HF020: A Study of Hyporheic Characteristics Along a Longitudinal Profile of Lookout Creek, Oregon, 2003
Notice
"As Is" Basis: All content, including maps and forecasts, is provided without warranties. Users are advised to independently verify critical information.
Citation
Haggerty, R.; Ninnemann, J. 2013. A Study of Hyporheic Characteristics Along a Longitudinal Profile of Lookout Creek, Oregon, 2003 Long-Term Ecological Research Andrews Forest LTER Site. [Database]. Available: https://andrewsforest-stage.forestry.oregonstate.edu/data/fsdb-data-catalog/HF020 Accessed 2026-05-10.
Abstract
Time series of tracer (Rhodamine WT) concentration data representing a "break-through curve" resulting from a single, multi-scale tracer test conducted along the length of Lookout Creek, from its 2nd-order headwaters through its 5th-order main stem. The longitudinal tracer test involved an in-stream injection of Rhodamine WT over 78 hrs, followed by monitoring at eight downstream locations for five months, starting in mid-June 2003 through the middle of November 2003. The injection site was located below the upper Old Growth Trail bridge. The monitoring sites include one downstream of the injection site, above and below the Cold Creek confluence, below the lower Old Growth Trail bridge, below Mack Creek confluence, above and below McRae Creek confluence, and at the HJA headquarters. Three additional inter-order tracer tests (IOTT) were carried out between each of the major stream confluences along Lookout Creek. The injection site for the McRae Creek IOTT was located below the McRae Cr. confluence and was monitored just downstream, at the end of the main floodplain, and at HJA headquarters. The injection site for the Mack Creek IOTT was located below the Mack Cr. confluence and was monitored just downstream, at an unnamed tributary midway between Mack Cr. and McRae Cr., and above the McRae Cr. confluence. The injection site for the Cold Creek IOTT was located below the Cold Cr. confluence and was monitored just downstream, at Longer Cr., and at the lower Old Growth Trail bridge. Concentration break through curves are available for all of the monitoring sites for the longitudinal and inter-order tracer tests. Flux break through curves are available for most of the monitoring sites. STAMMT-L model estimates for hyporheic exchange is listed for most of the monitoring sites.
Coverage
Temporal coverage: 2003-06-14 to 2003-11-15
Geographic coverage: Lookout Creek Catchment
Spatial coverage:
Bounds: W -122.25276000, E -122.11756400, N 44.23357900, S 44.21329300
Purpose
- The primary goal of this research project is to quantitatively measure the temporal scales of hyporheic exchange along a stream network. Our goal is to examine how hyporheic exchange varies with increasing stream size. Many previous studies focus on single stream reaches or on several reaches of similar sized streams, whereas we examined the residence time of water in the hyporheic zone over increasing length scales in a single stream. Prior work with tracer data and analysis using a transient storage model with an exponential residence time distribution (RTD) suggests that hyporheic parameters, primarily volume and mean residence time, are both spatially and temporally scale-dependent. However, recent work hypothesizes that the scale-dependence may be partially addressed by using a power-law RTD (Haggerty et al., 2002). Our research tests this hypothesis with several multi-scale tracer tests in a single stream.
Project
Title: Long-Term Ecological Research
Personnel
-
Sherri L. Johnson - Principal Investigator US Forest Service ;Pacific NW Research Station ;3200 SW Jefferson Way, Corvallis, OR, 97331, USAPhone: 541-758-7771Email: sherri.johnson2@usda.gov, sherri.johnson@oregonstate.edu
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Julia A. Jones - Principal Investigator Oregon State University;Department of Geosciences; Wilkinson Hall 104, Corvallis, OR, 97331-5506, USAPhone: (541) 737-1224Email: Julia.Jones@oregonstate.edu, geojulia@comcast.netORCID: http://orcid.org/0000-0001-9429-8925
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Matthew G Betts - Principal Investigator Department of Forest Ecosystems and Society; 201E Richardson Hall; College of Forestry; Oregon State University, Corvallis, OR, 97331Phone: (541) 737-3841Email: matt.betts@oregonstate.edu
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Michael P. Nelson - Principal Investigator Department of Forest Ecosystems and Society; 201K Richarson Hall; College of Forestry; Oregon State University, Corvallis, OR, 97331Phone: 541-737-9221Email: mpnelson@oregonstate.eduORCID: http://orcid.org/0000-0001-6917-4752
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David Bell - Principal Investigator Email: david.bell@usda.gov, david.bell@oregonstate.edu
Abstract
- The H.J. Andrews Experimental Forest is a living laboratory that provides unparalleled opportunities for the study of forest and stream ecosystems in the central Cascade Range of Oregon. Since 1980, as a part of the National Science Foundation Long Term Ecological Research (NSF-LTER) program, the Andrews Experimental Forest has become a leader in the analysis of forest and stream ecosystem dynamics.
