College of Agricultural Equipment Engineering, Henan University of Science and Technology, Luoyang, Henan, China.
PLoS One. 2023 Jan 17;18(1):e0280525. doi: 10.1371/journal.pone.0280525. eCollection 2023.
At present, the measurement of tillage depth is mainly based on manual measurement, but the manual raking method results in low measurement accuracy and high labor intensity. Due to the complexity of soil, theoretical research on tillage depth is relatively scarce. In order to provide a new research direction and research idea for soil stratification, topsoil was taken as the research object of this paper. The correlation between penetration resistance and penetration depth of a probe in a cultivated soil was studied, and a mathematical model was established. There is a certain similarity between the process of spherical cavity expansion and the process of probe penetration, so we introduced the theory of spherical cavity expansion into the modeling of penetration resistance of the cultivated soil. In this paper, the spherical cavity expansion theory of unsaturated soil was used as the basis for solving the penetration resistance. And the unified strength criterion was employed as a yield condition of the soil to set a stress solution and a displacement solutionin into of the probe penetrating into the elasto-plastic zone of the cultivated soil to determine the model of expansion force. We have carried out indoor tests to revise the expansion force model. Firstly, according to the range of soil density and water content in the field, the soil densities were classified into 1.1×103kg/m3, 1.2×103kg/m3 and 1.3×103kg/m3, and the water contents were divided into 10%, 15% and 20%. In addition, the orthogonal tests were performed at different levels. The soil was put into the barrel, and the probe was inserted into the soil in the barrel at the speed of 8mm/s to determine the test values of the change of the probe penetration resistance with depth. Finally, the expansion force model was fitted with the results of the indoor test, and coefficient B was introduced to express the influence degree of density and water content on the resistance. Coefficient B was substituted into the expansion force model to obtain the penetration resistance model of the cultivated soil. Through the goodness of fit analysis of the penetration resistance model, the results show that the overall average goodness of fit of the penetration resistance modelat was up to 0.871 at different water contents and densities, which was a good fit and could present novel insights into the study relating to soil stratification theory.
目前,耕作深度的测量主要采用人工测量,但人工耙地的方法导致测量精度低、劳动强度大。由于土壤的复杂性,耕作深度的理论研究相对较少。为了为土壤分层提供新的研究方向和研究思路,本文以表土为研究对象,研究了探针在耕作土壤中的穿透阻力与穿透深度的相关性,建立了数学模型。探针在耕作土壤中的穿透过程与球形孔扩张过程具有一定的相似性,因此将球形孔扩张理论引入耕作土壤的穿透阻力建模中。本文以非饱和土的球形孔扩张理论为基础,求解穿透阻力。并采用统一强度准则作为土壤的屈服条件,建立了探针进入耕作土壤弹塑性区的应力解和位移解,确定了膨胀力模型。我们进行了室内试验来修正膨胀力模型。首先,根据田间土壤密度和含水量的范围,将土壤密度分为 1.1×103kg/m3、1.2×103kg/m3 和 1.3×103kg/m3,含水量分为 10%、15%和 20%。此外,在不同水平上进行了正交试验。将土壤装入桶中,以 8mm/s 的速度将探针插入桶中的土壤中,确定探针穿透阻力随深度变化的测试值。最后,用室内试验结果对膨胀力模型进行拟合,并引入系数 B 来表示密度和含水量对阻力的影响程度。将系数 B 代入膨胀力模型,得到耕作土壤的穿透阻力模型。通过对穿透阻力模型的拟合优度分析,结果表明,在不同的含水量和密度下,穿透阻力模型的整体平均拟合优度达到 0.871,拟合效果较好,能够为土壤分层理论的研究提供新的思路。