Stream Solute Export and Biogeochemistry in the Luquillo Mountains, Puerto Rico Richard L. Brereton William H. McDowell University of New Hampshire University.

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Presentation transcript:

Stream Solute Export and Biogeochemistry in the Luquillo Mountains, Puerto Rico Richard L. Brereton William H. McDowell University of New Hampshire University of New Hampshire

El Yunque National Forest, PR The only tropical rainforest in the U.S. 70% of runoff is withdrawn (Crook 2005) LTER since 1988 CZO since 2009

Tropical Montane Wet Forest

Two Very Different Watersheds Rio Mameyes Volcaniclastic bedrock 3.5 m/y of rain Lower avg. elevation Rio Icacos/Blanco Granodiorite bedrock 4.5 m/y of rain Higher avg. elevation

Volcaniclastic: Rio Mameyes Bisley watersheds Q. Sonadora Granodiorite Rio Icacos Q. Guaba

Quebrada Sonadora - low flow

Controls on stream chemistry Major ions reflect lithology and sea salt Dilution at high flows Silica dilution is among highest measured (Godsey et al. 2009) TSS increases with flow Biogeochemical puzzle: Carbon and Nitrogen

Shanley, McDowell, and Stallard 2011 “Boomerang” effect of DOC in the Icacos

El Yunque, 1984

1989 – Hurricane Hugo (Inches of rain) Category 4 Hurricane: 226 km/hr sustained Study Area

Bisley Experimental Watersheds Before HugoAfter Hugo

Georges, 1998 Category 3, 175 km/hr sustained

Mameyes headwaters – 2005

Weathering products and DOC: no response to hurricanes Icacos after Georges

Nitrate response in two small watersheds after Georges ( ) Volcaniclastic (Prieta) Quartz diorite (Guaba)

Two larger basins, Sonadora (254 ha) and Icacos (326 ha) after Georges ( ) Pre-Hurricanes Rio Icacos Q. Sonadora

What makes nitrate behave so differently from other solutes? Why the slower return to baseline in granodiorite watersheds?

Biogeochemical controls on N flux to streams Hydrologic flow path – groundwater? surface runoff? Residence time – contact with soils What is the matrix? Redox conditions – climate Riparian denitrification NO 3 N 2 ON 2

Groundwater monitoring wells Transects across catena

Bisley – volcaniclastic Riparian zone: Denitrification “hotspot” periodically anaerobic C source high retention time Modified from McDowell et al. 1992

Icacos trib. – granodiorite watershed Riparian Zone Slope Stream: Flows into Icacos Modified from McDowell et al Key: NO 3 NH 4

Icacos – slow recovery

Conclusions Luquillo stream chemistry reflects lithology overlain by vegetation, climate, disturbance history Hurricanes cause dramatic shifts in forest biogeochemistry, reflected in stream nitrate peaks Riparian zones hold the key to understanding long-term nitrogen dynamics in the Luquillo Mountains

Acknowledgements Funding from NSF-LTER, NSF Ecosystems, NSF-CZO, USFS IITF, UPR, UNH Collaborators include F. Scatena, A. Lugo, D. Schaefer, C. Asbury, J. Merriam, J. Potter, and others Field and laboratory assistance from M. Salgado, M.J. Sanchez, J. Bithorn, J. Merriam, J. Potter, J. Orlando, and others

Questions? Riparian Zone Slope Stream: Flows into Icacos Modified from McDowell et al Key: NO 3 NH 4