古农安雅泥火山的电阻率测量

Primasari Cahya Wardhani, Bagas Aryaseta, Nia Dwi Puspitasari
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引用次数: 0

摘要

过去的石油和天然气钻探活动被认为是泥火山现象的成因。泥火山可能危及周围环境,包括居民。因此,绘制区域地图对于制定减灾计划至关重要。其中一个潜在的泥火山是古农安雅泥火山。通过电阻率测量,获得了古农安雅泥火山的地下构造。结果表明,在0 ~ 4 m深度的土结构顶部存在极低的电阻率值。这种土壤结构被认为是泥火山的表现形式,以湿润的粘土与盐水相结合。在随后的深度,距离顶部4到5.5米,是一层砂质粘土。它的特点是具有中高电阻率值。在水深5.5 ~ 10.5 m处,电阻率值非常高。该砂岩层极有可能是古农-安雅尔地区的原生底土地层。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Electrical Resistivity Survey of the Gunung Anyar Mud Volcano
The past oil and natural gas drilling activities have been presumed to cause a Mud Volcano phenomenon. The Mud Volcano potentially danger its surroundings, including the inhabitants. Thus, mapping the zone will be essential to have a mitigation plan. One of the potential Mud Volcanoes is the Gunung Anyar Mud Volcano. By using a resistivity survey, this research aims to obtain the subsurface structure of the Gunung Anyar Mud Volcano. The results show that very low resistivity values are located at the top of the soil structure with 0 to 4 meters depth. This soil structure is believed to be a manifestation of a mud volcano in the form of moistened clay associated with salt water. At subsequent depths, 4 to 5.5 meters from the top, is a layer of sandy clay. It is characterized by moderate to high resistivity values. At a depth of 5.5 to 10.5 meters, the resistivity value is very high. This sandstone layer is most likely a native subsoil formation in the Gunung Anyar area.
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