性,。結(jié)果表明 :土壤-土壤恢復系數(shù)( CR1)、 土壤-土壤滾動摩擦因數(shù)( RF1),、 土壤-土壤表面能( SE1)對濕黏土自然 堆積坡度系數(shù)( CS1)有顯著影響;土壤-小麥靜摩擦因數(shù)( SF2),、 土壤-小麥滾動摩擦因數(shù)(RF2)、 土壤-小麥表面能( SE2)對 土壤-小麥混合物坍塌堆積坡度系數(shù)( CS2)有顯著影響;獲得最優(yōu)參數(shù)組合方案:CR1為0.12,、RF1為0.35,、SE1為3.90 J/m2、SF2 為 0.48,、RF2 為 0.29,、SE2 為1.69 J/m2;優(yōu)化模型下各驗證試驗的相對誤差分別為 7.16%(準靜態(tài)壓縮試驗)、10.41%(滾動 壓縮試驗),、14.42%(田間試驗),。研究結(jié)果可為鎮(zhèn)壓過程中土壤-種子互作特性研究和濕黏地小麥播種機設(shè)計提供參考。

    Abstract:

    Numerical simulations utilizing the discrete element method(DEM)represent a robust approach for investigating the dynamic properties and displacement behaviors of subsoil seeds during the process of post-sowing suppression. The parameters associated with the soil-seed discrete element model played a crucial role in determining the accuracy of the simulation outcomes. However, the wet clay prevalent in the middle and lower reaches of the Yangtze River exhibited elevated water content and significant viscosity. Consequently, conventional soil parameters failed to adequately represent the physical characteristics of this wet clay, resulting in a lack of precise parameters for the discrete element model of wet clay-wheat interactions. The contact parameters of the wet clay-wheat interaction model during post-sowing suppression were calibrated. Initially, based on physical tests and significance analysis, the initial range of parameter values was determined, followed by the identification of parameters that exerted a significant influence on the natural accumulation slope coefficient. Subsequently, a regression model was developed to establish the relationship between each key parameter and the slope coefficient by using response surface methodology. This process yielded multiple superior combinations of soil-soil and soil-wheat parameters. Thereafter, the discrepancies in the force-displacement curves between actual compression tests and simulation tests were analyzed to select the optimal parameter combination. Finally, the accuracy of the parameter model was assessed by comparing the simulated values with the actual results from quasi-static compression tests, rolling compression tests, and field tests. The results indicated that the soil-soil restitution coefficient(CR1), soil-soil rolling friction coefficient(RF1), and soil-soil interfacial surface energy(SE1)significantly influenced the natural accumulation slope coefficient of wet clay(CS1). Moreover, the soil-wheat static friction coefficient(SF2), soil- wheat rolling friction coefficient(RF2), and soil-wheat interfacial surface energy(SE2 )also had a significant impact on the natural accumulation slope coefficient of wet clay-wheat mixture(CS2). The optimal parameter combination was identified as follows:CR1 was 0.12, RF1 was 0.35, SE1 was3.90 J/m2, SF2 was 0.48, RF2 was 0.29, and SE2 was1.69 J/m2. Additionally, the relative errors for each validation test under the optimized model were 7.16% for the quasi-static compression test, 10.41% for the rolling compression test, and14.42% for the field test.

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羅偉文,申海洋,顧滿,凌潔,顧峰瑋,吳峰,胡志超.濕黏地播后鎮(zhèn)壓過程土壤-小麥交互模型參數(shù)標定[J].農(nóng)業(yè)機械學報,2024,55(s1):147-155. LUO Weiwen, SHEN Haiyang, GU Man, LING Jie, GU Fengwei, WU Feng, HU Zhichao. Parameter Calibration of Discrete Element Model for Wet Clay Soil- Wheat Mixture for Simulating Compaction Process[J]. Transactions of the Chinese Society for Agricultural Machinery,2024,55(s1):147-155.

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  • 收稿日期:2024-06-18
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  • 在線發(fā)布日期: 2024-12-10
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