New Mexico Geological Society Annual Spring Meeting — Abstracts

The 1.2 Ma Valles Caldera in northern New Mexico hosts a hydrothermal system that has been characterized by Goff and Janik, 2000 and references therein as consistent with a young igneous model. This study aims to determine the geochemical processes that govern the attenuation of chemical components released by hydrothermal activity in streams draining the Jemez mountains. The Sulphur Springs are the primary vents of the Valles acid-sulfate hydrothermal system, emitting waters with pH <3 and high concentrations of Al (60-800 mg/L) and SO₄^2- (1,800-10,000 mg/L). Sulphur Springs discharges into Sulphur Creek, imparting a similarly low-pH, high-Al, high-SO₄^2- signature. Further downstream, these signatures are attenuated by the interaction of Sulphur Creek with the similarly low-pH Redondo Creek and the circumneutral, snowmelt-fed Río San Antonio. The Sulphur Creek field area is a particularly useful natural laboratory to conduct this study due to the wide range of in-stream pH and salinity conditions. Additionally, Sulphur Creek waters mix with waters of diverse composition of both hydrothermal and meteoric origin at multiple confluences along its run. The wide range of conditions found in this field area make it possible to discriminate between many processes that control attenuation.

This study uses major ion and stable isotope compositions and field parameters of collected water samples as geochemical tracers to identify attenuation processes. Due to the low pH of many of the samples, charge balancing of the waters required additional steps, including partitioning total sulfate species into SO₄^2- and HSO₄^- and geochemical modelling using software such as PhreeqC. Data collected for this study suggests the importance of dilution and pH-changes in attenuating high concentrations of dissolved solids. Mixing analysis at the many confluences Sulphur Creek has along its flowpath is required to identify attenuation on a more granular level. Furthermore, additional investigation is needed to identify seasonal changes in the geochemistry of the system that may have an impact on the attenuation of the hydrothermal components. Hydrothermally-affected waters from the Yellowstone caldera are used for comparison with Valles waters in this study.

References:

1. Goff, F. and Janik, C, 2000, Geothermal Systems: Encyclopedia of Volcanoes, p. 817-834.
2. McCleskey, R.B., Nordstrom, D.K., Susong, D.D., Ball, J.W., Holloway, J.M., 2010a, Source and fate of inorganic solutes in the Gibbon River, Yellowstone National Park, Wyoming, USA: I. Low-flow discharge and major solute chemistry: Journal of Volcanology and Geothermal Research, v. 193, p. 189-202.
3. McCleskey, R.B., Nordstrom, D.K., Susong, D.D., Taylor, H.E., 2010b, Source and fate of inorganic solutes in the Gibbon River, Yellowstone National Park, Wyoming, USA. II. Trace element chemistry: Journal of Volcanology and Geothermal Research, v. 196, p. 139-155.
4. Nordstrom, D.K., McCleskey, R.B., and Ball, J.W., 2009 Sulfur geochemistry of hydrothermal waters in Yellowstone National Park: IV Acid-sulfate waters: Applied Geochemistry, v. 24, p. 191-207.