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赖氨酸芽孢杆菌GW-2菌株诱导碳酸盐矿物的形成
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  • 英文篇名:Lysinibacillus sp. GW-2 strain mediated mineralization of carbonate minerals
  • 作者:郭文文 ; 李福春 ; 吕杰杰
  • 英文作者:Guo Wenwen;Li Fuchun;Lü Jiejie;Zaozhuang University;College of Resources and Environmental Sciences,Nanjing Agricultural University;
  • 关键词:赖氨酸芽孢杆菌 ; 方解石 ; 球霰石 ; 形态
  • 英文关键词:Lysinibacillus sp.;;calcite;;vaterite;;morphology
  • 中文刊名:NJDZ
  • 英文刊名:Journal of Nanjing University(Natural Science)
  • 机构:枣庄学院;南京农业大学资源与环境科学学院;
  • 出版日期:2019-03-30
  • 出版单位:南京大学学报(自然科学)
  • 年:2019
  • 期:v.55;No.245
  • 基金:国家自然科学基金(41673083,41172308);; 中国科学院黄土与第四纪地质国家重点实验室开放课题(SKLLQG1309);; 山东省自然科学基金(ZR2016DB34);; 枣庄学院博士科研启动基金(2013BS03);枣庄学院国家基金预研究项目(102061805)
  • 语种:中文;
  • 页:NJDZ201902016
  • 页数:11
  • CN:02
  • ISSN:32-1169/N
  • 分类号:155-165
摘要
为研究细菌促进碳酸盐矿物形成的机理,在B4培养基中对一株分离自土壤的赖氨酸芽孢杆菌GW-2菌株进行了为期40 d的培养实验,同时完成了一组加灭活菌的对照实验.在实验过程中,对培养液中的细菌数量、pH、Ca~(2+)浓度、沉淀物重量等进行测定.用X-射线衍射仪(X-ray diffraction,XRD)对矿物种类进行测定,用扫描电子显微镜(Scanning Electron Microscopy,SEM)对矿物形态进行观察.实验结果表明:(1)GW-2菌株具有促进碳酸盐矿物生成的能力,且随着培养时间的延长,沉淀物的重量逐渐增加;(2)GW-2菌株诱导下形成的矿物经历方解石→方解石+球霰石的转化;(3)矿物形态主要为由三角板片构成的碗状和由花瓣状构成的半球.
        In order to understand the formation mechanism of carbonate minerals mediated by bacteria,culture experiments with a duration of 40 days were performed under the mediation of sinibacillus sp.(strain GW-2)isolated from soils using B4 medium. At the same time,the same medium with autoclaved bacteria was done as the control. During the cultivation,bacterial density,pH value,calcium concentration,precipitate quantities were measured. X-ray diffraction(XRD)was used to determine mineral species,and scanning electron microscopy(SEM)was used to observe mineral morphologies. The results were as follows:(1)Strain GW-2 could induce the precipitation of carbonate minerals,the quantities of carbonate gradually increased with incubation time.(2)The minerals induced by strain GW-2 experienced from calcite to calcite and vaterite with culture time.(3)The morphologies were almost bowl-shaped with a lot of triangle on their surface and hemisphere with petaline shape.
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