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底栖和浮游病毒衰变实验:基于模型的分析及其适用性。

Benthic and pelagic viral decay experiments: a model-based analysis and its applicability.

作者信息

Fischer Ulrike R, Weisz Willy, Wieltschnig Claudia, Kirschner Alexander K T, Velimirov Branko

机构信息

Center for Anatomy and Cell Biology, Research Group General Microbiology, Medical University of Vienna, Vienna, Austria.

出版信息

Appl Environ Microbiol. 2004 Nov;70(11):6706-13. doi: 10.1128/AEM.70.11.6706-6713.2004.

Abstract

The viral decay in sediments, that is, the decrease in benthic viral concentration over time, was recorded after inhibiting the production of new viruses. Assuming that the viral abundance in an aquatic system remains constant and that viruses from lysed bacterial cells replace viruses lost by decay, the decay of viral particles can be used as a measure of viral production. Decay experiments showed that this approach is a useful tool to assess benthic viral production. However, the time course pattern of the decay experiments makes their interpretation difficult, regardless of whether viral decay is determined in the water column or in sediments. Different curve-fitting approaches (logarithmic function, power function, and linear regression) to describe the time course of decay experiments found in the literature are used in the present study and compared to a proposed "exponential decay" model based on the assumption that at any moment the decay is proportional to the amount of viruses present. Thus, an equation of the form dVA/dt = -k x VA leading to the time-integrated form VAt = VA0 x e(-k x t) was used, where k represents the viral decay rate (h(-1)), VAt is the viral abundance (viral particles ml(-1)) at time t (h), and VA0 is the initial viral abundance (viral particles ml(-1)). This approach represents the best solution for an accurate curve fitting based on a mathematical model for a realistic description of viral decay occurring in aquatic systems. Decay rates ranged from 0.0282 to 0.0696 h(-1) (mean, 0.0464 h(-1)). Additionally, a mathematical model is presented that enables the quantification of the viral control of bacterial production. The viral impact on bacteria based on decay rates calculated from the different mathematical approaches varied widely within one and the same decay experiment. A comparison of the viral control of bacterial production in different aquatic environments is, therefore, improper when different mathematical formulas are used to interpret viral decay experiments.

摘要

在抑制新病毒产生后,记录了沉积物中病毒的衰减情况,即底栖病毒浓度随时间的降低。假设水生系统中病毒丰度保持恒定,且裂解细菌细胞释放的病毒可替代因衰减而损失的病毒,那么病毒颗粒的衰减可作为病毒产生的一种度量。衰减实验表明,这种方法是评估底栖病毒产生的有用工具。然而,无论在水柱还是沉积物中测定病毒衰减,衰减实验的时间进程模式都使其难以解释。本研究采用了文献中用于描述衰减实验时间进程的不同曲线拟合方法(对数函数、幂函数和线性回归),并与基于在任何时刻衰减都与现存病毒量成比例这一假设提出的“指数衰减”模型进行比较。因此,使用了形式为dVA/dt = -k×VA的方程,其积分形式为VAt = VA0×e^(-k×t),其中k代表病毒衰减率(h⁻¹),VAt是时间t(h)时的病毒丰度(病毒颗粒·ml⁻¹),VA0是初始病毒丰度(病毒颗粒·ml⁻¹)。这种方法是基于数学模型对水生系统中实际发生的病毒衰减进行准确曲线拟合的最佳解决方案。衰减率范围为0.0282至0.0696 h⁻¹(平均值为0.0464 h⁻¹)。此外,还提出了一个数学模型,可对细菌生产的病毒控制进行量化。在同一衰减实验中,基于不同数学方法计算出的衰减率对细菌的病毒影响差异很大。因此,当使用不同数学公式解释病毒衰减实验时,比较不同水生环境中细菌生产的病毒控制是不合适的。

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