为建立潜育化稻田微生物改良技术,采用MWMM(modified wolfe’s mineral medium)培养基富集微好氧FeOB,结合16S rRNA测序等技术鉴定菌株种类,分别采用100 mL 10^(6)(T1)、10^(7)(T2)、10^(8)(T3)CFU/mL菌株发酵液处理潜育化水稻土,评价...为建立潜育化稻田微生物改良技术,采用MWMM(modified wolfe’s mineral medium)培养基富集微好氧FeOB,结合16S rRNA测序等技术鉴定菌株种类,分别采用100 mL 10^(6)(T1)、10^(7)(T2)、10^(8)(T3)CFU/mL菌株发酵液处理潜育化水稻土,评价菌株对潜育化水稻土壤的还原性物质、土壤养分、氮循环功能基因丰度和水稻秧苗生长的影响,并利用16S rRNA高通量测序技术评价该菌株对土壤微生态的影响。结果显示:筛选到的对Fe^(2+)具有较强氧化作用的FeOB为球形赖氨酸芽孢杆菌WH07(Lysinibacillus sphaericus WH07);相比于CK,土壤氧化还原电位(Eh)显著提高(P<0.05),并由负电位转为正电位;T1、T2、T3处理土壤还原性物质总量分别减少26.47%、41.53%、53.19%,亚铁含量分别减少0.37%、21.50%、50.09%,亚锰含量分别减少7.84%、21.57%、37.25%。土壤碱解氮含量分别显著增加15.50%、27.38%、48.90%(P<0.05),速效磷分别显著增加12.52%、17.34%、27.38%(P<0.05),速效钾分别显著增加11.56%、17.20%、19.34%(P<0.05),有机质分别显著增加8.66%、22.22%、45.05%(P<0.05),pH显著分别增加3.40%、8.94%、16.99%(P<0.05)。土壤AOAamoA基因丰度分别增加11.94%、14.68%、33.83%,nosZ基因丰度分别增加42.97%、75.78%、118.75%,nifH基因丰度分别增加38.29%、51.05%、216.13%,UreC基因丰度分别增加16.74%、54.51%、60.94%。水稻株高分别增加5.44%、10.98%、36.00%,叶龄分别增加10.21%、23.42%、36.94%,鲜质量增加分别12.61%、22.52%、28.38%,白根数分别增加10.14%、32.92%、46.81%。土壤微生物多样性指数Chao1和Shannon指数相比于CK均显著降低(P<0.05)。门水平上相对丰度前10的土壤细菌中,有8个显著下调(P<0.05),如Proteobacteria等、2个(Bacteroidetes和Firmicutes)显著上调。在相对丰度前50的属中,3个处理分别有20、19、22个属显著上调(P<0.05),包括Macellibacteroides等6个FeOB;25个属在3个处理中均显著下调(P<0.05),包括MBNT15等4个铁还原菌。调控网络分析显示菌株WH07潜在地与FeOB协同改善土壤理化性质和生物活性,最终促进了秧苗生长。结果表明,应用菌株WH07显著改善了潜育化水稻土壤理化性质,改变了土壤微生物群落结构和功能。展开更多
Biochar is widely used to improve soil physical properties and carbon sequestration. However, few studies focuse on the impact of maize stalk biochar on labile organic carbon(LOC) pool and the relationship between phy...Biochar is widely used to improve soil physical properties and carbon sequestration. However, few studies focuse on the impact of maize stalk biochar on labile organic carbon(LOC) pool and the relationship between physical properties and LOC fractions. A field positioning experiment was performed in Mollisols region of Northeast China to evaluate the influence of maize stalk biochar on the spatial distribution and temporal changes of physical properties and LOC fractions. Maize stalk biochar treatments included C1(1.5 kg·hm^(-2)), C2(3 kg·hm^(-2)), C3(15 kg·hm^(-2)), C4(30 kg·hm^(-2)), and CK(0). The results showed that maize stalk biochar increased soil water contents(SWC) and soil porosity(SP), but reduced bulk density(BD). Maize stalk biochar reduced dissolved organic carbon(DOC) contents in the 0-20 cm soil layer, ranging from 0.25 g·kg^(-1) to 0.31 g·kg^(-1) in harvest period, while increased in the 20-40 cm soil layer. In addition, the application of biochar had a significant impact on the spatial distribution and temporal change of SWC, BD, SP, DOC, hot-water extractable carbon(HWC), acid hydrolyzed organic carbon(AHC Ⅰ, Ⅱ), and readily oxidized organic carbon(ROC). High amounts of maize stalk biochar up-regulated the contents of soil organic carbon SOC, HWC, AHC Ⅰ, AHC Ⅱ, and ROC. In addition, SWC and SP were the key physical factors to affect LOC fractions. In conclusions, maize stalk biochar could improve physical properties, and then influence LOC fractions, and maize stalk biochar could be used as an organic amendment for restoring degraded soils governed by their rates of addition.展开更多
