Department of Soil Science, University of Saskatchewan, Saskatoon, Canada.
Appl Environ Microbiol. 1979 Apr;37(4):686-92. doi: 10.1128/aem.37.4.686-692.1979.
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/cm with an average of 0.33 g/cm. 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/cm with an average of 0.8 g/cm. 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.
直接测量土壤生物量需要转换因子,以便将测量的体积转换为微生物的质量。本研究测定了从土壤中分离出的两种细菌、五种真菌和一种酵母的转换因子。通过在两种培养基中进行摇瓶培养、琼脂平板培养和在 34、330 和 1390 kPa 负压下保持的膜上培养来模拟自然发生的水分胁迫条件。观察到的转换因子(即干重与湿体积的比值)通常随水分胁迫的增加而增加。真菌的比值范围为 0.11 至 0.41 g/cm,平均值为 0.33 g/cm。假设 80%的水和湿重比重为 1.1,对早期数据进行修正需要 1.44 的转换因子。细菌和酵母的干重比重范围为 0.38 至 1.4 g/cm,平均值为 0.8 g/cm。如果细胞含水量不超过 50%且无灰分超过 10%,则这些高值仅在这种情况下出现,并且尚未提出用于修正细菌生物量的过去数据的特定转换因子。细菌和酵母的高转换因子不能用热固定导致的细胞收缩来解释,但在制备过程中的收缩不能完全排除。水分胁迫会影响各种生物的 C、N 和 P 含量,随着水分胁迫的增加,灰分含量增加。尽管需要进一步的工作来获得生物体积和生物量之间的准确转换因子,特别是对于细菌,但本研究清楚地表明,在定量土壤微生物生物量时,不能将在摇瓶培养中生长的微生物的比重以及水和养分含量的现有数据应用于微生物。