Vishwakarma Pranjali, Dubey Suresh Kumar
Department of Botany, Centre of Advanced Study, Banaras Hindu University, Varanasi, India.
J Basic Microbiol. 2007 Aug;47(4):351-7. doi: 10.1002/jobm.200610282.
A laboratory incubation experiment was conducted in tropical rain-fed (red soil) and irrigated (black soil) rice agroecosystem during the crop growing season to determine the effect of the type of soil, cultivation practices and the age of plant on MOB (methane oxidizing bacteria) population size and their activities. The average value of MOB population size was 11.7 +/- 4.5 x 10(5) cells g(-1) soil, with a range of 3.1 +/- 0.4 to 21.2 +/- 1.0 x 10(5) cells g(-1) soil for red soil, which was lower in comparison to black soil where population size varied between 84.2 +/- 3.8 and 289.4 +/- 7.0 x 10(5) cells g(-1) soil with an average of 182.8 +/- 53.5 x 10(5) cells g(-1) soil. The highest population size was recorded during the grain maturation stage which gradually declined during the grain filling, flowering and tillering stages of the rice plants. The HSD test indicated a significant variation in the MOB population size with the varying ages of the plant. CH4 oxidizing capacity was higher in black soil as compared to red soil. The highest CH4 oxidizing capacity was found at the grain-filling stage in both the soil types. The differences in soil types and cultivation practices, pattern of variation in MOB population size and methane oxidation were found similar in both the sites under the influence of plant age, even though the detected values differed significantly.
在作物生长季节,于热带雨林旱作(红壤)和灌溉(黑壤)水稻农业生态系统中开展了一项实验室培养实验,以确定土壤类型、栽培措施及植株年龄对甲烷氧化细菌(MOB)种群数量及其活性的影响。MOB种群数量的平均值为11.7±4.5×10⁵ 个细胞 g⁻¹土壤,红壤中该数值范围为3.1±0.4至21.2±1.0×10⁵ 个细胞 g⁻¹土壤,与黑壤相比更低,黑壤中种群数量在84.2±3.8至289.4±7.0×10⁵ 个细胞 g⁻¹土壤之间变化,平均值为182.8±53.5×10⁵ 个细胞 g⁻¹土壤。最高种群数量出现在水稻籽粒成熟阶段,在灌浆、开花和分蘖阶段逐渐下降。最小显著差数法检验表明,MOB种群数量随植株年龄不同存在显著差异。与红壤相比,黑壤的CH₄氧化能力更高。两种土壤类型中,最高CH₄氧化能力均出现在灌浆期。尽管检测值差异显著,但在植株年龄的影响下,两个地点土壤类型和栽培措施的差异、MOB种群数量变化模式及甲烷氧化情况均相似。