Thermal Energy Reduction in Papermaking Industries

2010 ◽  
Vol 43 (7) ◽  
pp. 212-216 ◽  
Author(s):  
Martin Brown ◽  
Puya Afshar ◽  
Hong Wang ◽  
Timofei Breikin
2012 ◽  
Vol 89 (1) ◽  
pp. 74-80 ◽  
Author(s):  
Iqbal M. Mujtaba ◽  
Elmahboub A. Edreder ◽  
Mansour Emtir

2021 ◽  
Vol 14 (8) ◽  
Author(s):  
Carlos Cuviella‑Suárez ◽  
Antonio Colmenar‑Santos ◽  
David Borge‑Diez

Author(s):  
E. Grover-Silva ◽  
D. A. McKahn ◽  
D. Weisbord

We present a methodology to assess the technical feasibility of building thermal energy reduction strategies from an architecturally diverse building stock that is not metered. While carbon emissions forecasting efforts are typically the domain of planning and policy, the process detailed here can inform institutional decision-making relative to investments in renewable energy, infrastructure, and offsets to further reduce carbon footprint. As a case study, we estimated the Smith College campus building thermal energy losses, an analysis which informed our Sustainability and Climate Action Plan [1]. Due to building specific physical constraints and planned renovations, different thermal envelope improvement scenarios were then considered to estimate the heating energy reduction potential of these envelope improvements. The current total heating energy consumption from 79 of our campus buildings was found to be 57,000 MMBTU/yr. Across the three building categories with minimal existing insulation and poor sealing conditions, the nominal annual thermal energy loss per square foot ranged from 27,000–37,000 BTU/ft2. Should envelope improvements be made targeting a 5 year simple payback, this annual thermal energy loss would be reduced by 40% to 34,000 MMBTU/yr. More extensive and less cost effective envelope improvements suggest further energy reductions approaching 30,000 MMBTU/yr (between 13,000–23,000 BTU/ft2/yr depending upon the building type).


2011 ◽  
Vol 44 (1) ◽  
pp. 6957-6962
Author(s):  
Puya Afshar ◽  
Martin Brown ◽  
Hong Wang ◽  
Jan Maciejowski

Author(s):  
W.P. De Lange

The Greenhouse Effect acts to slow the escape of infrared radiation to space, and hence warms the atmosphere. The oceans derive almost all of their thermal energy from the sun, and none from infrared radiation in the atmosphere. The thermal energy stored by the oceans is transported globally and released after a range of different time periods. The release of thermal energy from the oceans modifies the behaviour of atmospheric circulation, and hence varies climate. Based on ocean behaviour, New Zealand can expect weather patterns similar to those from 1890-1922 and another Little Ice Age may develop this century.


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