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Surface Water Quality Data from Beaver-Impacted Streams; Trail Creek and East River, Colorado 2025

Creators: Sam Pierce, Jessica Pall
Year: 2026
DOI: 10.15485/3022760
License: CC-BY 4.0
Location: Trail Creek (TC) is a snow-dominated headwater tributary to the Taylor River located within the greater Taylor Park watershed in Gunnison County, Colorado, USA, and part of the Upper Colorado River Basin (UCRB). The watershed is situated at high elevation within the Rocky Mountains and is characterized by long-duration seasonal snowpack, spring snowmelt-driven runoff, and low winter baseflow typical of montane headwater systems. Trail Creek has undergone extensive low-tech process-based restoration through the installation of several hundred beaver dam analogs (BDAs) and associated structures designed to mimic natural beaver dams and historical wood accumulations. These structures have increased hydraulic complexity, enhanced overbank flooding, and promoted the development of ponded and multi-thread channel conditions. The system now includes free-flowing channel segments, ponded impoundments, return-flow channels, and seepage faces along dam structures, providing strong spatial gradients in hydrologic connectivity and biogeochemical conditions. The watershed is underlain primarily by Proterozoic crystalline rocks, including felsic intrusive igneous lithologies (e.g., granitic compositions), which weather to produce coarse alluvial sediments in valley bottoms. Valley fill deposits consist of heterogeneous mixtures of sand, gravel, cobble, and organic-rich floodplain sediments that support riparian vegetation and seasonal wetland development. Trail Creek provides a field setting for evaluating how beaver-mediated and restoration-driven changes in hydrology influence surface water–floodplain exchange, solute transport, and elemental partitioning in mountain headwaters. Additional metadata describing specific sampling locations, instrumentation, and reach delineations are provided within this data package.
Temporal extent: 2025-06-19 to 2025-09-17
Bounding box: 38.891°N to 38.928°N, -106.958°W to -106.599°W
Publisher: ESS_DIVE
Tags: EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > SURFACE WATER, CATEGORICAL:GCMD Cations, Anions, Dissolved organic carbon, Specific conductivity, pH, Dissolved oxygen, Oxidation reduction potential, VARIABLE:NONE ESS-DIVE File Level Metadata Reporting Format, ESS-DIVE CSV File Formatting Guidelines Reporting Format, ESS-DIVE Water-Soil-Sediment Chemistry Reporting Format, Alpine & Subalpine Ecology, Plant Biology, Hydrology & Watersheds, Snow & Ice, Groundwater, Water Quality, Geology & Tectonics, Geochemistry & Isotopes, Weather & Atmospheric Science, Community Planning, Recreation & Tourism, Gunnison Basin, Research Programs

Description

This data package contains surface water chemistry measurements collected in 2025 to evaluate how beaver damming and low-tech process-based stream restoration influence water quality and metal mobility in mountainous headwater systems of the Upper Colorado River Basin. Sampling was conducted at Trail Creek (Taylor Park watershed, Colorado), a tributary undergoing restoration through installation of low-tech process-based structures (i.e., beaver dam analogs), and at off-channel beaver ponds within the East River floodplain (East River watershed, Colorado). Samples were collected along longitudinal transects spanning upstream control reaches, beaver-influenced ponded reaches, and downstream segments. Additional samples were collected from near-surface pore waters within a beaver dam seepage face. The dataset includes concentrations of major and trace elements measured by inductively coupled plasma–mass spectrometry (ICP-MS) and inductively coupled plasma–optical emission spectrometry (ICP-OES), major anions measured by ion chromatography (IC), and dissolved organic carbon (DOC; reported as non-purgeable organic carbon, NPOC). Samples were size-fractionated at 0.45 micrometers (µm), 0.22 µm, and 0.02 µm to distinguish particulate (>0.45 µm), colloidal (0.22–0.02 µm), and dissolved (<0.02 µm) fractions. The data package consists of comma-separated value (.csv) files containing tabulated chemical concentration data, sample metadata (site identifiers, geographic coordinates, sampling dates, fraction type), and quality control flags. All files are provided in open, non-proprietary formats that can be accessed using standard data analysis software such as Microsoft Excel, R, Python, MATLAB, or other programs capable of reading .csv files. Units, detection limits, and analytical methods are documented in accompanying metadata files. The dataset is designed to support analyses of (1) how beaver impoundment and restoration structures alter elemental partitioning and transport, (2) the role of iron and organic carbon in mediating trace metal mobility, and (3) reach-scale changes in water quality across restoration gradients. This work was supported by the Watershed Function Science Focus Area at Lawrence Berkeley National Laboratory funded by the US Department of Energy, Office of Science, Biological and Environmental Research under Contract No. DE-AC02-05CH11231. Part of this work was performed at SLAC Accelerator Laboratory funded by the US Department of Energy, Office of Science, Biological and Environmental Research under Contract No. DE-AC02-76SF00515.

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