【目的】土壤微生物量碳氮和水溶性有机碳氮是土壤中最活跃的碳氮组分,是衡量土壤碳氮周转与养分有效性的重要指标。探讨秸秆配施氮肥、氮肥用量及基追比例对稻田土壤微生物量碳氮、水溶性有机碳氮、易氧化有机碳和速效氮的影响,明确秸...【目的】土壤微生物量碳氮和水溶性有机碳氮是土壤中最活跃的碳氮组分,是衡量土壤碳氮周转与养分有效性的重要指标。探讨秸秆配施氮肥、氮肥用量及基追比例对稻田土壤微生物量碳氮、水溶性有机碳氮、易氧化有机碳和速效氮的影响,明确秸秆还田条件下水稻生长季不同氮肥用量与基追比的土壤活性碳氮变化特征,为稻麦轮作区秸秆还田的氮肥管理提供理论依据。【方法】2012—2015年在湖北省荆门市田间试验中设置施氮量、秸秆配施氮肥和施氮时期3个大田试验。施氮量:不施氮(N0),推荐施氮(165 kg·hm^-2,N165),习惯施氮(195 kg·hm^-2,N195);秸秆配施氮肥:秸秆移除(CK),秸秆还田(移栽前将上季小麦秸秆全部还田,S),秸秆还田+习惯施氮量(SN),秸秆还田+推荐施氮量(SF),秸秆还田+推荐施氮量+腐解菌剂(SM);施氮时期:基施﹕拔节期﹕抽穗期氮肥施用比例为7﹕3﹕0(R1),5﹕3﹕2(R2),10﹕0﹕0(R3)。【结果】秸秆还田+习惯施氮量(SN)显著提高了水稻拔节期土壤微生物量碳(SMBC)含量,但是其成熟期水溶性有机碳含量(DOC)显著降低。秸秆还田+推荐施氮量(SF)显著提高了水稻拔节期土壤水溶性有机氮含量(DON)。腐解菌剂的施用显著降低了水稻成熟期DON含量,拔节期易氧化有机碳含量(ROC)也显著降低。秸秆还田下增加氮肥用量显著提高了水稻抽穗期和灌浆期土壤速效氮含量(AN);推荐施氮处理(165 kg N·hm^-2)的DON和AN含量显著升高;农民习惯施氮处理(195 kg N·hm^-2)降低了DON和AN含量;增加追施氮肥比例对土壤SMBC和DOC含量无明显影响,但提高了水稻拔节期SMBN和ROC含量。【结论】施氮量及其基追比是影响秸秆还田下稻田土壤活性碳氮含量的主要因素,合理配施氮肥能提高土壤微生物量碳、速效氮及水溶性有机氮等活性碳氮组分含量,增加追肥比例也能提高水稻生育期内土壤活性碳氮含量。展开更多
Introduction:In Central Himalaya,anthropogenic activities have led to the widespread replacement of Banj oak(Quercus leucotrichophora)forest by Chir pine(Pinus roxburghii)for decades.This study was conducted to determ...Introduction:In Central Himalaya,anthropogenic activities have led to the widespread replacement of Banj oak(Quercus leucotrichophora)forest by Chir pine(Pinus roxburghii)for decades.This study was conducted to determine how natural Banj oak,Chir pine,and mixed oak-pine forest would differ in soil microbial biomass and soil nutrients.Soil microbial biomass nitrogen(SMBN)and phosphorus(SMBP),soil organic carbon(SOC)total nitrogen(TN),and total phosphorus(TP)in the 0 to 15 cm soil layer were investigated in the Central Himalayan region in the stands of Banj oak,mixed oak-pine,and Chir pine forest.Results:The SMBN and SMBP were significantly higher in Banj oak and mixed oak-pine forest as compared to Chir pine forest.The ratios of SMBN to TN(SMBN/TN)and SMBP to TP(SMBP/TP)were significantly higher in the Chir pine forest,indicating that in this forest,the proportion of microbial biomass N and P to total soil N and P was higher as compared to Banj oak forest.A similar pattern of variation was found in relation to season across the forests,all with an apparent peak in the rainy season.Conclusion:These results indicate that low microbial biomass N and P may be one of the reasons to create a nutrient poor site in Chir pine forest.The collection of pine litter by local people also impairs the return of nutrients to the soil and makes it difficult for Banj oak to re-invade areas occupied by Chir pine.This calls for cautions in large-scale conversions of the Banj oak forests to coniferous plantations as a forest management practice on concerns of sustaining soil productivity.展开更多