文摘为建立潜育化稻田微生物改良技术,采用MWMM(modified wolfe’s mineral medium)培养基富集微好氧FeOB,结合16S rRNA测序等技术鉴定菌株种类,分别采用100 mL 10^(6)(T1)、10^(7)(T2)、10^(8)(T3)CFU/mL菌株发酵液处理潜育化水稻土,评价菌株对潜育化水稻土壤的还原性物质、土壤养分、氮循环功能基因丰度和水稻秧苗生长的影响,并利用16S rRNA高通量测序技术评价该菌株对土壤微生态的影响。结果显示:筛选到的对Fe^(2+)具有较强氧化作用的FeOB为球形赖氨酸芽孢杆菌WH07(Lysinibacillus sphaericus WH07);相比于CK,土壤氧化还原电位(Eh)显著提高(P<0.05),并由负电位转为正电位;T1、T2、T3处理土壤还原性物质总量分别减少26.47%、41.53%、53.19%,亚铁含量分别减少0.37%、21.50%、50.09%,亚锰含量分别减少7.84%、21.57%、37.25%。土壤碱解氮含量分别显著增加15.50%、27.38%、48.90%(P<0.05),速效磷分别显著增加12.52%、17.34%、27.38%(P<0.05),速效钾分别显著增加11.56%、17.20%、19.34%(P<0.05),有机质分别显著增加8.66%、22.22%、45.05%(P<0.05),pH显著分别增加3.40%、8.94%、16.99%(P<0.05)。土壤AOAamoA基因丰度分别增加11.94%、14.68%、33.83%,nosZ基因丰度分别增加42.97%、75.78%、118.75%,nifH基因丰度分别增加38.29%、51.05%、216.13%,UreC基因丰度分别增加16.74%、54.51%、60.94%。水稻株高分别增加5.44%、10.98%、36.00%,叶龄分别增加10.21%、23.42%、36.94%,鲜质量增加分别12.61%、22.52%、28.38%,白根数分别增加10.14%、32.92%、46.81%。土壤微生物多样性指数Chao1和Shannon指数相比于CK均显著降低(P<0.05)。门水平上相对丰度前10的土壤细菌中,有8个显著下调(P<0.05),如Proteobacteria等、2个(Bacteroidetes和Firmicutes)显著上调。在相对丰度前50的属中,3个处理分别有20、19、22个属显著上调(P<0.05),包括Macellibacteroides等6个FeOB;25个属在3个处理中均显著下调(P<0.05),包括MBNT15等4个铁还原菌。调控网络分析显示菌株WH07潜在地与FeOB协同改善土壤理化性质和生物活性,最终促进了秧苗生长。结果表明,应用菌株WH07显著改善了潜育化水稻土壤理化性质,改变了土壤微生物群落结构和功能。
基金Supported by the National Natural Science Foundation of China Project(31770582)。
文摘Biochar is widely used to improve soil physical properties and carbon sequestration. However, few studies focuse on the impact of maize stalk biochar on labile organic carbon(LOC) pool and the relationship between physical properties and LOC fractions. A field positioning experiment was performed in Mollisols region of Northeast China to evaluate the influence of maize stalk biochar on the spatial distribution and temporal changes of physical properties and LOC fractions. Maize stalk biochar treatments included C1(1.5 kg·hm^(-2)), C2(3 kg·hm^(-2)), C3(15 kg·hm^(-2)), C4(30 kg·hm^(-2)), and CK(0). The results showed that maize stalk biochar increased soil water contents(SWC) and soil porosity(SP), but reduced bulk density(BD). Maize stalk biochar reduced dissolved organic carbon(DOC) contents in the 0-20 cm soil layer, ranging from 0.25 g·kg^(-1) to 0.31 g·kg^(-1) in harvest period, while increased in the 20-40 cm soil layer. In addition, the application of biochar had a significant impact on the spatial distribution and temporal change of SWC, BD, SP, DOC, hot-water extractable carbon(HWC), acid hydrolyzed organic carbon(AHC Ⅰ, Ⅱ), and readily oxidized organic carbon(ROC). High amounts of maize stalk biochar up-regulated the contents of soil organic carbon SOC, HWC, AHC Ⅰ, AHC Ⅱ, and ROC. In addition, SWC and SP were the key physical factors to affect LOC fractions. In conclusions, maize stalk biochar could improve physical properties, and then influence LOC fractions, and maize stalk biochar could be used as an organic amendment for restoring degraded soils governed by their rates of addition.