- Long-term field experiments and measurement programs have focused on climate dynamics, streamflow, water quality, and vegetation succession. Currently researchers are working to develop concepts and tools needed to predict effects of natural disturbance, land use, and climate change on ecosystem structure, function, and species composition.
- The Andrews Experimental Forest is administered cooperatively by the USDA Forest Service Pacific Northwest Research Station, Oregon State University and the Willamette National Forest. Funding for the research program comes from the National Science Foundation (NSF), US Forest Service Pacific Northwest Research Station, Oregon State University, and other sources.
Funding
Data were provided by the HJ Andrews Experimental Forest research program, funded by the National Science Foundation's Long-Term Ecological Research Program (DEB 2025755), US Forest Service Pacific Northwest Research Station, and Oregon State University. National Science Foundation: DEB1440409
Study Area Description
-
Long-Term Ecological Research The Andrews Forest is situated in the western Cascade Range of Oregon, and covers the entire 15,800-acre (6400-ha) drainage basin of Lookout Creek. Elevation ranges from 1350 to 5340 feet (410 to 1630 m). Broadly representative of the rugged mountainous landscape of the Pacific Northwest, the Andrews Forest contains excellent examples of the region's conifer forests and associated wildlife and stream ecosystems. These forests are among the tallest and most productive in the world, with tree heights of often greater than 250 ft (75 m). Streams are steep, cold and clean, providing habitat for numerous aquatic organisms.
Associated Party
-
Roy Haggerty
Role: Principal InvestigatorDept. of Geosciences;Wilkinson 104;Oregon State University, Corvallis, OR, 97331, USAPhone: 541-737-1210Email: haggertr@geo.oregonstate.edu
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Michael N. Gooseff
Role: Other ResearcherDept. of Civil & Environmental Engineering, University Park, PA, 16802, USAEmail: mgooseff@gmail.com, mgooseff@engr.colostate.edu
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Steven M. Wondzell
Role: Other ResearcherPacific Northwest Research Station; Corvallis Forestry Sciences Lab; 3200 SW Jefferson Way, Corvallis, OR, 97331, USAPhone: 541-758-8753Email: steve.wondzell@usda.gov
-
Roy Haggerty
Role: CreatorDept. of Geosciences;Wilkinson 104;Oregon State University, Corvallis, OR, 97331, USAPhone: 541-737-1210Email: haggertr@geo.oregonstate.edu
-
Jeffery J. Ninnemann
Role: CreatorBellingham, WA, USAPhone: 360-756-9308, 360-661-3546
Contact
-
Information Manager
Andrews Forest LTER Program, US Forest Service Pacific Northwest Research Station, 3200 SW Jefferson Way, Corvallis, OR, 97331Email: hjaweb@fsl.orst.edu
-
Roy Haggerty
Dept. of Geosciences;Wilkinson 104;Oregon State University, Corvallis, OR, 97331, USAPhone: 541-737-1210Email: haggertr@geo.oregonstate.edu
Publisher
-
Andrews Forest LTER Site
Role: PublisherForest Ecosystems and Society Department in Forestry, Oregon State University, 201K Richardson Hall, Corvallis, OR, 97331-5752Phone: (541) 737-8480Email: lterweb@fsl.orst.edu
Study Description
Time series of tracer (Rhodamine WT) concentration data representing a "break-through curve" resulting from a single, multi-scale tracer test conducted along the length of Lookout Creek, from its 2nd-order headwaters through its 5th-order main stem. The longitudinal tracer test involved an in-stream injection of Rhodamine WT over 78 hrs, followed by monitoring at eight downstream locations for five months, starting in mid-June 2003 through the middle of November 2003. The injection site was located below the upper Old Growth Trail bridge. The monitoring sites include one downstream of the injection site, above and below the Cold Creek confluence, below the lower Old Growth Trail bridge, below Mack Creek confluence, above and below McRae Creek confluence, and at the HJA headquarters. Three additional inter-order tracer tests (IOTT) were carried out between each of the major stream confluences along Lookout Creek. The injection site for the McRae Creek IOTT was located below the McRae Cr. confluence and was monitored just downstream, at the end of the main