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Journal of Architectural Conservation The role of four key structures in the creation and survival of cultural landscapes in the desert environment of Iran Maryam Rafiee Fanooda a Faculté des Sciences Humaines et Sociales, Université Jean Monnet, Saint-Etienne, France Published online: 06 Dec 2014. To cite this article: Maryam Rafiee Fanood (2014) The role of four key structures in the creation and survival of cultural landscapes in the desert environment of Iran, Journal of Architectural Conservation, 20:3, 184-196 JournalofArchitecturalConservation,2014 Vol.20,No.3,184–196,http://dx.doi.org/10.1080/13556207.2014.985490 The role of four key structures in the creation and survival of cultural landscapes in the desert environment of Iran Maryam RafieeFanood* FacultédesSciencesHumainesetSociales,UniversitéJeanMonnet,Saint-Etienne,France Cultural landscapes in the desert environment of Iran were created according to specific climatic conditions and differ from those in other climates. Scarcity of water resources in these regions has led to the invention and application of unique measures for the supply, maintenance and use of water. The qanat, cistern, ice-house and wind catcher are ingenious measures that have had key roles in the settlement of man in desert regions of Iran and ideallyaddressedthespecificneedsofeachcommunityovercenturies.Thisstudyillustrates the significance and relationship of these elements in the creation and survival of cultural landscapes in the desert environment of Iran. To this end, their features are discussed and analyze separately and as ensembles which in turn presents a sustainable way of living in desertregions. Keywords:culturallandscape;desertenvironment;qanat;cistern;ice-house;windcatcher Introduction Culturallandscapesrepresentthecombinedworksofnatureandofman.Theyareillustrativeof theevolutionofhumansocietyandsettlementovertime,undertheinfluenceofthephysicalcon- straints and/or opportunities presented by their natural environment and of successive social, economic and cultural forces, both external and internal.1 With this UNESCO definition in mind,inthecentralplateauofIranwheredesertispredominant,thereisahugewealthofcultural landscapes. The scale, dimensions and forms of cultural landscapes vary immensely, and may range from quite small, contained landscapes (such as a small saffron farm in South Khorasan Province)tovast,extensiveareas(suchasthehistoriccityofYazd).Smallerculturallandscapes may themselves form part of more extensive cultural landscape areas. However, these rich and varied landscapes seem to be in permanent or potential danger that might cause irreversible deterioration or even disappearance if urgent measures are not taken by the decision-making sectors. They are being threatened by uncontrolled urban and rural development, insufficient knowledgeofinhabitantsandstakeholdersaboutmanagementtechniquesandlackofawareness oftheirsignificanceaspartofasustainablewayoflivingformanycommunitiesandasanattrac- tion for culture, tourism andscience. Themeaningandsignificanceofculturallandscapesislargelyderivedfromtherelationship betweenthelandscapeandtheelementswithinthatlandscape,aswellastherelationshipbetween theindividual elements themselves. Thus landscape meaning and significance canbe lost when important components of a cultural landscape are removed or evidence relating the feature to *Email:Maryrafi[email protected] ©2014Taylor&Francis Journal of Architectural Conservation 185 thelandscapesettingvanishes.2Thispaperexplorestheroleofsomeofthesekeyelementsinthe creation and survival of cultural landscapes in the desert environment of Iran through history. Although each cultural landscape encompasses a great variety of elements and components that differ one from another, this study particularly focuses on four common structures which have been used for the supply, maintenance and use of water in the arid environment of Iran. The most important and the most basic key structure is the qanat, a sustainable water supply system,which,inconjunctionwithotherstructuressuchascisterns,ice-housesandwindcatchers, has provided comfortable living conditions for desert environment inhabitants. Climate conditions of thedesert environmentof Iran AdesertenvironmentcoversthecentralandeasternpartsofIran.Overall,itsclimaticconditionis characterised by: . Limited waterresources; . Warm anddry summers, cold and hard winters; . Lowrainfall; . Lowhumidity; . Scant vegetation; . Largevariation between day andnight temperatures; and . Dusty winds and sandstorms.3 InthecaseofYazdcity,oneofthedriestcitiesinthecenterof Iran,theaverageannualrainfallis 60mm.Thesummertemperaturesareveryfrequentlyabove40°C,withblazingsunshineandno humidity;evenatnightthetemperaturesareratheruncomfortable.Inthewinter,thedaysremain mildandsunny,butthenightshaveverycoldtemperaturesthatcanfallbelow0°C.Theseasonal temperaturesvarywidely;rangingbetween+45°Cinsummerto−20°Cinwinter,furthermorethe temperature