Passive Heating & Cooling Design for the 21St Century
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Passive Heating & Cooling Design for the 21st Century Passive solar heating, shading, evaporative cooling, natural ventilation, and effective use of thermal mass offer durable, climate-responsive, socially-in- clusive pathways to thermal comfort and thermal architectural delight. Pas- sive heating and cooling guidelines have changed little in decades, however, despite new insights into solar radiation transmission, fluid mechanics, ma- terials science, and climate modeling, as well as more powerful and efficient field instruments and vastly improved computational tools. With energy con- sumption an inescapable reality of architectural practice, and with passive strategies offering the lowest embodied-energy solutions, educators and researchers must bring passive heating and cooling design into sync with current energy science. This is the goal of my work. 1 Sunspaces in a Land of Fog and Moss . 2 2 Oregon Sunspace Redesign / Build . 6 3 Thermal Batteries for Buildings . 8 4 Hybrid Ventilation in a Chicago Academic Center . 12 5 Passive Cooling in Everett Community College Offices. 14 6 Night Cooling of Mass in the Vernonia K-12 School . 16 7 3-D Thermal Bridging in Wall Assemblies . 16 8 Natural Ventilation in the Lillis Business Complex . 17 9 Teaching: Passive Heating and Cooling Design . 18 10 Relevant Funding Programs . 20 Contents Pyranometer deployed in a sunspace Alexandra Rempel, Ph.D., M.Arch., 2013 Fig 7 Figure 7. 95 35 a) Gates Measured 90 Modeled 85 30 80 25 75 70 20 Figure 3. Figure 3. Figure 4. Figure 4. 65 60 15 Temperature (ºC) Temperature Temperature (ºF) (ºF) Temperature 55 50 10 45 Figure 4. Figure 4. Figure 4. Figure 4. Fig 7 a) Gatesa) Gates a) Gates a) Gates a) Gatesa) Gates a) Gates a) Gates a) Gates 40 5 Figure 2. 4.11 4.12 4.13 4.14 4.15 4.16 4.17 4.18 4.19 4.20 4.21 Sunspaces in a 0-6a 100-6a 1210 8 12 11 8 11 11 10 11 10 0-6a 100-6a574666 120-6a1017 8574666 120-6a 11 1117 8 16 11 11 11 15 10 16 11 14 15 10 0-6a 14 171069980-6a574666 1117 16106998574666 11 15 16 14 15 14 95hours,106998 confirming106998 that the mass was active in solar per- 35 6a-noon 106a-noon 1210 8 12 11 8 10 11 9 10 9 6a-noon 106a-noon575655 1210 8575655 12 11 8 10 11 9 10 9 575655575655 6a-noon 166a-noon 1016 14 10 12 14 10 126a-noon 10 166a-noon96876 1016 1496876 10 12 14 10 12 10 90formance96876b) Shaw but96876 also, as shown below, losing substantial noon-6p 11noon-6p 1411 12 14 17 12 13 17 13 13 13noon-6p 11noon-6pnoon-6p687977 141117 12noon-6p687977 14 10 1717 12 19 13 10 17 16 13 19 13 12 16 13noon-6p 12 17noon-6p961097687977 1017 19961097687977 10 16 19 12 16 12 961097961097 Land of Fog and Moss 85heat to underlying soil. 30 6p-mid 116p-mid 1211 9 12 13 9 11 13 10 11 10 6p-mid 116p-mid6757656p-mid 121117 96757656p-mid 12 12 1317 9 17 11 12 13 15 10 17 11 12 15 10 6p-mid 12 176p-mid10675765 1217 7 1710675765 1210 15 7 17 8 12 10 15 7 8 12 7 10 710 10 7 8 10 7 8 7 80 b) Shaw b) Shaw b) Shaw b) Shaw Interpretation of passive solar field data with EnergyPlus b) Shaw b) Shaw b) Shaw b) Shaw 25 75 models: Un-conventional wisdom from four sunspaces in 0-6a 6748880-6a 6748880-6a 6748880-6a4424450-6a674888144424450-6a 914 15 9 13 15 13 130-6a 13 140-6a85877442445 914 1585877442445 9 13 15 13 13 13 Models85877 (below)85877 showed close correspondence to mea- 6a-noon 8989986a-noon 8989986a-noon 8989986a-noon45555489899813455554 913 12 9 9 12 8 9 8 1375654455554 913 1275654455554 9 9 12 8 9 8 70 7565475654 Eugene, Oregon. Building and Environment 2013, 60:158-172. 