DECOMPOSITION OF PHOSPHORUS-CONTAINING COMPOUNDS IN AQUEOUS AND POLYSACCHARIDE SOLUTIONS OF ORGANIC ACIDS

I.M. Malinovska
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Abstract

The purpose was to study the patterns of dissolution (solubilization) of phosphorus-containing minerals in aqueous and polysaccharide solutions of organic acids in order to model the mechanism of mineral destruction by soil bacteria synthesizing organic acids and exopolysaccharides. Methods. Model, laboratory-analytical, microbiological, statistical. Results. The destructive effect of organic acids on minerals is manifested both in aqueous and polysaccharide solutions. The introduction of bacterial polysaccharide into an aqueous solution of acids increases the decomposition of phosphorus-containing minerals by 1.34̶ 4.96 times. The influence of the chemical structure of acid molecules on the intensity of mineral decomposition is mainly manifested in the presence of bacterial polysaccharide, while in an aqueous solution the effectiveness of acid action depends on the nature of the mineral being destroyed. To the maximum degree, polysaccharide increases the destruction of minerals in a solution of citric acid: molten magnesium phosphate ̶ 2.55 times, thermophosphate ̶ 2.11 times, phosphate flour ̶ 4.96 times. Decomposition of phosphorus compounds in solutions of ascorbic and oxalic acids enhances bacterial polysaccharide to a lesser extent than in citric acid solution. Modeling the destruction of phosphorus-containing minerals under non-sterile conditions (soil conditions) made it possible to establish that organic acids under non-sterile conditions are subject to consumption by soil microbiota, especially ascorbic and citric acids, and to a lesser extent - succinic. Aqueous solutions of organic acids after 18 hours of incubation in non-sterile conditions lose their leaching activity by 1.06 ̶12.1 times. The introduction of a polysaccharide into aqueous solutions of acids makes it possible to avoid their rapid consumption by microorganisms, because of which the efficiency of mineral leaching under non-sterile conditions decreasшes by only 5–20% compared to sterile ones. Conclusions. The introduction of a bacterial polysaccharide into a solution of organic acids enables the latter to be transferred to a sorbed state, as a result of which their susceptibility to consumption by microorganisms is sharply reduced. Thus, polysaccharide-forming bacteria not only destroy minerals more intensively than microorganisms synthesizing only low-molecular-weight metabolites, but also synthesize a more stable and long-term functioning leaching complex in the soil.
有机酸的水溶液和多糖溶液中含磷化合物的分解
目的研究含磷矿物在有机酸水溶液和多糖溶液中的溶解(增溶)规律,模拟土壤细菌合成有机酸和外多糖对矿物的破坏机制。方法。模型,实验室分析,微生物学,统计学。结果。有机酸对矿物质的破坏作用在水溶液和多糖溶液中都表现出来。将细菌多糖引入酸性水溶液,使含磷矿物的分解提高1.34 ~ 4.96倍。酸分子的化学结构对矿物分解强度的影响主要表现在细菌多糖的存在上,而在水溶液中,酸作用的有效性取决于被破坏矿物的性质。在最大程度上,多糖增加了柠檬酸溶液中矿物质的破坏:熔融磷酸镁2.55倍,热磷酸盐2.11倍,磷酸盐粉4.96倍。抗坏血酸和草酸溶液中磷化合物的分解对细菌多糖的增强程度低于柠檬酸溶液。模拟含磷矿物在非无菌条件下(土壤条件)的破坏,可以确定在非无菌条件下有机酸受到土壤微生物群的消耗,特别是抗坏血酸和柠檬酸,在较小程度上-琥珀酸。有机酸水溶液在非无菌条件下培养18小时后,其浸出活性降低1.06 - 12.1倍。在酸的水溶液中引入多糖可以避免微生物对其的快速消耗,因此在非无菌条件下decreasшes矿物浸出的效率仅比无菌条件下的5-20%。结论。将细菌多糖引入有机酸溶液中,使有机酸转移到吸附状态,其结果是它们对微生物消耗的敏感性急剧降低。因此,形成多糖的细菌不仅比只合成低分子量代谢物的微生物更能强烈地破坏矿物质,而且还能在土壤中合成一个更稳定和长期运作的淋滤复合物。
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