floodplain, and at HJA headquarters. The injection site for the Mack Creek IOTT was located below the Mack Cr. confluence and was monitored just downstream, at an unnamed tributary midway between Mack Cr. and McRae Cr., and above the McRae Cr. confluence. The injection site for the Cold Creek IOTT was located below the Cold Cr. confluence and was monitored just downstream, at Longer Cr., and at the lower Old Growth Trail bridge. Concentration break through curves are available for all of the monitoring sites for the longitudinal and inter-order tracer tests. Flux break through curves are available for most of the monitoring sites. STAMMT-L model estimates for hyporheic exchange is listed for most of the monitoring sites. The primary goal of this research project is to quantitatively measure the temporal scales of hyporheic exchange along a stream network. Our goal is to examine how hyporheic exchange varies with increasing stream size. Many previous studies focus on single stream reaches or on several reaches of similar sized streams, whereas we examined the residence time of water in the hyporheic zone over increasing length scales in a single stream. Prior work with tracer data and analysis using a transient storage model with an exponential residence time distribution (RTD) suggests that hyporheic parameters, primarily volume and mean residence time, are both spatially and temporally scale-dependent. However, recent work hypothesizes that the scale-dependence may be partially addressed by using a power-law RTD (Haggerty et al., 2002). Our research tests this hypothesis with several multi-scale tracer tests in a single stream. Instrumentation - HF020
Purpose: The primary goal of this research project is to quantitatively measure the temporal scales of hyporheic exchange along a stream network. Our goal is to examine how hyporheic exchange varies with increasing stream size. Many previous studies focus on single stream reaches or on several reaches of similar sized streams, whereas we examined the residence time of water in the hyporheic zone over increasing length scales in a single stream. Prior work with tracer data and analysis using a transient storage model with an exponential residence time distribution (RTD) suggests that hyporheic parameters, primarily volume and mean residence time, are both spatially and temporally scale-dependent. However, recent work hypothesizes that the scale-dependence may be partially addressed by using a power-law RTD (Haggerty et al., 2002). Our research tests this hypothesis with several multi-scale tracer tests in a single stream.
Methods
Method Steps
Method Step 1
No method step description paragraphs listed.
Instrumentation - HF020
- The longitudinal tracer test and McRae Creek inter-order tracer test was facilitated by a Fluid Meter Inc. (FMI) DC injection pump (model # RHB1). The Mack Creek and Cold Creek inter-order tracer tests were conducted using a new Fluid Meter Inc. AC injection pump (model # QG150, with a Q1CKC pump head). The discharges in the streams were measured using a Marsh-McBirney, Inc Flo-MateTM flow meter. The concentration of RWT was measured using a Turner DesignTM model 10-AU fluorometers and Teledyne ISCOTM samplers.
Processing Procedure - HF020
- In order to calculate flux breakthrough curves we needed to have a continuous record of discharge for each site. The discharge hydrographs of each site was estimated using a linear hydrograph regression from gauged watersheds within the H.J. Andrews. The hydrograph watershed regression was accomplished using point discharges gathered by Jeff Ninnemann and Charles Fardy throughout the summer and matched with one of the 10 gauged watersheds for a best fit linear regression. The linear relationship established between individual site discharges and watershed gauge datum was then used to estimate a discharge for each individual monitoring site.
Sampling
Study Extent
- This study was conducted along the main stem of Lookout Creek in the H.J. Andrews. Monitoring sites included sites below the upper old growth trail bridge, above and below the Cold Cr. confluence, above and below the Mack Cr. confluence, above and below the McRae Cr. confluence, at the first valley constriction below the concrete bridge, and at the Headquarters.
