Abstract

The effects of western juniper (Juniperus occidentalis) control on understory vegetation and soil water content were studied at the watershed-scale. Seasonal differences in topsoil (12 cm) water content, as affected by vegetation structure and soil texture, were evaluated in a 96-ha untreated watershed and in a 116-ha watershed where 90% juniper was removed in 2005. A watershed-scale characterization of vegetation canopy cover and soil texture was completed to determine some of the potential driving factors influencing topsoil water content fluctuations throughout dry and wet seasons for approximately one year (2014–2015). We found greater perennial grass, annual grass, and shrub cover in the treated watershed. Forb cover was no different between watersheds, and as expected, tree canopy cover was greater in the untreated watershed. Results also show that on average, topsoil water content was 1% to 3% greater in the treated watershed. The exception was during one of the wettest months (March) evaluated, when soil water content in the untreated watershed exceeded that of the treated by <2%. It was noted that soil water content levels that accumulated in areas near valley bottoms and streams were greater in the treated watershed than in the untreated toward the end of the study in late spring. This is consistent with results obtained from a more recent study where we documented an increase in subsurface flow residence time in the treated watershed. Overall, even though average soil water content differences between watersheds were not starkly different, the fact that more herbaceous vegetation and shrub cover were found in the treated watershed led us to conclude that the long-term effects of juniper removal on soil water content redistribution throughout the landscape may be beneficial towards restoring important ecohydrologic connections in these semiarid ecosystems of central Oregon.

Highlights

  • The relationships between soil water content and vegetation cover are highly impacted by the ongoing shift from grassland to woodland-dominated landscapes occurring in many arid and semiarid regions worldwide

  • Tree canopy cover was estimated at 27% of total area

  • Average annual untreated watershed is composed of 50% Westbutte, 20% Madeline, and 3% Simas series [24]

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Summary

Introduction

The relationships between soil water content and vegetation cover are highly impacted by the ongoing shift from grassland to woodland-dominated landscapes occurring in many arid and semiarid regions worldwide. This change in vegetation-soil water dynamics has the potential to disrupt the ecological and hydrological balance of these water-limited regions [1,2,3]. Research in native grasslands of Oklahoma found Juniper spp. to be negatively correlated with soil water content, water storage, infiltration rates, and stream flow [6]. Encroachment tends to lead to an increase of bare ground, which significantly alters erosion and overland flow rates, depending on the amount of litter beneath the canopy patches [10,11,12]

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