Empirical Equation between Predominant Frequency and Sediment Thickness in Plampang, West Nusa Tenggara

E. R. Iswanto, Theo Alvin Riyanto, H. Suntoko
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Abstract

Soil characteristics mapping is one of the essential aspects in the development of a region. Soil characteristics such as the predominant frequency and thickness of the sediment layer are needed to ensure the capacity of soil against the load of an infrastructure construction. The existence of tectonic activity causes West Nusa Tenggara Province to be an area with high seismic activity. Along with the plan to accelerate the development of the Samota Area, seismic studies are one of the aspects that determine project feasibility. The predominant frequency value from the results of microtremor measurements is used in the development of an empirical formula to predict soil thickness in the Plampang area. The empirical formula from previous research is used as a conformity test of the empirical formula obtained. Empirical equations are then used to map variations in sediment thickness in the Plampang area, which are justified based on geological data. The results of the sediment thickness map based on the empirical formula for the Plampang area showed a good correlation with the predominant frequency and also showed a good correlation with the results of the formula that has been carried out by previous studies.
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西努沙登加拉普兰邦主要频率与沉积厚度之间的经验公式
绘制土壤特性图是一个地区发展的重要方面之一。土壤特性,如沉积层的主要频率和厚度,是确保土壤承受基础设施建设负荷的必要条件。构造活动的存在导致西努沙登加拉省成为地震活动频繁的地区。随着萨莫塔地区开发计划的加快,地震研究是决定项目可行性的一个方面。微震波测量结果中的主要频率值被用于制定经验公式,以预测 Plampang 地区的土壤厚度。先前研究中的经验公式被用来对所获得的经验公式进行一致性测试。然后利用经验公式绘制 Plampang 地区沉积厚度变化图,并根据地质数据进行论证。根据经验公式绘制的普兰邦地区沉积厚度图结果显示与主要频率有很好的相关性,同时也显示与之前研究的公式结果有很好的相关性。
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