- The Longitudinal Tracer Test was conducted along the main stem of Lookout Creek. The injection site was located ~30 m downstream of the upper old growth trail bridge. There were eight monitoring sites below the injections site. Three fluorometer sites were stationed on Lookout Creek just up stream of Cold Cr., Mack Cr., and McRae Cr.. The fluorometers were 1032 m (Site 2), 4145 m (Site 6), and 8,907 m (Site 11) downstream of the injection site (as shown in Figure 1). One ISCO sampler was located 84 m below the injection site (not shown on map). Four additional ISCO monitoring sites were established below each of the confluences and near the base of the basin. The ISCO monitoring sites were 1,137 m (Site 4), 5,126 m (Site 7), 9,327 m (Site 12), and 14,274 m (Site 14) (Figure 1).
- Three additional tracer tests were also conducted between each major confluence within Lookout Creek. These inter-order tracer tests encompassed changes in stream scale from a 3-order drainage basin to a 5-order drainage basin.
- The first inter-order tracer test was a conducted between the confluence of McRae Creek and the H.J. Andrews headquarters. The injection site was located ~150 m downstream of the McRae Creek confluence (site 11). This tracer test was monitored 5,367 m downstream at the H.J. Andrews headquarters with a fluorometer (Site 14). The concentration of dye was also monitored 1,465 m downstream by an ISCOtm sampler at a position in the stream where the geomorphology changes from a floodplain to a constrained valley (Site 13). An additional ISCO sampler was located 420 m below the injection site (Site 12).
- The second inter-order tracer test was a conducted between the confluence of Mack Creek and McRae Creek. The injection site was located ~25 m downstream of the Mack Creek confluence (site 7). This tracer test was monitored 3,457 m downstream above the McRae Cr. confluence with a fluorometer (site 10). It was also monitored 1,001 m downstream by an ISCOtm sampler at the largest tributary between Mack and McRae Cr (site 9). An additional ISCO sampler was located 25 m below the injection site (Site 8).
- The third IOTT was a conducted between the confluence of Cold Creek and Mack Creek. . The injection site was located ~10 m downstream of the Cold Creek confluence (site 3). This tracer test was monitored 3,054 m downstream at a site above the Mack Cr. confluence with a fluorometer (site 6) and 2,105 m downstream by an ISCO sampler at Longer Cr.(site 5), the largest tributary between Mack and McRae Cr.. An additional ISCO sampler was located 46 m below the injection site (Site 4).
- Sampling frequency: a range of every 30 seconds to monthly
Sampling Description
- Stream discharge at the injection sites during the injections for the longitudinal tracer test and the inter-order tracer tests were measured by wading, using a Marsh-McBirney model 200 flow meter (Marsh-McBirney, Inc., Fredrick, MD, USA). Stream discharge during the duration of the tracer tests was measured at the USGS gauge house at the below headquarters on Lookout Creek. Hydrograph regressions were used with gauged watersheds within the H.J. Andrews to estimate a continuous discharge for all sites. Turner DesignTM model 10-AU fluorometers (Turner Designs, Inc, Sunnyvale, CA) were used to monitor concentrations at some sites. All samples collected with ISCO auto samplers (ISCO, Inc., Lincoln, NE) were analyzed with the same Turner Designs fluorometers (Turner Designs, Inc, Sunnyvale, CA). Four continuous injection tracer experiments were performed over various lengths of Lookout Creek in the HJ Andrews Experimental Forest.
