Zhao Xiaorong, Lin Qimei, Li Baoguo
Department of Soil & Water Sciences, China Agricultural University, Beijing 100094, China.
Wei Sheng Wu Xue Bao. 2002 Apr;42(2):236-41.
Four insoluble phosphates of ferric phosphate (Fe-P), aluminum phosphate (Al-P), fluorapatite (FAP) and rock phosphate (RP) were used as a sole phosphorus resource for some phosphate-solubilizing microorganisms. It was found that there was significant difference in solubilizing these phosphates by the tested isolates. The fungi normally were more powerful than the bacteria in dissolving the phsophates. The microorganisms generally solubilized more phosphate when supplied with NO3- than with NH4+. However, the isolates of 2TCiF2 and 4TCiF6 had much higher capacity to solubilize FAP and Al-P respectively in NH4+ medium. Most of the isolates solubilized readily FAP and RP, and then Al-P. Ferric phosphate was the least soluble to these isolates. Only isolate 2TCiF2 showed strong ability to solubilize Fe-P. In particular, two Aspergillus sp. had much higher capacity of dissolving Fe-P when suppled with NO3-. The isolates of Evwinia sp. 4TCRi22 and Enterobacter sp. 1TCRi15 had higher capacity of solubilizing FAP. But two Arthrobacter sp. showed the highest activity in RP medium. It is supposed that complexion of organic acids with metals may be the main reason for these isolates to solubilize the phosphates. However, other chelant substances may be much more important for Enterobacter sp. and Erwinia sp. to release phosphorus from the phsphates.
磷酸铁(Fe-P)、磷酸铝(Al-P)、氟磷灰石(FAP)和磷矿石(RP)这四种不溶性磷酸盐被用作某些解磷微生物的唯一磷源。研究发现,受试菌株在溶解这些磷酸盐方面存在显著差异。通常,真菌在溶解磷酸盐方面比细菌更具优势。与以NH4+为氮源相比,微生物在以NO3-为氮源时通常能溶解更多的磷酸盐。然而,2TCiF2和4TCiF6菌株分别在NH4+培养基中溶解FAP和Al-P的能力要强得多。大多数菌株能轻易溶解FAP和RP,然后是Al-P。磷酸铁对这些菌株的溶解性最差。只有2TCiF2菌株表现出较强的溶解Fe-P的能力。特别是,两种曲霉属菌株在以NO3-为氮源时溶解Fe-P的能力要强得多。欧文氏菌属4TCRi22菌株和肠杆菌属1TCRi15菌株溶解FAP的能力较强。但两种节杆菌属菌株在RP培养基中表现出最高的活性。据推测,有机酸与金属的络合可能是这些菌株溶解磷酸盐的主要原因。然而,其他螯合物质可能对肠杆菌属和欧文氏菌属从磷酸盐中释放磷更为重要。