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Is Mudflow in Sidoarjo, East Java Due To The Pumping Mechanism of Hot Air Bubbles?: Laboratory Simulations and Field Observations

机译:在Sidoarjo,East Java是泥泞的,由于热气泡的泵送机制?:实验室模拟和现场观测

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Extraordinary mudflow has happened in Sidoarjo, East Java, Indonesia since 2006. This mud comes from the giant crater that is located close to the BJP - 01. Thousands of homes have been submerged due to mudflow. Till today this giant mud crater is still has great strength despite the mud flowing over 8 years. This is a very rare phenomenon in the world. This mud flow mechanism raises big questions, because it has been going on for years, naturally the mudflow will stop by itself because the pressure should be reduced. This research evaluates all aspects of integrated observations, laboratory tests and field observations since the beginning of this ongoing mudflow. Laboratory tests were done by providing hot air bubbles into the fluid inside the inverted funnel showed that the fluid can flow with a high altitude. It is due to the mechanism of buoyant force from air bubbles to the water where the contrast density of the water and the air is quite large. Quantity of air bubbles provides direct effect to the debit of fluid flow. Direct observation in the field, in 2006 and 2007, with TIMNAS and LPPM ITB showed the large number of air bubbles on the surface of the mud craters. Temperature observation on the surface of mud crater is around 98 degree C whereas at greater depth shows the temperature is increasingly rising. This strengthens the hypothesis or proves that the mud pumping mechanism comes from buoyant force of hot air bubbles. Inversion gravity images show that the deep subsurface of main crater is close to volcanic layers or root of Arjuna mountain. Based on the simulation laboratory and field observation data, it can be concluded that the geothermal factor plays a key role in the mudflow mechanism.
机译:自2006年以来,印度尼西亚侧奥拉茹曾发生了非凡的泥泞。这种泥土来自于靠近BJP - 01的巨型火山口。由于泥流,成千上万的家庭已经淹没。直到今天,尽管泥浆过多8年,但这种巨大的泥浆火山口仍然具有很大的力量。这是世界上一种非常罕见的现象。这种泥浆流动机制提出了大问题,因为它已经进行了多年,因此,由于压力应该减少,因此泥浆将自然停止。这项研究评估了自这个正在进行的泥流开始以来的综合观测,实验室测试和现场观测的所有方面。通过在倒漏斗内的流体中提供热空气气泡来完成实验室测试,显示流体可以用高空流动。由于来自气泡到水的浮力力的机制,水和空气的对比度密度相当大。气泡的数量为流体流动的借方提供直接影响。在该领域的直接观察,2006年和2007年,用Timnas和LPPM ITB显示泥浆陨石坑表面上的大量气泡。在泥浆火山口表面的温度观察约为98摄氏度,而在更大的深度上显示温度越来越升高。这加强了假设或证明泥浆泵送机构来自热气泡的浮力力。反转重力图像表明,主要火山口的深层地下靠近阿尔金山的火山层或根。基于模拟实验室和现场观察数据,可以得出结论,地热因子在泥浆机制中起着关键作用。

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