Assessing hillslope sediment generation potential by tree throw: a preliminary field study along a small river valley in the Jura Mountains, northwest Switzerland

• Main Authors: P. Greenwood, J. Bauer, N. J. Kuhn
• Format: Article
• Language: deu
• Published: Copernicus Publications 2021-07-01
• Series: Geographica Helvetica
• Online Access: https://gh.copernicus.org/articles/76/319/2021/gh-76-319-2021.pdf
• ISSN: 0016-7312; 2194-8798

<p>A preliminary field-based investigation was undertaken in a small (<span class="inline-formula"><i>&lt;</i></span> 10 km<span class="inline-formula">²</span>) river valley located in the mountainous Jura region of northwest Switzerland. The aims of the work were to assess sediment generation and annual sediment transport rates by tree throw on forested hillslopes and to document surface hydrology characteristics on four fresh tree throw mounds associated with recent tree throws over a 24 d monitoring period. For the tree throw mounds, average sediment recovery ranged from 7.7–28.2 g (dry weight), equivalent to a suspended sediment concentration of 145.2–327.8 g L<span class="inline-formula">⁻¹</span>, and runoff coefficients ranged from 1.0 %–4.2 %. Based on a soil bulk density value of 1044 kg m<span class="inline-formula">⁻³</span>, upslope runoff generation areas were denuded by an average of 0.14 mm within the 24 d monitoring period, representing an erosion rate equivalent to 2.1 mm a<span class="inline-formula">⁻¹</span>. This means that a ca. 50 cm high tree throw mound could theoretically persist for around 200–250 years. For tree throw work, the dimensions of 215 fallen trees were measured and their locations mapped in 12 separate locations where tree throw was prominent along the river valley, representing a cumulative area equivalent to 5.3 ha (average density equivalent to 43 trees ha<span class="inline-formula">⁻¹</span>). The 215 tree throws generated a total of 20.1 m<span class="inline-formula">³</span> of fine sediment (<span class="inline-formula"><i>&lt;</i></span> 2 mm dia.), or the equivalent of <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M9" display="inline" overflow="scroll" dspmath="mathml"><mrow><mn mathvariant="normal">3.8</mn><mo>×</mo><msup><mn mathvariant="normal">10</mn><mrow><mo>-</mo><mn mathvariant="normal">4</mn></mrow></msup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="51pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="2c2bb69a6de2d248a8af41efd010c6cb"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="gh-76-319-2021-ie00001.svg" width="51pt" height="14pt" src="gh-76-319-2021-ie00001.png"/></svg:svg></span></span> m<span class="inline-formula">³</span> m<span class="inline-formula">⁻²</span>. The process of tree throw was originally attributed to two extreme weather events that occurred across west and central Europe in late December 1999. Taking the 18-year period since both storms, this represents an annual sediment transport rate of <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M12" display="inline" overflow="scroll" dspmath="mathml"><mrow><mn mathvariant="normal">2.7</mn><mo>×</mo><msup><mn mathvariant="normal">10</mn><mrow><mo>-</mo><mn mathvariant="normal">5</mn></mrow></msup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="51pt" height="13pt" class="svg-formula" dspmath="mathimg" md5hash="a6c13535aab15599c44b043c70cfed2b"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="gh-76-319-2021-ie00002.svg" width="51pt" height="13pt" src="gh-76-319-2021-ie00002.png"/></svg:svg></span></span> m<span class="inline-formula">³</span> m<span class="inline-formula">⁻¹</span> a<span class="inline-formula">⁻¹</span>. Exploring the relationship with wind on fall direction, however, 65.5 % of mapped tree throws (<span class="inline-formula"><i>n</i>=</span> 143) generally fell in a downslope direction irrespective of hillslope aspect on which they were located. Given the similar fall orientation for most trees, this infers that severe storms may not have been responsible for the majority of tree throws, but instead, their upheave might be related to root failure. Given the relative maturity (average age 41 years) of fallen trees in this river valley, our data suggest that once trees attain a certain age, their physiognomy (i.e. height, mass, and centre of gravity) compromises their ability to remain securely anchored. We tentatively attribute this possibility to the presence of bedrock close to the surface, and to the shallow soil profile overlaying the steep rocky slopes. More in-depth studies are required to firstly confirm our findings, and secondly, tree throw studies should be undertaken in other Jura mountain river valleys to assess whether these results are representative.</p>