铁还原菌Shewanella oneidensis MR-1对铁磷复合物中铁、磷释放规律的影响
发布时间:2018-11-07 10:19
【摘要】:中国南方红壤中的磷素大多以铁磷复合物的形式被固定于土壤中,磷的利用率较低。通过向土壤中添加以S.oneidensis MR~(-1)为主的生物肥料,促进土壤磷的释放,减少外源磷肥的输入,以期达到保护环境和资源节约的目的。采用室内模拟试验,在纯化学培养的条件下,采用接种S.oneidensis MR~(-1)的厌氧体系进行培养,分别以磷吸附态的水铁矿(水铁矿-磷)、磷吸附态的针铁矿(针铁矿-磷)和磷酸铁(FePO_(4-)磷)作为体系唯一的磷素和Fe(Ⅲ)来源,3种磷均为土壤中铁磷复合物的组成成分。结果表明,S.oneidensis MR~(-1)对3种铁磷复合物中的Fe(Ⅲ)产生了还原效应并将其还原成Fe(Ⅱ),且Fe(Ⅱ)质量浓度随试验时间延长总体呈先增长后稳定的变化趋势;当3组加入S.oneidensis MR~(-1)的体系Fe(Ⅱ)质量浓度均为最高时,Fe(Ⅱ)平均生成速率表现为:针铁矿(30.44 mg·L~(-1)·d~(-1))水铁矿(21.05 mg·L~(-1)·d~(-1))磷酸铁(6.62 mg·L~(-1)·d~(-1));3组加入S.oneidensis MR~(-1)的体系Fe(Ⅲ)质量浓度与初始质量浓度相比较均发生了改变,在针铁矿-磷-菌体系中Fe(Ⅲ)质量浓度极低,而水铁矿-磷-菌体系和磷酸铁-磷-菌体系中则大量存在Fe(Ⅲ);至试验结束时,磷酸铁-磷-菌体系中总磷质量浓度是初始时的2.3倍,而针铁矿-磷-菌和水铁矿-磷-菌体系的总磷约为初始质量浓度的1/10。因此,S.oneidensis MR~(-1)利用磷酸铁-磷的过程会促进磷的释放,使磷酸铁中磷得以活化,而利用针铁矿-磷和水铁矿-磷的过程则会消耗磷,不会造成磷累积。
[Abstract]:Phosphorus in red soil of southern China is mostly immobilized in the form of iron-phosphorus complex, and the utilization rate of phosphorus is low. In order to protect the environment and save resources, S.oneidensis MR~ (-1) was added to the soil to promote the release of soil phosphorus and reduce the input of exogenous phosphorus fertilizer. In laboratory simulation experiment, the anaerobic system inoculated with S.oneidensis MR~ (-1) was used to culture under pure chemical culture conditions, respectively, and the ferrite (pyrite phosphate) adsorbed by phosphorus was used. Phosphorus-adsorbed goethite (goethite-phosphorus) and ferric phosphate (FePO_ (4-) P) were the sole sources of phosphorus and Fe (鈪,
本文编号:2316050
[Abstract]:Phosphorus in red soil of southern China is mostly immobilized in the form of iron-phosphorus complex, and the utilization rate of phosphorus is low. In order to protect the environment and save resources, S.oneidensis MR~ (-1) was added to the soil to promote the release of soil phosphorus and reduce the input of exogenous phosphorus fertilizer. In laboratory simulation experiment, the anaerobic system inoculated with S.oneidensis MR~ (-1) was used to culture under pure chemical culture conditions, respectively, and the ferrite (pyrite phosphate) adsorbed by phosphorus was used. Phosphorus-adsorbed goethite (goethite-phosphorus) and ferric phosphate (FePO_ (4-) P) were the sole sources of phosphorus and Fe (鈪,
本文编号:2316050
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