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首页> 外文期刊>American Journal of Physics and Applications >Geoelectrical characterization of rock formations underlying Idonyi River, Amaeke-Abam, Southeastern Nigeria
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Geoelectrical characterization of rock formations underlying Idonyi River, Amaeke-Abam, Southeastern Nigeria

机译:尼日利亚东南部Amaeke-Abam,Idonyi河下的岩层的地电特征

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The geoelectrical characterization of soils underlying the Idonyi River Dam site Amaeke-Abam, Southeastern Nigeria has been carried out with a view to determining the presence or otherwise of deleterious matter along the dam axis down to a depth of 37m below the surface; evaluate the geo-structural setting of the concealed bedrock, the fracture pattern and possible dam seepage along the dam axis and its banks as well as giving suggestions on any other measures/studies that may be needed for a proper engineering design. The study area is around the river located between latitudes 5°34'N - 5°37'N and longitudes 7°39'E - 7°42'E. Heights above sea level in the area range from 68 to 91 meters. The survey was carried out with Abem Terrameter SAS 1000C. The sounding stations were laid out in three (3) profiles; eight (8) VES on each profile. A total of twenty-four (24) VES data were conducted. The Schlumberger electrode configuration was adopted to a total spread length of 110 meters (AB/2 of 55 meters). Results showed that resistivity values of between 182 and 2637Ωm at the eastern part of the River and another range of 6.2 to 848Ωm in the western end suggest overriding sandy substratum to east and overriding shaly characteristics to the west. These results show clearly that the area around Idonyi is porous with relatively higher sandy fractions.The derived parameters on both sides of the river agreed with the standard parameters required for a dam construction. The failure of a previous dam near the river is thus attributable to much seepage due to overriding sandy substratum. To avoid the seepage, the base of the dam should be blanketed with an impervious material such as shale. The area, being the most fertile area (phosphatic Ameki units) with CRIN, NRRI, FRIN, RCRIN having research institutes near the river, a dam is necessary here and this study has shown that it is possible to have a dam with solid foundation. However, we suggest a baseline data survey of water quality before any construction so as to monitor any contamination trend due to impoundment.
机译:尼日利亚东南部Idonyi河大坝遗址Amaeke-Abam下方土壤的地电特征已经确定,以确定沿大坝轴线直至地表以下37m的有害物质的存在与否;评估隐蔽基岩的地质结构设置,裂缝模式以及沿坝轴线及其堤岸可能发生的坝渗漏,并就适当工程设计可能需要的任何其他措施/研究提供建议。研究区域位于北纬5°34'-北纬5°37'和东经7°39'-东经7°42'之间的河流周围。该地区的海拔高度在68至91米之间。这项调查是使用Abem Terrameter SAS 1000C进行的。测深站以三(3)个配置文件布局;每个配置文件上的八(8)VES。总共进行了二十四(24)个VES数据。采用斯伦贝谢电极配置,总铺展长度为110米(AB / 2为55米)。结果表明,该河东部的电阻率值在182至2637Ωm之间,西端的电阻率范围在6.2至848Ωm之间,这表明东部地区覆盖了砂质岩层,而西部地区则覆盖了泥质特征。这些结果清楚地表明,爱多尼(Idonyi)周围地区是多孔的,含沙量相对较高。河道两侧的推导参数与​​大坝建设所需的标准参数一致。因此,在河边的前一个水坝的失败归因于由于覆盖的沙质底层而造成的大量渗漏。为避免渗漏,应在坝基上铺一层不可渗透的材料,例如页岩。该地区是CRIN,NRRI,FRIN和RCRIN最富饶的地区(磷化Ameki单位),在河边设有研究机构,因此这里有必要修建水坝,这项研究表明,有可能建立一个坚实基础的水坝。但是,我们建议在进行任何施工之前,先对水质进行基线数据调查,以监测由于蓄水造成的任何污染趋势。

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