淤泥土土工织物加筋模型室内试验

None Eko Budianto, None Dina Limbong Pamuttu, None Hairulla Hairulla, None Daud Andang Pasalli
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摘要

Merauke Regency是一个低地地区,软土占主导地位。克服粉土沉降的方法之一是采用土工布对粉土进行加固。土工布的作用是固定土壤表面,使土壤不会下沉。本研究旨在确定土工布加固前后粉土的承载力。采用试验方法,采用添加土工布(TS600型无纺布)增强粉土承载能力的方法。将粉土承载力试验分为不使用土工布加固和在10 cm、20 cm和30 cm深度分别用1层、2层和3层土工布加固的几种变化。在实验室进行的研究结果表明,与初始条件相比,使用土工布材料增加粉土的承载能力有所增加。不使用土工布的土壤土沉降幅度更大,即在5 kN荷载下,沉降量为20.3 mm。单层土工布加固材料在5 kN荷载下减少10.97 mm,两层土工布加固材料在5 kN荷载下减少8.09 mm,三层土工布加固材料在5 kN荷载下减少6.01 mm。由此可见,采用土工布加固可以减少粉土的沉降。
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Geotextile Reinforcement Model Laboratory Test on Silt Soil
Merauke Regency is a lowland area that has soft soil which predominates. One of the methods to overcome the subsidence in silt soil, it is necessary to strengthen it by using geotextiles. The function of the geotextile is to hold the soil surface so that there is no subsidence in the soil. This study aims to determine the carrying capacity of silt soil before and after being given geotextile reinforcement.The study used an experimental method using the addition of Geotextile (non-woven type TS600) to strengthen the carrying capacity of silt soil. The silt soil carrying capacity test was divided into several variations, namely without using geotextile reinforcement and reinforced with 1 layer, 2 layers, and 3 layers of geotextile at a depth of 10 cm, 20 cm and 30 cm.The results of research conducted in the laboratory, the use of geotextile materials to increase the carrying capacity of silt soil has increased compared to the initial conditions. Soil without using geotextiles has a greater decrease, namely at a load of 5 kN there is a settlement of 20.3 mm. By using a single layer geotextile reinforcement material at a load of 5 kN there was a decrease of 10.97 mm, while using a two layer geotextile reinforcement material at a load of 5 kN there was a decrease of 8.09 mm, and using a three layer geotextile reinforcement material with a load of 5 kN there was a decrease of 6.01 mm. It can be concluded that the use of geotextile reinforcement can reduce the settlement of silt soil.
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