斯里兰卡地质地形中潜在钾肥来源矿物/岩石的识别

T. Nivethithan, K. Ariyawansha
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摘要

由于斯里兰卡的农业集约化,对钾肥投入的需求很高。然而,在斯里兰卡的地质环境中,虽然含钾矿物和岩石丰富,但主要钾肥来源的存在是最少的。因此,勘探含钾矿床是满足我国钾肥需求的必要条件。在这方面,本研究的重点是调查斯里兰卡地质地形中可直接用作钾肥或替代现有钾肥的含钾矿物和岩石。在样品采集过程中,在Matale、Kaikawala和Kadugannawa地区采集了长石、云母等含钾矿物和含钾片麻岩样品。处理后的样品进行了主要氧化物浓度、K浓度和表面形貌分析。分析结果表明,钾的实际浓度最高的是正长石(10.35 w/w%),其次是黑云母(9.95 w/w%),其他岩石最低。结果表明,黑云母云母(Kaikawala)和黑云母片麻岩(Matale)的钾回收潜力最大,而正长石(Kaikawala)的钾回收潜力最小。然而,建议进一步研究开发这种钾肥,并评估其应用在经济上是否可行。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Identification of Potential Minerals/Rocks in Sri Lankan Geological Terrain as Source of Potassium (K) Fertilizer
Due to the agricultural intensification in Sri Lanka, there is a high demand for potassium (K)-fertilizer inputs. However, in the Sri Lankan geological setting, the presence of major potash sources is minimum though the K- bearing minerals and rocks are abundant. Therefore, exploration of K-bearing mineral deposits is essential to cater the demand of K-fertilizer in the country. In this regard, this research is focused on investigating the K-bearing minerals and rocks in Sri Lankan geological terrain which can be used as K-fertilizers directly or as alternatives for currently available K-fertilizers. During sample collection, K-bearing minerals, such as feldspar and mica and K-bearing gneiss rock samples were collected from Matale, Kaikawala and Kadugannawa areas. Processed samples were subjected to analyse major oxide concentrations and K concentrations and surface topography. Analyses revealed that the highest actual potassium concentrations were presented in orthoclase feldspar (10.35 w/w%) and then biotite mica (9.95 w/w%) whereas other rocks showed the lowest. Based on the results, biotite mica (Kaikawala) and biotite gneiss (Matale) displayed the highest potential for K recovery, whilst the least potential for K recovery was shown in orthoclase feldspar (Kaikawala). However, further studies are recommended to develop this K-fertilizer and to assess whether its application is economically viable.
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