Faust M A, Aotaky A E, Hargadon M T
Appl Microbiol. 1975 Nov;30(5):800-6. doi: 10.1128/am.30.5.800-806.1975.
Survival of Escherichia coli MC-6 of fecal origin in an estuarine environment as affected by time, water temperature, dissolved oxygen, salinity, and montmorillonite in diffusion chambers has been elucidated. Several in situ physical parameters were recorded simultaneously, and viable cell numbers were estimated. The survival of the bacteria varied seasonally. Montmorillonite addition extended the time needed for a 50% reduction of the viable cell population (t1/2) of cells by 40% over the t1/2 of cells in Rhode River water alone. The effect of this clay was not significantly greater between 50- to 1,000 mug/ml montmorillonite concentrations. In all experiments, the relationships among pairs of variables were studied by regression and correlation analysis. The slope between viable cell numbers and water temperatures increased about 50% for each 10 C increment in temperature and gave a correlation coefficient r = 0.617, significant at 95% confidence level. A similar correlation coefficient, r = 0.670, was obtained between water temperature and t1/2 of the initial cell population. In all experiments regressions were performed considering all variables after bacteria had been in the Rhode River environment for 3 days. Coefficient of multiple determination was estimated as R2 = 0.756. Approximately 75.6% of the variance of viable cell numbers can be explained by variation in water temperature, dissolved oxygen, and salinity. Simple correlation coefficients within the regression steps were also computed. Survival of bacteria was closely and negatively correlated with increasing water temperature (r = -0.717). It is suggested that water temperature is the most important factor in predicting fecal coliform survival from point and nonpoint sources in assessing water quality in an estuarine ecosystem.
已阐明了粪便来源的大肠杆菌MC - 6在河口环境中,受扩散室中的时间、水温、溶解氧、盐度和蒙脱石影响下的存活情况。同时记录了几个原位物理参数,并估算了活菌数量。细菌的存活呈现季节性变化。添加蒙脱石使活菌数量减少50%所需的时间(t1/2)比仅在罗德河水中的细胞t1/2延长了40%。在蒙脱石浓度为50至1000微克/毫升之间,这种黏土的效果并无显著差异。在所有实验中,通过回归和相关分析研究了变量对之间的关系。温度每升高10℃,活菌数量与水温之间的斜率增加约50%,相关系数r = 0.617,在95%置信水平下显著。在水温与初始细胞群体的t1/2之间也获得了类似的相关系数r = 0.670。在所有实验中,在细菌置于罗德河环境3天后,考虑所有变量进行回归。多重决定系数估计为R2 = 0.756。活菌数量约75.6%的方差可由水温、溶解氧和盐度的变化来解释。还计算了回归步骤中的简单相关系数。细菌的存活与水温升高密切负相关(r = -0.717)。有人提出,在评估河口生态系统水质时,水温是预测点源和非点源粪便大肠菌群存活的最重要因素。