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Physico-chemical properties and bacterial population in flooded rice soils

机译:淹水水稻土的理化特性和细菌种群

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The physicochemical properties, aerobic and anaerobic bacterial population in alluvial and acid sulphate soils and roots of rice plants were studied in the present study. There was slight variation in pH of soil from 5.47 in alluvial soil to 5.15 in acid-sulfate soil.Higher organicmatter content was observed in pokkali than alluvial soil. The total nitrogen and sulfate are higher in alluvial soil, than pokkali. Flooded rice soils are predominantly with anaerobic environment with micro sites of nutrient poor or rich conditions. The total population of DNB bacteria in alluvial soil was considerable whereas the population of NB bacteria in flooded alluvial soil wasmore than that of the DNB bacteria under aerobic conditions. On the contrarily, DNB were dominated under anaerobic conditions. Flooded conditions are favorable for the growth of oligotrophic bacteria especially those capable of growing under anaerobic conditions. The anaerobic oligotrophic bacterial populationwas higher than the population of aerobic oligotrophic bacteria in the roots of rice plant.
机译:本研究研究了冲积和酸性硫酸盐土壤以及水稻根系的理化特性,需氧和厌氧细菌种群。土壤的pH值从冲积土壤的5.47到酸性硫酸盐土壤的5.15略有变化.pokkali的有机物含量高于冲积土壤。冲积土壤中的总氮和硫酸盐含量高于pokkali。淹水的水稻土主要处于厌氧环境,微量营养元素贫乏或丰富。在有氧条件下,冲积土壤中DNB细菌的总数量是可观的,而淹水冲积土壤中的NB细菌的数量要大于DNB细菌的数量。相反,DNB在厌氧条件下占主导地位。淹水条件有利于寡营养细菌的生长,特别是那些能够在厌氧条件下生长的细菌。水稻根系中厌氧的贫营养菌的数量高于需氧的贫营养菌的数量。

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