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Investigation of cavities and karstic features at Al-Amal city, Qattamiya, Egypt by using 3-D inversion of VES data

机译:利用VES数据的3-D反演研究埃及Qattamiya的Al-Amal城市的洞穴和岩溶特征。

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In the past few years, construction extended extraordinarily to the southeast of Cairo, Egypt, where limestone caves occur. The existence of caves and sinkholes represents a hazard for such new urban areas. The state is planning to construct a new housing community there. Therefore, it is important to map and delineate these natural voids and cavities before construction.Recently, cavity imaging by means of geophysical surveys became more common. In this paper, DC resistivity survey had been applied at Al-Amal city, east of Qattamiya, Cairo to image the shallow subsurface and possibly karstic features and cavities. Thirty-two vertical electrical soundings were measured using the common Schlumberger array of electrode configuration with a maximum AB/2 spacing of 200 m. A 3-D inversion scheme was applied to the measured data. The results of VES data inversion subdivided the shallow subsurface section in the study area into three main geoelectrical units. The uppermost unit composed of sand, gravel and fossiliferous limestone with high resistivity values and small thickness. The second unit is composed of sandy clay and clay with low resistivity values. The third unit is considered to be the bed rock, where it consists of consolidated sand, limestone and marl with relatively high resistivity values.The results elucidated many geoelectrical variations which could be interpreted as litho-facies variations. It was also revealed that, the area is dissected by some normal faults affecting the second and third geoelectrical units. In addition,numerous cavernous structures could be elucidated at shallow to intermediate depths. These features are too important to be taken into account during the housing development plans.
机译:在过去的几年中,建筑工程异常扩展到埃及开罗的东南部,发生了石灰石洞穴。洞穴和下沉坑的存在对这种新的城市地区构成了危害。该州计划在那里建设一个新的住房社区。因此,重要的是在施工之前对这些自然的空隙和空腔进行制图和描绘。最近,借助地球物理勘测的空腔成像变得越来越普遍。本文在开罗Qattamiya以东的Al-Amal市进行了直流电阻率测量,以对浅层地下以及可能的岩溶特征和空洞进行成像。使用通用的斯伦贝谢电极配置阵列(最大AB / 2间距为200 m)测量了32个垂直电测深。将3-D反演方案应用于测量数据。 VES数据反演的结果将研究区域的浅层地下部分细分为三个主要的地电单元。最上层的单元由电阻率值高和厚度小的砂,砾石和化石石灰石组成。第二个单元由砂质粘土和低电阻率的粘土组成。第三单元被认为是基岩,由固结的砂,石灰石和泥灰岩组成,具有较高的电阻率值。结果阐明了许多地电变化,可以解释为岩相变化。还发现,该区域被一些影响第二和第三地电单元的正常断层所分割。另外,可以在浅至中深度阐明大量的海绵状结构。这些功能非常重要,无法在住房开发计划中予以考虑。

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