Effect of plot size and precipitation magnitudes on the activation of soil erosion processes using simulated rainfall experiments in vineyards
Metadata
Show full item recordEditorial
Frontiers
Materia
Plot size Land management Applied research Viticulture Soil erosion processes Surface runoff Rainfall simulator
Date
2022-09-13Referencia bibliográfica
Neumann, M... [et al.] (2022), Effect of plot size and precipitation magnitudes on the activation of soil erosion processes using simulated rainfall experiments in vineyards. Front. Environ. Sci. 10:949774. doi: [10.3389/fenvs.2022.949774]
Sponsorship
Technology Agency of the Czech Republic TJ02000234; Ministry of Agriculture, Czech Republic QK1810341 QK1910029 QK22010261; Grant Agency of the Czech Technical University in Prague SGS 20/156/OHK1/3T/11Abstract
Soil erosion is recognized as a threat to humankind and to natural ecosystems
when sustainable limits are exceeded. Several researchers have used various
tools, such as rainfall simulators, to assess extreme rainfall events and nonsustainable
soil management practices. However, combinations of two
different devices of different sizes has not been tested before, especially in
vineyards. The aim is to verify whether plot size, connectivity processes and
rainfall distribution affect the activation of soil erosion. In this research on soils
cultivated with vineyards in the Moravia Region in the south-eastern part of the
Czech Republic, we have performed various rainfall simulation experiments
with a small device (1 × 1 m) and with a large device (8 × 1 m). Our results show
that the surface runoff was approximately 30% higher on the small plot than on
the large plot. The large rainfall simulator produced sediment concentration
that was up to 3 times higher, and soil loss that was up to 1.5 times higher, even
when the surface runoff was 30%–50% lower for the large rainfall simulator. We
therefore conclude that there is a clear influence of surface length and plot size
on surface runoff, soil loss and sediment concentration activation. When
planning their experiments, researchers need to consider that the type of
device can have a drastic influence on the final results. Two devices
subjected to the same rainfall intensity (60mmh−1) can produce very
different results, e.g., depending on plot size and kinetic energy. Our results
can be effectively used to plan soil protection measures and to inform local
authorities about areas prone to flooding and about loss of sediments.