Effects of agriculture and seasonality on the soil hydrophysical
properties of high-Andean dry páramo grasslands
Abstract
One of the most essential ecosystem services provided by high-Andean
páramos is streamflow buffering. A combination of soil, vegetation and
climate characteristics provides páramos with an exceptional ability to
store, regulate and supply water, particularly in their natural state.
However, páramo catchments are seldom pristine. Agriculture is one of
the most widespread human activities in páramos and considerably affects
their soil hydrophysical properties. This research assesses how soil
properties are affected by the conversion from natural páramo vegetation
to fallow, onion, or potato crops. We measured Soil Organic Matter
(SOM), Bulk density (Bd), pH and electric conductivity (EC) at three
depths (0–5, 10–15 and 20–25 cm), in a stratified random survey of
different land uses in the Eastern Cordillera of Colombia. Samples were
collected in wet and dry seasons. Agricultural use affects all the
studied properties, increasing Bd (+0.11 g cm-3), decreasing SOM
(-5.5%), and increasing pH (+1.3) and EC (+187 µS cm-1). Seasonality
did not have a significant effect on the studied properties under
natural vegetation; however, there were significant differences between
wet season and dry season in agricultural soils in SOM (-7.2% and
+5.7% in fallow and potato crop, respectively) and Bd (-0.22 gr cm-3 in
crops). These changes show that agriculture in páramo grasslands leads
to a significant decrease in soil porosity and water-holding capacity,
which affects adversely the ecosystem hydrological regulation capacity.
This paper contributes to a better understanding of the complexity of
Andean páramos and provide crucial information to improve soil
management, a key aspect for ensuring the sustainable provision of
hydrological ecosystem services offered by Andean and other mountain
ecosystems.