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淹水培养条件下土壤微生物生物量碳、氮和可溶性有机碳、氦的动态
引用本文:仇少君,彭佩钦,荣湘民,刘强,唐麒.淹水培养条件下土壤微生物生物量碳、氮和可溶性有机碳、氦的动态[J].应用生态学报,2006,17(11):2052-2058.
作者姓名:仇少君  彭佩钦  荣湘民  刘强  唐麒
作者单位:[1]中国科学院亚热带农业生态研究所亚热带农业生态重点实验室,长沙410125 [2]湖南农业大学资源环境学院,长沙410128 [3]中国农业大学资源环境学院,北京100094
基金项目:中国科学院知识创新工程项目(KZCX3-SW-441)和中国科学院知识创新领域前沿资助项目(02200220020223).
摘    要:以洞庭湖区2个典型水稻土(红黄泥和紫潮泥)为对象,研究了25℃、淹水培养条件下稻草-硫铵配施和单施硫铵处理土壤微生物生物量碳、氮(SMBC、SMBN)和可溶性有机碳、氦(SDOC、SDON)的动态变化.结果表明,SMBC、SMBN和SDOC、SDON在培养前期达到峰值,之后降低,并趋于稳定.添加底物后,2种土壤不同处理土壤微生物生物量碳与有机碳(SMBC/TC)和土壤微生物生物量氮与全氮(SMBN/TN)的平均值都在2%-3%之间变化;可溶性碳与全碳(SDOC/TC)的平均值为1%左右,可溶性氮与全氮(SDON/TN)平均值为5%-6%.2种土壤中SMBC峰值单施硫铵处理最大,但与稻草-硫铵配施处理差异均不显著;SMBN、SDOC和SDON峰值稻草-硫铵配施最大.稻草.硫铵配施与单施硫铵处理中,低肥力红黄泥的SMBN、SDOC和SDON峰值差异显著;而高肥力紫潮泥SMBN和SDOC峰值差异不显著.前7d,SMBC/SMBN〈10;14d后,同一时刻单施硫铵处理SMBC/SMBN〉稻草.硫铵配施.不同处理的SDOC!SDON3d时最大.28d时最小.

关 键 词:土壤微生物生物量碳  土壤微生物生物量氮  土壤可溶性有机碳  土壤可溶性有机氮  水稻土
文章编号:1001-9332(2006)11-2052-07
收稿时间:2005-12-20
修稿时间:2006-09-28

Dynamics of soil microbial biomass and dissolved organic carbon and nitrogen under flooded condition.
QIU Shaojun, PENG Peiqin, RONG Xiangmin, LIU Qiang, TANG Qi.Dynamics of soil microbial biomass and dissolved organic carbon and nitrogen under flooded condition.[J].Chinese Journal of Applied Ecology,2006,17(11):2052-2058.
Authors:QIU Shaojun  PENG Peiqin  RONG Xiangmin  LIU Qiang  TANG Qi
Institution:1 Key Laboratory of Subtropical Agro-ecology, Institute of Subtropical Agriculture, Chinese Academy of Science, Changsha 410125, China; 2 College of Resource and Envirnament , Hunan Agricultural University, Ch, angsha 410128, China ; 3 College of Resource and Enrironment, China Agricultural University, Beijing 100094, China
Abstract:With reddish yellow soil (RYS) and alluvial purple soil (APS), the two typical paddy soils in the Dongting Lake floodplain of China as test soils, an incubation test was conducted at 25 degrees C to study the dynamic changes of soil microbial biomass and dissolved organic carbon and nitrogen under flooded condition. Three treatments were installed, i.e., control (CK), ammonium sulfate (N), and rice straw powder plus ammonium sulfate (S-N). The results showed that during incubation, soil microbial biomass carbon (SMBC), soil microbial biomass nitrogen (SMBN), soil dissolved organic carbon (SDOC), and soil dissolved organic nitrogen (SDON) reached their maximum initially, decreased thereafter, and tended to be stable. After amending the substrates to the two soils, the averages of SMBC to soil total carbon, SMBN to soil total nitrogen, SDOC to soil total carbon, and SDON to soil total nitrogen were 2% - 3%, 2% - 3%, 1% or so, and 5% - 6%, respectively. In the two soils, the peak values of SMBC in treatment N and those of SMBN, SDOC and SDON in treatment S-N were the highest, while those of SMBC in treatments N and S-N had no significant difference. The peak values of SMBN, SDOC and SDON in RYS were significantly different between treatments N and S-N, while no significant difference was observed between the peak values of SMBN and SDOC in APS, because the fertility of RYS was lower than that of APS. In the first 7 days of incubation, SMBC/SMBN ratio was < 10, while after 14 days of incubation, this ratio was higher in treatment N than in treatment S-N at the same time in the same soil. The SDOC/SDON ratio in all treatments was the highest at the 3rd d, and the lowest at the 28th d of incubation.
Keywords:Soil microbial biomass carbon  Soil microbial biomass nitrogen  Soil dissolved orgnic carbon  Soil dissolved organic nitrogen  Paddy soil  
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