Qiu Shaojun, Peng Peiqin, Rong Xiangmin, Liu Qiang, Tang Qi
Key Laboratory of Subtropical Agro-ecology, Institute of Subtropical Agriculture, Chinese Academy of Science, Changsha 410125, China.
Ying Yong Sheng Tai Xue Bao. 2006 Nov;17(11):2052-8.
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.
以中国洞庭湖平原两种典型水稻土——红黄壤(RYS)和冲积性紫色土(APS)为供试土壤,在25℃下进行室内培养试验,研究淹水条件下土壤微生物生物量及溶解性有机碳、氮的动态变化。设置3个处理,即对照(CK)、硫酸铵(N)、稻草粉+硫酸铵(S-N)。结果表明,培养期间,土壤微生物生物量碳(SMBC)、土壤微生物生物量氮(SMBN)、土壤溶解性有机碳(SDOC)和土壤溶解性有机氮(SDON)均先升高后降低,最终趋于稳定。两种土壤添加底物后,SMBC与土壤总碳、SMBN与土壤总氮、SDOC与土壤总碳、SDON与土壤总氮的平均比值分别为约2% - 3%、2% - 3%、1%左右和5% - 6%。两种土壤中,处理N的SMBC峰值以及处理S-N的SMBN、SDOC和SDON峰值最高,处理N和S-N的SMBC峰值差异不显著。RYS中处理N和S-N的SMBN、SDOC和SDON峰值差异显著,而APS中SMBN和SDOC峰值差异不显著,这是因为RYS的肥力低于APS。培养前期7天内,SMBC/SMBN比值<10,培养14天后,同一土壤相同时间内处理N的该比值高于处理S-N。各处理的SDOC/SDON比值在培养第3天最高,第28天最低。