Spatial Sampling Units
-
Site 00 - LTT Injection
W -122.11756400, E -122.11756400, N 44.22178700, S 44.22178700Altitude: 1036 to 1036 meter
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Site 01 - Longitudinal Tracer Test Injection ISCO Site
W -122.11817300, E -122.11817300, N 44.22294400, S 44.22294400Altitude: 1030 to 1030 meter
-
Site 02 - Longitudinal Tracer Test Above Cold Creek Site
W -122.12568300, E -122.12568300, N 44.22817900, S 44.22817900Altitude: 926 to 926 meter
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Site 03 - Cold Creek injection
W -122.12623100, E -122.12623100, N 44.22837200, S 44.22837200Altitude: 914 to 914 meter
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Site 04 - Longitudinal Tracer Test Below Cold Creek Site and
W -122.12684200, E -122.12684200, N 44.22854800, S 44.22854800Altitude: 902 to 902 meter
-
Site 05 - Cold Creek Inter-Order Tracer Test Longer Creek Si
W -122.14919500, E -122.14919500, N 44.23357900, S 44.23357900Altitude: 774 to 774 meter
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Site 06 - Longitudinal Tracer Test Above Mack Creek Site and
W -122.15956100, E -122.15956100, N 44.23203600, S 44.23203600Altitude: 731 to 731 meter
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Site 07 - Longitudinal Tracer Test Below Mack Creek Site
W -122.16831200, E -122.16831200, N 44.22768800, S 44.22768800Altitude: 655 to 655 meter
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Site 08 - Mack Creek Inter-Order Tracer Test Injection ISCO
W -122.16888400, E -122.16888400, N 44.22796300, S 44.22796300Altitude: 652 to 652 meter
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Site 09 - Mack Creek Inter-Order Tracer Test Middle Tributar
W -122.17916800, E -122.17916800, N 44.23037800, S 44.23037800Altitude: 612 to 612 meter
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Site 10 - Longitudinal Tracer Test Above McRae Creek Site an
W -122.20667900, E -122.20667900, N 44.23310400, S 44.23310400Altitude: 559 to 559 meter
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Site 11 - McRae Creek injection
W -122.21037000, E -122.21037000, N 44.23339000, S 44.23339000Altitude: 548 to 548 meter
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Site 12 - Longitudinal Tracer Test Below McRae Creek Site an
W -122.21483100, E -122.21483100, N 44.23216100, S 44.23216100Altitude: 536 to 536 meter
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Site 13 - McRae Creek Inter-Order Tracer Test Floodplain Sit
W -122.22479300, E -122.22479300, N 44.22879000, S 44.22879000Altitude: 499 to 499 meter
-
Site 14 - Longitudinal Tracer Test Headquarters Site and McR
W -122.25276000, E -122.25276000, N 44.21329300, S 44.21329300Altitude: 426 to 426 meter
Software
No software entries listed in this EML file.
Keywords
- LTER controlled vocabulary: geology (theme), geomorphology (theme), hydrology (theme), water (theme), hyporheic zone (theme)
Taxonomic Hierarchy
No taxonomic hierarchy listed in this EML file.
Data Entities
| # | Entity | Metadata | Data |
|---|---|---|---|
| 1 |
HF02001
HF02001 Multi-scale tracer tests: Dye tracer test concentration breakthrough curves |
METADATA | DATA |
Metadata
HF02001 - HF02001
Object name: HF02001.csv
Records: N/A
Attributes: 14
Temporal coverage: 2003-06-14 to 2003-06-21
File size: 8803917 byte
Checksum (MD5): c49ff2ec119cecdc73bc753aaa7011a0
Format: headers=1, recordDelimiter=\r\n, fieldDelimiter=,, quoteCharacter=", orientation=column
Constraints (2)
-
primaryKey: PRIMARY HF02001.DATANUM, HF02001.SITENAME
-
notNullConstraint: NOTNULL HF02001.BASIN_REG, HF02001.CONCEN, HF02001.DATANUM, HF02001.DATE, HF02001.DBCODE, HF02001.DISCHARGE, HF02001.ENTITY, HF02001.MASSFLUX, HF02001.SITE, HF02001.SITENAME, HF02001.TEST, HF02001.TIME
Attributes (14)
DBCODE - char(10) (nominal)
ID: HF02001.DBCODE
FSDB Database Code
Type system: Microsoft SQL Server 2008
Code definitions (1)
-
HF020
FSDB Database Code
ENTITY - numeric(1,0) (interval)
ID: HF02001.ENTITY
Entity number
Type system: Microsoft SQL Server 2008
Unit: number
Precision: 1
Numeric domain: type=natural, min=1.0000 (exclusive=false), max=1.0000 (exclusive=false)
SITE - char(7) (ordinal)
