Datasets

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DTS_RawData_Rantoul Site

DTS conducted in two adjacent wells, one cased (40m) and the other one, uncased borehole (100m) in east central Illinois. The DTS cable was installed vertically in both boreholes, attached to the PVC pipe in the cased borehole and sealed against the sidewall with bentonite grout in the uncased borehole. Thermal profiles were measured and analyzed in the subsurface in both scenarios in different months from 2015-2017

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C-Baseline Soil Properties

Baseline soil properties collected from representative sites throughout the Clear Creek Watershed. The samples were collected at depths of 0 to 5 cm and 5 to 10 cm along sampling grids in the characterization fields. Each grid consisted of four transects at different catena positions (i.e., crest, shoulder, backslope, toe) and three downslope transects following the main flow paths. Samples were collected in November 2015. bulk soil properties, including bulk density, texture, pH, and aggregate stability as well as organic geochemistry and isotopic signatures (i.e., total C and N, d13C/d15N, lignin content, lipids, and fatty acids). A portion of the samples has been archived for future analyses.

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S-Baseline Soil Properties

Baseline soil properties collected from representative sites throughout the Upper Sangamon River Basin. The samples were collected at depths of 0 to 5 cm and 5 to 10 cm along sampling grids in the characterization fields. Each grid consisted of four transects at different catena positions (i.e., crest, shoulder, backslope, toe) and three downslope transects following the main flow paths.Samples were collected in November 2015. bulk soil properties, including bulk density, texture, pH, and aggregate stability as well as organic geochemistry and isotopic signatures (i.e., total C and N, d13C/d15N, lignin content, lipids, and fatty acids). A portion of the samples has been archived for future analyses.

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Clear Creek ISCO sediments and POC

Sediment concentrations, organic C concentrations, total N concentrations, C and N stable isotopes collected on suspended sediments from Clear Creek for multiple storm events between 2014-2016 as functions of time and discharge.