@misc{ChabbiRumpelGrootesetal., author = {Chabbi, Abad and Rumpel, C. and Grootes, Pieter M. and Gonzales-Perez, J. A. and Delaune, R. D. and Gonzales-Vila, F. and Nixdorf, Brigitte and H{\"u}ttl, Reinhard F.}, title = {Lignite degradation and mineralization in lignite-containing mine sediment as revealed by 14C activity measurements and molecular analysis}, series = {Organic Geochemistry}, volume = {37}, journal = {Organic Geochemistry}, number = {8}, issn = {0146-6380}, doi = {10.1016/j.orggeochem.2006.02.002}, pages = {957 -- 976}, language = {en} } @techreport{BrandtBensHuettl, author = {Brandt, B. F. and Bens, Oliver and H{\"u}ttl, Reinhard F.}, title = {Alternative Landnutzung auf Rekultivierungsstandorten ohne Oberbodenauftrag}, publisher = {Helmstedt}, abstract = {"Studie im Auftrag der BraunschweigischenKohlen-Bergwerke AG", 103}, language = {de} } @incollection{GruenewaldKlemHuettl, author = {Gr{\"u}newald, Uwe and Klem, Doris and H{\"u}ttl, Reinhard F.}, title = {Zusammenschau "Wasser- und Stoffdynamik in Kippenkomplexen"}, publisher = {Berlin ; New York : de Gruyter}, isbn = {3-11-016308-X}, language = {de} } @misc{SchaafGerwinGruenewaldetal., author = {Schaaf, Wolfgang and Gerwin, Werner and Gr{\"u}newald, Uwe and H{\"u}ttl, Reinhard F. and K{\"o}gel-Knabner, Ingrid and Munch, Jean Charles}, title = {Patterns and processes of initial ecosystem development in an artificial catchment}, language = {en} } @inproceedings{SchaafGerwinVesteetal., author = {Schaaf, Wolfgang and Gerwin, Werner and Veste, Maik and Biemelt, Detlef and H{\"u}ttl, Reinhard F.}, title = {Monitoring program at the artificial catchment "chicken creek", Germany}, language = {en} } @misc{FischerBergmannHuettl, author = {Fischer, Thomas and Bergmann, Charlotte and H{\"u}ttl, Reinhard F.}, title = {Soil carbon and nitrogen budget in Scots pine (Pinus sylvestris L) stands along an air pollution gradient in Eastern Germany}, language = {en} } @misc{BergmannFischerHuettl, author = {Bergmann, Charlotte and Fischer, Thomas and H{\"u}ttl, Reinhard F.}, title = {Significance of litter- and humus-layer quality for rates and forms of N cycling in moder- to rawhumus-moder profiles under Scots pine (Pinus sylvestris L.)}, language = {en} } @misc{SproeteFischerVesteetal., author = {Spr{\"o}te, Roland and Fischer, Thomas and Veste, Maik and Raab, Thomas and Wiehe, Wolfgang and Lange, Philipp and Bens, Oliver and H{\"u}ttl, Reinhard F.}, title = {Biological topsoil crusts at early successional stages on recultivated post-mining sites in Brandenburg, NE Germany}, language = {en} } @misc{SchaafBiemeltHuettl, author = {Schaaf, Wolfgang and Biemelt, Detlef and H{\"u}ttl, Reinhard F.}, title = {Initial development of the artificial catchment 'Chicken Creek' - monitoring and survey 2005-2008}, publisher = {Cottbus : Research Center Landscape Development and Mining Landscapes (FZLB)}, issn = {1867-7800}, language = {en} } @misc{FischerVesteBensetal., author = {Fischer, Thomas and Veste, Maik and Bens, Oliver and H{\"u}ttl, Reinhard F.}, title = {Dew formation on the surface of biological soil crusts in central European sand ecosystems}, series = {Biogeosciences}, volume = {9}, journal = {Biogeosciences}, issn = {1726-4189}, doi = {10.5194/bg-9-4621-2012}, pages = {4621 -- 4628}, abstract = {Dew formation was investigated in three developmental stages of biological soil crusts (BSC), which were collected along a catena of an inland dune and in the initial substrate. The Penman equation, which was developed for saturated surfaces, was modified for unsaturated surfaces and used for prediction of dewfall rates. The levels of surface saturation required for this approach were predicted using the water retention functions and the thicknesses of the BSCs. During a first field campaign (2-3 August 2011), dewfall increased from 0.042 kg m-2 for the initial sandy substrate to 0.058, 0.143 and 0.178 kg m-2 for crusts 1 to 3, respectively. During a second field campaign (17-18 August 2011), where dew formation was recorded in 1.5 to 2.75-h intervals after installation at 21:30 CEST, dewfall increased from 0.011 kg m-2 for the initial sandy substrate to 0.013, 0.028 and 0.055 kg m-2 for crusts 1 to 3, respectively. Dewfall rates remained on low levels for the substrate and for crust 1, and decreased overnight for crusts 2 and 3 (with crust 3 > crust 2 > crust 1 throughout the campaign). Dew formation was well reflected by the model response. The suggested mechanism of dew formation involves a delay in water saturation in near-surface soil pores and extracellular polymeric substances (EPS) where the crusts were thicker and where the water capacity was high, resulting in elevated vapor flux towards the surface. The results also indicate that the amount of dewfall was too low to saturate the BSCs and to observe water flow into deeper soil. Analysis of the soil water retention curves revealed that, despite the sandy mineral matrix, moist crusts clogged by swollen EPS pores exhibited a clay-like behavior. It is hypothesized that BSCs gain double benefit from suppressing their competitors by runoff generation and from improving their water supply by dew collection. Despite higher amounts of dew, the water availability to the crust community decreases with crust development, which may be compensated by ecophysiological adaptation of crust organisms, and which may further suppress higher vegetation or mosses.}, language = {en} }