difference between the daytime and night-time is also high and can range from an average of 11.9°C to 20.7°C.4 Several features of the traditional structures are designed to take advantage of thiswide temperature range in desert regions. Four key structuresof cultural landscapes in the desert environment Qanat Water is not only vital for human existence, but also of substantial importance in any food production process as well as essential for environmental sustainability. Three thousand years ago, Iranian people, with their knowledge of underground water resources, understand- ingofgravityanduseofaseeminglysimpletechniqueofdiggingwellsandtunnels,wereable to overcome the water shortage in arid and semi-arid regions.5 They developed indigenous methods for harvesting and Extracting their scarce groundwater in a sustainable manner in an area where there have been no other water resources. This technique, which is called qanat, has maintained its significance and function in the survival of many communities in the country until the present. Themaingoalsofconstructingqanatshavebeentoprovidehygienicdrinkingwaterandirri- gation for agriculture; however, there have been secondary purposes, which allowed the popu- lation to live comfortably in a desert environment. To fulfill these purposes the qanat has operated in conjunction with other structures such as cisterns for water storage, ice-houses for ice storage, wind catchers for air conditioning,andwatermills forgrindinggrains.6 186 M.R. Fanood Qanatsexpressalongandintimaterelationshipbetweenpeopleandtheirnaturalenvironment, andwithoutthemthousandsofvillagesandtownswouldnothavecomeintoexistence.Bamand its cultural landscape, which was placed on the World Heritage List in 2004, is an outstanding example of the interaction of man and nature in a desert environment by using the qanats; the existence of life in the oasis was based on these underground irrigation canals.7 The irrigation system of the majority of the Persian Gardens, placed on the World Heritage List in 2011, has alsobeen based on the qanat system. Qanats have been maintained in all, except Bagh-e Eram, Bagh-e ChehelSotun and Bagh-e Dolat Abad, where urban development has forced the closure of qanat sources and replaced them with wells.8 However, it is evident that most of these unique gardens would not have been created and survived over centuries without qanats, as there have been noother water resources for irrigation in those regions. Qanats are generally constructed on the slopes of piedmont alluvial fans, in intermontane basins, and along alluvial valleys. In these locations, this groundwater collection system has longbroughtwatertothesurfaceandsupportedsettlementinregionswherenoothertraditional watertechnologywouldwork.9Qanatsconsistofseriesofwell-likeshaftsconnectedbyagently slopingtunnel. The main components of the qanatas presented in Figure 1 are: . Mazhar or aquifer where the water flows above the ground ator nearsettlement site; . Gallery,whichisanalmosthorizontaltunneldugtogetaccesstothegroundwaterreserve andto transfer it to the earth surface; . Wetsection,whichisinfact anundergrounddrain intowhichgroundwaterseeps.Thisis the water producingsection of the qanat; and . Drysection,whichisthedown-slopesection,merelyactingasthetransportationsectionof the qanat; Figure1. Cross-sectionandmainfeaturesofatypicalqanat. Journal of Architectural Conservation 187 . Shafts,whicharewellssituatedalongthegalleryinordertofacilitatesoilextractionaswell as ventilation anddredging;and . Mother well,which marks the furthest extent of the qanat from the aquifer.10 Cultivated land and settlement sites are situated downwards from thepoint where the water surfaces.Theimmediateoutlet,mazhar,isthepointwherepeopletakewateranditisgenerally locatedinthemainsquareofavillage.TheMazharisanimportantfeature,whichiswellmain- tainedandmortaredtopreventwaterpenetrationintothesoil.11Downstreamofthemazhar,water runs through open or covered ditches with lateral branches to the neighbourhood, gardens and fields. Cisterns, ice-houses, Hammams or public baths, mosques and watermills were built along the route of the water canals in the most suitable locations.12 Payabs, which are sloping corridors with steps leading from the surface to the qanat’s canal beneath residential areas, were also built along the line of the qanat for taking drinking water directly from the qanat.13 After these communal needs have been met, the water is collected from ditches in special pools and then distributed to the farms. Whatisremarkableabouttheqanatisitstraditionalwatermanagementanddivisionsystem, which has provided maximum efficiency, fair distribution and suitable maintenance of water in arid regions of Iran. Water distribution for irrigation is done proportionately according to the land shares of farmers so that each one receives his just share of the water at the proper time.14 Different methods have been used for measuring the water share, which vary from area to area according