INSTITUT FÜR KUNST UND ARCHITEKTUR
ADP ANALOGUE DIGITAL PRODUCTION CMT CONSTRUCTION MATERIAL TECHNOLOGY
www.akbild.ac.at/ika
ESC ECOLOGY SUSTAINABILITY CULTURAL HERITAGE
INSTITUTE REVIEW FOR ART SUMMER AND 2020 ARCHITECTURE
ADP Wolfgang Tschapeller Damjan Minovski Charlotte Beaudon-Römer Lucas Fischötter Maximilian Gallo Jessie Gao Yingqi Christopher Gruber Armin Mayerhofer Jonathan Moser Dana Radzhibaeva Roxanne Seckauer Vincent Wörndl Reviewers and guests Hugo Dworzak Niels Jonkhans Jochen Käferhaus Hannes Mayer Daniela Mitterberger Niklavs Paegle Eva Sommeregger
Heat, Ice Cores, Manganese Nodules is a multi-part project consisting of three basic research projects, which are Earth, Global Climate History and Vienna, as well as ten individual subprojects, which are Wreck for Two by Charlotte Beaudon Römer, Livingscape by Lucas Fischötter, Halo by Maximilian Gallo, Algae by Jessie Yingqi Gao, 780nm Thermal Shadow by Christopher Gruber, Chemosynthesis Cave by Armin Mayerhofer, Wir bauen ein Haus, dann fällt der Strom aus… by Jonathan Moser, Cloud by Dana Radzhibaeva, Writing 2100 by Roxanne Seckauer, and Six Degrees of Freedom by Vincent Wörndl. Furthermore, the project consists of an analysis of an area, the oil port Lobau, and of the detailed exploration of rituals and routines in space and time, such as washing your hands, sleeping, eating and storing, as well as of the observation that the Earth has a diameter of some 84,314 kilometres, that it has existed for around 4.35 billion years, and that it could potentially continue to exist for 1.5 to 12 billion years more. As if it were a game to put HEAT in relation to ICE CORES, and to force the HEAT that melts everything into entropy with the cooling cold of the ICE. If it is a game, then it is not mine, but that of history. Racing against time, researchers began in the last century first to drive holes into the ice, then to dig them and gradually to drill them. 10 metres at first, then 60 metres, and at the turn of the last century even boreholes with a depth of more than 3,600 metres. To dig for what? TIME and the FUTURE is what they were digging for! Because depth at the same time also means years. In the case of the EPICA1 borehole that went 3,200 metres deep, it means 900,000 years – that cover the last eight Ice Age cycles, and with them the knowledge that a sudden increase in greenhouse gases means a sudden rise in temperatures, meaning in heat, and that the average temperature of the Earth could rise by about 4.5 degrees Celsius by the year 2100.2 That may not
seem like a lot, but it is, at least in geological terms, since such a temperature was last detected in the early Neogene, i.e. some 10 to 20 million years ago. This leap is so immense that the few thousand years of the history of building, long considered an eternity, could suddenly mutate into a ridiculously short, but potentially massively fatal3 phenomenon up for debate. Was the culture of building a mistake? Should we close architectural history at this point? Should we open a new one? Should our own skin be enough? Moreover, is it enough for our own skin to be enough? If it becomes a controllable breeding surface: “fig. 3.1 the body as a breeding surface of bacteria”; if it evaporates in a controlled way subject to our will: “fig. 4 main water evaporation areas – sweating: f. feet and toes; g. stomach and genitals; h. armpit l+r; i. head; j. hand l+r”; if it cultivates external organs, such as: “fig. 5 pocket water collection reservoir: k. connecting pipe+fabric system; l. water reservoir including bacteria cleaning system”; or if it is protected by semi-biological add-ons: “fig. 6 pocket heating element thermal circuit (warming or cooling): m. upper extremities; n. knee joints; o. foot including toes”; and is it enough if it protects subjective thoughts by means of: “fig. 7.1 counter surveillance top layer – thermal protection camouflaging the surface/behaviour/stealth wear”? 4 Is all that enough? And what if we lose this skin? “If we lose it, we are not able to live!” 5 Can ice cores and manganese tell us something about the space around us, then? Yes, they can! As natural archives, they are data carriers in addition to their material appearance. They seem to know everything, and seem to be a sort of radar, a mirror of the future. Via transfer functions, knowledge can be extracted from them; knowledge about everything, apparently, if only the transfer function is intelligent enough. Enormous space-time continuums can be extrapolated. The radius of action and possibility, but also the space of responsibility is radically expanded, “macro-comprehensive/microincisive”, as Buckminster Fuller put it. What, then, do the contributors to the project Heat, Ice Cores, Manganese Nodules call “macro-comprehensive”? They begin with a definition of the Earth: “However, what do we call Earth? Is it the planet bounded by its