南京大学学报(自然科学版) ›› 2013, Vol. 49 ›› Issue (6): 767.
赵玉连1,代群威1,2**,董发勤2,蒋沁芮1,唐 俊1,陈 武3
Zhao Yu-Lian1, Dai Qun-Wei1,2, Dong Fa-Qin2, Jiang Qin-Rui1,Tang Jun1, ChenWu3
摘要: 本文主要目的是探讨两株土壤菌与蒙脱石相互作用过程。选取了土壤中革兰氏阳性菌、革兰氏阴性菌各1株,分别与钙蒙脱石相互作用。在实验中,对葡萄糖消耗率、pH值随时间的变化趋势进行分析,发现蒙脱石对两株土壤菌的生长有一定的缓冲促进作用。蒙脱石在与土壤菌作用后,矿物晶体结构发现变化,层间距增大,C轴方向堆垛有序程序降低;FTIR分析结果表明,蒙脱石与土壤菌作用后,不仅出现了来自土壤菌的新峰,而且粘土矿物结构基团分子环境也发生改变,说明土壤菌在生长代谢产物进入蒙脱石矿物层间域内,使得蒙脱石底面间距增大。对比两株土壤菌对蒙脱石的作用效果可知,革兰氏阳性菌起着主导作用。
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