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Influence of Groundwater Level to Slope Displacement by Geodetic Method

机译:地下水位对地理位置方法的影响

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In the rainy season, Indonesia often experience landslide disasters. Rainwater flows on the surface of the ground and partially into the ground, and changing the groundwater level (GWL) which can cause pressure on surrounding material. Water becomes the main factor that triggered landslides because water causes pressure force on the slopes that are prone to move. With the geometric approach, slope material displacement vectors can be known, including the origin of the material pressure using dynamic mathematical model that considers GWL. The data was used 5 campaigns of GPS observations. The results are obtained the correlation coefficients between coefficient changes in groundwater levels to the vector position as a representative of correlation between the physical and geometric parameters. There is relatively strong because of the value of the average correlation coefficient is 0.91997. Further, curves between changes in groundwater levels and the displacement position shows that the greater the groundwater levels, the greater the material position shift occurs.
机译:在雨季,印度尼西亚经常经历滑坡灾害。雨水在地面上流动并部分地进入地面,改变了可能对周围材料引起压力的地下水位(GWL)。水成为触发山体滑坡的主要因素,因为水导致容易移动的斜坡上的压力。利用几何方法,可以知道斜率材料位移矢量,包括使用考虑GWL的动态数学模型的材料压力的来源。使用该数据5个GPS观察活动。作为物理和几何参数之间的相关性的代表性,获得了地下水位的系数变化与矢量位置之间的系数变化之间的相关系数。由于平均相关系数的值为0.91997,相对强劲。此外,地下水位和位移位置之间的变化之间的曲线表明地下水位越大,就会越大。

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