Modeling soil aggregate fracture using the discrete element method

被引:24
作者
Foldager, Frederik F. [1 ,5 ]
Munkholm, Lars J. [2 ]
Balling, Ole [1 ]
Serban, Radu [3 ]
Negrut, Dan [3 ]
Heck, Richard J. [4 ]
Green, Ole [5 ]
机构
[1] Aarhus Univ, Dept Mech & Prod Engn, Inge Lehmanns Gade 10, DK-8000 Aarhus C, Denmark
[2] Aarhus Univ, Dept Agroecol, Blichers Alle 20, DK-8830 Tjele, Denmark
[3] Univ Wisconsin, Dept Mech Engn, 1513 Univ Ave, Madison, WI 53706 USA
[4] Univ Guelph, Sch Environm Sci, Guelph, ON N1G 2W1, Canada
[5] Agro Intelligence ApS, Agro Food Pk 13, DK-8200 Aarhus N, Denmark
关键词
DEM; Aggregate strength; Aggregate fracture; Soil modeling; TENSILE-STRENGTH; SIMULATION; PARAMETERS; PARTICLES; DYNAMICS; POROSITY;
D O I
10.1016/j.still.2021.105295
中图分类号
S15 [土壤学];
学科分类号
090301 [土壤学];
摘要
The Discrete Element Method (DEM) is a suitable approach for modeling and simulating arable soil and tillage processes. In this work, we focus on modeling soil fragmentation which is a vital element of many soil treatments. We present a method for computing the indirect tensile strength of soil aggregates through simulation. DEM aggregates are constructed as spherical clusters of smaller spherical particles. A number of indirect tensile tests are conducted using simulated aggregates from which the critical polar force and tensile strength are identified. We propose a method for introducing random voids such that the distribution of simulated tensile strength corresponds to a given Weibull distribution. We propose to scale the number of voids linearly with the measured porosity of the aggregates. This approach showed better performance than introducing a constant number of voids. We identified that the friction between the sub-spheres can be related to the characteristic strength and the number of voids is related to the spread of strengths in the Weibull distribution. The calibration and validation are performed on experimental data. Based on this approach, the synthetic DEM aggregates allow for deriving the aggregate strength as a function of aggregate size. The results are based on fracturing individual aggregates but can be extended to simulations involving multiple interacting aggregates.
引用
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页数:11
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