to the local conditions and the volume of the water available. The most commonmeasureinthedesertregionsofIranhasbeenbasedontime,whichledtotheinvention of aspecial water clockto calculate the lengthof irrigation for each farm.15 QanatshavebeeninwideuseassustainablewatersuppliesthroughoutthearidlandsofIran until today for several reasons: they are made of local materials and are resistant to natural disasters and deliberate destruction in war; they use no source of power other than gravity; and water is transported for substantial distances with minimal loss through evaporation and with littlerisk of pollution.16 Cistern Thecistern,orĀbanbār,isatraditionalreservoirfordrinkingwaterthatwasusuallybuiltatthe centreofthecityorvillage,oncaravanroutesandinsideprivatedwellings.Thecisternwasoneof the constructions developed in arid regions of Iran as part of a water management system to ensuretheavailabilityofdrinkingwaterthroughoutthehot,dryseasonswheneventhepermanent water supply,the qanat, would diminish. TheearliestcisternsarebelievedtohavebeenconstructedalongsidetheriseofearlyPersian civilizations.ThewaterreservoirofTchoghaZanbil,anElamitecityintheKhuzestanprovince, stillsurvivesfromthesecondmillenniumBC.Therearealsoremnantsofcisternsandwaterways atPersepolis,thecapitaloftheAchaemenidEmpirefromthesixthcenturyBC.17However,most extantcisternscantodaybetracedtothelateSafavidandQajardynasties(eighteenthtotwentieth centuries). Theprimeobjectiveinconstructingacisternwastoprovideatotallywaterproofcontainerfor alargevolumeofwaterwhileallowingproperventilationandaccess.Thetypicalcisterngener- ally consists of three key elements: the water reservoir, which was built undergroundlevel to enablepropercooling,resistancetowaterpressureandimpactsofearthquakes;thepassageway to a platform where a faucet is used to take water; and the wind catcher, which is used for ventilation (Figure 2).18 Two types of structures have been noted: first, a cylindrical reservoir 188 M.R. Fanood Figure2. Cross-sectionofapubliccistern. with a dome, which was generally built for public cisterns in towns or along caravan routes (Figure 3). Their capacity generally varies from 300 to 3000 cu m depending on their depth and diameter. Second, a rectangular reservoir with flat roof supported by piers or pillars, which was often built into the foundation of private houses for domestic use and ventilation. Each of thesestructureswasmarkedbyaportalthatopenedintoastaircasedescendingtoavaultedpas- sageway,leading downto the reservoir.19 Cisternsweremadefromspecialbricksandwaterproofmortarcalledsārūj,whichisthought toberesistanttowaterpenetration.Waterwasmainlybroughttothecisternbyspecialchannels leading from the main qanat or, alternatively, where no qanats were available the water was collectedfromsporadictorrentialrainfallintheariddesertareaoftheIranianplateau.Thecisterns werefilledduringthewinterwithcoldwateratatemperaturejustabovefreezingtokeepthewater cool throughout the year.20 Water remained quite cool inside the cistern, since it was generally Figure3. ApubliccisterninArdestan,IsfahanProvince,2012. Journal of Architectural Conservation 189 built beneath ground level and was insulated with very thick walls.21 Domed roofs, which are used to cover cisterns, have a good thermal performance. Some of them had an escape vent in the centre, which enabled them to cool water by air convection while protecting it from dust andotherpollution(Figure4a).Somecisterns,mostparticularlyinYazdprovince,wereequipped withoneormorewindcatchers.Thepressuredifferencebetweentheairenteringfromthewind towersandtheairleavingfromthetopofthedomecausedanaturalairflowoverthewatersurface (Figure4b).Thisprocess,whichisdescribedinthefollowingsection,resultedintheevaporation and subsequent cooling of water.22 Wind catcher Thewindcatcher,orBādgir,isatraditionalventilatingdevicethathasprovidednaturalaircon- ditioninginthebuildingsofhotandaridregionsofIranforcenturies.Themostcommonuseof windcatchersistocoolandventilatetwointeriorspacesatdifferentlevels:thebasementandthe summerlivingroomonthegroundfloor.Theywerealsobuiltontothelivingquartersofcaravan- serais, over prayer halls of mosques, and above the cisterns as mentioned above. Awindcatchergenerallyconsistsofawindtower,whichisachimney-likestructurewithone endinthebasementofthebuildingandtheotherendpositioningabovetheroof.Thewindtower isdividedintoverticalairpassageswithventsatthetopinoneormoresidesofthetower’sheadto catchtheprevailingwind(Figure5).23 Airtrappedintheventsofthetoweriscooledasitfirst passesoverawaterreservoirorsmallpondinthebasement;alternatively,orinaddition,insome places mats were often placed across the vents over which water might be thrown on summer afternoons.24 The qanat’s canal, which passes beneath the basement, has also been used to increase the humidity and the coolness of the airflow. The flow of the incoming air from the wind catcher is directed across the vertical shaft opening of the qanat to the basement that creates a lower pressure and draws