湿黏地播后镇压过程土壤-小麦交互模型参数标定
CSTR:
作者:
作者单位:

作者简介:

通讯作者:

中图分类号:

基金项目:

江苏省自然科学基金项目(BK20221187)和中国农业科学院创新工程项目


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

Fund Project:

  • 摘要
  • |
  • 图/表
  • |
  • 访问统计
  • |
  • 参考文献
  • |
  • 相似文献
  • |
  • 引证文献
  • |
  • 资源附件
  • |
  • 文章评论
    摘要:

    离散元仿真是研究播后镇压过程中土下种子受力特性与移位规律的有效途径,土壤-种子离散元模型及其参数显著 影响仿真结果。但长江中下游湿黏地土壤含水率高、黏性强,常规土壤参数无法与其物理性质相匹配,缺乏准确的土壤- 小麦离散元模型参数。本研究对播后镇压过程中湿黏土与小麦交互模型的接触参数进行标定。基于物理实测试验与显著性分析试验,初步获取参数取值范围,筛选出对自然堆积坡度系数影响显著的参数;通过响应面试验,获取各关键参数与坡 度系数的回归模型和多组较优土壤-土壤参数、土壤-小麦参数组合方案,对比实际压缩试验与仿真试验的位移-力曲线误差,筛选出最佳参数组合方案;通过对比准静态压缩试验、滚动压缩试验及田间试验的模拟值与实际值,评估参数模型的准确性。结果表明 :土壤-土壤恢复系数( CR1)、 土壤-土壤滚动摩擦因数( RF1)、 土壤-土壤表面能( SE1)对湿黏土自然 堆积坡度系数( CS1)有显著影响;土壤-小麦静摩擦因数( SF2)、 土壤-小麦滚动摩擦因数(RF2)、 土壤-小麦表面能( SE2)对 土壤-小麦混合物坍塌堆积坡度系数( CS2)有显著影响;获得最优参数组合方案:CR1为0.12、RF1为0.35、SE1为3.90 J/m2、SF2 为 0.48、RF2 为 0.29、SE2 为1.69 J/m2;优化模型下各验证试验的相对误差分别为 7.16%(准静态压缩试验)、10.41%(滚动 压缩试验)、14.42%(田间试验)。研究结果可为镇压过程中土壤-种子互作特性研究和湿黏地小麦播种机设计提供参考。

    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.

    参考文献
    相似文献
    引证文献
引用本文

罗伟文,申海洋,顾满,凌洁,顾峰玮,吴峰,胡志超.湿黏地播后镇压过程土壤-小麦交互模型参数标定[J].农业机械学报,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.

复制
分享
文章指标
  • 点击次数:
  • 下载次数:
  • HTML阅读次数:
  • 引用次数:
历史
  • 收稿日期:2024-06-18
  • 最后修改日期:
  • 录用日期:
  • 在线发布日期: 2024-12-10
  • 出版日期:
文章二维码