ID: HF02001.SITE
Monitoring site number
Type system: Microsoft SQL Server 2008
Code definitions (15)
-
TT-0
Site 00 - LTT Injection
-
TT-1
Site 01 - Longitudinal Tracer Test Injection ISCO Site
-
TT-2
Site 02 - Longitudinal Tracer Test Above Cold Creek Site
-
TT-3
Site 03 - Cold Creek injection
-
TT-4
Site 04 - Longitudinal Tracer Test Below Cold Creek Site and
-
TT-5
Site 05 - Cold Creek Inter-Order Tracer Test Longer Creek Si
-
TT-6
Site 06 - Longitudinal Tracer Test Above Mack Creek Site and
-
TT-7
Site 07 - Longitudinal Tracer Test Below Mack Creek Site
-
TT-8
Site 08 - Mack Creek Inter-Order Tracer Test Injection ISCO
-
TT-9
Site 09 - Mack Creek Inter-Order Tracer Test Middle Tributar
-
TT-10
Site 10 - Longitudinal Tracer Test Above McRae Creek Site an
-
TT-11
Site 11 - McRae Creek injection
-
TT-12
Site 12 - Longitudinal Tracer Test Below McRae Creek Site an
-
TT-13
Site 13 - McRae Creek Inter-Order Tracer Test Floodplain Sit
-
TT-14
Site 14 - Longitudinal Tracer Test Headquarters Site and McR
SITENAME - char(15) (ordinal)
ID: HF02001.SITENAME
Monitoring site name
Type system: Microsoft SQL Server 2008
Code definitions (17)
-
CC_IOTT_AMC
Cold Creek Inter-Order Tracer Test Above Mack Creek Site #6
-
CC_IOTT_INJ
Cold Creek Inter-Order Tracer Test Injection ISCO Site #4
-
CC_IOTT_ALC
Cold Creek Inter-Order Tracer Test Longer Creek Site #5
-
LTT_ACC
Longitudinal Tracer Test Above Cold Creek Site #2
-
LTT_AMC
Longitudinal Tracer Test Above Mack Creek Site #6
-
LTT_AMcRC
Longitudinal Tracer Test Above McRae Creek Site #10
-
LTT_BCC
Longitudinal Tracer Test Below Cold Creek Site #4
-
LTT_BMC
Longitudinal Tracer Test Below Mack Creek Site #7
-
LTT_BMcRC
Longitudinal Tracer Test Below McRae Creek Site #12
-
LTT_HQ
Longitudinal Tracer Test Headquarters Site #14
-
LTT_INJ
Longitudinal Tracer Test Injection ISCO Site #1
-
MC_IOTT_AMcRC
Mack Creek Inter-Order Tracer Test Above McRae Creek Site #10
-
MC_IOTT_INJ
Mack Creek Inter-Order Tracer Test Injection ISCO Site #8
-
MC_IOTT_MT
Mack Creek Inter-Order Tracer Test Middle Tributary Site #9
-
McRC_IOTT_FP
McRae Creek Inter-Order Tracer Test Floodplain Site #13
-
McRC_IOTT_HQ
McRae Creek Inter-Order Tracer Test Headquarters Site #14
-
McRC_IOTT_INJ
McRae Creek Inter-Order Tracer Test Injection ISCO Site #12
TEST - char(10) (nominal)
ID: HF02001.TEST
Longitudinal Tracer Test
Type system: Microsoft SQL Server 2008
Code definitions (2)
-
LTT
Longitudinal Tracer Test
-
IOTT
Inter-Order Tracer Test
DATANUM - numeric(5,0) (interval)
ID: HF02001.DATANUM
Sample number
Type system: Microsoft SQL Server 2008
Unit: number
Precision: 1.000000
Numeric domain: type=natural, min=1.0000 (exclusive=false), max=27775.0000 (exclusive=false)
DATE - datetime (dateTime)
ID: HF02001.DATE
Date of measurement
Type system: Microsoft SQL Server 2008
Date format: YYYY-MM-DD
TIME - int (ratio)
ID: HF02001.TIME
Time elapsed since the beginning of tracer test
Type system: Microsoft SQL Server 2008
Unit: number
Precision: 1.000000
Numeric domain: type=integer, min=0.0000 (exclusive=false), max=13300790.0000 (exclusive=false)
CONCEN - numeric(6,3) (interval)
ID: HF02001.CONCEN
Concentration of rhodamine wt, corrected to near zero from background fluorescence
Type system: Microsoft SQL Server 2008
Unit: micrograms per liter
Precision: 0.010000
Numeric domain: type=whole, min=0.0000 (exclusive=false), max=242.4100 (exclusive=false)
MASSFLUX - numeric(7,2) (interval)
ID: HF02001.MASSFLUX
Mass flux rate of rhodamine at corresponding time
Type system: Microsoft SQL Server 2008
Unit: micrograms per second
Precision: 0.010000
Numeric domain: type=whole, min=0.0000 (exclusive=false), max=5967.2700 (exclusive=false)
DISCHARGE - numeric(5,1) (interval)
ID: HF02001.DISCHARGE
Stream flow rate
Type system: Microsoft SQL Server 2008
Unit: liters per second
Precision: 0.100000
Numeric domain: type=whole, min=0.0000 (exclusive=false), max=767.4000 (exclusive=false)
BASIN_REG - char(15) (ordinal)
ID: HF02001.BASIN_REG
Best fit regression basin hydrograph used to estimate discharge of site
Type system: Microsoft SQL Server 2008
Code definitions (6)
-
MACK
Mack Creek guaged hydrograph used to estimate discharge using a linear hydrograph regression
