joao PESSOA/PB石灰岩岩土特征

N. Sousa, A. Soares
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引用次数: 0

摘要

在Paraíba州首府约奥佩索阿地区的底土中含有丰富的稀土,由于开采经济且运输成本低,因此有利于将其作为矿石使用。然而,作为沉积岩,当暴露于水的存在时,它是可溶的。本文建议对该地区的石灰石进行表征,以评估其作为混凝土骨料的应用。进行了以下测试:晶粒实密度;干容重;水吸收;在干燥和饱和条件下的磨损、抗压强度和物理分析;电子显微镜;x射线衍射;田间试验。结果表明,它是由碳酸钙(caco3)组成,吸水率高,耐磨性和耐压性低,应限制在某些类型的建筑中使用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
CARACTERIZAÇÃO GEOTÉCNICA DA ROCHA CALCÁRIA DE JOÃO PESSOA/PB
is abundant in the subsoil of the region of João Pessoa, capital of the State of Paraíba, favouring its use as aggregate, due to economic extraction and low transport costs. However, being a sedimentary rock, it is soluble when exposed to the presence of water. This paper proposes to characterize the limestone from that region, in order to assess its application as aggregate for concrete. The following tests were performed: grain real density; dry bulk density; water absorption; abrasion, compressive strength and physical analyses, in dry and saturated conditions; electron microscopy; X-ray diffraction; and field trials. The results indicated that it is composed of calcium carbonate (CaCO 3 ), with high water absorption rate and low abrasion and compressive resistance, concluding that its use should be restricted to certain types of constructions.
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