Abstract

The vernacular architecture in many regions in Eastern Austria was characterized by the use of unfired clay, at least until the 19th century, and in some areas until the 20th century. Farmhouses and associated farm buildings, such as storage buildings or press houses for the production of wine and cider, were erected using different earth construction techniques. The study area stretches from the Weinviertel, a region located in the province of Lower Austria in the north-east of Austria, to the Burgenland, a region located in the south-east of Austria, which belonged to Western Hungary until 1921. From a geological point of view, in the east of Austria—in the Vienna Basin and the Molasse Zone—huge areas of Tertiary clay are covered with loess deposits, which is the best-known basic material used in local earth-building traditions. A core question in the research on vernacular earthen heritage focuses on the impact of the geological conditions in Eastern Austria on the local earth-building techniques. The mineralogical composition of the different clays had an impact on the local building techniques. From a material-culture point of view, research on the relationship between the mineralogical properties of clay resources and local building techniques sheds light on the factors which influenced the evolution of certain vernacular building features. Tertiary clays and loess from the Pleistocene favoured the making of earth lumps, cob walls and adobe bricks over the whole Eastern Austrian region. Contrarily, regions in Burgenland with a high amount of gravel preferred, by tradition, to make walls by ramming. The clay mineral smectite acts as a binding agent in earth-building techniques over the whole investigated region—Weinviertel, Burgenland and Western Hungary.

Highlights

  • The properties of the raw materials used for building purposes are crucial to understanding the technologies used in historical building structures

  • The study area stretches from the Weinviertel, a region located in the province of Lower Austria in the north-east of Austria, to the Burgenland, a region located in the south-east of Austria, which belonged to Western Hungary until 1921

  • From a geological point of view, in the east of Austria—in the Vienna Basin and the Molasse Zone—huge areas of Tertiary clay are covered with loess deposits, which is the best-known basic material used in local earth-building traditions

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Summary

Introduction

The properties of the raw materials used for building purposes are crucial to understanding the technologies used in historical building structures. The type and quantity of clay minerals affect the physical behaviour of clay as a building material, e.g., its abilities to transport and store humidity, or to swell and shrink [1,2]. One notable difference between clay and other commonly used solid natural building materials such as timber or stone is clay’s capacity to reversibly transform from a solid to a plastic consistency, and vice versa. Clay minerals can be mixed with organic fibrous materials such as straw or hemp, etc., in order to temper and reinforce it. Key publications on earth-building in Eastern Austria are collected here [3,4,5,6,7,8,9]

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