atmospheric layers, or is it all the space that humans occupy by various instruments, calculations and devices? If that is the case, then our Earth has many further boundaries, which are defined by the satellites orbiting in space around our planet. In total, humans have sent up 4,987 satellites, out of which 1,957 are currently active. All of them have a purpose – 85 are for space science and observation, 137 are for navigation, 223 for technology development, 735 are for Earth science and observation, and the remaining 777 are for communication services, and some of them are not listed due to special military operations. Additionally, the unused “dead” satellites are also orbiting around and creating a graveyard; in this case, we enter Earth through a network of dead and alive machines. About half of all satellites are in low Earth orbit, just a few hundred kilometres above the surface; a twentieth is in medium Earth orbit, around 20,000 km up, and the rest are in geostationary orbit, at an altitude
of 35,786 km. Considering the depth of the planet and the geostationary altitude, Earth, in this case, has a diameter of 84,314 km.” 6 Then what do they call “macro-comprehensive” in terms of time? What can we expect? How are we doing for time? “The beginning of Earth is defined by the formation of the Earth’s core with an error range of 50 million years. A time scale has to place year zero at the birth of Earth, which takes away the anthropocentric understanding, to measure anything and everything from the point in time we are at now […] that is, at around 4.543 billion years from the birth of Earth. The predicted death of Earth varies from 1.5 billion years to around 12 billion years from now, depending on unforeseeable developments like eruptions of volcanoes, collisions with massive asteroids, gradual convergence towards the sun, global warming, and so on. We have taken the most pessimistic approach and let Earth die in 1.5 billion years, but still leave open the opportunities […]. Then we have set up time and temperature on an axis and pieced together a multitude of graphs of temperature throughout the entire lifespan of Earth […]. The different natures of data sets pose a challenge: firstly, the data comes in different resolutions; secondly, most of the data does not refer to absolute temperatures but to deviations from the global baseline temperature; thirdly, data taken from paleoclimatological sources like fossils, ice cores or rocks do not come in temperature units but in concentrations of molecules and elements such as CO2. […] We have […] tried the best […] to translate them into one graph with the correct size in time and levels in temperature to a general overview of Earth’s climate history. And if we have applied the data correctly, in 2100 Vienna could reach a temperature mean value of approx. 28°C7 during summer while at the moment this value lies at around 24°C.” 8 And what do they think could be “micro-incisive”? “Wien Energie currently supplies 380,000 households with district heating. That is one third of all Viennese households. District heating therefore plays a central role in the energy system and is projected to become even more important. In the future, most of the district heating energy comes from waste incineration and cogeneration plants and systems. The development of renewable energy sources, such as biomass, green gas, geothermal, solar thermal, heat pumps, and waste heat from production plants is essential for the expansion of environmentally friendly district heating. The decarbonization potential for district heating is estimated at 100%, if fossil fuels were no longer used as sources of energy. This goal is set to be achieved by Vienna by 2050.” 9 What else could “micro-incisive” mean? “I looked around as usual and no one seems like they are awake yet, so I held on to the surface of the eating area and got myself up from the cleaning gel. I looked through the jelly down to my black sleeping cabin. As soon as I left,
HTC HISTORY THEORY CRITICISM GLC GEOGRAPHY LANDSCAPES CITIES
to save space, of course it shrank into a small piece, like a raisin. “Raisin”, the word popped up in my head, a form of dried grape with a lot of concentrated sugar, seems to be one of the nutrients we used to get from nature through eating, with lots of processing. Eating was very different back then […]. I walked down through my hallway to the position of eating. Like any day before, I stand there without much going through my brain, letting the pipes inside me naturally extend towards the gaps in the walls. Soon, fellow Chlorella will pass on to me some nutrition and oxygen. I am waiting for the substances to pass through my body and be transferred to something useful for Chlorella in return […]. I can feel that I’m slightly moving around, because the whole space is moving the space. “The flood is still there.” I remember the storm yesterday, now we are higher up in the air, lifted by the water. This happens quite often, and the water was simply refilled in every space. With the full sun and the remaining flood, it should be a happy day […]. 10 Wolfgang Tschapeller Design Studio BArch2, MArch
