Global Warming and Third Generation Algal Biofuels : A Review

2021 ◽  
Vol 37 (1) ◽  
pp. 155-165
Author(s):  
Ashwani Kumar ◽  
2012 ◽  
Vol 16 (05) ◽  
pp. 24-43

Combining Modern Life Sciences Toolbox to Tackle Current Bottlenecks for Algal Biofuels. Biodiesel: From Lab to Industry. Biofuels from Microorganisms. Membranes for Biofuel Separation. Carbon Dioxide Bio-mitigation and Third Generation Biofuel - The Way Forward.


2020 ◽  
Vol 839 ◽  
pp. 51-56
Author(s):  
Oleg B. Tsvetkov ◽  
Igor V. Baranov ◽  
Yuriy A. Laptev ◽  
Alexander V. Sharkov ◽  
Vladimir V. Mitropov ◽  
...  

Since the 1987 Montreal Protocol, chlorinated refrigerants (CFCs and HCFCs) have been pointed out as responsible for the destruction of the ozone layer. The chemical industry has realized suitable replacement for CFC-12 and for HCFC-22 e.g. HFC-134a, HFC-404A, HFC-410A, HFC-507. This generation of refrigerants developed by the chemical industry can be characterized by the no ozone depleting potential and long atmospheric lifetime resulting in global warming potential. The contribution of the HFCs to the global warming brings up to discussion whether the HFCs should be considered as a transitional substance. Historically the use of natural and ecologically safe refrigerants was a strategy to eliminate environmental problems and avoid uncertainties with synthetic replacement fluids. Since ammonia is toxic, carbon dioxide provide high pressure, and the hydrocarbons are flammable, the general conclusion is often drawn that natural fluids gave safety problems. This paper will describe the possibilities of application as working fluids in low-temperature engineering refrigeration, heat pumping and organic Rankine cycles of the hydrofluoroolefins (HFOs) as third generation of synthetic working fluids.


OALib ◽  
2014 ◽  
Vol 01 (03) ◽  
pp. 1-10
Author(s):  
Divya Srivastav ◽  
Ajay Pratap Singh ◽  
Ajay Kumar

2015 ◽  
Vol 9 (4) ◽  
pp. 358-367 ◽  
Author(s):  
Ao Xia ◽  
Christiane Herrmann ◽  
Jerry D. Murphy

2018 ◽  
Vol 26 (02) ◽  
pp. 1850013 ◽  
Author(s):  
Sachin Gupta ◽  
Narasimha Kalyan Karanam ◽  
Ramakrishna Konijeti ◽  
Abhishek Dasore

The third-generation refrigerants belonging to hydrofluorocarbons (HFCs) do not contribute to ozone depletion. However, HFCs are listed as greenhouse gases by Kyoto Protocol because of their relatively high global-warming potential (GWP). At present the research is now mainly focused on refrigerants with zero ozone depletion potential (ODP) and less GWP, which are termed as Fourth generation refrigerants. This paper analyzes the advancement in refrigerants, and presented the different options in choosing a refrigerant with respect to international agreements to curb the stratospheric ozone depletion and global warming. The hydrofluoroolefins (HFOs) i.e., fourth generation refrigerants are available in limited quantities and also their performance is not completely tested in different applications. Hence this paper aims at assessing the performance of fourth generation refrigerants in terms of their mass flow rate requirement and COP for a specified cooling load and compared with the existing third generation refrigerants in usage. It is found that fourth generation refrigerants COP is low and mass flow rate and power requirements are high. However, HFO1234ze(E) can replace R134a as its performance is almost similar to R134a with an added advantage of low GWP.


2019 ◽  
Vol 3 (2) ◽  
pp. 221-231 ◽  
Author(s):  
Rebecca Millington ◽  
Peter M. Cox ◽  
Jonathan R. Moore ◽  
Gabriel Yvon-Durocher

Abstract We are in a period of relatively rapid climate change. This poses challenges for individual species and threatens the ecosystem services that humanity relies upon. Temperature is a key stressor. In a warming climate, individual organisms may be able to shift their thermal optima through phenotypic plasticity. However, such plasticity is unlikely to be sufficient over the coming centuries. Resilience to warming will also depend on how fast the distribution of traits that define a species can adapt through other methods, in particular through redistribution of the abundance of variants within the population and through genetic evolution. In this paper, we use a simple theoretical ‘trait diffusion’ model to explore how the resilience of a given species to climate change depends on the initial trait diversity (biodiversity), the trait diffusion rate (mutation rate), and the lifetime of the organism. We estimate theoretical dangerous rates of continuous global warming that would exceed the ability of a species to adapt through trait diffusion, and therefore lead to a collapse in the overall productivity of the species. As the rate of adaptation through intraspecies competition and genetic evolution decreases with species lifetime, we find critical rates of change that also depend fundamentally on lifetime. Dangerous rates of warming vary from 1°C per lifetime (at low trait diffusion rate) to 8°C per lifetime (at high trait diffusion rate). We conclude that rapid climate change is liable to favour short-lived organisms (e.g. microbes) rather than longer-lived organisms (e.g. trees).


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