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dc.contributor.authorChen, Xindi
dc.contributor.authorZhang, Changkuan
dc.contributor.authorPaterson, David M.
dc.contributor.authorTownend, Ian H.
dc.contributor.authorJin, Chuang
dc.contributor.authorZhou, Zeng
dc.contributor.authorGong, Zheng
dc.contributor.authorFeng, Qian
dc.identifier.citationChen , X , Zhang , C , Paterson , D M , Townend , I H , Jin , C , Zhou , Z , Gong , Z & Feng , Q 2019 , ' The effect of cyclic variation of shear stress on non-cohesive sediment stabilization by microbial biofilms : the role of ‘biofilm precursors’ ' , Earth Surface Processes and Landforms , vol. Early View .
dc.identifier.otherPURE: 257337853
dc.identifier.otherPURE UUID: 885ce7fb-b207-4e52-8add-e6dc46f6aa13
dc.identifier.otherRIS: urn:26177A3C0DF8A05B6D46A77A11EB74CB
dc.identifier.otherORCID: /0000-0003-1174-6476/work/53548928
dc.identifier.otherScopus: 85060926001
dc.identifier.otherWOS: 000469991600009
dc.descriptionThis work was supported by the National Natural Science Foundation of China (NSFC, Grant Nos. 51620105005, 51879095, 51579072, 41606104). D. M. Paterson received funding from the MASTS pooling initiative (The Marine Alliance for Science and Technology for Scotland) and the NERC Blue-coast consortium (N E/N016009/1) and their support is gratefully acknowledged. MASTS is funded by the Scottish Funding Council (grant reference HR09011) and contributing institutions. X. D. Chen received funding from the China Scholarship Council.en
dc.description.abstractBiofilm mediated intertidal sediments exhibit more complex erosional behaviour than abiotic systems. A major feature of intertidal systems is the exposure to repeated cycles of high and low shear created by tidal conditions and also less predictable episodic events, such as storms. There is very little information on how biofilm-forming communities respond to these conditions. In this study, the effects of both single and repeated-cycles of shear on the stability of newly developed bio-sedimentary beds was examined. Cleaned sand, without any potential biostabilization, was used as the control. For the single-cycle scenario, biofilms were incubated on a non-cohesive sandy bed under prolonged low shear periods varying between 5 and 22 days, after which erosional stress was applied. No significant biostabilization was observed for the youngest bio-sedimentary bed (after five days of low shear incubation). After 22 days, microbial communities were characterized by a firmly attached surface biofilm. To cause erosion, greater hydrodynamic stress (0.28 Pa) was required. The erosional behaviour of the underlying sand was also affected in that bedform ripples noted in the control system were no longer observed. Instead, a sudden ‘mass erosion’ took place (0.33 Pa). The one-cycle scenario indicated that significant biostabilization of sand only occurred after a relative long calm period. Under repeated cycles of stress (five days of low stress followed by high stress event and re-incubation, repeated for four cycles = 20 days), frequent cyclic disturbance did not degrade the system stability but enhanced biostabilization. The properties of the sub-surface sediments were also affected where erosion rates were further inhibited. We hypothesize that organic material eroded from the bed acted as a ‘biofilm precursor’ supporting the development of new biofilm growth. A conceptual framework is presented to highlight the dynamics of bio-sedimentary beds and the effects of growth history under repeated-cycles.
dc.relation.ispartofEarth Surface Processes and Landformsen
dc.rights© 2019, John Wiley & Sons, Ltd. This work has been made available online in accordance with the publisher's policies. This is the author created accepted version manuscript following peer review and as such may differ slightly from the final published version. The final published version of this work is available at
dc.subjectBiofilm detachmenten
dc.subjectSediment erosionen
dc.subjectBiofilm regrowthen
dc.subjectBio-sedimentary systemen
dc.subjectGE Environmental Sciencesen
dc.subjectEarth and Planetary Sciences (miscellaneous)en
dc.subjectEarth-Surface Processesen
dc.subjectGeography, Planning and Developmenten
dc.titleThe effect of cyclic variation of shear stress on non-cohesive sediment stabilization by microbial biofilms : the role of ‘biofilm precursors’en
dc.typeJournal articleen
dc.contributor.institutionUniversity of St Andrews. Sediment Ecology Research Groupen
dc.contributor.institutionUniversity of St Andrews. School of Biologyen
dc.contributor.institutionUniversity of St Andrews. Marine Alliance for Science & Technology Scotlanden
dc.contributor.institutionUniversity of St Andrews. Scottish Oceans Instituteen
dc.contributor.institutionUniversity of St Andrews. St Andrews Sustainability Instituteen
dc.description.statusPeer revieweden

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