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Discussion papers | Copyright
https://doi.org/10.5194/soil-2018-25
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Original research article 08 Aug 2018

Original research article | 08 Aug 2018

Review status
This discussion paper is a preprint. It is a manuscript under review for the journal SOIL (SOIL).

Dynamic modelling of weathering rates – Is there any benefit over steady-state modelling?

Veronika Kronnäs1, Cecilia Akselsson1, and Salim Belyazid2 Veronika Kronnäs et al.
  • 1Department of Physical Geography and Ecosystem Science, Lund University, 223 62 Lund, Sweden
  • 2Department of Physical Geography, Stockholm University, 106 91 Stockholm, Sweden

Abstract. Weathering rates are of considerable importance in estimating the acidification sensitivity and recovery capacity of soil, and are thus important in the assessment of the sustainability of forestry in a time of changing climate and growing demands for forestry products. In this study, we modelled rates of weathering in mineral soil at two forested sites in southern Sweden included in the SWETHRO monitoring network using two models. The aims were to determine whether the dynamic model ForSAFE gives comparable weathering rates as the steady-state model PROFILE, and whether the ForSAFE model provided useful extra information on weathering behaviour.

The average weathering rates calculated with ForSAFE were very similar to those calculated with PROFILE for the two modelled sites. The differences between the models regarding the weathering of certain soil layers seemed to be due mainly to differences in calculated soil moisture. The weathering rates provided by ForSAFE vary seasonally with temperature and soil moisture, as well as on longer time scales, depending on environmental changes. Long-term variations due to environmental changes can be seen in the ForSAFE results, for example: the weathering of silicate minerals is suppressed under acidified conditions due to elevated aluminium concentration in the soil, whereas the weathering of apatite is accelerated by acidification. The weathering of both silicates and apatite is predicted to be enhanced by increasing temperature during the 21st century. In this part of southern Sweden, precipitation is assumed to be similar to today’s level during the next forest rotation. However, in parts of Sweden with projected decreasing soil moisture, weathering might not increase despite increasing temperature.

These results show that the dynamic ForSAFE model can be used for weathering rate calculations and that it gives average results comparable to those from the PROFILE model. However, dynamic modelling provides extra information on the variation in weathering rates with time, and offers much better possibilities for scenario modelling.

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Weathering rates in forest soils are important for sustainable forestry, but can't be measured. In this paper, we have modelled weathering with the often used PROFILE model, as well as with the dynamic model ForSAFE, better suited in a changing climate, with changing human activities, but never before tested for weathering calculations. We show that ForSAFE gives comparable weathering rates as PROFILE, but that it shows the variation in weathering with time and is good for scenario modelling.
Weathering rates in forest soils are important for sustainable forestry, but can't be measured....
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