PEMODELAN KADAR AIR PADA SIFAT FISIK STABILISASI TANAH GAMBUT

Mohammad Syaiful Pradana, Awawin Mustana Rohmah
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Abstract

Abstract : Peat soil is an organic soil with very low carrying capacity and high compressibility. The condition is less profitable for civil engineers in building a civil foundation foundation. One method of peat soil improvement can be done with astabilization method that more environment-friendly and cheaper than other methods. Laboratory based peat stabilization studies to increase carrying capacity, reduce compression and improve peat soil physical properties have been conducted in Indonesia. The results of laboratory studies shown in the graph are still limited by time and content of the mixture. Therefore, further research is needed on the mathematical model toward the physical properties of peat soil stabilization. In this research will be formulated mathematical model of water content on the physical properties of peat soil stabilization. The model is derived from the fluid equation through porous media based on the principle of continum and controlvolume. The model is then resolved numerically by different method until MacCormack scheme with two steps are predictor step using forward difference and correctorstep using backward difference. The MacCormack scheme has the advantage of solving fluid flow equations and continuity. The model is then simulated and validated by comparing the simulation results with the real system. From the simulation results obtained the water content gradually decreased, the decrease is almost close to zero. In addition, it can be seen the difference in decrease in moisture content at each test point although in small quantities. Keywords: Moisture Content, MacCormack, Peat Soil Stabilization.
水能物质稳定土壤的水能建模
摘要泥炭土是一种低承载力、高压缩性的有机土壤。在这种情况下,土木工程师在建造土木基础时利润较低。稳定法是泥炭土改良的一种方法,它比其他方法更环保、更经济。在印度尼西亚进行了以实验室为基础的泥炭稳定研究,以增加承载能力、减少压缩和改善泥炭土壤的物理性质。图中所示的实验室研究结果仍然受到时间和混合物含量的限制。因此,泥炭土稳定物理特性的数学模型有待进一步研究。本研究将建立含水率对泥炭土物理性质稳定的数学模型。该模型基于连续体和控制体积原理,由多孔介质流体方程推导而来。然后通过不同的方法对模型进行数值分解,直到两步MacCormack格式分别是使用前向差分的预测步和使用后向差分的校正步。MacCormack格式具有求解流体流动方程和连续性的优点。将仿真结果与实际系统进行对比,对模型进行了仿真验证。从模拟结果来看,含水率逐渐减小,减小量几乎接近于零。此外,可以看到各测试点的含水率下降量虽然较小,但存在差异。关键词:含水率,麦考马克,泥炭土稳定
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