Abstract

Mountain environments, including the Andean páramo grasslands of Ecuador, are important water source areas. They are often sites of programs and policies intended to achieve multiple management objectives, such as carbon sequestration, biological conservation, and water resource protection; yet such environments are often data poor. This creates challenges for programs that compensate landowners for protecting ecosystem services and uncertainty regarding which land uses are compatible. For example, does afforestation for carbon sequestration complement or hinder efforts to protect water resources in Andean páramos? We compared characteristics of high-elevation soil profiles at sites in two Ecuadorian páramo study areas and measured soil–water properties to assess whether changes in land use affected the soil hydrology. Using a space-for-time substitution, we compared soils in plantations of pines and Polylepis racemosa in grasslands with different grazing and burning regimes. Methods included soil description in soil pits; soil moisture measurement in soil pits and across surface transects; tracer studies of soil–water movement; and laboratory determination of bulk density, particle size, and humic acid composition. Of the land uses examined, only afforestation significantly affected soil moisture, whereas soil properties did not differ among grassland burning and grazing regimes. The results suggest that afforestation of páramos hinders the production of water and they underscore the need for further investigation to inform the trade-offs needed in managing páramo landscapes to support multiple ecosystem services.

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