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基于壓實分析模型的土壤應(yīng)力傳遞系數(shù)研究
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國家自然科學(xué)基金項目(41371238)


Soil Stress Transmission Coefficient Based on Compaction Analytical Model
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    摘要:

    機械壓實是造成土壤退化的重要原因之一,,研究并預(yù)測土壤應(yīng)力有助于科學(xué)規(guī)劃田間機械使用,緩解壓實問題,?;诜治瞿P皖A(yù)測土壤應(yīng)力的關(guān)鍵在于選擇合適的集中系數(shù)。然而在已有的研究中集中系數(shù)取值混亂,,導(dǎo)致該模型使用時存在很大爭議,,其原因在于對該參數(shù)隨土壤環(huán)境的變化缺乏規(guī)律性認(rèn)識。本文通過對集中系數(shù)表達(dá)式的進(jìn)一步推導(dǎo),,在理論上提出了能夠代表土壤環(huán)境對集中系數(shù)影響的無量綱參數(shù)σz/σ0,,定義為應(yīng)力傳遞系數(shù)(STC)?;谒就梁忘S棕壤兩種土壤,,通過控制含水率和濕密度于室內(nèi)重塑30種狀態(tài)的土壤,,在單軸壓縮實驗中運用土壓力傳感器測量計算應(yīng)力傳遞系數(shù),建立應(yīng)力傳遞系數(shù)與土壤環(huán)境參數(shù),,如含水率,、干密度和先期固結(jié)壓力等之間的相關(guān)性分析。結(jié)果表明應(yīng)力傳遞系數(shù)隨土壤含水率的增大而增大,,土壤初始干密度和先期固結(jié)壓力與應(yīng)力傳遞系數(shù)之間負(fù)相關(guān)性明顯,。根據(jù)所得應(yīng)力傳遞系數(shù)計算相應(yīng)土壤狀態(tài)下的集中系數(shù),其取值在1.20~12.39之間,,與以往的研究結(jié)果相差不大,,但包含了關(guān)于集中系數(shù)隨土壤環(huán)境變化的具體信息。這意味著作為一個穩(wěn)定可測的無量綱參數(shù),,應(yīng)力傳遞系數(shù)為集中系數(shù)的計算提供了一個相對科學(xué)的方法,,在定量描述土壤環(huán)境對集中系數(shù)影響的同時,完善了分析模型,。

    Abstract:

    Predicting soil stress with analytical models requires proper selection of the models’ concentration factor. But due to the insufficient knowledge about the effects of soil conditions on stress transmission, little is known about how the concentration factor varies with soil states and loading conditions. The function of the concentration factor was transformed and a dimensionless factor σz/σ0 standing for soilinduced attenuation on the stress transmission was defined as the soil stress transmission coefficient and is denoted as STC. Since soil stress transmission property is affected by soil states and loading conditions, a modified oedometer testing setup with a soil stress sensor was used to evaluate controlled soil properties on STCs. Totally 30 soil states were tested by controlling soil water contents and bulk densities based on different soil styles. Correlation analysis was performed between measured STCs and soil state parameters, i.e. water content, bulk density and soil strength. The highly linear correlation between soil stress and applied surface stress indicated a stable STC for each particular soil state. STC was also found both linearly decreased with dry bulk density and precompression stress. The backcalculation of concentration factor from measured STCs illustrated that the proposed solution for soil stress transmission provided a means to define concentration factor for each soil state with measured result. Concentration factor varied from 1.20 to 12.39, being in agreement with the past reports. And the detail of how the concentration factor was affected by the changed states of soils was provided.

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賀亭峰,叢文杰,BELAL Eisa Adam,丁啟朔,楊艷山,霍連飛.基于壓實分析模型的土壤應(yīng)力傳遞系數(shù)研究[J].農(nóng)業(yè)機械學(xué)報,2017,48(6):59-65. HE Tingfeng, CONG Wenjie, BELAL Eisa Adam, DING Qishuo, YANG Yanshan, HUO Lianfei. Soil Stress Transmission Coefficient Based on Compaction Analytical Model[J]. Transactions of the Chinese Society for Agricultural Machinery,2017,48(6):59-65.

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  • 收稿日期:2016-10-23
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  • 在線發(fā)布日期: 2016-12-11
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