2017
DOI: 10.1007/978-3-658-16074-6
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Lehrbuch der Bauphysik

Abstract: Die Deutsche Nationalbibliothek verzeichnet diese Publikation in der Deutschen Nationalbibliografie; detaillierte bibliografische Daten sind im Internet über http://dnb.d-nb.de abrufbar.

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Cited by 8 publications
(5 citation statements)
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“…As for the treatment NC-27CP, a consolidant with explicitly hydrophobic components, its lasting water repellence could be proved by the low WAC values even after 6 months of curing. The WAC values can be classified as water repellent and water hindering [83] (p. 215). The slight differences in the 6 months WAC of this product between both lithotypes is also confirmed by the contact angles of water—96.78° for Schlaitdorf Sandstone and 87.26° for St. Margarethen Limestone .…”
Section: Resultsmentioning
confidence: 99%
“…As for the treatment NC-27CP, a consolidant with explicitly hydrophobic components, its lasting water repellence could be proved by the low WAC values even after 6 months of curing. The WAC values can be classified as water repellent and water hindering [83] (p. 215). The slight differences in the 6 months WAC of this product between both lithotypes is also confirmed by the contact angles of water—96.78° for Schlaitdorf Sandstone and 87.26° for St. Margarethen Limestone .…”
Section: Resultsmentioning
confidence: 99%
“…One possible explanation for the extreme temperatures is the absence of latent heat fluxes and the poor thermal conductivity of the medium, so that the absorbed radiation was largely converted into heat. Such effects occur, for example, in the insulation of houses, which, due to their poor thermal conductivity, reduce the heating of the building behind them, but reach high temperatures at the radiation conversion surface [38]. Thus, a plant seed located close to the moss surface (more mobile species may retreat to cooler microhabitats) is temporarily exposed to extremely high temperatures, which could adversely affect germination.…”
Section: The Interplay Of Direct Sunlight Canopy Cover and Ground Vegetationmentioning
confidence: 99%
“…An often-described characteristic is the moderating effect of extremes, mainly temperature, wind and moisture, through forests [21,36,37]. An important driver for the temperature of the near-surface is the amount of incoming solar radiation, i.e., diffuse and beam radiation, and absorptivity of the irradiated medium, which converts the absorbed energy into latent heat fluxes (evaporation) or sensible heatfluxes (heating) [21,38,39]. Each layer of vegetation, from the tree canopy to young trees, shrubs, and herbaceous vegetation, represents an insulating layer that affects incoming radiation through processes of reflection, absorption or transmission [5,6].…”
Section: Introductionmentioning
confidence: 99%
“…According to the description of the profile in WUFI Plus, data for heat emission per person was based on VDI 2078:1996 (DIN 1946-2) [36], and data for other heat sources was based on DIN V 4108-6 [37] and acquired from Nipkow et al [38]. Furthermore, data for the moisture production was according to Kunze [39] and Lutz et al [40]. Finally, data for the CO 2 production was acquired from VDI 4300-7 [41].…”
Section: Simulationsmentioning
confidence: 99%