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首页> 外文期刊>Zeitschrift fuer pflanzenernaehrung und bodenkunde >Theoretical principles for modelling soil strength and wheeling effects — a review —
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Theoretical principles for modelling soil strength and wheeling effects — a review —

机译:模拟土体强度和轮子效应的理论原理 — 综述 —

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AbstractPhysical and mechanical processes in structured unsaturated soils are very complex and are still more difficult to understand or to predict if tillage processes and plant growth effects are included. Based on the definitions of stresses, strain and combined processes, mathematical models will be defined in the literature review and some proofs will be given.The stress‐strain‐failure processes are non‐linear and irreversible or hysteretic. They should be coupled as the various processes are not independent of each other. If mechanical properties and processes in structured unsaturated soils are considered, the stress and strain tensors have to be quantified by the combined application of Stress State Transducers (SST) and Displacement Transducer Systems (DTS) in order to derive the stress and strain components in soils.Depending on soil development or tillage system both stress and strain components vary to a great extent and result in differing physical and ecological soil properties. Each soil deformation has to be coupled to hydraulic properties, because deformation and failure in soils depend on the advection and diffusion processes and their history and vice versa. These coupled, non‐linear and hysteretic processes can be modelled using modern numerical methods, such as the finite element method (FEM). A brief description of the modelling procedures is given in this paper. Empirical models are available to define soil strength, stress distribution and changes in physical properties due to loading or loosening, their results can be primarily used as a first rough estimation e.g. for mapping purposes.However, the theoretical modelling procedures have now advanced beyond our understanding of these processes and our ability to measure the material parameters and the field boundary conditions. This paper describes some of these problems such as the coupled nonlinear irreversible behaviour of unsaturated structured soils. In addition the FEM approach as the most applicable instrument can be used to predict changes in ecological properties like permeability, moisture characteristics and failure/yield behaviour o
机译:摘要结构性非饱和土的物理力学过程非常复杂,如果包括耕作过程和植物生长效应,则更难理解或预测。基于应力、应变和组合过程的定义,在文献综述中定义数学模型,并给出一些证明。应力-应变-失效过程是非线性的、不可逆的或滞后的。它们应该是耦合的,因为各种过程不是相互独立的。如果考虑结构性非饱和土的力学性质和过程,则必须通过应力状态传感器(SST)和位移传感器系统(DTS)的组合应用来量化应力和应变张量,以便得出土壤中的应力和应变分量。根据土壤发育或耕作系统的不同,应力和应变成分都会有很大差异,并导致不同的物理和生态土壤特性。每种土壤变形都必须与水力特性相耦合,因为土壤的变形和破坏取决于平流和扩散过程及其历史,反之亦然。这些耦合、非线性和滞后过程可以使用现代数值方法(例如有限元法 (FEM))进行建模。本文简要介绍了建模过程。经验模型可用于定义土壤强度、应力分布和由于加载或松动引起的物理性质变化,其结果主要可用作首次粗略估计,例如用于测绘目的。然而,理论建模程序现在已经超出了我们对这些过程的理解以及我们测量材料参数和场边界条件的能力。本文描述了其中的一些问题,例如非饱和结构土的耦合非线性不可逆行为。此外,有限元法作为最适用的工具,可用于预测生态特性的变化,如渗透率、水分特性和破坏/屈服行为。

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