Garmasheva L L, Kovalenko N K, Pidgorskyi V S, Livinska O P, Voychuk S L, Oleschenko L T, Tomia T V, Lobunets T E
Mikrobiol Z. 2016 Jul;78(4):11-24.
To characterize the interaction of Lactobacillus plantaruni 337D UKM B-2627 strain, which has probiotic properties, with kaolinite and montmorillonite.
The methods of infrared spectroscopy, transmission electron microscopy, the adsorption-structural static volumetric method, microbiological and statistical methods were used.
The characteristics of the porous space of clay mineral particles were practically did not change compared with initial samples during the interaction with L. plantarum 337D UKM B-2627 strain cells, pore size distribution had become wider due to the emergence of large diameter pores, reduced surface area, but the adsorption capacity and the layered structure of clay minerals preserved. For the first time the ef- fect of kaolinite and montmorillonite on growth of L. plantaruni 337D strain in vitro was studied. The greatest stimulating effect of clay minerals was observed within two hours of cultivation. The specific growth rate of L. plantaruni 337D strain was in 5.2 times higher when cultured in MRS medium with 4 % of kaolinite and 6 times more - in MRS medium with 1 % montmorillonite versus control. The presence in the medium of kaolinite or montmorillonite slowed the process of reducing pH during growth of the L. plantarum 337D strain, compared with the control. In the presence of montmorillonite pH decreased more slowly than in the presence of kaolinite. The difference between initial pH value of medium with 4 % kaolinite and after two h (ApH) was 10 times less in comparison with the control. At the same time, pH of the medium with 1 % or 4 % montmorillonite began to decrease after 4 hours of cultivation.
Different effect on the growth of L. plantarum 337D strain due to differences of physical and chemical characteristics of kaolinite and montmorillonite used in the study.
表征具有益生菌特性的植物乳杆菌337D UKM B - 2627菌株与高岭石和蒙脱石的相互作用。
采用红外光谱法、透射电子显微镜法、吸附结构静态容量法、微生物学方法和统计学方法。
与初始样品相比,在与植物乳杆菌337D UKM B - 2627菌株细胞相互作用期间,粘土矿物颗粒的孔隙空间特征实际上没有变化,由于大直径孔隙的出现,孔径分布变宽,表面积减小,但粘土矿物的吸附容量和层状结构得以保留。首次研究了高岭石和蒙脱石对植物乳杆菌337D菌株体外生长的影响。在培养两小时内观察到粘土矿物的最大刺激作用。与对照相比,当在含有4%高岭石的MRS培养基中培养时,植物乳杆菌337D菌株 的比生长速率高5.2倍,在含有1%蒙脱石的MRS培养基中高6倍。与对照相比,培养基中高岭石或蒙脱石的存在减缓了植物乳杆菌337D菌株生长过程中pH降低的过程。在蒙脱石存在下,pH下降比在高岭石存在下更慢。含有4%高岭石的培养基的初始pH值与两小时后(ΔpH)的差异比对照小10倍。同时,含有1%或4%蒙脱石的培养基在培养4小时后pH开始下降。
由于本研究中使用的高岭石和蒙脱石的物理和化学特性不同,对植物乳杆菌337D菌株的生长有不同影响。