6a-noon 6a-noon 6a-noon 6a-noon sured air temperatures, mass surface temperatures, and 20 noon-6p 13noon-6p 1313 14 13 19 14 14 19 13 14 13noon-6p 13noon-6pnoon-6p7781087 131312 14noon-6p7781087 13 9 1912 14 15 14 9 19 10 13 15 14 8 10 13noon-6p 8 12noon-6p758647781087 912 15758647781087 9 10 15 8 10 8 65heat75864 fluxes,75864 predicting 80-95% of the variability in the 6p-mid 786111096p-mid 786111096p-mid 786111096p-mid4436556p-mid78611109144436556p-mid 1014 15 10 12 15 11 126p-mid 11 146p-mid86876443655 1014 1586876443655 10 12 15 11 12 11 60 8687686876 data and allowing them to be used to gain further in- 15 c) Page c) Page c) Page c) Pagec) Page c) Page c) Page c) Page (ºC) Temperature Temperature (ºF) Temperature 55 What would it take for passive solar heating to (°C) Temperature 0-6a 80-6a 158 11 15 13 11 12 13 11 12 11 0-6a 80-6a486776 150-6a815 11486776 150-6a 12 1315 11 15 12 12 13 13 11 15 12 15 13 11 0-6a 15 150-6a97878486776 1215 1597878486776 12 13 15 15 13 15 sight97878 into heat97878 gain and loss pathways. Please see publi- perform well in the cloudy, rainy winters of Eugene, 50 10 6a-noon 76a-noon 147 12 14 11 12 7 11 6 7 6 6a-noon 76a-noon6a-noon487643 14714 126a-noon487643 14 10 1114 12 11 7 10 11 7 6 11 7 7 7 6 6a-noon 7 146a-noon86644487643 1014 1186644487643 10 7 11 7 7 7 cation86644 for further86644 details. Oregon? With a West Coast Marine climate (Köp- a)b) Shaw 45 noon-6p 8noon-6p 148 14 14 11 14 7 11 9 7 9 noon-6p 8noon-6pnoon-6p488645 14813 14noon-6p488645 14 10 1113 14 12 7 10 11 5 9 12 7 9 5 9 noon-6p 9 13noon-6p76735488645 1013 1276735488645 10 5 12 9 5 9 Fig 7 7673576735 40 5 pen Cfb) and high latitude, the Pacific Northwest’s 6p-mid 96p-mid 159 12 15 14 12 11 14 10 11 10 6p-mid 96p-mid5878666p-mid 15915 125878666p-mid 15 11 1415 12 15 11 11 14 10 10 15 11 12 10 10 6p-mid 12 156p-mid86857587866 1115 1586857587866 11 10 15 12 10 12Fig 7 8685786857 4.11Agreement 4.12 4.13between 4.14 Measured 4.15 4. and16 Modeled 4.17 4.18 Air Temperatures 4.19 4.20 4.21 overcast skies disguise a solar resource unexpect- d) Cashmand) Cashman d) Cashmand) Cashmand) Cashmand) Cashman d) Cashmand) Cashman 95 35 c) Page 0-6a 9977750-6a 9977750-6a 9977750-6a5544430-6a9977751178785544430-6a 117878Figure0-6a 7. 1178780-6a64444554443117878644445544439590 6444464444 35 edly well-matched to its mild winters and long, cool a) Gates Measured 6a-noon 8878546a-noon 8878546a-noon 8878546a-noon6a-noon4544328878541076316a-noon4544321076316a-noon 1076316a-noon64321454432107631643214544329085 6432164321 30 springs. Yet passive solar heating is rarely practiced (°F) Temperature Modeled noon-6p 81081075noon-6p 81081075noon-6p 81081075noon-6pnoon-6p56554381081075107741noon-6p565543107741noon-6p 107741noon-6p54420565543107741544205655435442054420 30 here, despite widespread enthusiasm for low-energy 8580 6p-mid 91088756p-mid 91088756p-mid 91088756p-mid5654436p-mid91088751288765654436p-mid 1288766p-mid 1288766p-mid64443565443128876644435654436444364443 25 8075 building design. e) Outsidee) Outside e) Outsidee) Outsidee) Outsidee) Outside e) Outsidee) Outside 25 7570 0-6a 380-6a 3538 42 35 41 42 45 41 52 45 52 0-6a 380-6a3265711 350-6a3835 423265711 350-6a 42 4135 42 41 45 42 41 45 52 41 45 52 45 52 0-6a 52 350-6a2657113265711 4235 412657113265711 42 45 41 52 45 52 265711265711 20 7065 6a-noon 406a-noon 3940 46 39 48 46 52 48 60 52 606a-noon 406a-noon6a-noon44891116 394039 466a-noon44891116 39 46 4839 46 48 52 46 48 52 60 48 52 60 52 606a-noon 60 396a-noon444891116 4639 8 48444891116 46 9 52 8 4811 60 9 5216 11 60 16 4 84 9 8 11 9 16 11 16 20 Field work. To investigate Eugene’s passive solar po- 65 47 4447 49 44 53 49 58 53 67 58 67 478 4447 744 498 44 9 49 53 74449 12 53 58 9 4953 14 58 67 12 5358 19 67 14 58 67 19 67 4478 4944 9 7 5378 4912 9 58 9 7 5314 12 67 12 9 5819 14 14 12 67 19 19 1460 7 19 97 12 9 14 12 19 14 19 tential, four sunspaces were instrumented January noon-6p noon-6p noon-6p noon-6pnoon-6p noon-6p noon-6p noon-6p 15 60 (ºC) Temperature 6p-mid 416p-mid 3841 44 38 45 44 49 45 56 49 56 6p-mid 416p-mid53779136p-mid 384138 4453779136p-mid 38 44 4538 44 45 49 44 45 49 56 45 49 56 49 56 6p-mid 56 386p-mid3779135377913 4438 453779135377913 44 49 45 56 49 56 (ºF) Temperature 55 377913377913 15 c) Page (ºC) Temperature through June 2011, measuring indoor and outdoor air Jan FebJan Mar Feb Apr Mar May Apr Jun May Jun Jan FebJanFeb Mar Feb Mar AprFeb Mar Apr May Mar Apr May Jun Apr May Jun May Jun Jun Feb MarFeb Apr Mar May Apr Jun May Jun (ºF) Temperature 55 50 10 temperature, humidity, mass surface temperatures, F) 50 ° 45 10 Air Temperatures (°F and °C) Mass Temperatures Fig 7 surface heat flux, mean radiant temperatures, and in- 45 Fig 740 5 40 4.11 4.12 4.13 4.14 4.15 4.16 4.17 4.18 4.19 4.20 4.215 cident solar radiation.