文摘【目的】土壤微生物量碳氮和水溶性有机碳氮是土壤中最活跃的碳氮组分,是衡量土壤碳氮周转与养分有效性的重要指标。探讨秸秆配施氮肥、氮肥用量及基追比例对稻田土壤微生物量碳氮、水溶性有机碳氮、易氧化有机碳和速效氮的影响,明确秸秆还田条件下水稻生长季不同氮肥用量与基追比的土壤活性碳氮变化特征,为稻麦轮作区秸秆还田的氮肥管理提供理论依据。【方法】2012—2015年在湖北省荆门市田间试验中设置施氮量、秸秆配施氮肥和施氮时期3个大田试验。施氮量:不施氮(N0),推荐施氮(165 kg·hm^-2,N165),习惯施氮(195 kg·hm^-2,N195);秸秆配施氮肥:秸秆移除(CK),秸秆还田(移栽前将上季小麦秸秆全部还田,S),秸秆还田+习惯施氮量(SN),秸秆还田+推荐施氮量(SF),秸秆还田+推荐施氮量+腐解菌剂(SM);施氮时期:基施﹕拔节期﹕抽穗期氮肥施用比例为7﹕3﹕0(R1),5﹕3﹕2(R2),10﹕0﹕0(R3)。【结果】秸秆还田+习惯施氮量(SN)显著提高了水稻拔节期土壤微生物量碳(SMBC)含量,但是其成熟期水溶性有机碳含量(DOC)显著降低。秸秆还田+推荐施氮量(SF)显著提高了水稻拔节期土壤水溶性有机氮含量(DON)。腐解菌剂的施用显著降低了水稻成熟期DON含量,拔节期易氧化有机碳含量(ROC)也显著降低。秸秆还田下增加氮肥用量显著提高了水稻抽穗期和灌浆期土壤速效氮含量(AN);推荐施氮处理(165 kg N·hm^-2)的DON和AN含量显著升高;农民习惯施氮处理(195 kg N·hm^-2)降低了DON和AN含量;增加追施氮肥比例对土壤SMBC和DOC含量无明显影响,但提高了水稻拔节期SMBN和ROC含量。【结论】施氮量及其基追比是影响秸秆还田下稻田土壤活性碳氮含量的主要因素,合理配施氮肥能提高土壤微生物量碳、速效氮及水溶性有机氮等活性碳氮组分含量,增加追肥比例也能提高水稻生育期内土壤活性碳氮含量。
文摘Introduction:In Central Himalaya,anthropogenic activities have led to the widespread replacement of Banj oak(Quercus leucotrichophora)forest by Chir pine(Pinus roxburghii)for decades.This study was conducted to determine how natural Banj oak,Chir pine,and mixed oak-pine forest would differ in soil microbial biomass and soil nutrients.Soil microbial biomass nitrogen(SMBN)and phosphorus(SMBP),soil organic carbon(SOC)total nitrogen(TN),and total phosphorus(TP)in the 0 to 15 cm soil layer were investigated in the Central Himalayan region in the stands of Banj oak,mixed oak-pine,and Chir pine forest.Results:The SMBN and SMBP were significantly higher in Banj oak and mixed oak-pine forest as compared to Chir pine forest.The ratios of SMBN to TN(SMBN/TN)and SMBP to TP(SMBP/TP)were significantly higher in the Chir pine forest,indicating that in this forest,the proportion of microbial biomass N and P to total soil N and P was higher as compared to Banj oak forest.A similar pattern of variation was found in relation to season across the forests,all with an apparent peak in the rainy season.Conclusion:These results indicate that low microbial biomass N and P may be one of the reasons to create a nutrient poor site in Chir pine forest.The collection of pine litter by local people also impairs the return of nutrients to the soil and makes it difficult for Banj oak to re-invade areas occupied by Chir pine.This calls for cautions in large-scale conversions of the Banj oak forests to coniferous plantations as a forest management practice on concerns of sustaining soil productivity.