cool air up from the qanat tunnel (Figure 6). In dry desert climates this can result in agreater than 15°C reduction in the air temperature coming from the qanat.25Somewindcatchers,asshowninFigure7,werebuiltawayfromthebuildingandcon- nectedtoitwithanundergroundductthatcouldserveseveralbuildings.Thehotaircooledeither by contact with the duct’swall thatwas damp dueto thewatering ofthegarden above it,or by passingoverapondinsidethebuilding.26Asaresult,thiscoolhumidairisabletocooltheother spacesinthebuilding byconvectionandevaporation.Theflowofairthroughdifferentpartsof buildingcan becontrolled by opening and closing the tower and building doors. Figure 4. Air circulation in a cistern (a) with vents on a domed roof; (b) with wind catchers (Bahadori 1978). 190 M.R. Fanood Figure5. ThewindtowerofGanjali-Khanbazaar,Kerman,2008. Awindtoweroperatesinvariouswaysduringdayandnightaccordingtofluctuationsinthe air temperature, the intensity of solar radiation, the wind velocity and other climatic variables. When there is little or no wind, the wind catcher operates according to temperature differences between day and night. The wind tower operates like a chimney when there is no wind at night. Heat that has been stored in walls during the day warms the cool night air in the tower. Thiscausesalowerpressureatthetopofthetower,whichdrawsupthewarmairinthebuilding. Coolnightairispulledintothebuildingthroughtheopendoorsandwindows.Whenthereisno wind during the day, the operation of the tower is the reverse of a chimney. Hot ambient air is cooledwhenitcomesintocontactwiththetowers’walls,whichhavebeencooledduringthepre- viousnight.Thecooleddenserairsinksdownthroughthetowerandcirculatesinthebuilding.27 Windcatchersindesertregionsarebuilteitherofmudbrickormorecommonlyofbakedbrick coveredwithmudplaster.Thesematerialsexhibitgoodresistanceagainstheattransmissionqual- ities, ensuring that the wind catcher operates effectively as a cooling system.28 To fulfill this purpose the orientation and height of the wind tower are also important. They may have vents at the top in one, two, or up to eight sides depending on the direction of the desired airflow at that specific location. In hot and dry regions, due to the low temperature and a higher wind velocity at greater heights, wind towers are built at high levels to enable them to trap such cur- rents. The highest wind tower in Iran built at Bagh-e Dolat Abad in Yazd city has vents in eight sides and rises about 34m abovethe roof of the garden pavilion itserves.29 Ice-house Ice-houses,orYakhchāls,arestructuresusedtoproduce,storeandpreserveicethroughoutthehot, aridregionsofIran.Icewasproducedinthecoldestperiodsofwinterandpeoplewouldusethe preservediceduringthelongandwarmsummers.Mostoftheice-houseswereapublicutilityand everyone could use the ice for conserving food, cooling drinks, and preparing ice-cream and Journal of Architectural Conservation 191 Figure6. Coolingsystemofawindcatcheralongwithaqanat(Bahadori1978). sorbetdesserts.30Althoughseveralhistoricalice-housesremain,nonecanbedatedtobeforethe Safavid dynasty (1501–1722). However, historical sources attest to the extensive use of ice for conservingfoodandcoolingdrinks,indicatingthatitwasalongestablishedpracticeinPersia.31 A typical ice-house consists of three main components: an ice-making pool, a great shade wall, and an ice reservoir (Figure 8a). The ice-making pools were long, rectangular, shallow pits, 100by10m with a depth of about 40to50cm, linedwith baked bricks that rendered them waterproof.Alongthesouthsideofthepoolwasatalltaperingwall,upto10mhighandstretch- ingfromeasttowestinordertoprovideshadefromthesunduringtheday,andthusaccelerating thefreezingprocessatnight.Thewallfurtherprotectedthepitsfromwind,whichcanalsohinder thefreezing process.32 Although snowfrom nearbymountains wasoccasionallystoredin ice-houses,mostice was madebyfreezingwaterinnearbyshallowpitsthatwerefilledwithwaterfromtheqanats.33The procedure is based on the high discrepancy of temperature between day and night in both summer and winter. Water froze in the pool when the temperature dropped to freezing during winternights.Inthemorning,beforesunrise,theicewasbrokenandstackedintheicereservoir where it was insulated with straw or saw dust andkept dry.34 Icereservoirsindesertregionsweremadebyconstructingabigadobedomeabovealargepit to the south of the shade wall. The dimensions of the ice reservoir were different. One of the biggest examples of an ice-house is in Meybod city, Yazd province, with a pit depth of 6m and a dome height of 13m (Figure 8b). The depth of the pit under the ground stabilises the

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and to transfer it to the earth surface; at Persepolis, the capital of the Achaemenid Empire from the sixth century BC.17 However, most used to cover cisterns, have a good thermal performance. Some of air temperature, the intensity of solar radiation, the wind velocity and other climatic variabl
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