钾溶解细菌中的有机酸释放长石中的钾离子

Thashmantha M.A.D.S., Ratnatilleke A.A.L.
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引用次数: 0

摘要

农业产量和质量取决于土壤中的养分含量。永久性农田通常养分不足,需要通过施肥来弥补。最近的研究发现,含钾化肥会造成一些环境问题,而且这些化肥价格昂贵。因此,利用斯里兰卡的原料开发一种向植物提供钾的新方法非常重要。在这方面,利用生物技术对长石进行生物转化以获得钾肥是非常有前景的。本研究的总体目标是探索钾溶解细菌中的有机酸如何从斯里兰卡的长石(Microcline- KAlSi3O8)中释放钾离子,以提高这些矿物质在更可持续的农业实践中的使用效率。在这项研究中,研究了柠檬酸、草酸、琥珀酸和酒石酸(钾溶解细菌产生的主要酸)对长石的溶解作用,涉及酸类型的影响、每种酸浓度的影响、长石粒度的影响、培养时间的影响以及 pH 值随时间的变化。将磨碎的长石(0.150-0.300 毫米和 0.075- 0.150 毫米)分别与 0.01、0.02、0.03、0.04 和 0.05 M 的每种有机酸进行不同时间(1、2.5 和 4 小时)的振荡,使用火焰光度计测量释放的钾离子浓度,并使用 pH 计测量 pH 值的变化。结果表明,长石的增溶程度受所用有机酸类型的影响。与无机酸(H2SO4)相比,某些有机酸在增溶长石方面更为成功。草酸和酒石酸从长石中释放钾的能力比其他酸高达 9 倍。当酸的浓度改变时,同一种酸的增溶作用不明显。随着粒度的减小,长石在所有酸中的溶解度都在增加。随着反应时间的延长,长石在几乎所有酸中的溶解度都有所提高。这些研究结果表明,草酸和酒石酸是增溶长石最成功的酸。找到分泌这些酸作为其主要副产品的细菌以及分泌这些酸的条件将对农业有益,长石可用于为农田提供钾。 关键词有机酸 长石 溶解
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Release of Potassium Ions from Feldspar by Organic Acids Present in Potassium-Solubilizing Bacteria
Agricultural production and quality are determined by the nutrient levels in the soil. Permanent agricultural lands are usually nutrient deficient and it is compensated by fertilization. Recent studies have found that potassium-bearing chemical fertilizers caused some environmental issues and these fertilizers are expensive. Therefore, the development of a new method for supplying potassium to plants using ingredients found in Sri Lanka is important. In this respect, the bioconversion of feldspar using biotechnological processing to obtain potassium fertilizers is very promising. The overall objective of this study is to explore the release of potassium ions from feldspar (Microcline- KAlSi3O8) found in Sri Lanka by organic acids present in potassium-solubilizing bacteria to improve the efficiency of these minerals to use in more sustainable agricultural practices. In this research, the solubilization of feldspar with citric, oxalic, succinic, and tartaric acids (the main acids that are produced by potassium solubilizing bacteria) was studied, concerning the effect of acid type, the effect of each acid concentration, the effect of particle size of feldspar, the effect of incubation time, and the changes in pH over time. Ground feldspar (0.150–0.300 mm and 0.075– 0.150 mm) was separately shaken with 0.01, 0.02, 0.03, 0.04 and 0.05 M of each organic acid for different periods (1, 2.5 and 4 hours) and the released potassium ion concentration was measured using a flame photometer and pH change was measured using a pH meter. The extent of solubilization of feldspar was shown to be influenced by the type of organic acid used. In comparison to inorganic acids (H2SO4), some organic acids were more successful in solubilizing feldspar. Both oxalic and tartaric acids showed a higher capability of releasing potassium from the feldspar than other acids by up to 9 folds. The solubilization was insignificant for the same acid when the acid concentration was changed. The solubility of feldspar in all acids increased as the particle size decreased. The solubilization of feldspar was increased practically in almost all acids as time increased. pH was increased in almost all acids when the reaction time was increased. These findings show that both oxalic and tartaric acids are the most successful acids in solubilizing feldspar. Finding bacteria that secrete these acids as their major byproducts and conditions that secrete these acids would be beneficial for agriculture and feldspar can be used to supply potassium to agricultural lands.  Keywords: Organic acids, Feldspar, Solubilization 
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