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Conversion of Biovolume Measurements of Soil Organisms Grown Under Various Moisture Tensions to Biomass and Their Nutrient Content

机译:在不同湿度下生长的土壤生物的生物量测量值转换为生物量及其养分含量

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摘要

Direct microscopic measurements of biomass in soil require conversion factors for calculation of the mass of microorganisms from the measured volumes. These factors were determined for two bacteria, five fungi, and a yeast isolated from soil. Moisture stress conditions occurring in nature were simulated by growth in two media using shake cultures, on agar plates, and on membranes held at 34, 330, and 1,390 kPa of suction. The observed conversion factors, i.e., the ratio between dry weight and wet volume, generally increased with increasing moisture stress. The ratios for fungi ranged from 0.11 to 0.41 g/cm3 with an average of 0.33 g/cm3. Correction of earlier data assuming 80% water and a wet-weight specific gravity of 1.1 would require a conversion factor of 1.44. The dry-weight specific gravity of bacteria and yeasts ranged from 0.38 to 1.4 g/cm3 with an average of 0.8 g/cm3. These high values can only occur at 10% ash if no more than 50% of the cell is water, and a specific conversion factor to correct past data for bacterial biomass has not yet been suggested. The high conversion factors for bacteria and yeast could not be explained by shrinkage of cells due to heat fixing, but shrinkage during preparation could not be completely discounted. Moisture stress affected the C, N, and P content of the various organisms, with the ash contents increasing with increasing moisture stress. Although further work is necessary to obtain accurate conversion factors between biovolume and biomass, especially for bacteria, this study clearly indicates that existing data on the specific gravity and the water and nutrient content of microorganisms grown in shake cultures cannot be applied when quantifying the soil microbial biomass.
机译:对土壤中生物量进行直接的显微镜测量需要转换因子,以便根据测量的体积计算微生物的质量。确定了两种细菌,五种真菌和从土壤中分离出的酵母菌的这些因素。自然条件下发生的水分胁迫条件是通过在琼脂平板和保持在34、330和1390 kPa吸力的膜上使用摇动培养物在两种培养基中生长来模拟的。观察到的转化因子,即干重与湿体积之比,通常随着水分胁迫的增加而增加。真菌的比例为0.11至0.41 g / cm 3 ,平均为0.33 g / cm 3 。假设水含量为80%,且湿重比重为1.1,则对早期数据的校正将需要1.44的转换系数。细菌和酵母的干重比重为0.38至1.4 g / cm 3 ,平均为0.8 g / cm 3 。如果不超过50%的细胞是水,那么只有在灰分为10%时才会出现这些高值,并且尚未提出纠正细菌生物质过去数据的特定转化因子。细菌和酵母的高转化率无法用热固定引起的细胞收缩来解释,但制备过程中的收缩不能完全消除。水分胁迫影响各种生物的碳,氮和磷含量,灰分含量随水分胁迫的增加而增加。尽管需要进一步的工作来获得生物量和生物量之间的准确转换因子,尤其是对于细菌,但这项研究清楚地表明,在定量土壤微生物时,不能利用现有比重以及摇瓶培养中生长的微生物的水和养分含量的现有数据。生物质。

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