-
USGS
USGS guaged hydrograph used to estimate discharge using a linear hydrograph regression
-
Direct USGS
Direct USGS guaged hydrograph used for discharge
-
WS03
WS03 guaged hydrograph used to estimate discharge using a linear hydrograph regression
-
WS02
WS02 guaged hydrograph used to estimate discharge using a linear hydrograph regression
-
Observed
Direct discharge measurements used to estimate discharge with a linear interpolation between daily measurements
TEMP - numeric(4,1) (interval)
ID: HF02001.TEMP
Water temperature
Type system: Microsoft SQL Server 2008
Unit: degrees Celsius
Precision: 0.100000
Numeric domain: type=whole, min=0.8000 (exclusive=false), max=19.9000 (exclusive=false)
TF1 - char(1) (nominal)
ID: HF02001.TF1
Water temperature flag
Type system: Microsoft SQL Server 2008
Code definitions (2)
-
Good value
-
M
Missing value
Units
| micrograms per liter | ug/l | massDensity | microgramPerLiter | kilogramPerMeterCubed | 0.000001 | micrograms per liter |
| liters per second | l/sec | volumetricRate | literPerSecond | literPerSecond | 1 | liters per second |
| micrograms per second | ug/sec | massFlux | microgramPerSecond | kilogramPerSecond | 0.000000001 | micrograms per second |
| degrees Celsius | deg c | temperature | celsiusDegree | kelvin | 1 | Degrees Celsius; a common unit of temperature; constantToSI=273.18 |
| number | number | dimensionless | number | dimensionless | 1 | dimensionless number, i.e., ratio, count |
Intellectual Rights
Data Use Agreement:
The re-use of scientific data has the potential to greatly increase communication, collaboration and synthesis within and among disciplines, and thus is fostered, supported and encouraged. This Data Set is released under the Creative Commons license CC BY "Attribution" (see: https://creativecommons.org/licenses/by/4.0/). Creative Commons license CC BY - Attribution is a license that allows others to distribute, remix, tweak, and build upon your work (even commercially), as long as you are credited for the original creation. This license accommodates maximum dissemination and use of licensed materials.
It is considered professional conduct and an ethical obligation to acknowledge the work of other scientists. The Data User is asked to provide attribution of the original work if this data package is shared in whole or by individual parts or used in the derivation of other products. A recommended citation is provided for each Data Set in the Andrews LTER data catalog (see: http://andlter.forestry.oregonstate.edu/data/catalog/datacatalog.aspx). A generic citation is also provided for this Data Set on the website https://portal.edirepository.org in the summary metadata page. Data Users are thus strongly encouraged to consider consultation, collaboration and/or co-authorship with the Data Set Creator.
While substantial efforts are made to ensure the accuracy of data and associated documentation, complete accuracy of data sets cannot be guaranteed and all data are made available "as is." The Data User should be aware, however, that data are updated periodically and it is the responsibility of the Data User to check for new versions of the data. The data authors and the repository where these data were obtained shall not be liable for damages resulting from any use or misinterpretation of the data.
General acknowledgement: Data were provided by the HJ Andrews Experimental Forest research program, funded by the National Science Foundation's Long-Term Ecological Research Program (DEB 2025755), US Forest Service Pacific Northwest Research Station, and Oregon State University.
Licensed
License: N/A
Maintenance
Maintenance update frequency: notPlanned
Description
- An update history is logged and maintained with each new version of every dataset.
Change History
-
Version1 (2007-07-13) Initial database level metadata entry from Word document using Administrative Interface.
-
Version2 (2008-03-05) Upoaded metadata and data to SQL using move_xls programs.
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Version3 (2013-09-09) Have not heard from Jeff Ninneman since 2006. Tried to contact him in 2008. Am making this database available online and uploading to PASTA.