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Calcite Dissolution by Brevibacterium sp. SOTI06: A Futuristic Approach for the Reclamation of Calcareous Sodic Soils

机译:短杆菌属的方解石溶解SOTI06:钙质钠盐土壤开垦的未来派方法

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摘要

Assessing the ability of soil microorganisms to dissolute poorly soluble native calcite to supply Ca2+ is a new area to be explored in reclaiming sodic soils by supplying adequate Ca2+ and reducing the recurrent sodicity. Hence, the present study aimed to isolate a calcite dissolving bacteria (CDB) from calcareous sodic soils and to understand the mechanism of calcite dissolution. Of the 33 CDB isolates recovered from the calcareous sodic soils of Tamil Nadu (Coimbatore, Ramnad, and Trichy), 11 isolates were screened for calcite dissolution based on titratable acidity. 16S rRNA gene sequence analysis of the three best isolates viz., SORI09, SOTI05, and SOTI06 revealed 99% similarity to Bacillus aryabhattai, 100% to B. megaterium, and 93% to Brevibacterium sp., respectively. Among them, Brevibacterium sp. SOTI06 released more Ca2+ (3.6 g.l−1) by dissolving 18.6% of the native calcite. The spectral data of FTIR also showed reduction in the intensity of calcite (55.36–41.27) by the isolate at a wave number of 1636 cm−1 which confirmed the dissolution. Besides producing organic acids (gluconic acid and acetic acid), Brevibacterium sp. SOTI06 also produced siderophore (91.6%) and extracellular polysaccharides (EPS, 13.3 μg. ml−1) which might have enhanced the calcite dissolution.
机译:通过供应充足的Ca 2 + 和还原来评估土壤微生物溶解难溶的天然方解石以供应Ca 2 + 的能力,是复垦苏打土壤的一个新领域。经常性的态度。因此,本研究旨在从钙质钠钙土中分离方解石溶解细菌(CDB),并了解方解石溶解的机理。从泰米尔纳德邦的钙质钠盐土壤中回收的33种CDB分离物(Coimbatore,Ramnad和Trichy)中,根据可滴定的酸度对11种分离物进行了方解石溶解的筛选。对三个最佳分离株,即SORI09,SOTI05和SOTI06的16S rRNA基因序列分析显示,与aryabhattai芽孢杆菌有99%的相似性,与巨大芽孢杆菌100%的相似性,与短杆菌属的93%的相似性。其中,短杆菌属。 SOTI06通过溶解18.6%的天然方解石释放出更多的Ca 2 + (3.6 g.l -1 )。 FTIR的光谱数据还显示,分离物在方波数1636 cm -1 下降低了方解石强度(55.36–41.27),证实了其溶解。除产生有机酸(葡萄糖酸和乙酸)外,Brevibacterium sp.。 SOTI06还产生铁载体(91.6%)和细胞外多糖(EPS,13.3μg。ml -1 ),这可能增强了方解石的溶解。

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