Evaluating Mechanisms of Short-term Woodland Salamander Response to Forest Management

Margenau, Eric L.; Wood, Petra Bohall; Brown, Donald J.; Ryan, Christopher W.

doi:10.1007/s00267-022-01735-3

Cited by 1 publication

(1 citation statement)

References 54 publications

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“…Forest restoration actions utilizing thinning operations and planned/managed fire are designed to reduce forest fuels and return natural fire regimes to the landscape [63]. Based on our results, the retention of logs in thinned and burned areas can provide microsites with warmer temperatures and enhanced soil moisture, which can contribute to wildlife habitat and biological diversity and promote ecosystem processes [17][18][19][20][21][22][23][24][25][26][27][28][29][30][31][32][33][34][35][36].…”

Section: Discussionmentioning

confidence: 94%

Influence of Mixed Conifer Forest Thinning and Prescribed Fire on Soil Temperature and Moisture Dynamics in Proximity to Forest Logs: A Case Study in New Mexico, USA

Parmenter

Losleben

2023

Forests

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Forest management activities often include fuels reduction through mechanized thinning followed by prescribed fire to remove slash. Management prescriptions may include the retention of logs for wildlife habitat and microsites for enhanced tree regeneration. We examined aboveground microclimate and belowground soil temperature and volumetric water content (VWC) dynamics beneath and adjacent to logs at 10, 20, and 30 cm depths in a mixed conifer forest. We assessed the soil variables over 7 years during pre-treatment, post-thinning, and post-fire using a Before–After/Control–Impact experimental design. We found that thinning and burning caused large increases in solar radiation and mean and maximum wind speeds, but only small changes in air temperature and humidity. The treatments increased the soil temperatures beneath the logs by up to 2.7 °C during spring, summer, and fall; the soil VWC increased from 0.05 to 0.08 m3/m3 year-round at 20 and 30 cm depths. Microsites 1–2 m away from the logs also showed soil temperature increases of up to 3.6 °C in spring, summer, and fall, while the measurements of the soil VWC produced variable results (moderate increases and decreases). The increased VWC in late winter/spring likely resulted from reduced plant transpiration and greater snow amounts reaching the ground without being intercepted by the forest canopy. Log retention on thinned and burned sites provided microsites with increased soil temperature and moisture in the top 30 cm, which can enhance soil ecosystem processes and provide refugia for invertebrate and vertebrate wildlife.

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