On the Influence of Biological Soil Crusts and Bryophytes on Soil Erosion and the Soil Water Balance in Temperate Forests

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dc.contributor.advisor Scholten, Thomas (Prof. Dr.)
dc.contributor.author Gall, Corinna
dc.date.accessioned 2024-01-24T13:54:58Z
dc.date.available 2024-01-24T13:54:58Z
dc.date.issued 2024-01-24
dc.identifier.uri http://hdl.handle.net/10900/149467
dc.identifier.uri http://nbn-resolving.de/urn:nbn:de:bsz:21-dspace-1494678 de_DE
dc.identifier.uri http://dx.doi.org/10.15496/publikation-90807
dc.description.abstract Soil erosion is a serious threat to the soil because it impairs the provision of important ecosystem services such as filtering water, providing nutrients and habitat for biology activity, storing carbon, and producing biomass. This also plays a crucial role in forest ecosystems where natural and anthropogenic disturbances expose bare soil to erosion. An important countermeasure is the rapid recolonization by vegetation. Especially in arid regions, biological soil crusts (biocrusts) are known to be pioneer colonizers of disturbed soils and to reduce soil erosion. Bryophytes also protect the soil and can have a positive effect on the soil water balance. However, the influence of bryophytes and biocrusts on soil erosion and the soil water balance in temperate forests is largely unexplored. This thesis investigated how biocrusts and bryophytes influence soil erosion and the soil water balance in skid trails of a temperate forest ecosystem in the Schönbuch Nature Park in South Germany. This included in-situ studies of soil erosion in the skid trails during vegetation succession and ex-situ studies of the influence of combinations of soil substrates and moss species (soil-moss combinations) on soil erosion. In addition, the water absorption and evaporation patterns in the soil-moss combinations were examined, also taking into account the structural traits of the moss species. Within this thesis, it was shown that bryophyte-dominated biocrusts significantly affected soil erosion and that bryophytes not only contributed more to erosion reduction than vascular vegetation, but also positively influenced the soil water balance. Surface runoff and soil erosion were decreased with moss covers, while the amount of percolated water was increased; however, these processes were superimposed by desiccation cracks and water repellency. Moss treatments exhibited lower water contents over time compared to bare treatments, highlighting the strong influence of moss covers and desiccation cracks on the soil water balance. Mosses were no barrier for infiltration in case of high precipitation rates and they did not store much of the applied water themselves, but passed it on to the soil. During desiccation, mosses with high leaf area index (LAI) had lower evaporation rates than mosses with low LAI, and they prevented desiccation of the soil substrates, although even dense moss covers did not completely seal the surface. en
dc.language.iso en de_DE
dc.publisher Universität Tübingen de_DE
dc.rights ubt-podok de_DE
dc.rights.uri http://tobias-lib.uni-tuebingen.de/doku/lic_mit_pod.php?la=de de_DE
dc.rights.uri http://tobias-lib.uni-tuebingen.de/doku/lic_mit_pod.php?la=en en
dc.subject.classification Bodenerosion , Moose , Wald , Bodenwasserhaushalt de_DE
dc.subject.ddc 500 de_DE
dc.subject.ddc 550 de_DE
dc.subject.ddc 580 de_DE
dc.subject.ddc 910 de_DE
dc.subject.other Bodenerosion de_DE
dc.subject.other Moose de_DE
dc.subject.other Bryophytes en
dc.subject.other Forest en
dc.subject.other Wald de_DE
dc.subject.other Soil erosion en
dc.subject.other Bodenwasserhaushalt de_DE
dc.subject.other Soil water balance en
dc.subject.other Biological soil crusts en
dc.subject.other Biologische Bodenkrusten de_DE
dc.title On the Influence of Biological Soil Crusts and Bryophytes on Soil Erosion and the Soil Water Balance in Temperate Forests en
dc.type PhDThesis de_DE
dcterms.dateAccepted 2023-05-08
utue.publikation.fachbereich Geographie, Geoökologie, Geowissenschaft de_DE
utue.publikation.fakultaet 7 Mathematisch-Naturwissenschaftliche Fakultät de_DE
utue.publikation.noppn yes de_DE


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