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Susanne K. Woche

Researcher at Leibniz University of Hanover

Publications -  65
Citations -  2313

Susanne K. Woche is an academic researcher from Leibniz University of Hanover. The author has contributed to research in topics: Soil water & Contact angle. The author has an hindex of 23, co-authored 58 publications receiving 1919 citations.

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Extended methodology for determining wetting properties of porous media

TL;DR: In this article, the Wilhelmy plate method (WPM) and modified capillary rise method (MCRM) were tested on 24 soils and the results showed that both WPM and MCRM are reliable for determining contact angles and particle surface energy over a wide range of porous material wettabilities.
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Modified sessile drop method for assessing initial soil-water contact angle of sandy soil

TL;DR: In this article, a modified sessile drop method was proposed for measuring the initial contact angle of powdered or granular material, which is made by placing a layer of uniform soil particles onto adhesive tape, adding droplets of deionized water, and reading off the contact angle at the three-phase boundary line with a goniometerfitted microscope immediately after placing the drops on the soil sample.
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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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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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Contact angle of soils as affected by depth, texture, and land management

TL;DR: In this article, the authors investigated contact angles and wetting properties as a function of depth for a wide range of agricultural and forest soils in Germany, and concluded that a coarse texture favours, in combination with other factors (mainly pH), hydrophobic SOM.