→ fig. 5 / p. 5 → fig. 14 / p. 8 → fig. 53-54 / p. 15 → fig. 58 / p. 17 1 European Project for Ice Coring in Antarctica 2 The year 2100, when according to RCP 8.5 an estimated increase of approx. 4.5°C average temperature measured against the average temperature of 1960-1990 is one of the likely scenarios (RCP 8.2). 3 IPCC WG1 Chapter 9 Buildings: “In 2010, the building sector accounted for […] 32% of global final energy consumption and 19% of energy-related CO2 emissions […]. This energy use and related emissions may double or potentially even triple by mid-century […].” https://www.ipcc.ch/site/assets/ uploads/2018/02/ipcc_wg3_ar5_chapter9.pdf [28/09/2020] 4 All quotes from: The Construction of Figures, in: 780nm Thermal shadows, Reports from another world, by Christopher Gruber (MArch4), p. 34 5 Last words, in: Writing 2100, by Roxanne Seckauer (BArch2) 6 Excerpt from: However, what do we call Earth then? by Christopher Gruber (MArch4), Jonathan Moser (MArch4), Dana Radzhibaeva (BArch2) 7 According to the ICPP AR5 RCP 8.5, which is the most pessimistic prediction. 8 Excerpt from: Global Climate History, a summary, by Charlotte Beaudon-Römer (BArch2), Lukas Fischötter (BArch2), Maximilian Gallo (BArch2), Jessie Gao Yingqi (visiting) 9 Excerpt from: Vienna, Hitze today and tomorrow, by Armin Mayerhofer (BArch2), Roxane Seckauer (BArch2), Vincent Xaver Wörndl (MArch4), quoting from: positionen.wienenergie.at; fernwärme.at; wienenergie.at 10 Excerpt from: Algae-Human Architecture, Narrative, by Jessie Gao Yingqi (visiting)
ADP Aristide Antonas Werner Skvara Olivia Ahn Pia Maria Bauer Christina Ehrmann Alexander Groiss Paula Hattenkerl Felix Knoll Diana Mudrak Maximilian Pertl
Anna-Elina Pieber Paul Schurich Ruben Stadler Sophia Stemshorn Marie Teufel Reviewers and guests Elina Axioti Gabu Heindl Nikolaus Hirsch Armin Linke Mona Mahall Heike Schuppelius
In this studio, an approach to the technical possibilities for cooling was put forward: the role of water, evaporation, shadow, wind, and the conversion of heat to energy were all investigated as options in several Viennese contexts. But then it became more important to refer to a changing social sphere. The characteristics of the social transformations to which more attention was channelled were recorded in a two-part process: it concerned the observation of the global transformation in regard to a generic social sphere, and a parallel investigation of a different local change of sociality in Vienna. In all these aspects, a remarkable effort was made to learn about different histories and global cultures of cooling. The technical investigation, far from being merely neutral research of contemporary techniques, delved into the cultures of cooling, as already practiced in Southern Europe, Africa and Asia. The studio first explored ideas of updating the city with existing methods of cooling, which could be transferred and influence the sociality of Vienna, together with some new population groups that inhabit the city and are more familiar with warm environments. We could call this city update a “Mediterranisation of Vienna”, a concept that was meant to work in two directions: First, priority should be given to simple and already known technologies originating from the Southern subaltern cultures, with existing solutions taking precedence over sophisticated, complicated and energy-consuming Northern solutions when it comes to issues of heat. Revisiting some aspects of the social sphere following the logic of various cooling principles, wherever they came from, was an important analytical part of the studio. On a second level, the studio explored ways in which this depressing investigation on climate change could be transformed into an experience that, in certain cases such as that of Vienna, could be combined with the social joys of good weather and a different social life to which it can give priority. The studio explored these questions in many different directions, concluding some of the appropriations of this exchange with a South that was already present in Vienna. Some examples of these strategies amounted to the use of imported ready-made technologies, to the idiosyncratic use of recorded structures of city life in the heat, and to understanding social heat as a further field of action, which was also interestingly juxtaposed with cooling as such. The global social sphere is able to capture city life through a number of protocols that could slowly become part of the urban infrastructure, considered as a set of freer social rules for post-network Vienna. Since the Web 2.0, the Internet has mainly functioned as a stabiliser of