In order to explore the nitrogen removal process in constructed wetlands(CW s),the moisture,ammonia nitrogen(NH4+-N),nitrate nitrogen(NO3"-N)and nitrification intensity in three wetland plant rhizosphere soils(Ac...In order to explore the nitrogen removal process in constructed wetlands(CW s),the moisture,ammonia nitrogen(NH4+-N),nitrate nitrogen(NO3"-N)and nitrification intensity in three wetland plant rhizosphere soils(Acorns calamus,Typha orientalis,Iris pseudacorus)were investigated at a relatively normal temperature range of15to25The relative abundance of ammonia-oxidizing bacteria(AOB)and ammonia-oxidizing archaea(AOA)were also achieved using fluorescence in situ hybridization(FISH).It is found that T.orientalis achieves the highest nitrification intensity of2.03m g(h?kg)while the second is I.pseudacorrs(1.74m g/(h?kg)),and followed by A.calamus(1.65m g/(h?kg))throughout the experiment.FISH reveals that the abundance of bacteria(1010g_1wet soil)is higher than that of archaea(109g_1wet soil),and AOBare the dominant bacteria in the ammonia oxidation process.The abundance of AOB in te rhizosphere soils from high to low T.orientalis(1.88x1010g"1),I pseudacorus(1.23x1010g1),A.calamus(5.07x109g"1)while the abundance of AOA from high to low ae I.pseudacorus(4.00x109g1),A.calamus(3.52x109g"1),T.orientalis(3.48x109g"1).The study provides valuable evidence of plant selection for nitrogen removal in CWs.展开更多
风干处理常对土壤中的硝化细菌数量和活性造成显著影响.为研究土壤硝化作用的干土效应,以分别发育于第四纪红土(quaternary red earth,Q)和红砂岩(tertiary red sandstone,S),利用方式为水稻(rice,R)与旱地(upland,U)的4个农田土壤的新...风干处理常对土壤中的硝化细菌数量和活性造成显著影响.为研究土壤硝化作用的干土效应,以分别发育于第四纪红土(quaternary red earth,Q)和红砂岩(tertiary red sandstone,S),利用方式为水稻(rice,R)与旱地(upland,U)的4个农田土壤的新鲜土与风干土为供试材料,进行35d的室内培养试验.结果表明,对于无外源铵输入的处理而言,旱地土壤QU的新鲜土和风干土的硝化率分别为48%和54%,SU则分别为76%和78%,硝化作用的干土效应均不显著(p>0.05);但干土效应却显著影响了水稻土的硝化作用(QR的新鲜土和风干土的硝化率分别为40%和89%,SR分别为76%和94%,p<0.01),且其风干土样的硝化作用表现出明显的微生物激活过程.外源铵的加入促进了土壤的硝化作用强度且使得旱地土壤的干土效应显著,所有供试土壤新鲜土的硝化率均显著高于风干土的硝化率.总之,土壤利用方式显著影响了硝化作用对干土效应的响应,而且利用方式和加铵对硝化作用的干土效应有着极显著的交互作用.展开更多
基金The National Natural Science Foundation of China(No.51479034,50909019)the Fundamental Research Funds for the Central Universities
文摘In order to explore the nitrogen removal process in constructed wetlands(CW s),the moisture,ammonia nitrogen(NH4+-N),nitrate nitrogen(NO3"-N)and nitrification intensity in three wetland plant rhizosphere soils(Acorns calamus,Typha orientalis,Iris pseudacorus)were investigated at a relatively normal temperature range of15to25The relative abundance of ammonia-oxidizing bacteria(AOB)and ammonia-oxidizing archaea(AOA)were also achieved using fluorescence in situ hybridization(FISH).It is found that T.orientalis achieves the highest nitrification intensity of2.03m g(h?kg)while the second is I.pseudacorrs(1.74m g/(h?kg)),and followed by A.calamus(1.65m g/(h?kg))throughout the experiment.FISH reveals that the abundance of bacteria(1010g_1wet soil)is higher than that of archaea(109g_1wet soil),and AOBare the dominant bacteria in the ammonia oxidation process.The abundance of AOB in te rhizosphere soils from high to low T.orientalis(1.88x1010g"1),I pseudacorus(1.23x1010g1),A.calamus(5.07x109g"1)while the abundance of AOA from high to low ae I.pseudacorus(4.00x109g1),A.calamus(3.52x109g"1),T.orientalis(3.48x109g"1).The study provides valuable evidence of plant selection for nitrogen removal in CWs.
文摘风干处理常对土壤中的硝化细菌数量和活性造成显著影响.为研究土壤硝化作用的干土效应,以分别发育于第四纪红土(quaternary red earth,Q)和红砂岩(tertiary red sandstone,S),利用方式为水稻(rice,R)与旱地(upland,U)的4个农田土壤的新鲜土与风干土为供试材料,进行35d的室内培养试验.结果表明,对于无外源铵输入的处理而言,旱地土壤QU的新鲜土和风干土的硝化率分别为48%和54%,SU则分别为76%和78%,硝化作用的干土效应均不显著(p>0.05);但干土效应却显著影响了水稻土的硝化作用(QR的新鲜土和风干土的硝化率分别为40%和89%,SR分别为76%和94%,p<0.01),且其风干土样的硝化作用表现出明显的微生物激活过程.外源铵的加入促进了土壤的硝化作用强度且使得旱地土壤的干土效应显著,所有供试土壤新鲜土的硝化率均显著高于风干土的硝化率.总之,土壤利用方式显著影响了硝化作用对干土效应的响应,而且利用方式和加铵对硝化作用的干土效应有着极显著的交互作用.
