Item talk:Q150145

Geochemistry and fluxes of gases from hydrothermal features at Newberry Volcano, Oregon, USA

We present the chemical and isotopic compositions of gases and fluxes of CO₂ from the hydrothermal features of Newberry Volcano, a large composite volcano located in Oregon's Cascade Range with a summit caldera that hosts two lakes, Paulina and East Lakes. Gas samples were collected from 1982 to 2021 from Paulina Hot Springs (PHS) on the shore of Paulina Lake, East Lake Hot Springs (ELHS) on the shore of East Lake, and Obsidian Flow Gas Seep (OFGS), an area of diffuse gas emissions. Surveys of CO₂ flux were conducted in 2020 at OFGS (1400 m²) and East Lake (4.1 km²). Gases from all three sites were CO₂-rich (≥79 mol% in dry gas) but showed considerable compositional variability over time due to interaction with ground and surface water. An increase in H₂S concentrations and decline in CO₂/H₂S ratios in ELHS gases coincided with a drop in East Lake water level from 1999 to 2021. ELHS and OFGS gases were high in CH₄ relative to PHS and the δ¹³C of CH₄ values for ELHS gases (−72.2 and − 63.6 ‰) reflected a predominantly biogenic origin. The dominant source of N₂ and Ar in PHS, ELHS, and OFGS samples was likely groundwater. Helium isotopic ratios (6.47 to 8.02 R_c/R_a) support a persistent source of magmatic He beneath Newberry caldera and consistently high values measured at OFGS and PHS relative to ELHS suggest distinct fluid flow paths from depth to the surface features. The δ¹³C of CO₂ and CO₂/³He values (−8.9 to −5.35 ‰ and 1.3 × 10⁹ to 4.6 × 10¹⁰, respectively) measured in gases reflect contributions of CO₂ from both mantle and crustal sources. Measured CO₂ fluxes at OFGS and East Lake ranged from 1 to 8808 and < 1 to 364 g m⁻² d⁻¹, respectively. A CO₂ emission rate of 0.5 t d⁻¹ was calculated for OFGS. The CO₂ emission rate estimated for East Lake was 30 t d⁻¹ and when compared to prior estimates, reflects steady-state lake degassing. An enhanced geochemical monitoring plan, including annual sampling of gases at ELHS, OFGS, and PHS for geochemical analysis, installation of a continuous lake-level monitoring station at East Lake, and annual CO₂ flux surveys at OFGS, would provide valuable background data and insights into any precursor volcanic activity. Integrating geochemical data with data from the real-time seismic and GPS network at Newberry Volcano could better resolve and interpret potential changes in its magma-hydrothermal system.