Paper No. 2
Presentation Time: 8:25 AM


JENSEN, A.E., Department of Geosciences, Idaho State University, Pocatello, ID 83201, MORA, C.I., Earth and Environmental Sciences, Los Alamos National Laboratory, Los Alamos, NM 87544, CROSBY, B.T., Dept. of Geosciences, Idaho State University, Pocatello, ID 83209 and LOHSE, K.A., Department of Biological Sciences, Idaho State University, Pocatello, ID 83209,

Warming of Arctic permafrost threatens the release of vast stores of carbon (C). On Arctic hillslopes, thermokarst features can grow very rapidly, altering soil structure, temperature (T), moisture and soil organic matter (SOM) distribution, and impacting the rate and nature of C release. To assess changes in soil C dynamics during formation and stabilization of these thermokarst features, we studied a very large, active retrogressive thaw slump located along the Selawik River, NW Alaska. The active slump has rapidly grown since initiation (2004), mobilizing > 0.5M m3 of ice and sediments. We defined a three-stage slump chronosequence composed of: (1) undisturbed peat and tussock tundra overlying thick glacial diamict and loess deposits; (2) the active slump, and; (3) an older, adjacent stabilized slump, re-colonized by black spruce, alder and various grasses. Over two field seasons, the chronosequence was measured for: peak summer soil CO2 efflux, depth profiles (to 50cm) of soil CO2, CH4, and SOM concentrations and δ13C, T, bulk density, calculated porosity, water filled pore space (WFPS), and effective diffusivity. In the active slump, soil T were 10-15°C warmer, and profile CO2 and CH4 were 3-100X higher than in the undisturbed tundra or stabilized slump. Yet, CO2 efflux from the active slump was <0.5X efflux from other parts of the chronosequence. Low effective diffusivity, particularly in the upper 20 cm, is attributed to settling of fines from thawed material flowing from the headwall, plugging porosity and dampening CO2 efflux. Across the chronosequence, values of δ13C-CO2, -CH4, and -SOM suggest CH4 and CO2 are forming under anaerobic conditions, except within the drier 2011 stabilized slump, where δ13C-CO2 profiles are consistent with well-drained, aerobic conditions. Our findings suggest that rapidly-formed, hillslope thermokarst features can profoundly alter soil environmental conditions and biophysical controls on C cycling in warming permafrost soils, and ultimately lead to stable soil states that support different vegetation and higher CO2 efflux. During active slumping, however, newly exposed mineral soils remain relatively saturated, with low effective diffusivity, dampening C efflux during thermokarst formation, despite permafrost warming.