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Marc-O. Goebel

Researcher at Leibniz University of Hanover

Publications -  20
Citations -  1063

Marc-O. Goebel is an academic researcher from Leibniz University of Hanover. The author has contributed to research in topics: Contact angle & Wetting. The author has an hindex of 12, co-authored 15 publications receiving 904 citations.

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Soil water repellency and its implications for organic matter decomposition – is there a link to extreme climatic events?

TL;DR: In this paper, the authors studied the effect of climate change on soil water repellency (SWR) and found that SWR is an important SOM stabilization mechanism that could become more important because of the increase in extreme events such as droughts and heat waves.
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Soil wettability, aggregate stability, and the decomposition of soil organic matter

TL;DR: In this article, the authors studied the significance of soil wettability with respect to both SOM mineralisation and aggregate stability in a loess-derived Gleyic Luvisol, either used as cropland or as grassland.
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Physical carbon-sequestration mechanisms under special consideration of soil wettability

TL;DR: In this paper, the effect of organic matter (OM) quantity and OM quality on physical protection of soil is investigated. And the authors conclude that a higher hydrophobicity of the OM appears to stabilize the organic C in soil, either caused by a specific reduced biodegradability of OM or indirectly caused by increased aggregate stability.
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Water potential and aggregate size effects on contact angle and surface energy

TL;DR: In this paper, the authors investigated the dynamics of contact angle due to variation of the water potential and found that the contact angle increased as water potential increased to a specific level, and then decreased again when water potential reached a certain level.
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Microbial cell-envelope fragments and the formation of soil organic matter: a case study from a glacier forefield

TL;DR: In this paper, the development of soil organic matter (SOM) along a chronosequence of a glacier forefield (Damma glacier) was evaluated by evaluating the surface coverage of microbial cell-envelope residues.