Fuel-Cell and Electrolysis By-Product D2O Improves Third Way to Mitigate CO2

Author(s):  
William Ernest Schenewerk

Rapid atomic power deployment may be possible without using fast breeder reactors or making undue demands on uranium resource. Using by-product D2O and thorium-U233 in CANDU and RBMK piles may circumvent need for either fast breeder reactors or seawater uranium. Atmospheric CO2 is presently increasing 2.25%/a (2.25 percent per year) in proportion to 2.25%/a exponential fossil fuel consumption increase. Roughly 1/3 anthropologic CO2 is removed by various CO2 sinks. CO2 removal is modeled as being proportional to 50-year-earlier CO2 amount above 280 ppm-C. Water electrolysis produces roughly 0.1 kg-D20/kWa. Material balance assumes each electrolysis stage increases D2O bottoms concentration times 3. Except for first electrolysis stage, all water from hydrogen consumption is returned to electrolysis. D2O enrichment from water electrolysis is augmented by using the resulting Hydrogen and Oxygen in fuel cells. Condensate from hydrogen consumption returns to the appropriate electrolysis stage. Fuel cell condensate originally from reformed natural gas may augment second-stage feed. Previously, recycling only hydrogen from combustion back to upper electrolysis stages allowed a 5%/a atomic power expansion. Using fuel-cells to augment upper-stage electrolysis enrichment increases atomic power expansion from 5%/a to 6%/a. Implementation of this process should start by 2020 to minimize peak atmospheric CO2 concentration to 850 ppm-C. Atomic power expansion is 6%/a, giving 45000 GW by 2100. World primary energy increases at the historic rate of 2.25%/a, exceeding 4000 EJ-thermal/a by 2100. J-electric ∼ 3J-thermal. CO2 maximum is roughly 850 ppm-C around year 2100. CO2 declines back below 350 ppm-C by 2250 if the 50-year-delay seawater sink remains effective. The 15-year global temperature rise hiatus is apparently caused by convective heat transfer into seawater. Presumably convective CO2 transfer into seawater also occurs by the same mechanism. Each decade rapid atomic power expansion is delayed results in a 100 ppm increase in maximum atmospheric CO2 concentration. 50 TW dispatchable CSP (concentrated solar power), including 2 TWa storage, costs 1600 trillion USD and covers two Australias.

2019 ◽  
Vol 16 (19) ◽  
pp. 3883-3910 ◽  
Author(s):  
Lina Teckentrup ◽  
Sandy P. Harrison ◽  
Stijn Hantson ◽  
Angelika Heil ◽  
Joe R. Melton ◽  
...  

Abstract. Understanding how fire regimes change over time is of major importance for understanding their future impact on the Earth system, including society. Large differences in simulated burned area between fire models show that there is substantial uncertainty associated with modelling global change impacts on fire regimes. We draw here on sensitivity simulations made by seven global dynamic vegetation models participating in the Fire Model Intercomparison Project (FireMIP) to understand how differences in models translate into differences in fire regime projections. The sensitivity experiments isolate the impact of the individual drivers on simulated burned area, which are prescribed in the simulations. Specifically these drivers are atmospheric CO2 concentration, population density, land-use change, lightning and climate. The seven models capture spatial patterns in burned area. However, they show considerable differences in the burned area trends since 1921. We analyse the trajectories of differences between the sensitivity and reference simulation to improve our understanding of what drives the global trends in burned area. Where it is possible, we link the inter-model differences to model assumptions. Overall, these analyses reveal that the largest uncertainties in simulating global historical burned area are related to the representation of anthropogenic ignitions and suppression and effects of land use on vegetation and fire. In line with previous studies this highlights the need to improve our understanding and model representation of the relationship between human activities and fire to improve our abilities to model fire within Earth system model applications. Only two models show a strong response to atmospheric CO2 concentration. The effects of changes in atmospheric CO2 concentration on fire are complex and quantitative information of how fuel loads and how flammability changes due to this factor is missing. The response to lightning on global scale is low. The response of burned area to climate is spatially heterogeneous and has a strong inter-annual variation. Climate is therefore likely more important than the other factors for short-term variations and extremes in burned area. This study provides a basis to understand the uncertainties in global fire modelling. Both improvements in process understanding and observational constraints reduce uncertainties in modelling burned area trends.


2000 ◽  
Vol 145 (2) ◽  
pp. 245-256 ◽  
Author(s):  
C. K. YODER ◽  
P. VIVIN ◽  
L. A. DEFALCO ◽  
J. R. SEEMANN ◽  
R. S. NOWAK

2009 ◽  
Vol 5 (3) ◽  
pp. 329-345 ◽  
Author(s):  
S. Bonelli ◽  
S. Charbit ◽  
M. Kageyama ◽  
M.-N. Woillez ◽  
G. Ramstein ◽  
...  

Abstract. A 2.5-dimensional climate model of intermediate complexity, CLIMBER-2, fully coupled with the GREMLINS 3-D thermo-mechanical ice sheet model is used to simulate the evolution of major Northern Hemisphere ice sheets during the last glacial-interglacial cycle and to investigate the ice sheets responses to both insolation and atmospheric CO2 concentration. This model reproduces the main phases of advance and retreat of Northern Hemisphere ice sheets during the last glacial cycle, although the amplitude of these variations is less pronounced than those based on sea level reconstructions. At the last glacial maximum, the simulated ice volume is 52.5×1015 m3 and the spatial distribution of both the American and Eurasian ice complexes is in reasonable agreement with observations, with the exception of the marine parts of these former ice sheets. A set of sensitivity studies has also been performed to assess the sensitivity of the Northern Hemisphere ice sheets to both insolation and atmospheric CO2. Our results suggest that the decrease of summer insolation is the main factor responsible for the early build up of the North American ice sheet around 120 kyr BP, in agreement with benthic foraminifera δ18O signals. In contrast, low insolation and low atmospheric CO2 concentration are both necessary to trigger a long-lasting glaciation over Eurasia.


Sign in / Sign up

Export Citation Format

Share Document