Simulation of Temperature Self-Regulation in a Bioreactor

A. A. Arzamastsev; E. N. Albitskaya

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Simulation of Temperature Self-Regulation in a Bioreactor

机译：生物反应器中温度自我调节的模拟

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The paper reports the construction of mathematical models to study the phenomenon of self-regulation (autostabilization) of temperature in the bioreactor of a continuous type with one or two biological objects. These models have been parametrically identified and their adequacy proved on the basis of experimental data. They have been used to find the boundaries of the existence of this phe-nomenon and to analyze its basic occurrences. The performed calculation experiments have shown how to use this phenomenon in practical applications.

机译：该论文报道了数学模型的构建，以研究具有一个或两个生物对象的连续型生物反应器中温度的自我调节（自稳定）现象。这些模型已经过参数识别，并根据实验数据证明了它们的适当性。他们已被用来寻找这种现象的存在边界，并分析其基本发生。进行的计算实验表明了如何在实际应用中使用这种现象。

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《Mathematical models and computer simulations》 |2011年第3期|共12页
作者
A. A. Arzamastsev; E. N. Albitskaya;
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原文格式 PDF
正文语种 eng
中图分类数学;
关键词
mathematical model; temperature autostabilization; self-regulation; population of micro-organisms; specific growth rate;

机译：数学模型温度自动稳定自我调节微生物种群比生长率;

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1. Simulation of Temperature Self-Regulation in a Bioreactor [J] . A. A. Arzamastsev, E. N. Albitskaya Mathematical models and computer simulations . 2011,第3期

机译：生物反应器中温度自我调节的模拟
2. Simulation of air and ground temperatures in PMIP3/CMIP5 last millennium simulations: implications for climate reconstructions from borehole temperature profiles [J] . A García-García1, F J Cuesta-Valero1, H Beltrami124, Environmental Research Letters . 2016,第4期

机译：上个千年模拟中PMIP3 / CMIP5中的空气和地面温度模拟：钻孔温度曲线对气候重建的影响
3. Next-generation polymerized human hemoglobins in hepatic bioreactor simulations [J] . Biotechnology Progress . 2020,第3期

机译：肝生物反应器模拟中的下一代聚合人血红蛋白
4. Simulation of Temperature Effect on Microalgae Culture in a Tubular Photo bioreactor for Local Solar Irradiance [C] . M. Shahriar, Ujjwal Kumar Deb, Kazi Afzalur Rahman BSME International Conference on Thermal Engineering . 2017

机译：用于局部太阳辐前的管状照相生物反应器中微藻培养温度效应的模拟
5. Anaerobic membrane bioreactors to treat municipal wastewater at ambient temperatures. [D] . Seib, Matthew D. 2015

机译：厌氧膜生物反应器可在环境温度下处理市政废水。
6. Towards temperature-dependent coarse-grained potentials of side-chain interactions for protein folding simulations. I: Molecular dynamics study of a pair of methane molecules in water at various temperatures [O] . Emil Sobolewski, Mariusz Makowski, Stanisław Ołdziej, -1

机译：迈向蛋白质折叠模拟的侧链相互作用的温度依赖性粗粒电势。 I：在不同温度下水中一对甲烷分子的分子动力学研究
7. The oceans mediate the response of global climate to natural and anthropogenic forcings. Yet for the past 2,000 years — a key interval for understanding the present and future climate response to these forcings — global sea surface temperature changes and the underlying driving mechanisms are poorly constrained. Here we present a global synthesis of sea surface temperatures for the Common Era (ce) derived from 57 individual marine reconstructions that meet strict quality control criteria. We observe a cooling trend from 1 to 1800 ce that is robust against explicit tests for potential biases in the reconstructions. Between 801 and 1800 ce, the surface cooling trend is qualitatively consistent with an independent synthesis of terrestrial temperature reconstructions, and with a sea surface temperature composite derived from an ensemble of climate model simulations using best estimates of past external radiative forcings. Climate simulations using single and cumulative forcings suggest that the ocean surface cooling trend from 801 to 1800 ce is not primarily a response to orbital forcing but arises from a high frequency of explosive volcanism. Our results show that repeated clusters of volcanic eruptions can induce a net negative radiative forcing that results in a centennial and global scale cooling trend via a decline in mixed-layer oceanic heat content. [O] . McGregor, Helen V., Evans, Michael N., Goosse, Hugues, 2015

机译：海洋调节了全球气候对自然和人为强迫的响应。然而，在过去的2,000年中（这是了解当前和未来气候对这些强迫的响应的关键间隔），全球海表温度变化及其潜在的驱动机制受到的约束很有限。在这里，我们提出了一个共同的时期（ce）的全球海面温度的全球综合，该综合来自57个符合严格质量控制标准的海洋重建项目。我们观察到从1到1800 ce的冷却趋势，对于显式测试重建中潜在的偏倚而言，该趋势很稳健。在801至1800 ce之间，表面降温趋势在质量上与地面温度重建的独立合成以及从使用过去外部辐射强迫的最佳估计的气候模型模拟集合推导出的海面温度合成在质量上是一致的。使用单一和累积强迫的气候模拟表明，从801到1800 ce的海洋表面冷却趋势主要不是对轨道强迫的反应，而是爆炸性火山爆发的频繁发生。我们的结果表明，火山喷发的反复簇可引起净的负辐射强迫，这会导致混合层海洋热量降低而导致百年和全球规模的降温趋势。

Simulation of Temperature Self-Regulation in a Bioreactor

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