• ISSN 1008-505X
  • CN 11-3996/S
赵小蓉, 林启美, 李保国, . C、N源及C/N比对微生物溶磷的影响[J]. 植物营养与肥料学报, 2002, 8(2): 197-204. DOI: 10.11674/zwyf.2002.0213
引用本文: 赵小蓉, 林启美, 李保国, . C、N源及C/N比对微生物溶磷的影响[J]. 植物营养与肥料学报, 2002, 8(2): 197-204. DOI: 10.11674/zwyf.2002.0213
ZHAO Xiao, LIN Qi, LI Bao, guo Department, of Soil, and Water, China Agricultural. Effect of C, N sources and C/N ratio on the solubilization of rock phosphate by some microorganisms[J]. Journal of Plant Nutrition and Fertilizers, 2002, 8(2): 197-204. DOI: 10.11674/zwyf.2002.0213
Citation: ZHAO Xiao, LIN Qi, LI Bao, guo Department, of Soil, and Water, China Agricultural. Effect of C, N sources and C/N ratio on the solubilization of rock phosphate by some microorganisms[J]. Journal of Plant Nutrition and Fertilizers, 2002, 8(2): 197-204. DOI: 10.11674/zwyf.2002.0213

C、N源及C/N比对微生物溶磷的影响

Effect of C, N sources and C/N ratio on the solubilization of rock phosphate by some microorganisms

  • 摘要: 以不同的氮源 (NH4+、NO3- 、尿素 )、不同的碳源 (葡萄糖、蔗糖、糖蜜和淀粉 )及碳氮比 (34∶1、20∶1、5∶1)为培养基研究不同C、N源和C/N比对微生物溶磷的影响。结果发现 ,曲霉 2TCiF2和 4TCiF6在以NO3-为氮源的培养基中表现出强的解磷活力 ,而节杆菌 1TCRi7和 1TCRi14的溶磷活性则在NO3-存在时降低 ,青霉 1TCRiF5、2TCRiF4、肠杆菌 1TCRi15和欧文氏菌 4TCRi2 2则只有在供给NH4+时 ,才具有溶解磷矿粉的能力。加入少量可溶性磷对大多数微生物的溶磷能力没有显著的影响。曲霉 2TCiF2在蔗糖为碳源时溶磷活力最高 ,节杆菌 1TCRi7只有在葡萄糖为碳源时才具有溶磷能力。培养基的C/N比越高 ,曲霉和欧文氏杆菌的溶磷活力越高 ,而青霉和肠杆菌则在C/N比最低时 ,其溶磷活力最强。这些微生物之所以具有溶解磷矿粉的能力 ,主要是由于分泌有机酸 ,但非有机酸物质的络合和螯合作用 ,可能在肠杆菌和欧文氏菌溶磷中起重要作用。氮源、碳源和碳氮比极大地影响微生物的代谢 ,尤其对分泌有机酸等物质的种类可能产生很大的影响。

     

    Abstract: Some phosphate solubilizing microorganisms were grown in liquid medium cultures with different nitrogen materials (NH4+, NO3-, urea), carbon materials (glucose, sucrose, molasses, starch) and C/N ratios (34∶1, 20∶1, 5∶1). Of the eight isolates tested,two isolates of Aspergillus sp. 2TCiF2 and 4TCiF6 had much higher capacity to dissolve rock phosphate when supplying with NO3- than with either NH4+ or urea. However, Arthrobacter sp.1TCRi7 and 1TCRi14 decreased their activities of dissolving rock phosphate at NO3- medium. Other isolates of Penicillium sp.1TCRiF5 and 2TCRiF4, Enterobacter sp.1TCRi15 and Erwinia sp.4TCRi22 showed strong ability to solubilize rock phosphate only at NH4+ medium. Little effect was found on phosphate solubilization when adding a small amount of available phosphate in the culture media. Carbon sources had strong influence on rock phosphate solubilization. The fungus of Penicillium sp.2TCiF2 showed the highest capacity to dissolve the rock when supplying sucrose. However, a bacterium of Arthrobacter sp.1TCRi7 had this ability only in the glucose medium. The isolates of Aspergillus sp. and Erwinia sp. had higher capacity of phosphate solubilization in larger C/N ratios of the media, but Penicillium sp. and Enterobacter sp. showed the highest activity in the lowest C/N ratio. The effect of C/N ratios was little in phosphate solubilization of rthrobacter sp. It is supposed that complexion of organic acids with metals may be the main reason for these isolates to solubilize the phosphate. In particular, other chelant substances may be much more important for Enterobacter sp. and Erwinia sp. to release P from the rock phosphate. Metabolisms and especially secretion of the nature of the organic acids by these microorganisms were greatly affected by nitrogen sources, carbon sources and C/N ratios.

     

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